School of Water Resources and Environment, China University of Geosciences (Beijing), No. 29 Xueyuan Road, Haidian District, Beijing 100083, PR China; MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing), Beijing 100083, PR China.
School of Water Resources and Environment, China University of Geosciences (Beijing), No. 29 Xueyuan Road, Haidian District, Beijing 100083, PR China; MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing), Beijing 100083, PR China; Institute of Groundwater and Earth Sciences, Jinan University, Guangzhou 510632, PR China.
J Contam Hydrol. 2018 Aug;215:1-10. doi: 10.1016/j.jconhyd.2018.06.002. Epub 2018 Jun 18.
Seawater intrusion and brine water/freshwater interaction have significantly affected agriculture, industry and public water supply at Laizhou Bay, Shandong Province, China. In this study, a two-dimensional SEAWAT model is developed to simulate the seawater intrusion to coastal aquifers and brine water/fresh water interaction in the south of Laizhou Bay. This model is applied to predict the seawater intrusion and brine water/freshwater interface development in the coming years. The model profile is perpendicular to the coastal line with two interfaces, freshwater-saline water interface near the shore and inland brine water-saline water-seawater interface. The hydrogeological parameters in the SEAWAT-2000 model are calibrated by the head and salinity measurements. The precipitation infiltration coefficient, boundary conditions and thicknesses of aquifers are studied in a sensitivity analysis. The predicted results indicate that equivalent freshwater head in shallow freshwater-saline water area will decline 2.0 m by the end of the forecasting period, caused by groundwater over-pumping for farmland irrigation. The groundwater head in the brine-saline water area will also decrease about 1.8 m by the end of forecasting period, caused by excessive brine mining. Salinity finally decreases below 105 g/L in the brine area, but increases in other areas and contaminates fresh groundwater resources.
海水入侵和卤水/淡水相互作用极大地影响了中国山东省莱州湾的农业、工业和公共供水。本研究中,构建了一个二维 SEAWAT 模型,用以模拟莱州湾南部沿海含水层的海水入侵和卤水/淡水相互作用。该模型被应用于预测未来几年的海水入侵和卤水/淡水界面的发展情况。模型剖面垂直于海岸线,有两个界面,靠近海岸的淡水-咸水界面和内陆卤水-咸水-海水界面。SEAWAT-2000 模型中的水文地质参数通过水头和盐度测量进行了校准。在敏感性分析中研究了降水入渗系数、边界条件和含水层的厚度。预测结果表明,由于农业灌溉过度抽取地下水,到预测期末,浅层淡水-咸水区域的等效淡水水头将下降 2.0 米。到预测期末,由于过度开采卤水,咸水区域的地下水位也将下降约 1.8 米。盐度最终会在卤水区域降至 105g/L 以下,但在其他区域会增加,并污染了淡水资源。