Groundwater, as a precious fresh water resource, has a profound impact
on the social and economic development in coastal areas. Western Yellow
Sea coast (WYSC), located in the eastern part of China, is one of the
most prosperous areas of China’s economic development and has a great
demand for water. WYSC is currently under increasing pressure from
groundwater pumped for regional development, and sustainable water
management throughout the region must be based on an understanding of
the hydrochemical processes that determine the quality of groundwater.
This study taking WYSC as the study area, 160 groundwater samples were
collected in the field and the content of Ca2+, Mg2+, Na+, K+, Cl-,
SO42-, HCO3-, F, Br, δ2H and δ18O in groundwater were tested. The
groundwater chemical characteristics, sources of groundwater substances,
hydrogeochemical processes and the difference between the Shandong part
(SDP) and Jiangsu part (JSP) were studied. The result shows that the
content sequence of main cations and anions in groundwater of WYSC are
Na+ > Ca2+ > Mg2+ > K+ and HCO3-
> Cl- > SO42-. The hydrochemical types of WYSC
groundwater are mainly Cl-Na, Cl-Ca, HCO3-Na and HCO3-Ca. The main
recharge source of groundwater in the WYSC is precipitation, and the
seawater and evaporation also affect the recharge process. The main
sources of dissolved substances in groundwater in the WYSC are mineral
dissolution, evaporation and seawater. The groundwater in SDP is
affected by modern seawater intrusion, while that in JSP may be affected
by ancient seawater intrusion. The dissolution and precipitation of
various minerals in the groundwater in the WYSC are affected not only by
regional conditions but also by seawater intrusion.