Judicial acts and decisions - Ekhirit-Bulagatsky District Court (Irkutsk region). Judicial acts and decisions - Ekhirit-Bulagatsky District Court (Irkutsk Region) Ekhirit Bulagatsky District Court

Irkutsk region.

Ekhirit-Bulagat district: general information

Formed in 1918.

Population - 31.6 thousand people.

Area - 5.2 thousand km 2 .

The average per capita income of the population is 5628 thousand rubles.

Telephone code: +7-39541.

Postal code - 669001.

The head of the district is Igor Petrovich Usov.

Administrative division

Social sphere

Education

To the education system municipality Ekhirit-Bulagat district includes:

40 educational institutions,

20 preschool educational institutions,

1 educational institution NGO/SPO,

2 institutions of further education,

2 regional state educational institutions.

The situation with preschool institutions. The queue today is about 800 people. In 2013, this problem was resolved in Aluzhino, where a kindergarten for 49 places opened its doors; in 2014, the picture will change radically in Ust-Ordynsky. Of course, for the better. In the regional center it is planned to commission three kindergartens at once: two with 98 places and one large one with 220 places. In a year, the construction of another one, designed for 147 children, will be completed. Thus, they will try very hard to implement the decree of the President of the Russian Federation and ensure by 2016 preschool education everyone local residents aged 3 to 7 years.

While the construction of new kindergartens is underway, in Ust-Ordynsky they are trying to solve the problem by expanding the existing ones. And in a rather unexpected way. The know-how of the Yolochka kindergarten is that a new group was opened in an apartment in a private house.

There are 4,500 students and more than 500 teachers in the district. In 2010, according to Rospotrebnadzor estimates, three educational institutions- in Novonikolaevsk, Khabarovsk and Kharazargai - were found not to comply with the requirements of SanPiN. They had to be hastily seriously reconstructed - about 15 million rubles were spent on each one. And now here is the Ust-Orda average comprehensive school No. 1 named after. V. Borsoeva, where the speaker of the Legislative Assembly of the Irkutsk Region Lyudmila Berlin once studied, is celebrating its half-century anniversary in a modern guise.

In 2013, a modern physical culture and health complex was opened, which was named after Konstantin Baimeev. Footballers, wrestlers, archers, and representatives of other sports practice here literally from morning to night.

In 2013, 37 million was spent on the overhaul of the Ekhirit-Bulagat intersettlement leisure center. The building, which turns 75 years old in 2014, last time repaired back in the 90s of the last century. In total, the Center employs more than 2 thousand people, three dozen teams of different directions work, and eight of them bear the title of national.

Economy

One of the most successfully developing agricultural enterprises in the Ekhirit-Bulagat region is the Tugutuysky agricultural enterprise. We started in 2009 with the cultivation of 1,500 hectares of land, recalls the director of the enterprise, Vladimir Monkhoev, the yield was 16 centners per hectare. Now about three thousand hectares are used for sowing, and up to 24 centners are harvested.

Up to 70 percent of sour cream and other dairy products sold by private traders at the Central Market and other markets are brought from the Ekhirit-Bulagat region.

Natives and residents of the Ekhirit-Bulagat region

1. Khaidurov Efim Leontievich - designer of sporting weapons, winner of the World and European Championships.
2. Boronoev Asalkhan Olzonovich - professor of philosophy and psychology at St. Petersburg State University.
3. Manzhuev Gennady Nikolaevich - master of sports of the USSR and international class in freestyle wrestling, head of the representative office of the Republic of Buryatia in Mongolia.
4. Badinnikov Viktor Yakovlevich - academician, rector of the State Technical University (St.

Physiographic characteristics of the Ekhirit-Bulagat region 1.1 Geographical position, boundaries, size of territory.Ekhirit-Bulagatsky district is a municipal entity in the southeast of the Irkutsk region. The administrative center is the village of Ust-Ordynsky. (Fig. 1) The Ekhirit-Bulagat district includes the territories of 13 rural settlements, a total of 51 settlements.

Municipalities (rural settlements):

Aluzhinskoe

Akhinskoye

Gakhanskoe

Zahalskoye

Kapsalskoe

Korsukskoe

Kulunkuiskoe

Novo-Nikolaevskoe

Oloiskoe

Tugutuyskoe

Ust-Ordynskoe

Kharazargai

Kharatai

Fig.1 Administrative-territorial division of the Irkutsk region

The numbers indicate the areas:

1 – Alarsky (UOBO), 2 – Angarsky, 3 – Balagansky, 4 – Bayandaevsky (UOBO), 5 – Bodaibinsky, 6 – Bokhansky (UOBO), 7 – Bratsky, 8 – Zhigalovsky, 9 – Zalarinsky, 10 – Ziminsky, 11 – Irkutsk, 12 – Kazachinsko-Lensky, 13 – Katangsky, 14 – Kachugsky, 15 Kirensky, 16 – Kuitunsky, 17 – Mamsko-Chuysky, 18 – Nizhneilimsky, 19 – Nizhneudinsky, 20 – Nukutsky (UOBO), 21 – Olkhonsky, 22 – Osinsky (UOBO), 23 – Slyudyansky, 24 – Taishetsky, 25 – Tulunsky, 26 – Usolsky, 27 – Ust-Ilimsky, 28 – Ust-Kutsky, 29 – Ust-Udinsky, 30 – Cheremkhovsky, 31 – Chunsky, 32 – Shelekhovsky, 33 – Ekhirit-Bulagatsky (UOBO)

Rice. 2 map of the Ust-Ordynsky Buryat district of the Irkutsk region

The name of the region is due to the residence of large tribal groups of Buryats - Ekhirits and Bulagats - who formed in this territory and settled throughout the Baikal region.

The Ekhirit-Bulagatsky district is located in the south of the Irkutsk region, occupies the south-eastern part of the Ust-Ordynsky Buryat district, borders in the northeast with Bayandaevsky, in the east - with Olkhonsky, in the south and southwest - with Irkutsk, in the west - with Bokhansky and in the north - with the Kachug districts. The administrative center is the village of Ust-Ordynsky. Before January 1, 2008 there was administrative center Ust-Ordynsky Buryatsky Autonomous Okrug. It was the only center of a subject of the Russian Federation with the status of a rural settlement (Fig. 2)

The area of ​​the district is 5.2 thousand sq. km, the population is 29.4 thousand people (as of 01/01/2010). The area is multinational. The indigenous population are the Buryats. Of other nationalities, Russians predominate, Ukrainians, Belarusians, Tatars, etc. are smaller.

The district is located in the Baikal region, occupies the southern part of the Lena-Angara plateau. Altitude above sea level above 1000 meters. The landscape of the district is determined by the Irkutsk-Balagan forest-steppe, within which it is located. The landscape of the district is very picturesque: spacious meadows and pastures, interspersed coniferous forests. The surface is heavily dissected by river valleys.

Most of the district is located within the Angara River basin and only a small, easternmost section lies in the Lena River basin. The territory of the district is irrigated by tributaries of the Angara River: Unga, Osa, Ida and Kuda. On the territory of the district there are small lakes in river valleys: Alyaty, Altarik, Orda, Angol.

Basic Natural resources districts: oil, combustible gas and condensate, coal, non-metallic Construction Materials(clay, gypsum).

1.2.Geological structure and relief

1. 2.1. Tectonics

Geotectonically, the area is located in the southern part of an ancient platform or ancient continent that was formed more than a billion years ago and has since been only occasionally covered by continental shallow seas. But before becoming a continent, this section of the earth's crust went through a complex evolution.

During the first three billion years on Earth, processes of formation and synthesis of almost all igneous, metamorphic, sedimentary rocks and minerals, ore formations occurred, and organic life, modern atmosphere, hydrosphere appeared, foundations were formed, the foundations of modern continents, which subsequently no longer experienced significant temperature effects and deformations. One of these continents was the Siberian Precambrian continental ancient platform, which was covered by the sea only at the very beginning of its existence.

The last sea left the territory of the district in the middle of the Paleozoic era, leaving numerous sedimentary rocks of the Vendian with an age of 650 - 570 million years, Cambrian (with an age of 570 - 505 million years) periods of the geological history of the Earth. During all this time, the territory of the district, tectonically, represented two regions with different morphologies.

Most of the territory of the district (Osinsky, Bokhansky, Nukutsky)

aligned with a section of the Siberian Platform submerged below sea level.

Smaller south- East End districts (Ekhirit-Bulagatsky, Bayandaevsky) was a more intensively subsiding area under sea level - a marginal trough, gravitating towards the edge of the platform and laid on a stable, solid platform foundation. The subsidence of the earth's crust in it was compensated by the accumulation of sedimentary rocks of the Late Proterozoic, Early Paleozoic, Mesozoic and Cenozoic ages. So, during the late Proterozoic - early Paleozoic (in the range of 650 - 400 million years ago), the marginal trough was filled with sediments, at the very bottom represented by sandstones, siltstones and mudstones. The thickness of these deposits determined from the data deep drilling(Fig. 3), is more than 300 m. These rocks lie directly on the strong crystalline formation of the platform, which in turn is composed of metamorphosed and highly deformed rocks formed during high temperatures and pressures. Consequently, before the arrival of the sea, the basement rocks must have cooled and turned into a sufficiently vast plain capable of containing an entire sea. Geologists called this sea the Angara-Lena Trough.

Sediments of a higher stratigraphic level, and therefore of a younger age, include sandy layers interspersed with siltstones, mudstones, carbonate rocks with interlayers of marls and anhydrites (Fig. 3). Around the turn of the Precambrian and Phanerozoic, tectonic movements slowed down significantly - the mountains stopped growing, and subsidence stopped. The so-called period of stable standing of the platform in a hot climate began, i.e., the Siberian continent at that time was somewhere in hot latitudes. From the ocean to the platform came sea ​​water. Here it evaporated, leaving layers of rock salt, limestone, dolomite, gypsum and anhydrite with a total thickness of 1300 - 1800 m.

Further, in the Middle Cambrian era, in all likelihood, the connection between the Cambrian seas and the ocean was disrupted. The seas often begin to dry up, and the carbonates remaining on the surface begin to erode and turn into flour, i.e., desert conditions are established in the district.

All this is told by the rocks of the Middle Cambrian deposits of the Verkholenskaya suite, the outcrops of which occupy vast areas in the northern part of the district (Fig. 3). The bottom, lowermost part of these deposits is composed of clayey-marly breccias with fragments of underlying dolomites of the Angara suite, which are replaced by dolomite flour.

Rice. 2. Geological section along the line of Tolban - Kudinsky Range.

