3 research outputs found
Analysis of flooded areas on the example of ground waters in Nazyvaevsk
Relevance of the research is caused by increasing negative impact of flooding areas, increasing damage, and reduced quality of life in the flooded areas. Directly in the Nazyvaevsk area more than 40 % of the area is flooded, and in the town more than half of the population suffers from flood. All these facts contributed to the choice of groundwater in Nazyvaevsk as the object of the research. Main aim of the study is to identify the causes of flooding, search for solutions to stabilize the situation of high level of ground water, predict the changes based on infiltration. The methods used in the study: analysis of long-term observations of the groundwater wells subsurface regime, identifying dependencies and graphical-analytical calculation of infiltration on the basis of the data collected. Results. The authors have analyzed the situation in areas with high levels of ground water with riverine (Tyujslinsk) and interfluvial (Nazyvaevsk) mode. Tyukalinsk has greater opportunities in input-output balance of groundwater and can neutralize anthropogenic impact due to Tyukalka River, which provides natural drainage. Territory of Nazyvaevsk has poor drainage conditions, as there are no rivers there, and flat relief, so the changes in the input balance of groundwater has a significant impact on the situation with flooding. The study revealed a large man-made contribution to the balance of groundwater of Nazyvaevsk, which led to serious problems with flooding at the region since 1980 to the present. According to preliminary calculations, this contribution is about 19,3 %
Degradation of flooding situation related to anthropogenic effects on the example of Tyukalinsk
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΡΠ°Π±ΠΎΡΡ ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½Π° ΡΠ²Π΅Π»ΠΈΡΠ΅Π½ΠΈΠ΅ΠΌ Π²Π»ΠΈΡΠ½ΠΈΡ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΠΎΠ³ΠΎ ΡΠ°ΠΊΡΠΎΡΠ° Π² ΡΠ°Π·Π²ΠΈΡΠΈΠΈ ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ ΠΎΡΠ²ΠΎΠ΅Π½Π½ΡΡ
ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΉ. Π ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΠ΅ Π³ΠΎΠ΄Ρ Π² ΠΠΌΡΠΊΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ ΠΏΠΎΠ΄Π²Π΅ΡΠ³Π°Π΅ΡΡΡ Π±ΠΎΠ»ΡΡΠΎΠ΅ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²ΠΎ Π½Π°ΡΠ΅Π»Π΅Π½Π½ΡΡ
