|本期目录/Table of Contents|

[1]胡小静,付 虹,张 翔,等.昭通地区流体观测井地下水地球化学特征*[J].地震研究,2020,43(04):630-637.
 HU Xiaojing,FU Hong,ZHANG Xiang,et al.Hydrogeo Chemical Characteristics of Groundwater in Seismic Observation Wells in Zhaotong Area[J].Journal of Seismological Research,2020,43(04):630-637.
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昭通地区流体观测井地下水地球化学特征*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
43
期数:
2020年04期
页码:
630-637
栏目:
出版日期:
2020-09-17

文章信息/Info

Title:
Hydrogeo Chemical Characteristics of Groundwater in Seismic Observation Wells in Zhaotong Area
作者:
胡小静1付 虹1张 翔1何德强2周晓成3李 丽4
(1.云南省地震局,云南 昆明 650224; 2.昭通市防震减灾局,云南 昭通 657099; 3.中国地震局地震预测研究所,北京 100036; 4.山西省地震局,山西 太原 030021)
Author(s):
HU Xiaojing1FU Hong1ZHANG Xiang1HE Deqiang2ZHOU Xiaocheng3LI Li4
(1.Yunnan Earthquake Agency,Kunming 650224,Yunnan,China)(2.Zhaotong Earthquake Agency,Zhaotong 657099,Yunnan,China)(3.Institute of Earthquake Forecasting,China Earthquake Administration,Beijing 100036,China)(4.Shanxi Earthquake Agency,Taiyuan 030021,Shanxi,China)
关键词:
流体观测井 地球化学特征 昭通地区
Keywords:
seismic observation wells hydrochemical characteristics Zhaotong area
分类号:
P315.724
DOI:
-
摘要:
对昭通地区12口流体观测井及其周边5个地表水体进行取样测试,分析其水化学组分和氢氧同位素,确定该地区流体观测井的地球化学背景特征,为该区流体测项的跟踪分析提供基础支撑。水岩平衡结果显示:相较于其它观测井,昭阳一中井地下水水岩平衡状态更接近于部分成熟水,表现为地下水补给过程缓慢,水岩作用程度较高; 其余观测井均处在未成熟水阶段,表现出补给路径较短,水岩相互作用较弱等特点。氢氧同位素组成显示:研究区内大多数流体观测井补给源均为大气降水,但补给方式略有差异。水化学组分演化过程显示:自2014年以来,大多数井含水层水体未发生新的水岩作用过程,并且与其附近的河流水力联系密切。
Abstract:
In order to discuss the hydrogeochemical background seismic observation wells in Zhaotong area and provide basic support for judging seismic chemical anomalies of the groundwater,we collected 17 water samples from 12 seismic observation wells and 5 surface water bodies,tested and analyzed the chemical components and hydrogen and oxygen isotopes of groundwater. The results of water-rock balance results revealed that the groundwater in the Zhaoyang No.1 Middle school well was characterized with long and slow recharge process,strong water-rock reaction,meaning partial equilibrated water,the other observation wells were classified as immature water,which were characterized with short recharge process and weak water-rock reaction. The isotope data of hydrogen and oxygen indicated that most of the seismic observation wells in the study area were originated from the atmospheric precipitation,and there were slightly different in the recharge modes. The evolution of chemical compositions of groundwater showed that most seismic observation wells had not experienced new water-rock reactions since 2014 and were closely related to the flowing river by 100 m in hydraulic connection.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2019-07-02
基金项目:基于地下流体资料震例回朔的亚失稳状态识别研究(2018YFC150330505)、云南省地震局科技人员传帮带培养任务(C3-201707)、2018年度震情跟踪定向工作任务(2018010301)及前兆观测中亚失稳现象研究(SKB-1936-01)联合资助.
通讯作者:付虹(1963-),女,研究员.主要从事地震综合预测研究.E-mail:fuhong@mail.eqyn.ac.cn

更新日期/Last Update: 2020-09-17