Legend

Types of platform cover:

1 – quaternary system;

2 – Neogene;

3 – Jurassic rocks;

4 – terrigenous rocks of the late and middle Cambrian;

5 – carbonate-halogen rocks of the Early Cambrian;

6 – rocks of the Vendian system.

Rocks of the basement of the Archean-Proterozoic platform:

7 – metamorphic, crumpled into folds;

8 – igneous (a – granites, b – diorites);

9 – faults and thrusts.

__________________________________________________________________

Above are variegated gypsum mudstones, marly dolomites with interlayers of siltstones and sandstones, then there are quartz and carbonate sandstones with interlayers of marls and siltstones, and at the very top there are mainly sandstones. The color of the rocks is predominantly reddish and spotted. The thickness of the Middle Cambrian formation of rocks is from 350 to 550 m.

The period of time between the Cambrian and Jurassic periods did not leave any geological traces in the form of rocks. It was during this period that the entire complex of previously formed rocks was deformed into folded structures of various sizes and morphologies.

Rice. 3. Geological structure[ 5 ]

The largest of them extend for many tens of kilometers (Fig. 4). Folding in the sedimentary cover of the platform is most intensely observed near, its edges along eastern outskirts within the Angara-Lena marginal trough. Complex linear narrow ridge-shaped shafts and troughs are widely developed here. As you move away from the edge of the platform towards its center, the intensity of the folds weakens, they become wider, flatter, and the angles on the wings decrease from 20-10°. The folds turn into box-like shapes, but do not lose their inherent large extent and asymmetry. Their northwestern wings are steeper, and their southeastern wings are flatter. The ratio of the height of the folds to their width is 0.1-0.09

The folds of the Angara-Lena trough can be traced for hundreds of kilometers parallel to the edge of the platform.

From the beginning of the Middle Jurassic era, the process of subsidence of the territory began to predominate and sedimentation processes resumed, thanks to which we have material evidence of the geological history of this period - rocks of the Jurassic system, which lie on the eroded and highly dissected relief of the Lower Cambrian rocks. In general, throughout the entire Siberian platform they are filled by an asymmetrical foothill trough, stretched along the edge of the platform along the Sayano-Baikal arch uplift that rises in the Jurassic. Its northwestern branch is called the Pre-Sayan foothill trough, and the northeastern branch is called the Pre-Baikal trough. The latter is superimposed on the Angara-Lena Paleozoic marginal trough.

In Jurassic times, the Pre-Baikal trough extended from the Irkutsk Sayan region to longitude s. Bayandai is no more than 150 km away.

The Pre-Baikal trough of Mesozoic time is filled with coal-bearing sediments with a thickness of 500-600 m in the area of ​​Irkutsk and no more than 300 m in the area of ​​the upper reaches of the river. Where. On the territory of the district, Jurassic formations are known in a significant part and are represented by continental, mainly clastic deposits of the lake-river type.

Rice. 4. Scheme of tectonic structures

The rocks of the Jurassic system indicate that during their formation the paleographic conditions of warm, humid landscapes existed in the district. Thus, coarse sediments tell about the existence of wide river valleys with winding river beds, and sandy-siltstone and clay rocks tell about the environment of wide river floodplains with numerous oxbow lakes, swamps, and lakes. The second half of the Mesozoic and almost the entire Paleogene were again an era of long-term regional leveling of the relief of the Siberian Platform under conditions of relative tectonic rest and a climate favorable for chemical weathering.

The most ancient Cenozoic rock complexes of the district are represented by unique Paleogene-Neogene deposits, which were formed along narrow private depressions of Mesozoic-Canozoic age. These sediments are represented by a variety of clays, often high-alumina, sandy loams, loams, sands and brown coals. Occasionally, shell limestones and calcareous fine-grained tuffites are observed. These deposits contain huge reserves of brick, refractory, drilling clays and brown coals. The thickness of the sediments reaches 250-300 m. They almost everywhere overlap the Cretaceous-Paleogene leveling surface, which is the result of long-term uplift or tectonic quiescence of the district territory. The area of ​​distribution of individual depressions with Paleogene-Neogene deposits borders the Pre-Baikal Cenozoic foothill trough, which in the district is mostly superimposed on the Angara-Lena Early Paleozoic marginal trough, and to a lesser extent on the Early Middle Jurassic foothill trough of the same name, described above. In the southwest it extends beyond the territory of the district and in the valley of the river. Angary smoothly merges with the Pre-Sayan Cenozoic foothill trough. From the river valley Angara, it extends to the city of Kirensk at a distance of almost 600 km and is one of the most noticeable neotectonic structures of the Siberian Platform.

The Cenozoic Pre-Baikal foothill trough, like its earlier predecessors, is located on the edge of the Siberian Platform and is compensatory in relation to the Baikal arched uplift. To the west, the Upper Lena Uplift, commensurate with it, is associated with the trough, which separates it from the Siberian Platform. The latter probably experienced slower uplift in the Cenozoic, and a plateau was formed on it. Absolute elevation marks of the uplift territory in the river basin. Where they fluctuate between 900-1000 m.

The width on the territory of the district reaches 90 km, its axis extends subparallel to the foot of the Baikal mountain region, its summit surface lies along the axis of the trough at levels of 400-900 m, and the hinge is inclined in the area of ​​the village. Bayandai to the northeast.

Modern deposits on the geochronological scale belong to the Quaternary or anthropogenic period and are represented by river boulder-pebble, pebble, sand and clay up to 60-80 m thick, distributed along modern large river valleys. Loose rocks are widespread on slopes and watersheds. Their thickness on slopes reaches 10-15 m, and on watersheds - 1.5-2 m

1.2.2. Relief

In orthographic terms, the district is located within the Leno-Angara flat upland, the absolute heights and dissection of which increase from south to north, and the relative elevation differences are 250-350 m. The lowest point of the district's relief is the level of the river. Hangars - 440 m, and the most high mountain located in the north of Bayandaevsky district - 1048 m.

The relief of the area was formed under the influence of recent tectonics, erosion-denudation processes and structural and lithological features of bedrock. Neotectonic movements determined the absolute elevation of the territory. They, according to scientists, determined the intensity of the formation of relief forms.

The main orographic structure of the district's territory is determined by the following megarelief elements: Leno-Angara plateau, slightly inclined to the south; northwestern spurs of the weakly dissected Onot Upland with absolute heights of up to 1000 m; plains of the Pre-Sayan and Pre-Baikal regions with absolute elevations of 500-700 m; Irkutsk-Cheremkhovo plain with a depth of 30-100 m; central part The relief of the Ekhirit-Bulagat region is occupied by the Kudinsk depression, which is a plain 60-80 km wide with a structural ridge-hollow relief. Quite narrow ridges have relative heights of 120-180 m.

The southwestern part of the same area falls within the Irkutsk depression; in the north-west the Kudinsk depression is bordered by the Kudinsky ridge, and in the south-east by the Onot Upland (Fig. 5).

The ridges are characterized by deep vertical dissection with absolute watershed elevations of 923 to 1000 m. The depth of incision of river and stream valleys reaches 270-360 m, and the maximum width is 10 km. Within the Kudinsk and Irkutsk depressions, a structural-erosive relief has developed, consisting of linearly elongated rather narrow ridges and intermountain depressions. The absolute elevations of the ridges range from 630 to 909 m, the depth of the erosional incision of the valleys is 120-190 m.

Microforms of cryogenic relief are associated with the widespread development of permafrost within the district. On floodplain and above-floodplain terrace deposits, gentle slopes of northern exposure, fissure-polygonal forms are formed, in wide valley bottoms - bulgunnyakhs up to 5-20 m high, seasonal heaving mounds, reaching in diameter from 8 to 20 m and 0.5-3.0 m height.

On the valley slopes and terraces with a thick cover of loose sediments, there are ravines reaching several hundred meters in length, 10-30 m in width and 2-7 m in depth. Here you can also find numerous potholes and gullies - future ravines.

Rice. 5. Orographic scheme

1.3. Climate

The climate of the region, located in the south of the Irkutsk region, is sharply continental with long cold winters, low precipitation throughout the year, and relatively hot short summers.

One of the main climate-forming factors is solar radiation reaching the earth; it, in turn, significantly depends on circulation air masses(which manifests itself through cloudiness and transparency of the atmosphere) and features of the underlying surface.

The main feature of the region’s climate – sharp continentality – is determined by atmospheric circulation. In winter, a powerful anticyclone forms in Eastern Siberia, in which clear, calm weather prevails, promoting heat loss earth's surface as a result of radiation. A characteristic feature of the summer circulation is the intensification of cyclonic activity, the frequent repetition of cloudy weather types with precipitation.

The arrival of solar radiation varies across the territory and is determined, first of all, by astronomical factors - the length of the day (Table 1) and the height of the sun above the horizon. In turn, the value of these parameters depends on the latitude of the place.

The length of the day within the district varies at the southern border of the territory from 7 hours 48 minutes; in the north - from 7 hours 26 minutes to 17 hours 06 minutes, respectively, on December 15 and June 15. From March to September, the length of the day increases as you move north, and from September to March it decreases.

The height of the sun at noon and the intensity of direct solar radiation on a horizontal surface under clear skies are shown in Table. 2.

Table 1

Sunrise time (at), sunset (w), length of day (p) on the 15th day of each month

Latitude

hail

Average solar time, h min by month

III

VII

VIII

XII

52 pp. w.

8 .02

7.17

6.16

5.05

4.07

3.39

3.57

4.43

5.53

6.23

7.17

8.01

16.16

17.11

18.02

18.55

19.45

20.21

20.15

19.27

18.17

17.09

16.09

15.49

8.14

10.00

11.46

13.50

15.38

16.42

16.18

14.44

12.44

10.50

8.50

7.48

54 p. w.

8.12

7.42

6.17

5.01

3.58

3.27

3.47

4.36

5.32

6.27

7.27

8.12

16.06

17.06

18.01

18.59

19.54

20.33

20.25

19.34

18.18

17.05

16.01

15.38

7.54

9.44

11.44

13.58

15.56

17.06

16.38

14.58

12.46

10.38

8.34

7.26

table 2

Altitude of the sun at noon, in degrees

latitude,

hail

III

VII

VIII

XII

52 pp. w.

16.8

24.9

35.8

47.7

56.8

61.3

59.6

52.2

41.1

29.6

19.6

14.7

54 p. w.

14.8

22.9

33.8

45.7

54.8

59.3

57.6

50.2

39.1

27.6

17.6

12.7

Table 3

Intensity of direct solar radiation, cal/cm²

latitude,

hail

III

VII

VIII

XII

52 pp. w.