ΠΏΡΠ½ΠΊΡΠΎΠ², Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅ ΠΈ ΠΌΠ΅ΡΡΠ½ΠΎΡΡΠΈ Ρ Π±Π»Π°Π³ΠΎΠΏΠΎΠ»ΡΡΠ½ΡΠΌΠΈ Π² ΡΠ΅Π»ΠΎΠΌ ΡΡΠ»ΠΎΠ²ΠΈΡΠΌΠΈ. ΠΠ΄Π½ΠΈΠΌ ΠΈΠ· ΡΠ°ΠΊΠΈΡ
Π½Π°ΡΠ΅Π»Π΅Π½Π½ΡΡ
ΠΏΡΠ½ΠΊΡΠΎΠ² ΡΠ²Π»ΡΠ΅ΡΡΡ Π³ΠΎΡΠΎΠ΄ Π’ΡΠΊΠ°Π»ΠΈΠ½ΡΠΊ, Π³Π΄Π΅ ΠΏΡΠΎΠ±Π»Π΅ΠΌΠ° ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ ΡΠ΅ΡΡΠ΅Π·Π½ΠΎ ΠΎΡΡΡΠ°Π»Π°ΡΡ Π² ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΠ΅ ΡΠ΅ΡΡΡΠ΅ Π³ΠΎΠ΄Π°, ΡΡΠΎ ΠΈ ΠΏΠΎΠ²Π»ΠΈΡΠ»ΠΎ Π½Π° Π²ΡΠ±ΠΎΡ ΠΎΠ±ΡΠ΅ΠΊΡΠ° ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ. Π¦Π΅Π»Ρ ΡΠ°Π±ΠΎΡΡ: Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ ΠΏΡΠΈΡΠΈΠ½ ΠΎΠ±ΠΎΡΡΡΠ΅Π½ΠΈΡ ΡΠΈΡΡΠ°ΡΠΈΠΈ Ρ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΠ΅ΠΌ, ΠΏΠΎΠΈΡΠΊ ΡΠ΅ΡΠ΅Π½ΠΈΠΉ ΠΏΠΎ ΡΡΠ°Π±ΠΈΠ»ΠΈΠ·Π°ΡΠΈΠΈ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ Ρ ΡΡΠ΅ΡΠΎΠΌ Π²Π»ΠΈΡΠ½ΠΈΡ ΡΠ΅ΠΊΠΈ, ΠΎΡΡΡΠ΅ΡΡΠ²Π»ΡΡΡΠ΅ΠΉ Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΉ Π΄ΡΠ΅Π½Π°ΠΆ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ. ΠΠ΅ΡΠΎΠ΄Ρ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ: Π°Π½Π°Π»ΠΈΠ· ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΡ
Π½Π°Π±Π»ΡΠ΄Π΅Π½ΠΈΠΉ Π·Π° ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΠΌΠΈ Π²ΠΎΠ΄Π°ΠΌΠΈ Π½Π° ΡΠΊΠ²Π°ΠΆΠΈΠ½Π°Ρ
ΡΠ΅ΠΆΠΈΠΌΠ½ΠΎΠΉ ΡΠ΅ΡΠΈ ΠΌΠΎΠ½ΠΈΡΠΎΡΠΈΠ½Π³Π° ΡΠΎΡΡΠΎΡΠ½ΠΈΡ Π½Π΅Π΄Ρ Ρ ΡΡΠ΅ΡΠΎΠΌ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π° Π²ΡΠΏΠ°Π²ΡΠΈΡ
ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ ΠΏΡΠΈΡΠΈΠ½Π½ΠΎ-ΡΠ»Π΅Π΄ΡΡΠ²Π΅Π½Π½ΡΡ
ΡΠ²ΡΠ·Π΅ΠΉ Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ Π³ΡΠ°ΡΠΎΠ°Π½Π°Π»ΠΈΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠ΅ΠΉ. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Ρ ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΠ΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ ΡΡΠΎΠ²Π½Ρ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
Π²ΠΎΠ΄, ΡΠ°Π·Π³ΡΡΠ·ΠΊΠ° ΠΊΠΎΡΠΎΡΡΡ
ΠΎΡΡΡΠ΅ΡΡΠ²Π»ΡΠ΅ΡΡΡ Π² ΡΠ΅ΠΊΡ Π’ΡΠΊΠ°Π»ΠΊΠ°. ΠΠ·ΡΡΠ΅Π½Π° ΠΈΠ½ΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΡΡΡ Π²ΡΠΏΠ°Π²ΡΠΈΡ
ΠΎΡΠ°Π΄ΠΊΠΎΠ² Π½Π° Π΄Π°Π½Π½ΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ Π·Π° ΠΏΠ΅ΡΠΈΠΎΠ΄Ρ ΠΎΠ±ΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ. ΠΡΡΠ²Π»Π΅Π½Ρ ΠΏΡΠΈΡΠΈΠ½Ρ ΠΌΠ΅Π΄Π»Π΅Π½Π½ΠΎΠ³ΠΎ ΡΡ
