| 000 | 03769nla2a2200493 4500 | ||
|---|---|---|---|
| 001 | 650832 | ||
| 005 | 20231030041006.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\16081 | ||
| 035 | _aRU\TPU\network\16080 | ||
| 090 | _a650832 | ||
| 100 | _a20161024a2016 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 105 | _ay z 100zy | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aGeochemical groundwater peculiarities of Paleogene sediments in S-E Western Siberia artesian basin _fA. A. Balobanenko [et al.] |
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| 203 |
_aText _celectronic |
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| 225 | 1 | _aHydrogeochemistry and Hydrogeoecology | |
| 300 | _aTitle screen | ||
| 320 | _a[References: 7 tit.] | ||
| 330 | _aThe 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 _tIOP Conference Series: Earth and Environmental Science |
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| 463 | 0 |
_0(RuTPU)RU\TPU\network\16030 _tVol. 43 : Problems of Geology and Subsurface Development _oXX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia _v[012030, 7 p.] _d2016 |
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| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aгеохимические особенности | |
| 610 | 1 | _aподземные воды | |
| 610 | 1 | _aпалеогеновые отложения | |
| 610 | 1 | _aЗападная Сибирь | |
| 610 | 1 | _aартезианские бассейны | |
| 610 | 1 | _aтаежные почвы | |
| 701 | 1 |
_aBalobanenko _bA. A. |
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| 701 | 1 |
_aL'gotin _bV. |
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| 701 | 1 |
_aDutova _bE. M. _chydrogeologist _cProfessor of Tomsk Polytechnic University, Doctor of geological and mineralogical sciences _f1956- _gEkaterina Matveevna _2stltpush _3(RuTPU)RU\TPU\pers\31021 |
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| 701 | 1 |
_aPokrovsky _bD. S. |
|
| 701 | 1 |
_aNikitenkov _bA. N. _cphysicist, hydrogeologist _cassociate Professor of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences _f1983- _gAleksey Nikolaevich _2stltpush _3(RuTPU)RU\TPU\pers\33263 |
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| 701 | 1 |
_aRaduk _bI. V. |
|
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ) _h100 _2stltpush _3(RuTPU)RU\TPU\col\18664 |
| 712 | 0 | 2 |
_aНациональный исследовательский Томский политехнический университет (ТПУ) _bИнститут природных ресурсов (ИПР) _bКафедра иностранных языков (ИЯПР) _h6735 _2stltpush _3(RuTPU)RU\TPU\col\18662 |
| 801 | 2 |
_aRU _b63413507 _c20170412 _gRCR |
|
| 856 | 4 | _uhttp://dx.doi.org/10.1088/1755-1315/43/1/012030 | |
| 856 | 4 | _uhttp://earchive.tpu.ru/handle/11683/35137 | |
| 942 | _cCF | ||