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Numerical simulation of seawater intrusion to coastal aquifers and brine water/freshwater interaction in south coast of Laizhou Bay, China

机译:莱州湾南岸海水侵入沿海含水层和盐水/淡水相互作用的数值模拟

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摘要

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.
机译:海水入侵和盐水/淡水相互作用严重影响了中国山东省莱州湾的农业,工业和公共供水。在这项研究中,建立了二维SEAWAT模型来模拟莱州湾南部的海水侵入沿海含水层和盐水/淡水相互作用。该模型用于预测未来几年的海水入侵和盐水/淡水界面的发展。模型剖面垂直于沿海线,具有两个界面,即靠近海岸的淡水-盐水界面和内陆盐水-盐水-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校准。通过敏感性分析研究了降水入渗系数,边界条件和含水层厚度。预测结果表明,由于农田灌溉地下水超量灌溉,到预测期末,淡水-咸水浅水区的当量淡水头将下降2.0μm。由于盐水开采过多,到预测期结束时,盐水盐水地区的地下水水头也将减少约1.8 m。盐度地区的盐度最终降低到105µg / L以下,但其他地区的盐度提高,并污染了新鲜的地下水资源。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2018年第8期|1-10|共10页
  • 作者单位

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing);

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing),Institute of Groundwater and Earth Sciences, Jinan University;

    Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory;

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing);

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing);

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing);

    School of Water Resources and Environment, China University of Geosciences (Beijing),MOE Key Laboratory of Groundwater Circulation and Environmental Evolution, China University of Geosciences (Beijing);

    Tianjin Center of China Geological Survey;

    Tianjin Center of China Geological Survey;

    Tianjin Center of China Geological Survey;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Seawater intrusion; Numerical simulation; Brine water and freshwater interaction; Density dependent interface;

    机译:海水入侵数值模拟盐水与淡水的相互作用密度依赖界面;

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