|本期目录/Table of Contents|

[1]丁风和,贺嘉伟,栾博文,等.宁夏南部及邻区地震观测井地下水埋藏类型综合评价[J].地震研究,2022,45(04):599-607.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0059]
 DING Fenghe,HE Jiawei,LUAN Bowen,et al.Comprehensive Evaluation of Groundwater Types of Seismic Observational Wells in South Ningxia and Its Adjacent Areas[J].Journal of Seismological Research,2022,45(04):599-607.[doi:10.20015/j.cnki.ISSN1000-0666.2022.0059]
点击复制

宁夏南部及邻区地震观测井地下水埋藏类型综合评价(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
45
期数:
2022年04期
页码:
599-607
栏目:
出版日期:
2022-08-20

文章信息/Info

Title:
Comprehensive Evaluation of Groundwater Types of Seismic Observational Wells in South Ningxia and Its Adjacent Areas
作者:
丁风和贺嘉伟栾博文杨学峰储翔
(宁夏回族自治区地震局,宁夏 银川 750001)
Author(s):
DING FengheHE JiaweiLUAN BowenYANG XuefengCHU Xiang
(Earthquake Agency of Ningxia Hui Autonomous Region,Yinchuan 750001,Ningxia,China)
关键词:
井水位 井-含水层系统 地下水埋藏类型 宁夏南部及邻区
Keywords:
well water level well-aquifer system groundwater type South Ningxia and its adjacent areas
分类号:
P315.723
DOI:
10.20015/j.cnki.ISSN1000-0666.2022.0059
摘要:
利用宁夏南部及邻区6口地震观测井的数字化水位和气压等资料,基于井水位对气压的阶跃响应函数、频谱分析法、潮汐波群相位超前或滞后法诊断和判别了各井井-含水层的地下水埋藏类型,并结合各井点近几年水化学离子样品测量结果,分析了各井的水—岩平衡状态,综合评价和讨论了各井-含水层系统的地下水埋藏类型。结果表明:6口井承压性由强到弱的顺序分别为平凉铁路井、静宁威戎井、固原东山坡井、西吉王民井、海原甘盐池井和平凉柳湖井,但受控于区域地形地貌、构造特征、井孔结构以及裂隙发育程度等,6口井不同程度与外界有着一定的水力联系。依据成井时的贮存埋藏条件定性判别的地下水埋藏类型与多方法综合判定的这些井的地下水埋藏类型不一致的原因为各井含水层的水力特性、裂隙发育程度、井孔结构和固体潮汐波频率存在差异。
Abstract:
Using digital data of water level and air pressure in six seismic observational wells including Ganyanchi well in Haiyuan,Wangmin well in Xiji,Dongshanpo well in Guyuan,Liuhu well and Tielu well in Pingliang and Weirong well in Jingning in South Ningxia and its adjacent areas,and based on the spectrum analysis method,the step response function method of well water level to air pressure,and the phase advance or lag method of tidal wave group,we determined the groundwater type of the aquifer in each well.And using the measurements of hydrochemical ion samples of each well in recent years,we analyzed the state of water-rock equilibrium in the wells,and comprehensively discussed the groundwater type of the aquifer of each well.The results show that the bearing strength of the six wells from the strongest to the weakest is Tielu well,Weirong well,Dongshanpo well,Wangmin well,Ganyanchi well and Liuhu well.Controlled by regional landform,structural characteristics,wellhole structure and fracture development,the six wells to some degree have hydraulic connections with the external environment.Finally,we analyzed the inconsistency between groundwater types of these wells judged according to the storage conditions at the time of well completion and the groundwater types of these wells judged according to the method proposed in this paper.The hydraulic property,degree of fracture development,the well-hole structure,and the tidal wave caused the inconsistency.

参考文献/References:


丁风和,范雪芳,戴勇,等.2017.井-含水层系统地下水埋藏类型定量分析和判别[J].地震学报,39(1):78-84.
丁风和,罗国富,戴勇.2021.地震观测井地下水承压性判定方法研究与实例[M].北京:地震出版社.
胡小静,付虹,张翔,等.2020.昭通地区流体观测井地下水地球化学特征[J].地震研究,43(4):630-637.
刘序俨,郑小菁,王林,等.2009.承压井水位观测系统对体应变的响应机制分析[J].地球物理学报,52(12):3147-3157.
王丽亚,郭海朋,李文鹏.2012.气压对观测井水位的影响及校正方法[J].水文地质工程地质,39(6):29-34.
杨柳,马建英,曹井泉,等.2014.利用华北地区承压井水位资料反演含水层体应变[J].中国地震,30(2):249-259.
张炜,王吉易,鄂秀满,等.1988.水文地秀化学预报地震的原理与方法[M],北京:教育科学出版社.
张炜斌.2013.京西北盆岭构造区温泉流体地球化学[D].北京:中国地震局地震预测研究所.
Ching-Fang S D.2018.Identification of individual efficiency for barometric pressure and ocean tide load simultaneously acted on deep aquifers adjacent to the West Pacific Ocean[J].Pure and Applied Geophysics,12(2):211-223.
Darner R A,Sheets R A.2012.Using existing data to estimate aquifer properties,Great Lakes region,USA[J].Groundwater,50(3):477-484.
Karimi S,Mohammadi Z,Samani N.2017.Geothermometry and circulation depth of groundwater in Semnan thermal springs,Northern Iran[J].Environmental Earth Sciences,76(19):651-659.
Piper A M.1944.A graphic procedure in the geochemical interpretation of water analysis[J].Trans Amer Geophys Union,25(1):27-39.
Rahi K A,Halihan T.2013.Identifying aquifer type in fractured rock aquifers using harmonic analysis[J].Groundwater,51(1):76-82.
Rasmussen T C,Crawford L A.1997.Identifying and removing barometric pressure effects in confined and unconfined aquifers[J].Ground Water,35(3):502-511.
Roeloffs E A.1996.Poroelastic techniques in the study of earthquake related hydrologic phenomena[J].Adv Geophys,3(7):135-195.
Rojstaczer S,Riley F S.1990.Response of the water level in a well to Earth tides and atmospheric loading under unconfined conditions[J].Water Resources Research,26(8):1803-1817.
Shi Z,Wang G.2016.Earthquakes switch aquifers from confined to semi-confined:Earthquake changed aquifer confinement[J].Geophysical Research Letters,4(3):112-120.
Stober I,Bucher K.1999.Origin of salinity of deep groundwater in crystalline rocks[J].Terra Nova,11:181-185.
Toll N J,Rasmussen T C.2007.Removal of barometric pressure effects and earth tides from observed water levels[J].Ground Water,45(1):101-105.
Weeks E P.1979.Barometric fluctuations in wells tapping deep unconfined aquifers[J].Water Resources Research,15(5):1167-1176.

备注/Memo

备注/Memo:
收稿日期:2021-11-05
基金项目:地震科技星火计划项目(XH19048)、宁夏自然科学基金项目(2020AAC03438)和地下流体监测与应用研究创新团队(CX2019-2)联合资助.

更新日期/Last Update: 2022-08-01