Abstract
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-, HCO3 -, CO3 2-, sometimes SO4 2- is predominant, on the other hand, the content of Ca2+, Mg2+, 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.
| Original language | English |
|---|---|
| Article number | 012012 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 33 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 15 Apr 2016 |
| Event | International Conference on Modern Problems of Hydrogeology, Geology Engineering and Hydrogeoecology of Eurasia, SPGE 2015 - Tomsk, Russian Federation Duration: 23 Nov 2015 → 27 Nov 2015 |
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ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)
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Geochemical peculiarities of nitric thermal waters in Jiangxi Province (SE-China). / Sun, Z.; Shvartsev, S. L.; Tokarenko, Olga Grigorievna; Zippa, E. V.; Gao, B.
In: IOP Conference Series: Earth and Environmental Science, Vol. 33, No. 1, 012012, 15.04.2016.Research output: Contribution to journal › Conference article
}
TY - JOUR
T1 - Geochemical peculiarities of nitric thermal waters in Jiangxi Province (SE-China)
AU - Sun, Z.
AU - Shvartsev, S. L.
AU - Tokarenko, Olga Grigorievna
AU - Zippa, E. V.
AU - Gao, B.
PY - 2016/4/15
Y1 - 2016/4/15
N2 - 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-, HCO3 -, CO3 2-, sometimes SO4 2- is predominant, on the other hand, the content of Ca2+, Mg2+, 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.
AB - 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-, HCO3 -, CO3 2-, sometimes SO4 2- is predominant, on the other hand, the content of Ca2+, Mg2+, 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.
UR - http://www.scopus.com/inward/record.url?scp=84971432552&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84971432552&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/33/1/012012
DO - 10.1088/1755-1315/33/1/012012
M3 - Conference article
AN - SCOPUS:84971432552
VL - 33
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012012
ER -