000 | 02409nlm1a2200397 4500 | ||
---|---|---|---|
001 | 667952 | ||
005 | 20231030042132.0 | ||
035 | _a(RuTPU)RU\TPU\network\39163 | ||
035 | _aRU\TPU\network\18613 | ||
090 | _a667952 | ||
100 | _a20220517a2016 k y0engy50 ba | ||
101 | 0 | _aeng | |
135 | _adrgn ---uucaa | ||
181 | 0 | _ai | |
182 | 0 | _ab | |
200 | 1 |
_aDistribution of inorganic pollutants over the depth of upper peat deposi _fO. G. Savichev |
|
203 |
_aText _celectronic |
||
300 | _aTitle screen | ||
320 | _a[References: 24 tit.] | ||
330 | _aA model of distribution of inorganic substances in the polluted waters of an oligotrophic bog has been developed and geomigratory calculations have been carried out on the example of Vasyugan Bog. It is shown that the most significant changes of mineralization of bog waters caused by the inflow of industrial waste waters from oil and gas production enterprises are referred to the high layer with a thickness of approximately 0.5–1.0 m. The creation of loam as an insulating barrier in the active layer of the bog helps reduce the negative impact on the waters, but does not preserve their baseline state on the lower layer. | ||
333 | _aРежим доступа: по договору с организацией-держателем ресурса | ||
461 | _tContemporary Problems of Ecology | ||
463 |
_tVol. 8, iss. 1 _v[P. 118-124] _d2015 |
||
610 | 1 | _aэлектронный ресурс | |
610 | 1 | _aтруды учёных ТПУ | |
610 | 1 | _abog waters | |
610 | 1 | _apollutants | |
610 | 1 | _ageomigratory calculations | |
610 | 1 | _aболотные воды | |
610 | 1 | _aзагрязнители | |
610 | 1 | _aторфяные залежи | |
700 | 1 |
_aSavichev _bO. G. _cgeologist _cProfessor of Tomsk Polytechnic University, doctor of geographical sciences _f1967- _gOleg Gennadievich _2stltpush _3(RuTPU)RU\TPU\pers\34024 |
|
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 _c20220517 _gRCR |
|
856 | 4 | _uhttps://doi.org/10.1134/S1995425515010114 | |
942 | _cCF |