Geochemistry and chemical evolution of saline lakes of Western Mongolia

Bibliographic Details
Parent link:Geochemistry International
Vol. 52, iss. 5.— 2014.— [P. 388-403]
Corporate Author: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Other Authors: Shvartsev S. L. Stepan Lvovich, Kolpakova M. N. Marina Nikolaevna, Isupov V. P., Vladimirov A. G., Ariunbileg S.
Summary:Title screen
This paper presents data on the major and trace element composition of saline lakes of western Mongolia. The main geochemical types of lakes distinguished in the study are soda-, chloride-, and sulfaterich lakes. Lake water equilibria with major carbonate, sulfate, chloride, and other rock-forming minerals were calculated. The results show that the major factors controlling the formation of each lake type include evaporation and water-rock interaction processes, and the latter factor plays a critical role in freshwater and soda lakes and only a minor role in chloride lakes. Special attention was given to the soda lakes and the factors controlling lake water chemistry.
Режим доступа: по договору с организацией-держателем ресурса
Published: 2014
Subjects:
Online Access:http://dx.doi.org/10.1134/S0016702914030070
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656103

MARC

LEADER 00000naa0a2200000 4500
001 656103
005 20250402100720.0
035 |a (RuTPU)RU\TPU\network\22494 
035 |a RU\TPU\network\21012 
090 |a 656103 
100 |a 20171024d2014 k||y0rusy50 ba 
101 0 |a eng 
135 |a drcn ---uucaa 
181 0 |a i  
182 0 |a b 
200 1 |a Geochemistry and chemical evolution of saline lakes of Western Mongolia  |f S. L. Shvartsev [et al.] 
203 |a Text  |c electronic 
300 |a Title screen 
320 |a [References: p. 402-403 (47 tit.)] 
330 |a This paper presents data on the major and trace element composition of saline lakes of western Mongolia. The main geochemical types of lakes distinguished in the study are soda-, chloride-, and sulfaterich lakes. Lake water equilibria with major carbonate, sulfate, chloride, and other rock-forming minerals were calculated. The results show that the major factors controlling the formation of each lake type include evaporation and water-rock interaction processes, and the latter factor plays a critical role in freshwater and soda lakes and only a minor role in chloride lakes. Special attention was given to the soda lakes and the factors controlling lake water chemistry. 
333 |a Режим доступа: по договору с организацией-держателем ресурса 
461 |t Geochemistry International 
463 |t Vol. 52, iss. 5  |v [P. 388-403]  |d 2014 
610 1 |a электронный ресурс 
610 1 |a труды учёных ТПУ 
610 1 |a подземные воды 
610 1 |a хлорид кальция 
610 1 |a численное моделирование 
610 1 |a система вода-порода 
610 1 |a насыщение 
610 1 |a вечная мерзлота 
610 1 |a геохимия 
610 1 |a природные воды 
610 1 |a рассолы 
610 1 |a соленые озера 
610 1 |a формирование 
610 1 |a Монголия 
701 1 |a Shvartsev  |b S. L.  |c Russian hydrogeologist, Doctor of Geological and Mineralogical sciences  |c Professor of the TPU, Member of the Academy of Natural sciences  |f 1936-  |g Stepan Lvovich  |3 (RuTPU)RU\TPU\pers\24144 
701 1 |a Kolpakova  |b M. N.  |c hydrogeologist  |c assistant Professor of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences  |f 1987-  |g Marina Nikolaevna  |3 (RuTPU)RU\TPU\pers\32555  |9 16477 
701 1 |a Isupov  |b V. P. 
701 1 |a Vladimirov  |b A. G. 
701 1 |a Ariunbileg  |b S. 
712 0 2 |a Национальный исследовательский Томский политехнический университет (ТПУ)  |b Институт природных ресурсов (ИПР)  |b Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)  |3 (RuTPU)RU\TPU\col\18664 
801 2 |a RU  |b 63413507  |c 20171218  |g RCR 
856 4 |u http://dx.doi.org/10.1134/S0016702914030070 
942 |c CF