|Table of Contents|

Environmental Hydrogeochemical Characteristics of Hot Springs in Tashkurgan Fault Zone of Xinjiang, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2022年第04期
Page:
699-712
Research Field:
水资源与水文地质
Publishing date:

Info

Title:
Environmental Hydrogeochemical Characteristics of Hot Springs in Tashkurgan Fault Zone of Xinjiang, China
Author(s):
ZHUANG Si-die1; 2;  ZHOU Xiao-cheng2*;  LI Peng-fei3;  SHI Zhe-ming1;  Saimai'ernaiji KAYIMU4;  ZHU Cheng-ying4;  YAN Yu-cong2
(1. School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China; 2. United Laboratory of High-pressure Physics and Earthquake Science(Key Laboratory of Earthquake Prediction), Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China; 3. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 4. Earthquake Administration of Xinjiang Uygur Autonomous Region, Urumqi 830011, Xinjiang, China)
Keywords:
hydrogeochemistry;  H-O isotopes;  Sr isotope;  thermal storage temperature;  water quality index;  hot spring;  water-rock equilibrium;  Xinjiang
PACS:
X142; P641.3
DOI:
10.19814/j.jese.2021.11028
Abstract:
Hydrogeochemical method is effective for studying the genesis of hot spring water and evaluating hot spring water resources. Six hot spring water samples collected from the Tashkurgan fault zone in Xinjiang in September, 2018 were selected. According to the concentration of major and trace elements, as well as H-O and Sr isotopes, the characteristics of hydrogeochemistry were analyzed, and the comprehensive water quality index(WQI)was used for water quality assessment. The results show that ① the spring water is generally alkaline with an average TDS of 1 036.13 mg·L-1; the chemical types of hot spring water are HCO3-Ca, HCO3-Na, and SO4-Na; the enrichment factor explains the control effect of regional metamorphic amphibolite, alkaline gneiss and intrusive granite on the characteristics of trace element content; ② the H-O isotopic compositions of spring water all distribute near the precipitation line, indicating that the recharge source is mainly meteoric water, and the recharge altitude is 4.3-5.6 km, which is consistent with the characteristics of evaporation in the arid and semi-arid climate of the plateau; the circulation depth is 1.4-2.1 km, which belongs to the circulating hot spring controlling heat and water in fault zone; ③ the water quality evaluation of major element shows that the collected hot spring water samples are not suitable for drinking water and agricultural water, and the F- concentration in the hot spring exceeds the standard; the water quality evaluation of trace element shows that the water quality identification index between 1 and 3 classes, the overall water quality is relatively primitive, but the local spatial distributions of B and As concentrations of Gongge'er and Ma'eryang hot springs are high, Li, Fe and F concentrations and water temperature of part hot springs reach the standard for medical hot springs, have effect of physical therapy and health care. The research results provide data support for geothermal research in Tashkurgan fault zone, and are of great significance for sustainable development and protection of local hot spring resources.

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Last Update: 2022-07-30