PMID- 33906040 OWN - NLM STAT- MEDLINE DCOM- 20210714 LR - 20210714 IS - 1873-6424 (Electronic) IS - 0269-7491 (Linking) VI - 284 DP - 2021 Sep 1 TI - Hydrochemical changes of a spring due to the May 30, 2014 Ms 6.1 Yingjiang earthquake, southwest China. PG - 117125 LID - S0269-7491(21)00707-7 [pii] LID - 10.1016/j.envpol.2021.117125 [doi] AB - Groundwater chemistry can be affected by and related to earthquakes, thus it is crucial to understand the hydrochemical changes and associated processes caused by earthquakes for post-seismic groundwater utilization. Here we reported the major ion concentrations changes of the Ganze Spring in response to the May 30, 2014 Ms 6.1 Yingjiang earthquake, southwest China based on the daily time series (from 1st January 2012 to 20th July 2014) of Ca(2+), Mg(2+) and HCO(3)(-) concentrations, as well as data of bulk strain and Peak Ground Velocity (PGV) recorded at a nearby station. The results showed that the entire hydrochemical response process can be divided into two stages after the earthquake occurred: 1). decline stage which was characterized by an increasingly decline of the three ion concentrations, indicating a gradually significant dilution effect. At first, the relationship of molar concentrations of ions showed no obvious changes; but later as the rate of decrease in ion concentrations increased, the relationship between Ca(2+) and HCO(3)(-) reversed from Ca(2+) excess to HCO(3)(-) excess, probably resulting from a relatively decreased Ca(2+) contribution from dissolution of gypsum and dolomite due to dilution in mixing water. 2). recover stage when the ion concentrations recovered gradually with relatively lower values than that at pre-earthquake, revealing the reduction of dilute water inflow. In combination with the bulk strain and PGV data, the study suggested that major ion concentrations changes are attributed to dilution effect due to new fracture creation or unclogging/clogging of fractures triggered by the earthquake. The results could enhance the understanding of earthquake induced water chemistry changes and could have implications for water resources management and security in tectonically active areas. CI - Copyright (c) 2021 Elsevier Ltd. All rights reserved. FAU - Chen, Liying AU - Chen L AD - State Key Laboratory of Biogeology and Environmental Geology & MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences, Beijing, 100083, China; School of Water Resources and Environment, China University of Geosciences, Beijing, 100083, China. FAU - Wang, Guangcai AU - Wang G AD - State Key Laboratory of Biogeology and Environmental Geology & MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences, Beijing, 100083, China; School of Water Resources and Environment, China University of Geosciences, Beijing, 100083, China. Electronic address: wanggc@pku.edu.cn. LA - eng PT - Journal Article DEP - 20210417 PL - England TA - Environ Pollut JT - Environmental pollution (Barking, Essex : 1987) JID - 8804476 RN - 0 (Water Pollutants, Chemical) SB - IM MH - China MH - *Earthquakes MH - Environmental Monitoring MH - *Groundwater MH - *Water Pollutants, Chemical/analysis MH - Water Quality OTO - NOTNLM OT - Carbonate spring OT - Co-seismic OT - Hydrochemical processes OT - Ion concentrations OT - Post-earthquake EDAT- 2021/04/28 06:00 MHDA- 2021/07/15 06:00 CRDT- 2021/04/27 20:19 PHST- 2020/05/24 00:00 [received] PHST- 2021/04/04 00:00 [revised] PHST- 2021/04/08 00:00 [accepted] PHST- 2021/04/28 06:00 [pubmed] PHST- 2021/07/15 06:00 [medline] PHST- 2021/04/27 20:19 [entrez] AID - S0269-7491(21)00707-7 [pii] AID - 10.1016/j.envpol.2021.117125 [doi] PST - ppublish SO - Environ Pollut. 2021 Sep 1;284:117125. doi: 10.1016/j.envpol.2021.117125. Epub 2021 Apr 17.