新疆甜水海地区红山湖泉水化学特征及其意义

doi:10.11720/wtyht.2023.2569

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Abstract

Focusing on the spring and lake water in the Hongshan Lake in the Tianshuihai area, Xinjiang, China, this study explored the formation process of the hydrochemical components in the water and the geochemical characteristics and sources of the water bodies through hydrogeochemical testing and analyses. Accordingly, the hydrocarbon-related hydrogeochemical information was obtained. The results are as follows: The spring water in the Hongshan Lake is weakly alkaline in general and dominated by brackish water. The mass concentration of main ions in the water bodies increases with increasing salinity. The water has a hydrochemical type of Na-HCO₃ and is mainly charged by atmospheric precipitation, which interacts with the surrounding rocks during the deep circulation along faults or fractures. The salinity, hydrochemical type, and characteristic coefficient of spring water indicate that the groundwater in this area features weak hydrodynamic force and deep metamorphic degree, which are similar to the characteristics of the formation water associated with hydrocarbon in oil fields. Therefore, it can be inferred that the geological environment in this area is conducive to the generation and preservation of hydrocarbon resources.

Key words： Hongshan Lake spring water geochemical characteristics hydrocarbon

Received: 18 October 2021 Published: 24 February 2023

ZTFLH:

P632

Corresponding Authors: PANG Shou-Ji E-mail: didaxr@163.com;psj0409@163.com

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	Rui XIAO
	Shou-Ji PANG
	You-Hai ZHU
	Shuai ZHANG
	Yi ZOU

Cite this article:

Rui XIAO,Shou-Ji PANG,You-Hai ZHU, et al. Hydrochemical characteristics and significance of the Hongshan Lake in the Tianshuihai area, Xinjiang, China[J]. Geophysical and Geochemical Exploration, 2023, 47(1): 39-46.

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https://www.wutanyuhuatan.com/EN/10.11720/wtyht.2023.2569 OR https://www.wutanyuhuatan.com/EN/Y2023/V47/I1/39

20])
a—geological structure map of West Kunlun and adjacent areas;b—geological sketch of study area;c—the distribution of water samples
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Simplified geological map of the research area (adapted from reference [20])
a—geological structure map of West Kunlun and adjacent areas;b—geological sketch of study area;c—the distribution of water samples

编号	采样点	矿化度/ (mg·L^-1)	水体化学类型	电导率/ (μs·cm^-1)	pH 值	δD _V-SMOW	δO _V-SMOW	阴、阳离子浓度/(mg·L^-1)
编号	采样点	矿化度/ (mg·L^-1)	水体化学类型	电导率/ (μs·cm^-1)	pH 值	δD _V-SMOW	δO _V-SMOW	F^-	Cl^-	$NO 3 -$	$SO 4 2 -$	Na⁺	$K +$	Mg²⁺	Ca²⁺	$HCO 3 -$
W1	间歇性冷泉水	2370	微咸水	3207	7.68	-96.1	-13.0	0.440	642	<0.08	94.5	555	25.3	47.9	113.0	891
W2	泉华水,水中出现钙华,池底发白	2102	微咸水	2897	7.98	-83.7	-11.3	0.540	616	<0.08	95.5	553	25.8	49.8	55.1	707
W3	泉华水,间歇性冷泉喷口处	1983	微咸水	2826	7.99	-84.5	-11.0	0.460	515	<0.08	83.4	499	24.5	45.7	68.9	747
W4	钙华区水	2093	微咸水	3032	7.98	-88.0	-11.3	0.520	573	<0.08	105.0	481	24.4	51.8	88.0	768
W5	最新形成的碳酸盐区	2091	微咸水	2963	7.4	-94.0	-12.6	0.560	506	<0.08	104.0	447	21.5	46.5	125.0	841
W6	冷泉渗流口	3076	咸水	2896	7.28	-93.9	-11.9	0.560	815	<0.08	112.0	693	28.9	55.9	186.0	1184
W7	底部呈红色的水体	2110	微咸水	4222	7.74	-91.0	-11.9	0.580	537	<0.08	93.0	495	24.4	49.5	93.1	817
W8	湖水样	119177	盐水	137000	8.07	-60.3	-8.1	<0.02	64082	<0.08	8938.0	41149	1238.0	2407.0	538.0	825

Results of water chemical analysis in the study area

Ion concentration diagrams
a—total concentration of major ions in the springs; b—total concentration of major ions in the lake; c—percentage of major anion; d—percentage of major cation

Piper diagram of ionic concentration in water samples from the study area

Relationship between hydrogen and oxygen isotope of the water samples in the study area

Gibbs diagram of the studied lakes in the study area

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