0.57

0.83

1.16

1.47

1.66

1.74

1.71

1.56

1.30

0.98

0.66

0.50

54 p. w.

0.51

0.38

1.10

1.42

1.62

1.70

1.67

1.52

1.25

0.92

0.60

0.44

The highest height of the sun is observed in June and is 61° 18' on the southern border and 59° 18' on the northern. The lowest - in December - 14° 42' on the southern border and 12° 42' on the northern. Accordingly, the value of solar radiation reaches 1.71 and 1.67 kcal/cm² month in July, and 0.50 and 0.44 kcal/cm² month in December. (Table 3) .

The radiation balance, which determines the residual heat at the earth's surface, is about 3 kcal/cm² in July, and only -0.5 - -0.8 kcal/cm² in December. A period with a long radiation balance, the time of heat accumulation by the underlying surface lasts about 8 months. The sign of the radiation balance changes in the spring at the beginning of March, in the fall in November. In the daily course of solar radiation and radiation balance, the maximum is observed at noon, since at this time the sun is at its highest height above the horizon during the day.

Atmospheric circulation. For temperate latitudes northern hemisphere characterized by west-east transfer of air masses. In general, for the year the movements of air masses from west to east predominate, which has a high percentage of repetition for many stations in the district, including Ust-Ordynskaya. In certain periods of the year, this mechanism is disrupted by the formation of baric maximum and minimum over most of the Asian continent or by the passage of surface cyclones and anticyclones through the territory of the district. The south of the Irkutsk region, which includes the district, is characterized by the fact that almost no Pacific air masses enter here. But very often this territory, in the rear of cyclones, is invaded by Arctic air, which, passing over the continent, is transformed into air of temperate latitudes.

In winter, the weather is determined mainly by the influence of the Asian anticyclone, which reaches its maximum development in January. Clear frosty weather prevails with a significant number of windless days.

Rice. 6. Air temperature and prevailing wind direction in January

Rice. 7. Air temperature and prevailing wind direction in July

Rice. 8. Annual precipitation amounts

Often at the beginning of winter there are warming events associated with the passage of cyclones from the southern and central regions of Western Siberia.

In spring, when the air temperature rises, the Asian anticyclone weakens, the number of cyclones coming from the southwest and west increases, bringing warm air from the regions of Central Asia and Kazakhstan. This causes sharp short-term warmings, which are replaced by strong winds and cold temperatures.

In summer, in contrast to winter, there is a general decrease in atmospheric pressure and the establishment of a cyclonic type of weather. The first half of summer is usually hot and dry, with many clear days. The second half of summer is rich in precipitation. This is due to the arrival of cycles from Mongolia.

In the first half of autumn, partly cloudy, dry weather with weak winds prevails, which is formed by anticyclones passing through the territory or cyclones coming from the Aral-Caspian basin. In the second half, the invasion of Arctic air masses, cooling and precipitation occurs more and more often. At the end of autumn, the formation of the Asian anticyclone begins.

Atmospheric pressure and prevailing winds. The most important condition, which determines the direction of transfer of air masses, is the distribution of atmospheric pressure at the earth's surface and relief. During the year, in the central and western parts of the district, winds of the north-western and south-eastern directions predominate; in the eastern part there is a high frequency of winds in the northern, north-western and north-eastern directions. The average monthly and annual wind speed for the Ust-Orda station in the Ekhirit-Bulagat region is shown in Table 4.

Air temperature. The air weakly absorbs radiation, so it is almost not heated by the sun's rays. It receives its main heat from the surface of the earth heated by the sun's rays.

Table 4

Average monthly and annual wind speed, m/s

Therefore, the onset of maximum air temperatures is always delayed relative to the moment of the greatest arrival of solar radiation.

For the Ust-Orda station, the average annual temperature is negative and amounts to -0.3º C. The change in average monthly temperatures in January and July is shown in Fig. 6-7.

The coldest month is January. In most of the district, the average air temperature in January is approximately -24º C and varies from -22º C to -26º C. The most low temperatures are observed in low relief forms, mainly in river valleys and small basins with absolute heights from 400 to 500 meters.

Heavy cold air “flows” here in winter during anticyclonic weather, forming “cold lakes” and surface inversions.

Three to five days in winter are observed with an average daily air temperature of -30º C to -35º C. The minimum temperature in these months is -29º C – -35º C. The temperature rise begins in February and occurs due to the increase in the height of the sun above the horizon and duration of sunshine. But the presence of snow cover in February-March delays the rapid rise in temperature. March throughout the district remains a cold month with significant negative air temperatures. A rapid increase in temperature begins in April with the melting of snow cover. Despite the fact that, in addition to the southern part of the district, in its central and northern regions the average daily air temperatures remain negative, they have small values. For Ust-Orda, the average daily temperature is -0.4º C. The transition of the average daily temperature through 0º C towards positive values ​​occurs from April 12 to 18. Its rapid growth begins in May-June. The warmest month is July. Average monthly temperatures in July vary from 14º C to 18º C, and average daily temperatures reach 25º C. Almost every year in the summer you can expect several days with average daily air temperatures above 30º C, less often they are observed at the end of May. The onset of intense heat in summer is associated with the arrival of tropical air. Such periods are fire hazardous and harmful to crops.

From August, the air temperature begins to slowly decrease, and at the end of the month night frosts are already possible. A sharp drop in temperature occurs in September, and it reaches 7-8º C. However, this month has many hot days with daytime temperatures in some years above 20º C. Until December, the temperature drops intensively by 8-12º C from month to month. The transition of the average daily temperature through 0º C towards a decrease occurs on October 12-16.

Precipitation. On average, precipitation falls from 250 to 400 mm per year, of which 78% is liquid precipitation, 16% is solid and 6% is mixed. A noticeable decrease in precipitation occurs from west to east (Fig. 8). This is due to the arrival of air masses from the west, northwest and north. And since the Eastern Sayan stretches from southeast to northwest, and the strike of the Lena-Angara plateau can be traced mainly from southwest to northeast, then, passing through ridges and hills, consistently leaving moisture on each windward slope , comes to the eastern part of the district dried up. A huge mass of lake water. Baikal has almost no effect on the moisture content of the district due to its high ridges. Thus, the most arid is the eastern part of the territory, which belongs to the Baikal depression within the district. This area has insufficient moisture and belongs to the risky farming zone.

Snow cover has a significant impact on climate. It delays the rise in air temperature in the spring, since a large amount of heat is spent on melting it, rather than warming the air. At the same time, it protects the soil from severe cooling and deep freezing, which is very important for a good wintering of plants. In the spring, when the snow melts, a lot of water is formed, which determines the spring regime of the rivers.

The first snow cover appears on October 14. As a rule, it does not remain for the winter and thaws under the influence of warming temperatures characteristic of this month. Stable snow cover appears on November 1-10 and disappears on April 8-11, the date of its complete disappearance is April 27 - May 4. The duration of the period of snow cover is 154 days. IN mountainous areas and at higher elevations the snow melts much later - at the end of May.

The height of the snow cover in steppe and forest-steppe areas varies between 10-25 cm and in forested areas - 40-60 cm. Deforested open areas are very often covered, the snow is completely blown away from them, or a small layer remains, which leads to deep freezing of these areas and makes farming difficult.

1.4. Water

The district's waters are represented by surface waters - rivers, lakes, swamps, reservoirs - and groundwater. Their regime and dynamics are determined by a complex combination of natural-climatic and anthropogenic factors.

1.4.1. Surface water

Most of the district is characterized by insufficient supply of surface water. In addition, the water of a number of surface sources is characterized by high mineralization and is suitable only for technical purposes.

The average module of surface runoff in the district as a whole does not exceed 1 l/s per km/² and varies from 0.3-0.7 l/s per km² in the left bank part of the district to 2.9-3.5 l/s per km² . Areas with the highest runoff module are located in the Osinsky and most of the Bayandaevsky districts, with the lowest runoff module in the Alarsky and Nukutsky districts.

The annual total runoff generated within the administrative boundaries of the district is 1.1 km² per year, i.e. slightly more than 0.1% of the river's transit flow. Hangars (Table 5).

Table 5

Surface runoff volume

Area

Area, thousand sq. km

Average drain module, l/s sq. km

Volume of surface runoff, cubic meters km/year

Angarsk

2,7

0,3

0,03

Bokhansky

3,7

1,3

0,15

Bayandaevsky

3,8

2,1

0,25

Nukutsky

2,4

0,5

0,04

Osinsky

4,4

2,9

0,40

Ekhirit-Bulagatsky

5,1

1,5

0,24

Total for the district:

22,1

1,6

1,11

One of the features of the district is the development of karst, which is highly developed in the coastal zone of the Bratsk reservoir, in the river basin. Kuda, in the vicinity of the villages of Gakhana, Khara-Nur-Khuty and Nuhe-Nur. The presence of karst is associated with the leakage of part of the surface water into karst massifs, which is especially noticeable in the river basin. Ides. Due to karst, certain areas are deprived of surface watercourses.

Even fairly large permanent watercourses are lost when crossing karst massifs.

Along with zones of surface water absorption, discharge zones are also noted. The discharge of karst waters is associated with the outlets of springs in the river basin. Wasps.

The district's rivers belong to the Yenisei and Lena basins. Watershed along the northeastern tip of the air. Most of the district's surface belongs to the river basin. Yenisei (the Angara river and its tributaries), the smaller one - to the river basin. Lena.

The river network is poorly and unevenly developed (Table 6). It is represented by sections of the river. Angara with its right tributaries Kuda, Ida, Osa and left rivers. Zalari and Ungoy. The Angara carries its waters across the territory of the district for 40 km and about 80 km along its border with the Usolsky and Irkutsk regions.

One of the main rivers of the district, Kuda, has a fairly extensive network of tributaries (Table 5). Its largest tributary is the Murin.

The density of the river network in the district varies from 0.1 to 1.0 km/km². The maximum is observed in the eastern part of the district - in the interfluve of the river. Murin and Bulga. The minimum is in the left bank part of the river. Angara and Ido-Osinsk interfluve. In the central part of the district, the density of the river network is 0.2-0.3 km/km².

Based on the type of water regime and the nature of feeding, the rivers of the district belong to the Middle Angara hydrological region of the Irkutsk region. The rivers are fed by mixed water and are supplied by snow, rain and, to a lesser extent, groundwater. The river regime in this area is characterized by: spring floods with a rise in water level from 1 to 4 m; summer rain floods, in some years exceeding the maximum flood; intermittent low water, with low water levels until individual rivers dry out in summer and autumn; stable winter low water, sometimes accompanied by complete freezing of rivers.

