| 000 | 03389nla2a2200469 4500 | ||
|---|---|---|---|
| 001 | 650835 | ||
| 005 | 20231030041006.0 | ||
| 035 | _a(RuTPU)RU\TPU\network\16084 | ||
| 035 | _aRU\TPU\network\16083 | ||
| 090 | _a650835 | ||
| 100 | _a20161024a2016 k y0engy50 ba | ||
| 101 | 0 | _aeng | |
| 105 | _ay z 100zy | ||
| 135 | _adrcn ---uucaa | ||
| 181 | 0 | _ai | |
| 182 | 0 | _ab | |
| 200 | 1 |
_aHydrogeochemical characteristics of water intakes from groundwater sources in Seversk _fA. I. Karmalov [et al.] |
|
| 203 |
_aText _celectronic |
||
| 225 | 1 | _aHydrogeochemistry and Hydrogeoecology | |
| 300 | _aTitle screen | ||
| 320 | _a[References: 10 tit.] | ||
| 330 | _aThe article describes the hydrogeochemical environment behavior analysis of groundwater intake which, in its turn. provides the utility and drinking water supply for Seversk. The reasons for temporary changes of the hydrogeochemical aquifer indicators in the producing areas have been highlighted. The main factor could be upset hydrodynamic conditions during long-term operation. Changed hydrogeochemical indicators have been revealed not only during the technological water treatment process but also during water transportation to consumers. Chemical composition water changes are related to secondary mineral and sludge formation on technological equipment. Precipitation is a polymineral mixture predominantly a ferrous phase. whereas phosphate and carbonate phases are secondary. Clay minerals are also found. | ||
| 461 | 0 |
_0(RuTPU)RU\TPU\network\2499 _tIOP Conference Series: Earth and Environmental Science |
|
| 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[012032, 6 p.] _d2016 |
|
| 610 | 1 | _aэлектронный ресурс | |
| 610 | 1 | _aтруды учёных ТПУ | |
| 610 | 1 | _aгидрохимические характеристики | |
| 610 | 1 | _aводозаборы | |
| 610 | 1 | _aподземные источники | |
| 610 | 1 | _aСеверск | |
| 610 | 1 | _aводоносные горизонты | |
| 701 | 1 |
_aKarmalov _bA. I. |
|
| 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 |
|
| 701 | 1 |
_aVologdina _bI. V. |
|
| 701 | 1 |
_aPokrovsky _bD. S. |
|
| 701 | 1 |
_aPokrovsky _bV. D. _cSpecialist in the field of higher professional education _cAnalyst of the Tomsk Polytechnic University _f1989- _gVitaly Dmitrievich _2stltpush _3(RuTPU)RU\TPU\pers\32204 |
|
| 701 | 1 |
_aKuzevanov _bK. K. _chydrogeologist _cengineer of Tomsk Polytechnic University _f1981- _gKonstantin Konstantinovich _2stltpush _3(RuTPU)RU\TPU\pers\37050 |
|
| 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 |
| 801 | 2 |
_aRU _b63413507 _c20170412 _gRCR |
|
| 856 | 4 | _uhttp://dx.doi.org/10.1088/1755-1315/43/1/012032 | |
| 856 | 4 | _uhttp://earchive.tpu.ru/handle/11683/35139 | |
| 942 | _cCF | ||