基于时移电阻率法的平谷局部地区地下水时空特征研究

doi:10.11720/wtyht.2023.1515

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Abstract

The plain area in Pinggu is a major groundwater source for Beijing.To ascertain the spatio-temporal distribution of groundwater in the study area without damaging the strata,this study,using the non-intrusive time-lapse resistivity method,conducted the reciprocal measurements with Wenner and dipole-dipole arrays in Beiyangjiaqiao Village,Pinggu District.The least-squares inversion results of the profile observation data and normalized data show that:(1)the phreatic and confined aquifers in the study area are approximately horizontally stratified,with the phreatic aquifer being recharged from the north and flowing from north to south;(2)during the entire observation period,the phreatic aquifer showed a drop in water level and leakage into the confined aquifer below;(3)the water content in the aeration zone increased from April 24,2021 to September 12,2021.In contrast,the water content in the confined aquifer remained relatively stable in this period,without experiencing significant changes.The results of this study lay the foundation for the subsequent research on Quaternary strata and groundwater in the study area.Moreover,they can be used as an important reference for the development,management,and utilization of groundwater in the study area and provide a new philosophy for research on the dynamic process of groundwater.

Key words： time-lapse resistivity method groundwater spatio-temporal distribution Pinggu Beijing

Received: 14 October 2022 Published: 11 October 2023

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	Articles by authors
	Kai-Fu LI
	Huan MA
	Yan ZHANG
	Wei-Long LI
	Ji-Yi JIANG
	Bin HUANG
	Long-Guan ZHANG
	Meng-Bo QIN

Cite this article:

Kai-Fu LI,Huan MA,Yan ZHANG, et al. Spatio-temporal distribution of groundwater in the local area of Pinggu,Beijing derived using the time-lapse resistivity method[J]. Geophysical and Geochemical Exploration, 2023, 47(4): 1002-1009.

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https://www.wutanyuhuatan.com/EN/10.11720/wtyht.2023.1515 OR https://www.wutanyuhuatan.com/EN/Y2023/V47/I4/1002

Stratigraphic columns of the monitoring boreholes

Comparison of different inversion methods for theoretical dynamics models and their synthetic time-lapse data

Geomorphology and survey line layout of study area

Observation scheme time-lapse resistivity method

Inversion results of time-lapse data of Wenner array

Inversion results of time-lapse normalized data of Wenner array

Inversion results of time-lapse data of Dipole-Dipole array

Inversion results of time-lapse normalized(T3/T2) data of Dipole-Dipole array

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