Table 6

Characteristics of the rivers of the Ekhirit-Bulagat region

Ust-Orda Buryat District

River

Annual runoff volume, million cubic meters. m

(observation point)

Angara (a tributary of the Yenisei)

763100 (village Buret)

Zalari (left tributary of the Angara)

15, 5 (Novonukutsky village)

Unga (left tributary of the Angara)

15.5 (Semenovsky village)

Ida (another tributary of the Angara)

103 (Morozova village)

Where (another tributary of the Angara)

56.9 (Bozoi village)

443 (Granoshchina village outside the district)

Murin (left tributary of the Kuda)

15.0 (village Zagatui)

Obusa (Osa tributary)

101 (Gorkhon village)

Osa (another tributary of the Angara)

143 (Osa village)

Kulenga (left tributary of the Lena)

271 (Belousovo village outside the district)

Manzurka (left tributary of the Lena)

303 (Zueva village outside the district)

The flood occurs in April-May and lasts 35-40 days. During this period, in areas with intensive karst distribution, the runoff is 35-50%, and in the rest - 55-60% of the annual one. After the spring rise, the water level decreases to minimum values, until small rivers dry up, and is held for 15-20 days until the onset of summer floods associated with rainfall in the second half of summer. Along the rivers there are 2-3 rain floods with a high water rise of up to 1 m, in rainy years - from 1.5 to 2 m. Summer flow in the rivers is 30-35% of the annual one. In the autumn, the water level in the rivers steadily and gradually decreases to minimum values ​​before freeze-up.

At the end of October the rivers freeze. The ice cover lasts from 160 to 170 days. Its thickness is 0.8-1.5 m. In places where rivers freeze to the bottom, ice forms, which increase the thickness of the ice to 2 m.

The flow of suspended sediment is determined by the erosive activity of rivers and anthropogenic factors. Depending on the erosion activity, the turbidity of the water in the rivers varies. The average erosion coefficient for the territory of the district is 7.0 t/km² per year, turbidity is from 25 to 50 g/m³. Rivers within the Manzur and Onot uplands, as well as in the upper reaches of the Osa and Obusa, are characterized by low turbidity. In the middle and lower reaches, turbidity increases. The main share of sediment falls during the period of spring floods and rain floods (80-90% of the annual one). Turbidity and sediment runoff during low-water periods decrease from source to mouth due to the weakening of the erosive activity of streams and an increase in water flow. During flood periods, an inverse relationship is observed.

Hydrochemical characteristics of rivers. The mineralization of river waters is determined by the climatic conditions of the region, the geological structure of the territory, the type of soil and the characteristics of the vegetation cover. The rivers of the district form the chemical composition in the southern part of the Irkutsk amphitheater among heavily gypsumed sedimentary rocks of Cambrian age under conditions of insufficient moisture. Here waters of hydrocarbonate and sulfate types are formed, with increased and high mineralization. Waters of the pp. belong to the sulfate type. Ida, Ungi, Kudy, the rest - to hydrocarbonate.

The mineralization of surface water varies throughout the year. It is lowest during the spring flood and is 100–200 mg/l for most rivers, and 250–300 mg/l for the Ida, Osa, and Unga, but during the period of floods it can decrease by 1.5–2.0 times. The greatest mineralization is observed during the winter low-water period before the snow melts, when the rivers are fed mainly by groundwater. During this period it reaches 1000 mg/l. And it varies within 500-1000 mg/l.

Thus, the waters of the district’s rivers can be classified as fresh with a low degree of mineralization in spring, medium in summer and high in winter.

1.4.2. Lakes

In terms of size, most lakes in the district have an area of ​​less than 1 km². The largest, located in the western part, is the lake. Alyat. Its length is 4 km and its maximum width is 0.5 km. Lake Alyaty is flowing. The river flows into it and flows out of it. Alar. The flow of the lake contributes to the rapid exchange of water in it. In total, there are more than 100 lakes within the district. The largest reservoirs are located in the left bank part of the river basin. Hangars. In the right bank half of the district, the lakes are much smaller in area, from one to several tens of hectares. For example, in the river basin There are 71 lakes in Kuda, but their total area is only about 2 km².

The lakes of the district belong to three genetic groups: karst, thermokarst and floodplain.

Karst lakes are found in the northwestern part of the district, in the Ekhirit-Bulagat and Bayandaevsky regions. The largest Karst lake is Lake. Khara-Nur, located on the right bank of the river. Kamenki. The length of the lake is 300 m, width - 200 m. It flows into the river. Blow. The water in the lake is low-mineralized, hydrocarbonate class, calcium.

Thermokarst lakes are common in the eastern and northeastern parts of the district. At the bottoms of valleys and valleys, in river valleys. Karst and thermokarst lakes often occur in the same area.

The largest thermokarst lake. Nuhe-Nur, located in the middle part of the Zadai-Tologoi valley, fills a depression on the surface of a high terrace. Its length is 60 m, width 10 m, prevailing depth 4-5 m. The total mineralization in the lake is high - 6500 mg/l, the water has a bitter taste, the concentration of sulfates predominates - 4365 mg/l. One and a half to two kilometers north of Lake Nuhe-Nur there is a group of lakes of thermokarst origin of smaller sizes. There are similar lakes in the Kurlunkun Pad, in the area of ​​dd. Idyga, Bahai and Bayandai. They are shallow, 1.0-1.5 meters deep, their length, as a rule, does not exceed 200 m, and their width is 100 m. The banks are very swampy, overgrown with sedge and reeds.

There are not many floodplain lakes. They have an elongated shape and are not large in size. A large floodplain lake is Lake. Ordynskoe. Its water surface area is 36.5 hectares. The lake has an elongated pear-shaped shape. Two well-defined capes jut into its middle part. The length of the lake is more than 900 m, the greatest width of the western section is 350 m, the eastern section is 500 m, the maximum depth is 16 m. The coastline is slightly indented and has a length of about 3 km. At the western end, a small bay turns into the river bed. Ordushki.

Floodplain lakes also include oxbow reservoirs formed as a result of meandering river beds.

According to the chemical composition of rivers, most lakes are classified as hydrocarbonate-calcium. In terms of mineralization level, they are fresh, with the amount of salts ranging from 500-800 mg/l. Lakes of karst origin have high mineralization. They contain a high content of sulfates and magnesium.

There are several dozen ponds within the district. Many previously existing ponds have now been eliminated. Only in the river basin There were about a hundred of them.

Considering that water resources for economic and domestic water supply are very limited, increasing the degree of their use can only be ensured by regulating flow through the restoration of destroyed ponds. Being the main regulators of flow, they maintain sufficient water near their water areas. high level groundwater.

1.4.3. The groundwater

According to hydrogeological characteristics, the territory of the district belongs to the East Siberian artesian region, which occupies a huge space from the Taimyr Peninsula in the north to Lake Baikal in the south, and is completely located within the even larger Angara-Lena artesian basin.

In a vertical section, groundwater can be divided into two hydrogeochemical zones or two levels. The upper floor occupies the very top part of geological formations and is distinguished by the fact that its waters have close water exchange with precipitation and surface waters of rivers and lakes. Here, mainly oxygen-nitrogen and nitrogen waters of atmospheric nutrition are developed. In areas of permafrost development, this level includes supra-permafrost hydrocarbonate waters. The thickness, thickness or depth of the waters of this floor is 200 m within the district.

The waters of the lower floor have no connection with the day surface and do not participate in the modern circulation of natural waters. They are of sedimentogenic, less often ancient infiltration origin. In this regard, the mineralization and chemical composition of these waters largely reflect the composition and mineralization of the waters of ancient seas, in which the accumulation of water-bearing rocks occurred.

The supra-permafrost hydrocarbonate waters of the upper floor have a mineralization of up to 0.5-1.0 g/kg, and in areas with shallow occurrence of halogen formations up to 3-10 and even 50-100 g/kg. Fresh waters here are calcium bicarbonate or slightly salted with mineralization up to 10 g/kg, calcium sulfate, sodium-calcium chloride-sulfate, calcium-sodium sulfate-chloride. There are also highly salty waters with a mineralization of more than 35 g/kg.

The waters of the lower floor are mainly methane, nitrogen-methane, and less often nitrogen-thermal and cold formation waters. In terms of the degree of mineralization, among these waters there are very strong (up to 350 g/kg) and even super-strong (up to 410-420 g/kg) brines with petroleum-type methane gases, hydrogen sulfide, potassium, and strontium.

The temperature of the district's groundwater near the surface of the platform's foundation will vary from 10 to 40ºС, i.e. it falls into the belt of cold, warm and slightly hot waters.

The waters of the upper floor have quite significant dynamic resources and provide river flow in winter. So, for example, river flow. Hangars due to underground supply in winter low water is 550-600 m³/s.

At the first drilling works (just north of the village of Novonukutsky), up to 200 m underground waters of the upper hydrogeochemical level are encountered, initially represented by fresh hydrocarbonate waters with a salinity of up to 0.5 g/kg. Then, closer to the 200 m mark, they are replaced by salty (1-3 g/kg) sulfate-calcium and sulfate-chloride calcium-sodium. The widely developed Middle Cambrian variegated sulfate rocks here allow us to assume such mineralization.

At the interval of 200-680 m of this hypothetical drilling, one can encounter groundwater of the second or lower hydrogeochemical level, represented first by salty sodium chloride (1-35 g/kg) waters, and then by brines (35-140 g/kg). Such mineralization and composition of waters are most likely, since at the beginning of the interval the host rocks will be limestones, dolomites, anhydrites and gypsum, and closer to the end of the interval - layers of rock salt of Early Cambrian age.

Under the pressure of overlying layers, groundwater can rise quite high from places of formation not only in wells, but also in zones weakened by faults. Thus, for example, daytime deep brines reach in the form of open or hidden discharge centers emerging at the bottom of rivers and lakes. But most often they do not rise to the surface of the earth, but form underground lakes and hidden discharge areas. The latter greatly complicate the extraction of fresh groundwater for domestic and drinking water supply and significantly worsen the geo-ecological situation.

Subaerial and especially hidden sources of brine discharge on the territory of the district are widespread in the Alarsky, Nukutsky, Osinsky and Bokhansky districts, in the valleys of the river. Ungi, Osy and on the coast of the Bratsk Reservoir (near the village of Khadakhan).

