Groundwater trace element changes were probably induced by the ML3.3 earthquake in Chaoyang district, Beijing

Abstract

Geochemical composition changes in groundwater related to earthquakes have been documented in previous studies, and most such studies focused on the changes in major ions, hydrogen, oxygen isotopes, and geochemical gases. Changes in trace elements were suggested to be more sensitive to small earthquakes than the commonly used chemical constituents such as major ions, yet they received less attention. Beijing is located in the Zhangjiakou-Bohai seismic belt and experiences frequent occurrences of small earthquakes. In this paper, we collected groundwater samples from a hot spring in Yanqing district of Beijing weekly from August 2021 to August 2022. Each water sample contained 41 trace chemical compositions. During the sampling, an earthquake with a magnitude of ML3.3 occurred in the Chaoyang district of Beijing on 3 February 2022, so these trace elements changes were systematically monitored before and after the earthquake: Li, Sc, Ti, and Pb elements had upward changes before the earthquake, while Cu, Nb, Th, Zn, Tl, and U elements had downward changes before the earthquake. Eu (rare earth elements) had upward changes after the earthquake. At the same time, the earthquake caused no significant changes in the groundwater level in the seismic monitoring well near the Songshan spring. Such responses indicate that trace elements are likely to be more sensitive to crustal strain than groundwater level. We considered that the earthquake-induced rock cracks before or after the earthquake caused enhancing water-rock interaction and led to the migration of trace elements between the water column and rocks, which is the mechanism to explain the trace elemental changes. This study probably provides a comprehensive assessment of the sensitivity of trace element constituents to the earthquake. Furthermore, we suggest that more long-term continuous monitoring and research of trace elements in Beijing and Zhangjiakou-Bohai Fault Zone should be considered to explore the response mechanism of groundwater geochemistry to earthquakes in the future.

Water Geochemistry and Stable Isotope Changes Record Groundwater Mixing After a Regional Earthquake in Northeast India

“…These signals need to be assessed relative to time‐series of earthquake‐induced changes in groundwater geochemistry data that require continuous, long‐term monitoring systems and usually manual sampling, alongside expensive and time‐consuming laboratory analyses (Woith et al., 2013; Xiang & Peng, 2023). To this end, there are recent and ongoing programs (Martinelli, 2020; Ouzounov et al., 2018) to monitor the hydrogeochemical properties of groundwater to search for precursors and document earthquake‐geochemical correlations for example, Russia (Kopylova & Boldina, 2019, 2020, 2021; http://www.emsd.ru/lgs/observations), China (Chen & Liu, 2023; Chen & Wang, 2021; Shi et al., 2013, 2020; Wang et al., 2018; Xiang & Peng, 2023; Yu et al., 2023), USA (Wang & Manga, 2015), Japan (Hosono & Masaki, 2020; Hosono et al., 2020; Itaba et al., 2010; Koizumi et al., 2019; Matsumoto & Koizumi, 2013; Nakagawa et al., 2020; Uyeda, 2013; https://gbank.gsj.jp/wellweb/GSJ_E/index.shtml), Iceland (Andren et al., 2016; Barbieri et al., 2021; Claesson et al., 2007; Skelton et al., 2019), Korea (Kaown et al., 2021; Kim et al., 2019, 2020; Lee et al., 2021), and Italy (Barberio et al., 2017, 2020; Binda et al., 2020; De Luca et al., 2018; Franchini et al., 2021; Martinelli et al., 2021; Rosen et al., 2018).…”