ΠΎΠ΄Π° ΡΠ°Π»ΡΡ
Π²ΠΎΠ΄ Π²Π΅ΡΠ½ΠΎΠΉ ΠΈ Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΡ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
Π²ΠΎΠ΄ Π² ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΠΉ ΠΏΠ΅ΡΠΈΠΎΠ΄. ΠΠ΅ΡΠΌΠΎΡΡΡ Π½Π° Π΄ΠΎΡΡΠ°ΡΠΎΡΠ½ΠΎ Π²ΡΡΠΎΠΊΡΡ ΡΠΏΡΡΠ³ΠΎΡΡΡ ΠΏΡΠΈΡ
ΠΎΠ΄Π½ΠΎ-ΡΠ°ΡΡ
ΠΎΠ΄Π½ΠΎΠ³ΠΎ Π±Π°Π»Π°Π½ΡΠ° (Π°ΡΠΌΠΎΡΡΠ΅ΡΠ½ΡΠ΅ ΠΎΡΠ°Π΄ΠΊΠΈ - ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΡΠ΅ - ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΠ΅ Π²ΠΎΠ΄Ρ) ΠΈ Π²ΡΡΠΎΠΊΡΡ ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡΡ ΠΊ ΠΎΡΠ²ΠΎΠ΄Ρ ΠΈΠ·Π±ΡΡΠΎΡΠ½ΠΎΠΉ Π²ΠΎΠ΄Ρ Π·Π° ΡΡΠ΅Ρ ΡΡΠ°Π½Π·ΠΈΡΠ½ΠΎΠΉ (ΠΏΠ΅ΡΠ΅ΡΠ΅ΠΊΠ°ΡΡΠ΅ΠΉ Π³ΠΎΡΠΎΠ΄) ΡΠ΅ΠΊΠΈ Π’ΡΠΊΠ°Π»ΠΊΠ°, ΠΌΠ½ΠΎΠ³ΠΎΡΠΈΡΠ»Π΅Π½Π½ΡΠ΅ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΡΠ΅ ΡΠΎΠΎΡΡΠΆΠ΅Π½ΠΈΡ, ΡΠ°ΠΊΠΈΠ΅ ΠΊΠ°ΠΊ: Π²ΠΎΠ΄ΠΎΠΏΡΠΎΠ²ΠΎΠ΄ΡΡΠΈΠ΅ ΡΡΡΠ±Ρ, ΠΏΠ»ΠΎΡΠΈΠ½Ρ, Π½Π°ΡΡΠΏΠ½ΡΠ΅ ΠΌΠΎΡΡΡ, Π΄ΠΎΡΠΎΠ³ΠΈ ΠΈ ΠΌΠ½. Π΄Ρ., Π²Π½ΠΎΡΡΡ ΡΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΉ Π²ΠΊΠ»Π°Π΄ Π² Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΉ Π΄ΡΠ΅Π½Π°ΠΆ, ΠΏΠΎΠ½ΠΈΠΆΠ°Ρ ΡΠ°ΡΡ
ΠΎΠ΄Π½ΡΡ ΡΠ°ΡΡΡ Π²ΠΎΠ΄Π½ΠΎΠ³ΠΎ Π±Π°Π»Π°Π½ΡΠ°. Π Π΅Π³ΡΠ»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΡΡΠΎΠΊΠ° ΡΠ΅ΠΊΠΈ ΠΏΡΠΈΠ²ΠΎΠ΄ΠΈΡ ΠΊ ΡΡ
ΡΠ΄ΡΠ΅Π½ΠΈΡ ΠΎΡΠ²ΠΎΠ΄Π° ΠΊΠ°ΠΊ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΡΡ
, ΡΠ°ΠΊ ΠΈ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
Π²ΠΎΠ΄, ΡΠ²Π΅Π»ΠΈΡΠΈΠ²Π°Ρ ΡΠΈΡΠΊΠΈ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ ΠΈ ΠΏΡΠΎΠ΄ΠΎΠ»ΠΆΠΈΡΠ΅Π»ΡΠ½ΠΎΡΡΡ Π²Π΅ΡΠ΅Π½Π½Π΅Π³ΠΎ ΠΏΠΎΠ»ΠΎΠ²ΠΎΠ΄ΡΡ.Relevance of the work is caused by the increase in the role of human factor in development of flooding areas. In recent years, in Omsk region spring flood exposed to a large quantity of settlements, including areas with satisfactory conditions. One of these settlements is Tyukalinsk where there are serious flooding problems in the last four years, that influenced the choice of the research object. The aim of the study is to identify the causes of deterioration of spring flood situation, to search for solutions to flooding stabilization taking into account the presence of the river, carrying out the natural drainage area. The methods: analysis of long-term observations of