In the river valley Kamenki, 18 km north-west of the village of Bayandai, are karst sinkholes 18 m deep and up to 200 m wide. There is a lake in which brines are unloaded, causing the mineralization of water at a depth of 2-3 meters to reach 190 g/l.

In the interval of 680-1940 meters, you will have to drill a well in completely saline and carbonate rocks, in connection with this you will probably have to deal with calcium chloride brines with a mineralization of 140-350 g / kg, and towards the end of the interval, with brines with a mineralization of 270 meters even more 350 g/kg. At the drilling interval of 1940-2660 meters, i.e. up to the foundation of the platform, there will be a slight decrease in the salinity of brines to 270-350 g/kg and a change in the chemical composition of the water to calcium-sodium chloride.

Next will be very strong metamorphic crystalline rocks of the platform foundation, containing only fractured and fissure-vein waters in fault zones, which in composition and magnitude of mineralization correspond to the more common brines, possibly of juvenile origin.

1.5. Soils

The soil cover of the region has been well studied. Soddy-forest brown soils are common along the slopes and watersheds. They lie under pine forests on the destruction products of Jurassic rocks and make up about 15% of the district's territory. A humus horizon 20 cm thick contains 3-8% humus, the pH is slightly acidic, and the mechanical composition is sandy loam.

Let us present the profile and chemical composition of humus-carbonate soils in the Ekhirit-Bulagat region (Table 7).

Table 7

Chemical composition humus-carbonate soils

Power,

cm

Humus,

Nitrogen

Movable

phosphorus

pH

Calcium

Sodium

Ekhirit-

Bulagat-

skiy

0-18

6,0

0,404

7,0

36,31

1,93

20-32

4,06

0,234

7,0

28,81

40-60

1,93

7,2

24,28

Humus-carbonate gray and brown soils have the following morphological structure:Ekhirit-Bulagat district, Kuda river, slope with birch forest .

A0 – absent.

A 0-18 cm. Dark brown, dusty up to 3 cm, and below there is a clearly defined granular structure. Medium loamy, with significant skeletal content. The transition to the next horizon is gradual.

18-35 cm. Brown, dusty-granular structure with a significant skeletal content.

From 35-78 cm. Light brown with a whitish tint due to the high lime content. Almost structureless, very loose, highly skeletal. From 78 cm there follows crushed stone from lime-clay rock. The soil boils from a depth of 15 cm.

Soddy-carbonate soils occupy about 30% of the district's territory and are located on different relief elements under forest and meadow-steppe vegetation. Subtypes are distinguished: brown (on red loams) and gray (on weathering products of limestone and dolomite). Soil profile up to 80-100. The humus horizon is 15-20 cm, humus in the 0-5 cm layer is up to 14%. Carbonates in leached soils lie at a depth of 50 cm, in typical soils they lie close to the surface, the pH is neutral or slightly alkaline. Mechanical composition: heavy loam.

Gray forest soils with signs of podzolization, formed on colluvium of Jurassic sandstones. Distributed on the left bank of the river. Hangars on the Ida-Kuda interfluve make up 10% of the district's territory. These are loamy and sandy loam soils with a humus horizon from 5 to 30 cm and a humus content from 2 to 5%, and in dark gray soils up to 10%. On non-carbonate sediments the pH is acidic, on carbonates in the lower part of the profile it is alkaline. Phytocenosis of gray forest soils.

Podzolic soils (1% of the district's territory) are found in isolated spots on watersheds and ancient terraces under light coniferous and moss forests. The thickness of the podzolic horizon is 7-15 cm, the humus horizon is 5-15 cm, the humus content is 1-4%, and the pH is acidic.

In the soil cover of the district, a significant role (up to 10%) is played by medium-deep and thin sub-humus chernozems. They develop on a carbonate basis and have a lumpy-silty structure. They are located on the surface of terraces and in gently sloping valleys under steppe and meadow-steppe vegetation. Soil-forming rocks are loess-like and heavy loams. On steeper slopes they are replaced by low-humus and thin washed-out gravelly chernozems. In the river valley Where in elevated areas there are chernozem-like, solonetzic, low-humus soils.

In the lower parts of the valleys, the soils are chernozem-like and slightly solonetzic. Among chernozems, solonetzic soils make up 75%, leached - 20% and carbonate - 5%. In accordance with the subtypes, the thickness of the humus horizon changes - 40-30-20 cm, the depth of carbonates - 70-10-0 cm. High humus content (16-17%) in leached chernozems, in the rest - 7.5-8.5 %; The pH of non-carbonate horizons is slightly acidic, while that of carbonate horizons is slightly alkaline. Mechanical composition: medium and heavy loams. Profile of chernozem soil located on the meadow terrace of the river. Murin on the ironing meadow, given in the book by I.V. Nikolaev “Soils of the Irkutsk Region”, is as follows:

A0 0-5 cm. Dark brown. The granular-silty structure is weakly expressed.

A2 5-35 cm. Dark in color, loamy, lumpy and powdery. The transition is gradual.

B1 39-69 cm. Brown, with dark spots, lumpy powdery, medium loam. The transition is gradual.

B2 72 cm and below. Reddish-brown with dark streaks. Light loam. Grey. Boils from 35 cm.

Within the Leno-Angara steppe there are leached and solonetzic chernozems. They are strictly confined to the average and partly to lower parts watersheds. The soil-forming rocks of chernozems are loess-like loams and sandy loams.

Carbonate chernozems have a humus horizon thickness of 20-35 cm. The color of horizon A is brownish-gray or grayish-brown. The structure is finely lumpy, the composition is loose. Carbonates rise to the surface. Pseudomycelium appears at a depth of 5-10 cm from the surface. Under horizons A lies a thin layer of loess-like loam ranging from 20-40 cm in size.

Solonetz chernozems are a fairly common subtype for the described territory. The thickness of their humus horizon, as a rule, does not exceed 30 cm. The color of the horizon rocks is brownish-gray or grayish-brown. The structure is lumpy, turning into columnar. The uppermost layer of horizon A, 3-5 cm thick, is atomized and structureless, and the rest of it is compacted; carbonates in the humus horizon are most often found at a depth of about 10 cm from the surface. This type of chernozem is classified as solonetzic, deeply effervescent.

In the district, about 12% of the total area is covered by meadow-chernozem soils. They are located along the bottoms of dry hollows, low parts of slopes and microrelief depressions on ancient terraces. An increased amount of moisture accumulates on these soils due to its arrival from higher surfaces and due to the presence of long-term seasonal permafrost, which persists much longer than on positive relief elements.

Meadow-chernozem soils are formed under grass-forb steppe meadows and sparse birch forests with a lushly developed grass cover. A large mass of herbaceous vegetation in harsh climatic conditions does not have time to completely decompose. Therefore, meadow-chernozem soils are distinguished by a large thickness of the humus horizon - on average up to 0.6-1.0 meters or more. The humus content is 9-15%, often 20% or more, the pH of the upper horizons is slightly acidic and neutral.

Below is a description of meadow-chernozem soils on the river. Kuluta Ekhirit-Bulagat district.

A0 0-60 cm. Intensely dark in color, loose, completely structureless up to a depth of 35 cm, below it is mixed with finely lumpy fragile units. The transition of horizons is gradual.

60-120 cm. Variegated color. Humus spots alternate with spots of the parent rock. Unstable lumpy structure.

From 120 cm and below, carbonate loam. Boils from 75-80 cm.

Negative elements of the relief are characterized by swampy silty-gley, humus-peaty soils. Peat thickness is up to 30 cm.

The most valuable in agriculture are chernozems, sulfur forest soils and soddy-carbonate brown soils. Their natural fertility is reduced as a result of long-term economic use, violation of agrotechnical methods of land cultivation, light mechanical composition of chernozems and gray forest soils, and lack of moisture, which can be compensated by reclamation methods. Soddy-carbonate loamy soils are susceptible to water erosion.

The plowing of forests in certain areas, where up to 60% of the area has been developed, has led to a change in the potential soil fertility and a deterioration in the quality of the land.

1.6. Vegetation

The vegetation of the area is rich and varied. Currently, it has been quite fully studied thanks to the work of many Siberian botanists (Novokonov, 1984; Popov, 1957, 1957,1959; Frolova, 1960,1979; Peshkova, 1972.1985; Malyshev, Peshkova, 1984)

The flora of the region is rich and diverse and includes about 800 plant species, 366 genera, 84 families from the departments: angiosperms, gymnosperms, ferns, lycopsids and horsetails. In addition to them, there are many dozens of species from the bryophytes and lichens departments. In the vegetation cover of the district, plants of different divisions play different roles. For example, the species diversity of gymnosperms is small, only 7 species, but their family representatives form coniferous taiga over large areas of the district. The overwhelming number of species, about 770, are flowering plants. They dominate almost all phytocenoses. The most floristically rich among them are the well-known families: Asteraceae (Asteraceae) - 98 species, Poaaceae (Geraceae) - 75, Sedgeaceae - 56, Ranunculaceae - 40, Brassicas (Cruciferae) - 35, Carnationaceae - 29, Lilyaceae - 22, Buckwheataceae and umbelliferous - 21 species each. Of other families, a noticeable role is played by the Norichaceae - 20, Lamiaceae (Lamiaceae) - 18, Chenopodiaceae (Cynaceae) - 17, Willow and Orchidaceae - 16 species each, Borageaceae - 14, Violetaceae - 13, Primroses - 11, Saxifragaceae - 10 species. The listed 20 families of flowering plants account for 79% of the district's flora, excluding mosses and lichens. (Fig. 10).

Rice. 10. Vegetation cover[ 5 ]

There are 384 species of plants that prefer to live in dry places - xerophytes. There are 240 species found in the forests, mostly mesophytes. In meadows and swamps under conditions of sufficient or excessive moisture, 295 species belonging to mesophytes and hygromesophytes grow. There are only 32 species of water-coastal hydrophytes and hygrophytes, 90 species of weed-ruderal and roadside ones.

The flora of the district includes many useful plants: food, fodder, medicinal, technical, melliferous, etc.

Edible wild plants are quite common. The flora of the district includes over 100 species of edible plants. In terms of nutritional value and taste, they are not inferior to cultivated ones. Unfortunately, not all of them are used for food in Siberia. For a long time, berry plants have been of greatest interest: currants, raspberries, lingonberries, blueberries, blueberries, honeysuckle, strawberries and wild strawberries, as well as bird cherry. Their tasty and healthy fruits are consumed fresh or made into preserves, jams, fruit drinks, vitamin drinks and juices.

