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Effect of saltwater intrusion on groundwater environment in Weihe River downstream, Shandong Province, China
Journal of Groundwater Science and Engineering 2019, 7 (3): 245-252
Published: 28 September 2019
Abstract PDF (5.5 MB) Collect
Downloads:8

Based on the geological and hydrogeological conditions along with dynamic changes of groundwater level, this paper analyzes the hydrodynamic characteristics of saltwater intrusion in the study area. According to monitoring data of groundwater quality, the distribution characteristics of macro component are analyzed, and then fuzzy comprehensive evaluation method is adopted to evaluate the impact of saltwater intrusion on groundwater environment. Concerning the influence degree of groundwater environment, the study area is divided into brine area, seriously influenced area, moderately influenced zone, slightly influenced zone and uninfluenced zone. The results can offer references for prevention and control of saltwater intrusion as well as the protection of water resources.

Issue
Characteristics analysis and model prediction of sea-salt water intrusion in lower reaches of the Weihe River, Shandong Province, China
Journal of Groundwater Science and Engineering 2016, 4 (2): 149-156
Published: 28 June 2016
Abstract PDF (43.9 MB) Collect
Downloads:14

Marine sedimentary strata are widely distributed in the coastal zone of the study area, and are rich in brine resources. The exploitation of underground water resources often first caused the intrusion of salt water in the marine strata. Based on the analysis of sea-salt water intrusion feature, the sea-salt water intrusion is divided into four stages: The occurrence and development stage (1976–1985), the rapid development stage (1986–1990), the slow development stage (1990–2000) and the stable development stage (2000–2015). Based on the comparative analysis of the relationship between seawater intrusion and influencing factors, this paper presents that the groundwater exploitation and the brine resources mining are the main control factors of sea-salt water intrusion. On this basis, we have established a numerical model of the sea-salt water intrusion. Using this model, we predicted the development trend of the sea-salt water intrusion. The results show that if the current development of groundwater and brine is maintained, the sea-salt water intrusion will gradually withdraw; once development of brine stops, sea-salt water will invade again. This provides the scientific basis for the rational exploitation of groundwater and the prevention of sea-salt water intrusion.

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