RETRACTED ARTICLE
Study of Water-rock Interaction with Hydrochemical and Isotopic Datum in Laizhou Bay
Liu Feng*, Ma Fengshan, Guo Jie, Ding Kuo
Article Information
Identifiers and Pagination:
Year: 2015Volume: 9
First Page: 90
Last Page: 97
Publisher ID: TOCENGJ-9-90
DOI: 10.2174/1874123101509010090
Article History:
Received Date: 16/09/2014Revision Received Date: 23/12/2014
Acceptance Date: 31/12/2014
Electronic publication date: 31/8/2015
Collection year: 2015
open-access license: This is an open access article distributed under the terms of the Creative Commons Attribution 4.0 International Public License (CC-BY 4.0), a copy of which is available at: https://creativecommons.org/licenses/by/4.0/legalcode. This license permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Abstract
Water-rock interaction of the groundwater in aquifer system has been analyzed and inferred with hydrochemical and isotopic datum in Laizhou Bay, eastern China. 32 samples of groundwater from three boreholes (96-5#, 96-6#, 112- 1#), couples of seawater, saline water, fresh water, surface water and rainfall are obtained in study area for hydrochemical and isotopic analyses. The origin of groundwater is generally concluded by stable isotope (§18O and §D) and the analytic results of Na+, Ca2+, Mg2+, Cl-, SO2- , HCO3- changing with depth, combined with total dissolved solids (TDS), electrical conductivity (EC), can be apparently proofs for serious water-rock interaction. The conclusion reveals that the origin of 96-5#, 112-1# is most likely saline water different from that the groundwater of 96-6# which is possible originated from fresh water, surface water or mixing of both. Compared the ion content of same borehole at different depth and different boreholes with same depth, the optimal area for building main well and mining area is determined eventually is around 96-5#.