Species from the families of buckwheat, lily, cereals, umbelliferae, cruciferous, asteraceae, etc. are of great nutritional importance. Various dishes can be prepared from wild plants: soups, cereals, salads, drinks and even baked bread. The richest in proteins are nettle, sorrel, and quinoa; The rhizomes of many aquatic and coastal plants are distinguished by a high starch content, and the rhizomes of the bracken fern contain up to 40-46% starch; birch sap is rich in sugars. There are also plenty of high-vitamin salad greens in the area: wild onions and garlic, dandelion, shepherd's purse, large plantain, chickweed and biting midge, etc.

When collecting food plants, remember that they will be beneficial if they are collected in environmentally friendly places, away from major highways and factories.

Certain conditions must also be observed when collecting medicinal plants, which are also rich in the flora of the district. About 300 plant species can be used to treat various ailments.

“Medicines grow” in the forest, in the field and even on the roads. For colds and coughs, diaphoretic syrups from raspberries, lingonberries, as well as flowering heads of meadow clover, licorice roots or infusions of thyme, caraway, and pine buds are good for colds and coughs.

Wild food plants are the bread for animals. There are over 200 species of them in the hayfields and pastures of the district. Cereals and legumes have the highest lump qualities as a source of valuable proteins and carbohydrates. Among the legumes, these are clover, alfalfa, sweet clover, china, peas - vetch, sainfoin; among the cereals are bluegrass, wheatgrass, rump, barley, foxtail, timothy, feather grass, chamomile, fescue, tonkonog, etc. Animals love to eat fragrant and bitter, as well as salty and sour herbs, which improve appetite and help recover from illness. Among such herbs, dandelion, wormwood, yarrow, sorrel, quinoa, and solyanka are known.

Almost all insect-pollinated plants are classified as honey plants. Sources of honey are nectar and pollen. In beekeeping, the most valued legumes are legumes (kleve, alfalfa, sweet clover, sainfoin), many rosaceae (rose hips, cinquefoil, meadowsweet), various umbelliferae, buckwheat, labiatae, noricaceae and, of course, fireweed, which grows in abundance in forest clearings and along expensive

The flora of the district also contains many other useful plants, for example, technical ones that provide construction (coniferous plants) and ornamental materials (their willow branches are used to weave baskets, and tassels are knitted from feather grass and sedge leaves for whitewashing walls). There are also essential oil plants - sources of aromatic substances for perfumery and medicine. These are calamus, or mystic root, thyme, mint, valerian, wild rosemary, etc. Tannins necessary for the special processing of animal skins, giving them elasticity and water resistance, can be obtained from the bark of spruce, larch, and various types of willow.

Of the plants that cause harm to humans, weeds and poisonous herbs should be noted. Among them, three groups are distinguished: weed-field, ruderal and roadside. Weeds in fields and gardens significantly reduce yields cultivated plants. They successfully compete with them and take away a lot nutrients, moisture, intercept light. The greatest harm is caused by rhizomatous and root-sprouting weeds, which reproduce intensively vegetatively. The most common among them are: creeping wheatgrass, horsetail, field sow thistle, etc.

Ruderal, or wasteland plants grow in wastelands near fences, on garbage and manure heaps, that is, on soils enriched with organic matter. They are usually distinguished by tall, erect stems and large, often spiny leaves. These are blue motherwort, deskureniya, rhizome, thistle, common wormwood and paniculata.

Roadside plants have their own adaptations. Their stems are not tall, they are recumbent, the leaves are small, and the large ones form basal rosettes. The veins in the leaves are very strong. The most common among them are plantain, dandelion, creeping clover, knotweed or bird's buckwheat, and disc chamomile.

The vegetation cover of the Ekhirit-Bulagat region is represented by a complex combination of steppes, meadows, swamps and bushes.

Steppe mud of vegetation. Steppe vegetation, as a rule, does not stretch in wide stripes (2-10 km) along the river. Angara, Osa, Ida, Unga, Kuda and their tributaries. Steppes occupy a small area compared to forests. Distributed along elevated areas of floodplain and above-floodplain terraces and adjacent mountain slopes. The latter have different steepnesses and bear the most diverse steppe vegetation, and the highly dissected topography allows the existence of a number of steppe groups with different ecology. According to G.A. Peshkova (1969), in the Angara region 5 subtypes of steppes can be distinguished: meadow, true, saz, desert and mountain.

Meadow steppes are located on gentle slopes and lower floodplain terraces on the most fertile, thick humus horizons of chernozems. Of these, the most common are chamomile steppes consisting of mycelium or Leimus ramosa. The basis of the grass stand of meadow steppes is made up of grasses: branched chamomile, bluegrass, combed grass, and combed wheatgrass. Of the legumes, there is quite a lot of crescent alfalfa, and of other herbs - goatweed, wormwood, fragrant onion, stemless cinquefoil and strawberries. Here, but along the higher ridges of the floodplain terraces and along the slopes with light sandy soils, thin-legged-fescue steppes spread. The dominant species in them are fescue, or Valis fescue, or slender-legged comb. The herbage is rich in hard sedge, Siberian thyme (thyme), white-tomented speedwell, and stemless cinquefoil. The set of these grasses indicates a state of severe vegetation breakdown under the influence of grazing.

Cirrus-feather grass meadow steppes are also characterized by a diversity of species composition and lush grass stand. Among the cereals common here, in addition to feather feather grass, are bluegrass, awnless brome, downy sheep, and steppe timothy. In the forbs, along with steppe plants (tuberiferous grasshopper, bedstraw, sandy sainfoin, lesser redwort, dwarf lily), meadow-forest and forest cannon species are often found (lupine clover, Siberian adonis, bearded wrestler, sweet-scented rose, long-haired anemone). Also characteristic are clumps and clearings of strawberries, sometimes separated into independent associations.

Of the real ones, tyrsa with hairy feather grass, wheatgrass and serpentine steppes are often found. They are distributed along the southern slopes of ridges and high terraces with leached sandy loam chernozems. The Tyrs steppes form a large number of associations, which is explained by the ability of feather grass to grow on soils of varying chemical and mechanical composition. The bulk of the grass stand is formed by a large number of associations, which is explained by the ability of feather grass to grow on soils of varying chemical and mechanical composition. The bulk of the grass stand is formed by grasses: feather grass, Lena fescue, thin-legged comb grass, and comb wheatgrass. Forbs are also rich in floristic terms. Here you can find cold wormwood, alpine aster, pale yellow scabiosa, forked cinquefoil, Angara astragalus, common edelweiss and other species. Species composition varies depending on the microrelief. In the depressions, the grass stand is very dense and lush, with an abundance of meadow species.

Both meadow and true steppes were plowed due to the fact that they are confined to more or less leveled flat areas with relatively fertile soils.

Saz steppes are distributed over meadow salt marshes on the first floodplain terraces of many rivers, and especially the river. Zalari, Ungi, Kudy. The highest areas of these terraces are occupied by Chinese chamomile, on weak depressions - by Pabo's chamomile, and closer to the terrace they give way to thickets of brilliant chiya. Depending on the predominance of one or another cereal, the formations of vomit and chiev steppes are distinguished. These cereals are usually accompanied by halophytic grasses: anesthesia thin-flowered, thermopsis lanceolata, Siberian knotweed, creeping kochia, Russian and saltmarsh creeper, Kornut's plantain, Gmelin's kermek, cold wormwood, nitrate wormwood.

The subtype of desert steppes includes the wormwood-nitrate formation, which also occurs in the same way as the saz steppes on the first floodplain terraces of the river. Unga, Kuda and other tributaries of the Angara. The edifier of these steppes - wormwood saltpeter - is accompanied by the same plants as in the saz steppes, but much more often here in microdepressions associations of saltwort, commonweed, hornwort, common tripolium, tellungiella solonetzova, and seaside milkweed are found in spots.

From the mountain steppes, fescue from Lena fescue is noted, and on flat terraces on soils with a thin humus horizon and a light mechanical composition - bluegrass steppes from Poa racemosus and retinata. Very often, sometimes over large areas, three formations similar in floristic composition are found: cold wormwood, stemless clapper and thyme. These steppes develop on steep southern slopes, as well as on rocky and gravelly soils in flat areas. These plants tend to tolerate heavy trampling. On over-grazed pastures and around watering places, they begin to dominate in place of feather grass, chamomile or thin-legged steppes.

Steppes in combination with aspen and birch, less often pine, forb-steppe forests, create a unique appearance of the Angara forest-steppe.

Meadow and swamp type of vegetation. Meadows develop along the bottoms of river valleys. Depending on the moisture conditions, real, steppe, swampy and peaty meadows are distinguished.

True meadows in the treeless part of the district grow on meadow-chernozem and sod-meadow soils in elevated areas of river valleys. Their grass stand is heterogeneous. The cereal base is created by creeping wheatgrass, meadow bluegrass, meadow fescue, awnless brome, giant bentgrass, and meadow foxtail. The herbage is dominated by cumin, common and Buryat, burnet, meadow clover, meadow rank, yarrow, meadow geranium, and many types of buttercup. Downstream in river valleys, the salinity of soddy-meadow soils increases. The first witnesses of the appearance in the soil are easy soluble salts Usually two cereals are short-horned barley and cane foxtail. These meadows represent a halophytic version of true large-grass grasses. They are used as hayfields. Their grass stand is lushly developed, the projective cover is 100%, the height is 50-60 cm. In addition to cereals, various grasses are constantly found. In areas used for grazing, cinquefoil, saltmarsh slider, stemless sow thistle, veinless sedge, astragalus furrow, bitter saussurea, Siberian knotweed, sea sorrel, and seaside trifog appear. The grass stand becomes thinned out, and bare areas of soil are covered with field crusts.

Steppe meadows are developed on less moist slopes and terraces. They have less projective cover, up to 70-80%, and other dominants appear in the grass stand. Of the cereals, these are bluegrass angustifolia and timothy grass; legumes – alfalfa, sweet clover, sweet peas. Excessively moist marshy meadows on meadow-marsh soils are formed by sedge, reed, and beckmanium formations. In peaty meadows on purulent-peaty-gley soils on permafrost, purple reed grass, soddy pike, soddy sedge, and cotton grass dominate. These are, as a rule, grassy, ​​unproductive meadows.

All meadows are feeding grounds. When agronomically correct use can be highly effective hayfields and pastures.

