西藏错那地热田水化学特征与物源机制

余浩文; 刘昭; 荣峰; 陈康; 男达瓦; 刘仕娟; 刘绍赟

doi:10.19509/j.cnki.dzkq.2021.0318

西藏错那地热田水化学特征与物源机制

doi: 10.19509/j.cnki.dzkq.2021.0318

余浩文^{1, 2, 3, 4,},
刘昭^{1, 2, 3, 4, ,},
荣峰⁵,
陈康^{1, 2, 3, 4},
男达瓦⁵,
刘仕娟⁶,
刘绍赟^{1, 2, 3, 4}

基金项目:

国家自然科学基金项目 41502220

中国地质调查局项目 12120114024601

西藏自治区自然科学基金重点项目 XZ202001ZR0044G

西藏自治区自然科学基金项目 XZ2019ZRG-158

详细信息

作者简介:
余浩文(1995-), 男, 现正攻读地质工程专业硕士学位, 主要从事水文地质方面的研究工作。E-mail: 2935458509@qq.com

通讯作者:
刘昭(1983-), 男, 副教授, 主要从事地热地质、水文地球化学及地下水科学教学及科研工作。E-mail: liuzhao0129@126.com

中图分类号: P618.4
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- 文章访问数: 949
- PDF下载量: 702
- 被引次数: 0
出版历程
- 收稿日期: 2020-11-20

Characteristics and source mechanism of geothermal field in Cuona, Tibet

Yu Haowen^{1, 2, 3, 4
,},
Liu Zhao^{1, 2, 3, 4
, ,},
Rong Feng⁵,
Chen Kang^{1, 2, 3, 4},
Nan Dawa⁵,
Liu Shijuan⁶,
Liu Shaoyun^{1, 2, 3, 4}

摘要

摘要: 错那县位于西藏自治区山南地区南部、喜马拉雅山脉中段，是我国重要的边境口岸。为了研究错那地区地热田的水化学特征与物源机制，通过对研究区的温泉点水样的水化学数据进行化验分析，结合研究区的地热地质条件，使用piper三线图和Gibbs图等分析了水化学特征和物质来源。在阐明几种主要的地热温度计原理和适用条件的基础上，利用各种地球化学温度计和多矿物平衡图解法对研究区地下热水进行了温度估算。基于综合分析，最终得出热储温度为117℃左右，分析出地下热水的水化学类型以HCO₃-Na型为主，并进行了相应的地热资源评价。这有助于查明地下热水物质来源，探明该地区地热资源，以便在今后为该地区的地热资源开发利用提供技术支持，同时也推动了生态环境的保护和能源结构的逐步改变。
- 西藏 /
- 地热田 /
- 水化学特征 /
- 物源机制
Abstract: Cuona county is located in the south of shannan region of Tibet and the middle of the Himalayas, which is an important border port in China. To study the characteristics and source mechanism of geothermal field in Cuona, we use hydrochemical meathods such as piper and Gibbs to analyze the hydrogeochemical characteristics and main material sources of the hot springs water with geothermal geological conditions. The temperature of reservoir in the research area is calculated by geothermometers and graphic method of multi-mineral balance after a detailed introduction of the principles of several methods.The comprehensive analysis results indicate that the geothermal reservoir temperature is about 117℃ and the study area is of HCO₃-Na type. The next step is to evaluate the resources. The research work we have done can identify main material sources and resources, provide technical support for the development and utilization of geothermal resources, meanwhile, promote ecological environmental protection and change energy structure in this region.
- Tibet /
- geothermal field /
- hydrogeochemical characteristic /
- source mechanism

HTML全文

图 1 研究区地质简图及采样点位置图

Figure 1. Geological sketch of the distribution and location of sampling points in the study area

下载: 全尺寸图片幻灯片

图 2 水样主要水化学指标箱型图

Figure 2. Box plot of the major chemical index of water samples

下载: 全尺寸图片幻灯片

图 3 研究区水样piper图

Figure 3. Piper diagram of water samples in the study area

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图 4 Q01采样点历年水质动态曲线图

Figure 4. Dynamic graph of water quality at sampling point Q01 over the years

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图 5 研究区天然水阳离子及阴离子Gibbs分布模式图

Figure 5. Gibbs distribution model of cations and anions of natural water samples in the study area

