Geochemical groundwater peculiarities of Paleogene sediments in S-E Western Siberia artesian basin; IOP Conference Series: Earth and Environmental Science; Vol. 43 : Problems of Geology and Subsurface Development
| Parent link: | IOP Conference Series: Earth and Environmental Science Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012030, 7 p.] |
|---|---|
| Corporate Authors: | , |
| 其他作者: | , , , , , |
| 總結: | Title screen The geochemical peculiarities of groundwater in Paleogene deposits in southeastern part of Western Siberia artesian basin are considered in the paper. Landscape, climate, geostructural and hydrogeological conditions define the water composition and quality peculiarities in this region. It has been established that ion-saline composition, mineralization and water quality changes arre governed by the horizontal zonal distribution. Groundwater of taiga landscapes generally is in equilibrium with kaolinite and quartz, mainly involving Ca- and Mg-montmorillonite, illite, carbonate minerals, sometimes barite. Groundwater in woodland grass and grassland, together with previously mentioned minerals, is usually in equilibrium with barite, colestine, and particularly, fluorite and gypsum. As a result, all relevant elements are removed from the groundwater and their accumulation level is restricted. |
| 語言: | 英语 |
| 出版: |
2016
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| 叢編: | Hydrogeochemistry and Hydrogeoecology |
| 主題: | |
| 在線閱讀: | http://dx.doi.org/10.1088/1755-1315/43/1/012030 http://earchive.tpu.ru/handle/11683/35137 |
| 格式: | 電子 Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650832 |
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| 200 | 1 | |a Geochemical groundwater peculiarities of Paleogene sediments in S-E Western Siberia artesian basin |f A. A. Balobanenko [et al.] | |
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| 225 | 1 | |a Hydrogeochemistry and Hydrogeoecology | |
| 300 | |a Title screen | ||
| 320 | |a [References: 7 tit.] | ||
| 330 | |a The geochemical peculiarities of groundwater in Paleogene deposits in southeastern part of Western Siberia artesian basin are considered in the paper. Landscape, climate, geostructural and hydrogeological conditions define the water composition and quality peculiarities in this region. It has been established that ion-saline composition, mineralization and water quality changes arre governed by the horizontal zonal distribution. Groundwater of taiga landscapes generally is in equilibrium with kaolinite and quartz, mainly involving Ca- and Mg-montmorillonite, illite, carbonate minerals, sometimes barite. Groundwater in woodland grass and grassland, together with previously mentioned minerals, is usually in equilibrium with barite, colestine, and particularly, fluorite and gypsum. As a result, all relevant elements are removed from the groundwater and their accumulation level is restricted. | ||
| 461 | 0 | |0 (RuTPU)RU\TPU\network\2499 |t IOP Conference Series: Earth and Environmental Science | |
| 463 | 0 | |0 (RuTPU)RU\TPU\network\16030 |t Vol. 43 : Problems of Geology and Subsurface Development |o XX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia |v [012030, 7 p.] |d 2016 | |
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| 610 | 1 | |a Западная Сибирь | |
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| 701 | 1 | |a Balobanenko |b A. A. | |
| 701 | 1 | |a L'gotin |b V. | |
| 701 | 1 | |a Dutova |b E. M. |c hydrogeologist |c Professor of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences |f 1956- |g Ekaterina Matveevna |3 (RuTPU)RU\TPU\pers\31021 |9 15251 | |
| 701 | 1 | |a Pokrovsky |b D. S. | |
| 701 | 1 | |a Nikitenkov |b A. N. |c physicist, hydrogeologist |c associate Professor of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences |f 1983- |g Aleksey Nikolaevich |3 (RuTPU)RU\TPU\pers\33263 |9 17008 | |
| 701 | 1 | |a Raduk |b I. V. | |
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