Swamps occupy a small part of the district's territory. Together with meadows, they form complexes in expanded river valleys and belong to the lowland type. Swamps are often fed by supra-permafrost perched waters, less often by groundwater. The soils are meadow-bog, saline to varying degrees, as well as soddy-meadow permafrost with well-defined gleying in the lower supra-permafrost part. These are grass and moss-grass, shrub and tree-shrub swamps. In the forested area, moss swamps overgrown with birch, spruce and larch are common. Hypnum mosses grow on the hummocks of such bogs, and cuckoo flax and sphagnum grow in the depressions between hummocks. Marsh wild rosemary, blueberries, cloudberries, as well as marsh horsetail and various types of sedges grow sporadically. Other plants include swamp chamedaphne and angustifolia cotton grass. In steppe areas, low-salt marshes are common, in which grasses play a significant role: marsh marigold, trifoliate, marsh cinquefoil, marsh triostrennik, and saltmarsh cinquefoil. This type of vegetation is partially used for haymaking, and after reclamation it is involved in agricultural production. Swamps in the upper reaches of rivers are of exceptionally important water protection and water regulation significance.

7. Animal world

The fauna of the Ekhirit-Bulagat region is rich. Of the 100 species of mammals living in the south of Eastern Siberia, more than 50 are represented here. Of the 274 species of birds living in the Irkutsk region, up to 70% of the total species composition is found in the district.

The taiga complex of the district belongs to the southern taiga faunal complex of the Irkutsk region. It occupies quite a vast territory. Of the birds here, the most typical are representatives of the gallinidae order, which remain to spend the winter in the taiga and are therefore well adapted to the harsh conditions of the cold season. Chickens lead a terrestrial lifestyle; food - catkins, buds, shoots, needles - is obtained mainly from trees.

The largest representative of this order is the common capercaillie. The weight of the male is 3-5.6 kg. At the end of March - beginning of April, wood grouse begin to visit traditional mating places. They walk through the snow and pick each other up. Males sing in the evening, first in the trees, and after dawn they descend to the ground, where wood grouse fly up to them. Wood grouse chicks are born after 26 days and grow quickly. After 10 days they can fly up into the trees. The composition of the food of these birds changes with age and seasons. The chicks feed on insects, then they eat flowers, and at the end of summer - berries, seeds and green parts of plants. In winter, wood grouse feed on pine nuts and pine needles. The hazel grouse is quite numerous from the order of gallinaceae; black grouse is less common. Chickens are hunted mainly by shooting with a gun, in the fall they hunt with huskies, and in the spring they are caught on a lek. Summer brood hunting is prohibited.

Other birds of the taiga zone include the black woodpecker, and a large number of passerines: waxwing, bluetail, flycatchers, nightingales, as well as siskin, redpoll, bullfinch, bee-eater, crossbill, nutcracker, jay, kuksha, pika, and tits that remain for the winter; from the order of owls - the great gray owl. Some birds make provisions for the winter.

The black stork is found in dense high-trunk forests. This rare species is listed in the Red Book of the Irkutsk region and Russia.

In the process of evolution, mammals have developed a number of adaptations for living in the taiga zone - these are wider paws for moving through the snow, a bushier tail, and sometimes a change in color to match the color of the snow. From the order of animals, the bear lives here, which is an omnivore and hibernates in the winter, the bear, distinguished by its reddish snow. The lynx is a typical inhabitant of the taiga; it feeds on forest birds, rodents, and hares. Hunts at dusk. In size it reaches 1 m in length with a small weight of 8 - 15 kg. Usually in the taiga, the weasel is the smallest predator, the ermine; the wolverine, which is called the hyena of the north, is less common because it eats carrion but can hunt rodents and birds.

The most common rodents in the taiga are squirrels, flying squirrels, chipmunks and voles.

Of the artiodactyls, the elk is the most adapted for life in the taiga. He easily walks through swamps and can swim. The moose feeds on various plants; in winter it eats shoots of young pine, aspen, and willow; when there is light frost, it gnaws at the bark of trees. This often has a negative impact on forest vegetation; trees often dry out and die. Moose can be attacked by wolves and sometimes by bears; young animals and calves are especially affected. Heavy snowy winters have a detrimental effect on moose numbers. The meat of the animal has a good taste, its skin is very tasty. Among other ungulates, the wapiti, a subspecies of red deer, is found in the district.

This complex is the most favorable for animal habitat, as it includes a multi-tiered deciduous forest and frequent shrubs and grasses. The most characteristic birds of this complex are the Great and Lesser Spotted Woodpeckers and the Wingtail; goshawk, sparrowhawk, black kite, buzzard; hawk and long-eared owls; forest pipit, shrike, several species of blackbirds, warblers, crickets, tits, buntings - common, red, dubrovnik, etc. Some birds deciduous forests remains to spend the winter, for example, goldfinch, crow, magpie, etc. Rare, listed in the Red Book of the Irkutsk region, are the blue magpie (noted on the Kuda River near the village of Kapsal; currently there is an expansion of its range; it settles in floodplain forests, along river banks, leads a nomadic lifestyle. It nests on willow and bird cherry at a height of 1.5 m); deryaba - a large thrush. Recorded in the Nukut and Ekhirit-Bulagat regions (dd. Bakhtai and Kudareyka).

This zone is inhabited by a viviparous lizard that prefers damp places.

Among the amphibians found on the territory of this complex is the sharp-faced frog, which is less demanding of humidity than the Siberian frog and winters on land.

Mammals of the taiga zone can also be observed in the forest-steppe zone. Of the order of artiodactyls, the most typical is the roe deer, which prefers mixed forests with well-developed undergrowth and grass cover. In winter, roe deer feed throughout the day. In summer it feeds on grass, leaves, thin shoots of trees and shrubs, in winter it feeds on twigs, digging out grass and lichens from under the snow. Many animals die from exhaustion and epizootics. In many places, roe deer are protected. To increase its numbers, it is necessary to organize winter feeding and fight against predators.

Animals and birds intensively influence the forest floor and soil. Many of them vigorously rummage through the litter, looking for food. The forest litter is penetrated by entire labyrinths of surface passages of moles, voles, and shrews, which also contributes to its aeration and decomposition.

A significant part of animals and birds feed on other animals, destroying a large number of forest pests. Insectivorous birds are forest orderlies. The most useful birds living all year round: tits, pikas, nuthatches and woodpeckers, which destroy insects at all stages of development. Along with birds, insects and mammals are destroyed: shrews, moles, bats, mouse-like rodents and badgers. They eat the larvae of May beetles and leaf rollers.

Many forest birds and animals forage for food not only in the forest, but also outside it: in fields and meadows.

These are enemies of such dangerous pests of cultivated plants as wireworms, beet weevils, etc.

Forest birds of prey, owls and corvids systematically hunt field rodents. Pigeons, buntings and other granivorous birds destroy weed seeds, and by collecting grains of cultivated plants in the fields, they reduce the food supply of harmful mouse-like rodents. At the same time, some forest birds and animals become agricultural pests.

Some species of forest birds and animals spread various diseases, including those dangerous to humans and domestic animals. The encephalitis virus is transmitted to people by ticks, whose hosts at certain stages of development are chipmunks, hares, squirrels, wolves, hazel grouse, pipit, etc. Animals of prey, partly rats and mice, can be carriers of the rabies virus.

The forest-steppe complex is represented by predatory animals - wolves and foxes, light polecats and badgers; from the order of ungulates - roe deer; from the order of insectivores - the Siberian mole and shrew. Of these, the rare one is the light-colored polecat, listed in the Red Book of the Irkutsk Region. It is marked along the river valley. Where. The ferret feeds on mouse-like rodents and ground squirrels.

Rare birds of the forest-steppe complex, listed in the Red Book of the Irkutsk Region, are the Lesser Sparrowhawk; saker falcon is a large falcon with relatively wide wings; Asian Godwit.

There are few refuges in this zone, so few birds of prey are confined to the steppes: falcon, hen harrier, imperial eagle, steppe eagle. There are many more species from the passerine order: sky lark, steppe pipit, stonechat, tree sparrow, etc. Almost all steppe birds run well and have a protective coloration. In winter, most of them leave the steppe due to lack of food. Very rare, listed in the Red Book of the Irkutsk Region and the USSR, is the demoiselle crane - the smallest of the cranes, living in fescue-feather grass and wormwood-grass steppes with sparse grass. IN last years Demoiselle cranes have been observed nesting on farmland. It feeds on seeds and plant sprouts, insects, lizards and small rodents. Recorded on migration in the Ekhirit-Bulagat region, in the vicinity of the village. Kudareika, Ust-Ordynsky, Elovka, Krasny Yar. In the summer it was spotted in the Bayandaevsky district.

In the steppe and forest-steppe zones, the common or quick lizard is found, listed in the Red Book of the Irkutsk region. The viper lives in the steppe and sometimes in the forest-steppe zone. This is a slow and phlegmatic snake. Its main food is voles, and less often small birds.

Mammals of the steppe zone mostly belong to the order of rodents. These are the long-tailed gopher, the tarbagan marmot and the field mouse, which has become rare and is listed in the Red Book of the Irkutsk region.

A rare species listed in the Red Book of the Irkutsk Region is the ogre - a red duck that nests in the hilly steppes in the presence of open reservoirs. Once upon a time, bustards lived in the Ekhirit-Bulagat steppes. Now this species from the Red Data Book of the Irkutsk Region and the RSFSR is extremely rare.

The fauna of the Bolt natural complexes and reservoirs is relatively diverse. More typical for the swamp are the coot, rail, and lapwing. The gray crane is rare. It is noted in the wetlands of the river basin. Where. Among the birds of prey found here are the marsh harrier, from the order of owls the short-eared owl, etc.

Mammals live near the reservoir: shrew, water rat.

Reservoirs and river floodplains can be foci of tularemia. In the transmission of infection, a primary role is played by semi-aquatic animals, as well as the beaver rat living near humans.

151.

Decision of September 5, 2013 in case No. 12-50/2013

Resolution of the magistrate of judicial district No. 134 of the Ekhirit-Bulagat district dated *** on finding Sabirov R.M. guilty of committing administrative offense, provided for in Art. 12.8 part 1 of the Code of Administrative Offenses and sentencing in the form of deprivation of the right to drive vehicles for a period of 1 year 6 months - leave unchanged, R. M. Sabirov’s complaint - without satisfaction. This decision comes into force immediately. Judge Asaeva L. A....

152.

Decision dated September 4, 2013

Satisfy the claims of the acting prosecutor of the Ekhirit-Bulagat region. Oblige the individual entrepreneur Alexander Dmitrievich Berdanosov to carry out certification of workplaces for working conditions with subsequent certification of the organization of work on labor protection, provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date the decision was made in final form.. .

153.

