Geochemical peculiarities of nitric thermal waters in Jiangxi Province (SE-China); IOP Conference Series: Earth and Environmental Science; Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia

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Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia.— 2016.— [012012, 6 p.]
Tác giả của công ty: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Tác giả khác: Sun Z., Shvartsev S. L. Stepan Lvovich, Tokarenko O. G. Olga Grigorievna, Zippa E. V. Elena Vladimirovna, Gao B.
Tóm tắt:Title screen
The chemical composition of nitric thermal waters in Jiangxi Province, SE-China, is considered. It is shown that the studied thermal waters are characterized by low TDS (293-412 mg/l), but they always have alkaline or highly alkaline pH values. It should be noted that the content of Na{+}, Si, F{-}, HCO[3]{-}, CO[3]{2-}, sometimes SO[4]{2-} is predominant, on the other hand, the content of Ca{2+}, Mg{2+}, Cl{-} is low. It has been established that the main factors responsible for low concentrations of some chemical elements and high concentrations of others are continuous dissolution of aluminosilicate minerals and simultaneous precipitation of the secondary minerals.
Ngôn ngữ:Tiếng Anh
Được phát hành: 2016
Loạt:Hydrogeochemistry
Những chủ đề:
Truy cập trực tuyến:http://dx.doi.org/10.1088/1755-1315/33/1/012012
http://earchive.tpu.ru/handle/11683/33974
Định dạng: Điện tử Chương của sách
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649469

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