groundwater in the wells of regime subsurface condition of monitoring network taking into account the amount of precipitation, identification of graphical-analytical dependencies and causality. Results. The authors have analyzed the long-term changes in groundwater levels, which enter into the river Tyukalka. They study the values of precipitation in the given territory for the periods of surveys. The causes of slow withdrawal of meltwater in spring and the accumulation of groundwater to the many years were identidied. Despite the relatively high elasticity of admission and expenditure parts of the water balance (precipitation - surface water - groundwater) and high capacity for allotment of excess water by transit (crossing the city) Tyukalka river, numerous man-made structures such as carrying water pipes, dams, bulk bridges, road and many others, contribute significantly to the natural drainage, reducing the expenditure side of water balance. Regulation of river flow leads to poor drainage of both surface and groundwater, increasing the risk of flooding and the duration of the spring flood
Analysis of flooded areas on the example of ground waters in Nazyvaevsk
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΡΠ°Π±ΠΎΡΡ ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½Π° Π²ΠΎΠ·ΡΠ°ΡΡΠ°ΡΡΠΈΠΌ Π½Π΅Π³Π°ΡΠΈΠ²Π½ΡΠΌ Π²Π»ΠΈΡΠ½ΠΈΠ΅ΠΌ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΉ, ΡΠ²Π΅Π»ΠΈΡΠ΅Π½ΠΈΠ΅ΠΌ ΡΡΠ΅ΡΠ±Π° ΠΈ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ΠΌ ΠΊΠ°ΡΠ΅ΡΡΠ²Π° ΠΆΠΈΠ·Π½ΠΈ Π½Π°ΡΠ΅Π»Π΅Π½ΠΈΡ, ΠΏΡΠΎΠΆΠΈΠ²Π°ΡΡΠ΅Π³ΠΎ Π½Π° ΠΏΠ°Π²ΠΎΠ΄ΠΊΠΎΠΎΠΏΠ°ΡΠ½ΠΎΠΉ ΠΌΠ΅ΡΡΠ½ΠΎΡΡΠΈ. ΠΠ΅ΠΏΠΎΡΡΠ΅Π΄ΡΡΠ²Π΅Π½Π½ΠΎ Π² ΠΠ°Π·ΡΠ²Π°Π΅Π²ΡΠΊΠΎΠΌ ΡΠ°ΠΉΠΎΠ½Π΅ ΠΏΠΎΠ΄Π²Π΅ΡΠΆΠ΅Π½ΠΎ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡ Π±ΠΎΠ»Π΅Π΅ 40 % ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ, Π° Π² ΡΠ°ΠΌΠΎΠΌ Π³ΠΎΡΠΎΠ΄Π΅ ΠΎΡ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΠΉ ΡΡΡΠ°Π΄Π°Π΅Ρ Π±ΠΎΠ»Π΅Π΅ ΠΏΠΎΠ»ΠΎΠ²ΠΈΠ½Ρ Π½Π°ΡΠ΅Π»Π΅Π½ΠΈΡ, Π²ΡΠ΅ ΡΡΠΎ ΡΠΏΠΎΡΠΎΠ±ΡΡΠ²ΠΎΠ²Π°Π»ΠΎ Π²ΡΠ±ΠΎΡΡ Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄ ΠΠ°Π·ΡΠ²Π°Π΅Π²ΡΠΊΠ° Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΎΠ±ΡΠ΅ΠΊΡΠ° ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ. Π¦Π΅Π»Ρ ΡΠ°Π±ΠΎΡΡ: Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ ΠΏΡΠΈΡΠΈΠ½ Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΡ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΠΉ, ΠΏΠΎΠΈΡΠΊ ΡΠ΅ΡΠ΅Π½ΠΈΠΉ ΠΏΠΎ ΡΡΠ°Π±ΠΈΠ»ΠΈΠ·Π°ΡΠΈΠΈ ΡΠΈΡΡΠ°ΡΠΈΠΈ Ρ Π²ΡΡΠΎΠΊΠΈΠΌ ΡΡΠΎΠ²Π½Π΅ΠΌ Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄, ΠΏΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠΉ Ρ ΡΡΠ΅ΡΠΎΠΌ ΠΈΠ½ΡΠΈΠ»ΡΡΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΈΡΠ°Π½ΠΈΡ. ΠΠ΅ΡΠΎΠ΄Ρ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ: Π°Π½Π°Π»ΠΈΠ· ΠΌΠ½ΠΎΠ³ΠΎΠ»Π΅ΡΠ½ΠΈΡ
Π½Π°Π±Π»ΡΠ΄Π΅Π½ΠΈΠΉ Π·Π° Π³ΡΡΠ½ΡΠΎΠ²ΡΠΌΠΈ Π²ΠΎΠ΄Π°ΠΌΠΈ Π½Π° ΡΠΊΠ²Π°ΠΆΠΈΠ½Π°Ρ
ΡΠ΅ΠΆΠΈΠΌΠ½ΠΎΠΉ ΡΠ΅ΡΠΈ ΠΌΠΎΠ½ΠΈΡΠΎΡΠΈΠ½Π³Π° ΡΠΎΡΡΠΎΡΠ½ΠΈΡ Π½Π΅Π΄Ρ, Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ Π³ΡΠ°ΡΠΎΠ°Π½Π°Π»ΠΈΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠ΅ΠΉ ΠΈ ΡΠ°ΡΡΠ΅Ρ ΠΈΠ½ΡΠΈΠ»ΡΡΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΈΡΠ°Π½ΠΈΡ Π½Π° ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠΈ ΡΠΎΠ±ΡΠ°Π½Π½ΡΡ
Π΄Π°Π½Π½ΡΡ
. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ: ΠΏΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Π° ΡΠΈΡΡΠ°ΡΠΈΡ Ρ Π³ΡΡΠ½ΡΠΎΠ²ΡΠΌΠΈ Π²ΠΎΠ΄Π°ΠΌΠΈ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΉ Ρ ΠΏΡΠΈΡΠ΅ΡΠ½ΡΠΌ (Π³ΠΎΡΠΎΠ΄ Π’ΡΠΊΠ°Π»ΠΈΠ½ΡΠΊ) ΠΈ ΠΌΠ΅ΠΆΠ΄ΡΡΠ΅ΡΠ½ΡΠΌ (Π³ΠΎΡΠΎΠ΄ ΠΠ°Π·ΡΠ²Π°Π΅Π²ΡΠΊ) ΡΠ΅ΠΆΠΈΠΌΠΎΠΌ. ΠΠΎΡΠΎΠ΄ Π’ΡΠΊΠ°Π»ΠΈΠ½ΡΠΊ ΠΎΠ±Π»Π°Π΄Π°Π΅Ρ Π±ΠΎΠ»ΡΡΠΈΠΌΠΈ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡΠΌΠΈ Π² Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠΌ ΡΠ΅Π³ΡΠ»ΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ ΠΏΡΠΈΡ
ΠΎΠ΄Π½ΠΎΡΠ°ΡΡ
ΠΎΠ΄Π½ΠΎΠ³ΠΎ Π±Π°Π»Π°Π½ΡΠ° Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄ ΠΈ ΡΠΏΠΎΡΠΎΠ±Π΅Π½ Π½ΠΈΠ²Π΅Π»ΠΈΡΠΎΠ²Π°ΡΡ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΠΎΠ΅ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ Π·Π° ΡΡΠ΅Ρ ΡΠ΅ΠΊΠΈ Π’ΡΠΊΠ°Π»ΠΊΠ°, ΠΊΠΎΡΠΎΡΠ°Ρ ΠΎΠ±Π΅ΡΠΏΠ΅ΡΠΈΠ²Π°Π΅Ρ Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΉ Π΄ΡΠ΅Π½Π°ΠΆ. Π’Π΅ΡΡΠΈΡΠΎΡΠΈΡ ΠΠ°Π·ΡΠ²Π°Π΅Π²ΡΠΊΠ° Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠ΅Π·ΡΠ΅ΡΡΡ ΡΠ»Π°Π±ΠΎΠΉ Π΄ΡΠ΅Π½ΠΈΡΠΎΠ²Π°Π½Π½ΠΎΡΡΡΡ, ΡΠ°ΠΊ ΠΊΠ°ΠΊ Π½Π΅ ΠΈΠΌΠ΅Π΅Ρ ΡΠ΅ΠΊ, ΠΈ ΠΎΠ±Π»Π°Π΄Π°Π΅Ρ ΡΠ°Π²Π½ΠΈΠ½Π½ΡΠΌ ΡΠ΅Π»ΡΠ΅ΡΠΎΠΌ, Π² Π²ΠΈΠ΄Ρ ΡΠ΅Π³ΠΎ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π² ΠΏΡΠΈΡ