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图 6 研究区水样Na-K-Mg三角图

Figure 6. Ternary diagram of Na-K-Mg of water samples in the study area

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图 7 研究区ZK02水样lg(Q/K)-t图

Figure 7. lg(Q/K)-t diagram of water samples at Point ZK02 in the study area

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图 8 研究区Q01水样lg(Q/K)-t图

Figure 8. lg(Q/K)-t diagram of water samples at Point Q01 in the study area

下载: 全尺寸图片幻灯片

表 1 研究区主要水化学组分测试结果

Table 1. Results of major hydrochemical properties of water samples in the study area

序号	水样编号	ρ(TDS)/(mg·L^-1)		阳离子ρ_B/(mg·L^-1)					阴离子ρ_B/(mg·L^-1)						SiO₂	Sr	pH	T/℃	属性
序号	水样编号	原始值	平均值	Li⁺	K⁺	Na⁺	Ca²⁺	Mg²⁺	NO₃^-	CO₃^2-	Cl^-	SO₄^2-	F^-	HCO₃^-	ρ_B/(mg·L^-1)		pH	T/℃	属性
1	H1	132.94	101.53	0.027	1.25	3.52	25.68	2.10	0.50	0	1.42	14.62	0.28	73.39	6.88	0.192	7.76	15	河流水
2	H2	142.67		0.020	0.70	3.62	25.68	2.92	< 0.02	—	1.42	3.85	0.17	91.41	9.01	0.196	8.00	17
3	H3	28.98		0.020	0.37	0.75	3.21	0	0.35	0	0.71	0.38	0.26	14.81	4.77	0.064	8.10	14
4	J01	234.11	308.35	0.020	1.23	9.92	40.14	3.89	6.70	0	7.09	25.01	0.22	124.88	9.24	-	7.86	5	地下水
5	ZK01	506.34		0.305	4.73	124.56	17.64	0.97	0.10	15.12	29.78	119.17	4.60	157.42	11.80	0.230	8.20	22.5
6	Q04	344.67		0.064	1.75	42.51	32.10	6.82	1.70	0	8.58	44.25	1.30	181.53	15.81	0.389	7.77	13
7	Q05	388.85		0.350	1.88	67.74	22.47	5.84	0.40	0	17.02	86.25	1.80	151.92	22.79	0.369	7.90	23
8	Q06	225.20		0.043	0.40	2.57	38.52	7.79	3.30	0	7.10	19.24	0.02	131.32	11.58	0.515	7.84	9
9	Q07	234.46		0.030	0.31	4.39	36.92	8.76	1.90	0	7.70	4.25	0.04	149.35	16.26	0.586	7.80	9
10	Q08	367.21		0.144	2.75	49.98	32.10	5.84	0.45	0	12.41	62.56	1.70	168.66	22.08	0.506	7.90	19
11	Q09	165.96		0.041	0.41	14.49	17.66	2.92	0.75	0	6.21	19.24	0.28	74.67	16.99	0.227	8.03	8
12	ZK02	327.25	361.95	0.235	1.61	62.86	13.83	0.97	0.20	29.64	12.76	43.25	3.30	78.83	68.20	0.063	8.93	55	地热水
13	Q01	396.65	361.95	2.790	3.59	83.25	11.24	0.97	4.50	17.73	3.19	96.20	4.70	83.68	69.10	0.146	8.83	56	地热水

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表 2 错那研究区温泉热储温度计算结果

Table 2. Calculation results of hot springs geothermal temperature in the study area of Cuona, Tibet

实验编号	二氧化硅温度计	钠钾温度计	钾镁温度计	钠钾钙温度计
实验编号	t/℃
Q01	118	133	71	727
ZK02	116	96	53	581
平均值	117	115	62	654

下载: 导出CSV

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