Decision dated September 4, 2013

The essence of the dispute: Disputes related to transactions with private houses and privatized apartments

The claims of Victoria Viktorovna Andreeva and Alexander Viktorovich Andreev are satisfied. Agreement for the sale and purchase of an apartment and land plot located at<адрес>from DD.MM.YYYY, concluded between Victoria Viktorovna Andreeva, Alexander Viktorovich Andreev on the one hand and Olga Petrovna Chebotnyagina, acting for herself and in the interests of minor children A, G, M and R on the other hand, terminate...

154.

Decision dated September 4, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The claim of Lidiya Abokshinovna Mikhailova will be satisfied. To establish the fact of adoption of Mikhailova Lidiya Abokshinovna, DD.MM.YYYY, born<адрес>, an inheritance that opened after the death of her father O, who died DD.MM.YYYY, in the form of a land share with an area<данные изъяты>ha. Recognize for Lidiya Abokshinovna Mikhailova, born DD.MM.YYYY, the right of ownership to a land share with an area of<данные изъяты>ha...

155.

Decision dated September 3, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Disputes related to inheritance of property

The claims of Vladimir Stepanovich Mazko to restore the period for acceptance of the inheritance and to establish the fact of acceptance of the inheritance are satisfied. Restore the deadline for Vladimir Stepanovich Mazko to accept an inheritance in the form of an apartment with total area <данные изъяты>sq.m., located at<адрес>, lost pension for December 2012, remaining after the death of M, deceased DD.MM.YYYY...

156.

Decision dated September 2, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Complaints about wrong. valid (abs.) - from violations of electoral legislation

In satisfying the application of Yevgeny Trofimovich Bardakhanov to recognize the decision of the Ekhirit-Bulagat Territorial Election Commission from DD.MM.YYYY No. illegal and cancel it, the obligation of the Ekhirit-Bulagat Territorial Election Commission to eliminate the violations committed, to refuse in full.

157.

Decision dated September 2, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

A reasoned court decision will be made DD.MM.YYYY.

The court decision can be appealed to the Irkutsk Regional Court within 5 days from the date the decision was made in final form...

158.

The essence of the dispute: Other public legal relations

DD.MM.YYYY The Ekhirit-Bulagat TEC adopted decision No., which scheduled elections for the post of head of the Ust-Ordynskoe municipality on September 8, 2013.

DD.MM.YYYY By decision of the election commission, Eduard Borisovich Borkhodoev, nominated by self-nomination, was registered as a candidate for the post of head of the municipality...<данные изъяты>Resolution of September 2, 2013 in case No. 5-39/2013<адрес>Ekhirit-Bulagatsky District Court (Irkutsk Region) - Administrative<адрес>...*** at 18.15 o'clock. Zabanov A.K., driving a car brand "<данные изъяты>» license plate number, moving along a country road from the side<данные изъяты>to the side<адрес>and crossing the highway 1P-418 at 64 km. when entering the main road from a secondary road, he did not give priority in traffic and collided with a car of the brand "<адрес>» license plate number

159.

under the control of B2, which was moving from the side

towards

along the main road...<адрес>Decision of September 2, 2013 in case No. 2-679/2013<адрес>Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

160.

Acting statement satisfy the head of PKU OIK-1 of the GUFSIN of Russia for the Irkutsk region. Establish in relation to Mikhailova O.V., born *** in

towards

161.

Acting statement satisfy the head of PKU OIK-1 of the GUFSIN of Russia for the Irkutsk region. Establish in relation to Mikhailova O.V., born *** in

towards

, administrative supervision in the form of administrative restrictions: -prohibit travel outside<данные изъяты>JAO without permission from the police, - to appear at the police station at the place of residence or stay for registration 2 times a month, for a period of one year for each restriction...<данные изъяты>Decision dated August 30, 2013

162.

Acting statement satisfy the head of PKU OIK-1 of the GUFSIN of Russia for the Irkutsk region. Establish in relation to Mikhailova O.V., born *** in

towards

163.

Acting statement satisfy the head of PKU OIK-1 of the GUFSIN of Russia for the Irkutsk region. Establish in relation to Mikhailova O.V., born *** in

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

Satisfy the claims of Alfa Bank OJSC. Collect from Boroldoeva N.S. in favor of OJSC Alfa-Bank debt under a lending agreement from *** in the amount

The statement of claim of Vladimir Vasilievich Kokourov is partially satisfied. Invalidate the descriptions of the location of the boundaries and turning points of a land plot with cadastral number, the permitted use is for running personal subsidiary plots located on the lands settlements, by the address:<адрес>...

164.

Decision dated August 29, 2013

towards

Claims of Elaeva T.S. to satisfy. Restore T.S. Elaeva the deadline for accepting the inheritance that opened after the death of *** husband E. The decision can be appealed to the Irkutsk Regional Court within one month from the date of its adoption. Judge Asaeva L. A....

165.

Determination dated August 29, 2013

towards

AND ABOUT. Head of the Ministry of Internal Affairs of Russia “Ekhirit-Bulagatsky” And appealed to the court with this statement, in which he asks to establish administrative supervision in relation to V. A. Rezenkov for a period of one year with the establishment of administrative restrictions. In support of the statement, he points out that V.A. Rezenkov has an unexpunged (unexpunged) conviction for committing crimes under Art. 111 part 1 of the Criminal Code Russian Federation(hereinafter referred to as the Criminal Code)...

166.

Decision dated August 29, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Other claims

Claims i.o. satisfy the Ekhirit-Bulagat district prosecutor. To oblige the individual entrepreneur Tatyana Valerievna Popova to carry out certification of workplaces for working conditions with subsequent certification of the organization of work on labor protection, to provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date the decision was made in final form.. .

167.

Decision dated August 29, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Labor disputes - others arising from labor

Claims i.o. satisfy the Ekhirit-Bulagat district prosecutor. Oblige the individual entrepreneur Valery Filippovich Gubin to carry out certification of workplaces for working conditions with subsequent certification of the organization of work on labor protection, provide conditions for employees to undergo medical examinations. The court decision can be appealed to the Irkutsk Regional Court within a month from the date of the decision in its final form.. .

168.

Decision dated August 29, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Disputes related to inheritance of property

In satisfying the claims of Khalimova Marina Viktorovna against Eremina E.M., the legal representative of the minor Khalimova M.R., Khalimov A.R. the inclusion of an apartment and a land plot in the inheritance mass and the recognition of ownership of the apartment and land plot shall be refused due to the omission of acceptance of the inheritance.

169.

Decision dated August 28, 2013

towards

The claims of Daglaeva G.K., ***, are partially satisfied. Recognize Daglaeva G.K. ownership of a residential building with a total area of ​​60, 29 sq.m., incl. residential 38, 2 sq.m., and a land plot of 1885 sq.m., located in<адрес>. The rest of the claims will be rejected. The decision can be appealed to the Irkutsk Regional Court within one month from the date of its adoption. Judge Asaeva L. A....

170.

Decision dated August 28, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

Statement by the prosecutor of the Ekhirit-Bulagat district L.M. Khulkhanova in the interests of an indefinite number of persons to satisfy. Recognize the inaction of the Duma of the municipality "Aluzhinskoye", expressed in the failure to bring the Charter of the municipal formation "Aluzhinskoye" into compliance with current legislation, as illegal. Oblige the Duma of the Aluzhinskoye municipality to make changes to the Charter of the Aluzhinskoye municipal formation in accordance with the requirements of the Federal Law of November 28...

171.

Decision dated August 27, 2013

towards

172.

Decision dated August 27, 2013

towards

173.

Decision dated August 27, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Disputes related to inheritance of property

To satisfy the statement of claim of Viktor Grigorievich Myasnikov. To establish the fact of ownership of B, DD.MM.YYYY.r., certificate of ownership of land, series No., issued by DD.MM.YYYY Komzem of the Ekhirit-Bulagat district in which the person in whose name the certificate was issued indicated B, No. (passport data ). Include in the hereditary mass remaining after the death of B, DD.MM.YYYY born, deceased DD.MM...

174.

Decision dated August 27, 2013

Ekhirit-Bulagatsky District Court (Irkutsk Region) - Civil

The essence of the dispute: Complaints about wrong. valid (abs.) - state authorities, local governments

Statement by the prosecutor of the Ekhirit-Bulagat district L.M. Khulkhanova in the interests of an indefinite number of persons to satisfy. Recognize the inaction of the Duma of the municipality "Akhinskoye", expressed in the failure to bring the Charter of the municipal formation "Akhinskoye" into compliance with current legislation, as illegal. Oblige the Duma of the municipality "Akhinskoye" to make changes to the Charter of the municipal formation "Akhinskoye" in accordance with the requirements of the Federal Law of November 28...

175.

Resolution of August 27, 2013

Preliminary investigation authorities D.A. Fedotov accused of committing theft, that is, the secret theft of someone else's property, committed with causing significant damage to a citizen. The crime was committed under the following circumstances: DD.MM...

• The essence of the dispute: Other claims

  Claims of Khabitueva E.P. partially satisfy. Collect in favor of Khabitueva E.P. from the Ministry of Finance of the Russian Federation at the expense of the Treasury of the Russian Federation, the lost old-age pension in the amount<данные изъяты>rub. The claim against the Administration of the Pension Fund of the Russian Federation in the Ust-Ordynsky Buryat District, FKU OIK-1 GUFSIN of Russia for the Irkutsk Region, GUFSIN of Russia for the Irkutsk Region shall be denied. Refuse to satisfy the claim of Khabitueva E.P. for the recovery of compensation for moral damage...

178.

Verdict of August 22, 2013 in case No. 1-81/2013

Ekhirit-Bulagatsky District Court (Irkutsk region) - Criminal

DD.MM.YYYY around 23.00 Kolosov A.Yu. was near the gr.'s house. E at address<адрес>, where he decided to steal a Shtil 180 chainsaw from the summer kitchen located in the courtyard of the said house, and also from under a barn, also located in the courtyard of the said house, to steal meat and beef belonging to gr. E Carrying out his criminal intent aimed at secretly stealing property E, Kolosov A.Yu...

• The essence of the dispute: Disputes related to inheritance of property

  To satisfy the statement of claim of Boris Nikolaevich Kondratyev. Establish the fact of ownership of M, DD.MM.YYYY birth certificate, series No. issued by DD.MM.YYYY Komzem of the Ekhirit-Bulagat district in which the person in whose name the certificate was issued indicated M, DD.MM .YYYY DOB, No. (passport details). To establish the fact that Boris Nikolaevich Kondratiev accepted the inheritance that opened after the death of mother M, DD.MM.YYYY.r., deceased DD.MM...