ΠΎΠ΄Π½ΠΎΠΌ Π±Π°Π»Π°Π½ΡΠ΅ Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄ ΠΎΠΊΠ°Π·ΡΠ²Π°Π΅Ρ ΡΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ Π²Π»ΠΈΡΠ½ΠΈΠ΅ Π½Π° ΡΠΈΡΡΠ°ΡΠΈΡ Ρ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡΠΌΠΈ. Π ΠΏΡΠΎΡΠ΅ΡΡΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π²ΡΡΠ²Π»Π΅Π½ Π±ΠΎΠ»ΡΡΠΎΠΉ Π°Π½ΡΡΠΎΠΏΠΎΠ³Π΅Π½Π½ΡΠΉ Π²ΠΊΠ»Π°Π΄ Π² Π±Π°Π»Π°Π½Ρ Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄ Π³ΠΎΡΠΎΠ΄Π° ΠΠ°Π·ΡΠ²Π°Π΅Π²ΡΠΊΠ°, ΠΏΡΠΈΠ²Π΅Π΄ΡΠΈΠΉ Ρ 1980 Π³. ΠΏΠΎ Π½Π°ΡΡΠΎΡΡΠ΅Π΅ Π²ΡΠ΅ΠΌΡ ΠΊ ΡΠ΅ΡΡΠ΅Π·Π½ΡΠΌ ΠΏΡΠΎΠ±Π»Π΅ΠΌΠ°ΠΌ Ρ ΠΏΠΎΠ΄ΡΠΎΠΏΠ»Π΅Π½ΠΈΡΠΌΠΈ Π² Π½Π°ΡΠ΅Π»Π΅Π½Π½ΠΎΠΌ ΠΏΡΠ½ΠΊΡΠ΅. ΠΠΎ ΠΏΡΠ΅Π΄Π²Π°ΡΠΈΡΠ΅Π»ΡΠ½ΡΠΌ ΡΠ°ΡΡΠ΅ΡΠ°ΠΌ ΡΡΠΎΡ Π²ΠΊΠ»Π°Π΄ ΡΠΎΡΡΠ°Π²Π»ΡΠ΅Ρ ΠΏΠΎΡΡΠ΄ΠΊΠ° 19,3 %.Relevance of the research is caused by increasing negative impact of flooding areas, increasing damage, and reduced quality of life in the flooded areas. Directly in the Nazyvaevsk area more than 40 % of the area is flooded, and in the town more than half of the population suffers from flood. All these facts contributed to the choice of groundwater in Nazyvaevsk as the object of the research. Main aim of the study is to identify the causes of flooding, search for solutions to stabilize the situation of high level of ground water, predict the changes based on infiltration. The methods used in the study: analysis of long-term observations of the groundwater wells subsurface regime, identifying dependencies and graphical-analytical calculation of infiltration on the basis of the data collected. Results. The authors have analyzed the situation in areas with high levels of ground water with riverine (Tyujslinsk) and interfluvial (Nazyvaevsk) mode. Tyukalinsk has greater opportunities in input-output balance of groundwater and can neutralize anthropogenic impact due to Tyukalka River, which provides natural drainage. Territory of Nazyvaevsk has poor drainage conditions, as there are no rivers there, and flat relief, so the changes in the input balance of groundwater has a significant impact on the situation with flooding. The study revealed a large man-made contribution to the balance of groundwater of Nazyvaevsk, which led to serious problems with flooding at the region since 1980 to the present. According to preliminary calculations, this contribution is about 19,3 %