School of Environmental Studies, China University of Geosciences, Wuhan, 430074, China.
Environ Sci Pollut Res Int. 2018 Nov;25(32):32524-32539. doi: 10.1007/s11356-018-3196-3. Epub 2018 Sep 20.
This study employed a modified DRASTIC model (AHP-DRASTIC model) and GALDIT model to evaluate the inherent vulnerability of shallow groundwater in Weibei Plain in Shandong Province of China and its vulnerability to seawater intrusion. The AHP-DRASTIC model uses the analytic hierarchy process (AHP) to determine the weight of each parameter and reduces the subjectivity of evaluation. The vulnerability map generated by the AHP-DRASTIC model shows four types of vulnerability: high (25.0%), higher (28.0%), moderate (29.7%), and low (17.3%), and the high-vulnerability areas are mainly distributed in the area north of Qingxiang Town and south of Changyi County. The distribution of high-vulnerability areas mainly related to the depth of groundwater table is 4-8 m, and the recharge of rainfall is 100-175 mm/year. The vulnerability map generated by the GALDIT model shows four types of vulnerability: high (33.5%), higher (23.4%), moderate (22.1%), and low (21.0%), and the high-vulnerability areas are mainly distributed in the coastal areas of Hanting District-Zhuli Town, the areas north of Linqu County, and the areas south of Shouguang County. The distribution of high-vulnerability areas mainly related to the distance between these areas and the coast is < 2.5 km, with aquifer thickness > 15 m. Total dissolved solid, NO, Cl, and SO are used to verify the accuracy of the DRASTIC model, the AHP-DRASTIC model, and the GALDIT model. The results show that the AHP-DRASTIC model is more suitable for the assessment of inherent vulnerability of shallow groundwater in the study area than the DRASTIC model, and human activities have a major impact on the verification of vulnerability and should be considered when conducting groundwater vulnerability verification. The results of this study can provide grounds for groundwater management and protection and land use planning in the study area and provide new ideas for groundwater vulnerability assessment in coastal areas.
本研究采用改进的 DRASTIC 模型(AHP-DRASTIC 模型)和 GALDIT 模型,评估了中国山东省潍北平原浅层地下水的固有脆弱性及其对海水入侵的脆弱性。AHP-DRASTIC 模型利用层次分析法(AHP)确定各参数的权重,降低评价的主观性。AHP-DRASTIC 模型生成的脆弱性图显示了四种脆弱性类型:高(25.0%)、较高(28.0%)、中等(29.7%)和低(17.3%),高脆弱性区主要分布在青香镇以北和昌邑县以南地区。高脆弱性区的分布主要与地下水位深度在 4-8 m 之间以及年降雨量在 100-175 mm 之间有关。GALDIT 模型生成的脆弱性图显示了四种脆弱性类型:高(33.5%)、较高(23.4%)、中等(22.1%)和低(21.0%),高脆弱性区主要分布在寒亭区-朱里镇沿海地区、临朐县北部地区和寿光县南部地区。高脆弱性区的分布主要与这些地区与海岸的距离<2.5 km 有关,含水层厚度>15 m。总溶解固体、NO、Cl 和 SO 用于验证 DRASTIC 模型、AHP-DRASTIC 模型和 GALDIT 模型的准确性。结果表明,与 DRASTIC 模型相比,AHP-DRASTIC 模型更适合评估研究区浅层地下水的固有脆弱性,人类活动对脆弱性的验证有重大影响,在进行地下水脆弱性验证时应予以考虑。本研究结果可为研究区地下水管理和保护以及土地利用规划提供依据,并为沿海地区地下水脆弱性评估提供新思路。