基于DRASTIC模型的天津市浅层孔隙地下水脆弱性评价、主控因子分析与分区管控

    Assessment of shallow porous groundwater vulnerability, main controlling factors and zonal management in Tianjin based on DRASTIC model

    • 摘要:
      研究目的 地下水脆弱性评价及主控因子识别是地下水污染精准防控与精细化分区管控的重要前提。为厘清天津市浅层孔隙地下水脆弱性空间分布规律,揭示其关键影响机制,弥补传统DRASTIC模型区域应用的局限性,为当地地下水资源保护和污染治理提供科学依据。
      研究方法 依托研究区地质、水文地质及污染源实地核查数据,采用DRASTIC评价模型,结合ArcGIS空间分析技术开展浅层孔隙地下水脆弱性定量评价,同时运用单参数敏感性分析法识别脆弱性主控因子。
      研究结果 天津市浅层孔隙地下水脆弱性可划分为较低、中等、较高3个等级,其中蓟州、宁河、中心城区等区域为中等脆弱性,蓟州北部于桥水库、宝坻、静海西部及滨海新区东南部为较高脆弱性区域。敏感性分析表明,地下水位埋深为核心主控因子,含水层渗透系数影响最弱。
      结论 天津浅层地下水整体以中、高脆弱性为主,水位埋深是调控区域地下水脆弱性的决定性因素。经典DRASTIC模型存在局部适用性缺陷,经针对性修正后可更好地适配研究区水文地质条件。研究成果可为天津市浅层地下水分区管控、污染防治及水资源可持续利用提供理论支撑。

       

      Abstract:
      Objectives Groundwater vulnerability assessment and main controlling factor identification serve as an essential prerequisite for precise groundwater pollution prevention and refined zonal management. This study aims to clarify the spatial distribution characteristics of shallow porous groundwater vulnerability in Tianjin, reveal its key influencing mechanisms, compensate for the regional application limitations of the traditional DRASTIC model, and provide a scientific basis for local groundwater resource protection and pollution control.
      Methods Based on the geological, hydrogeological, and field pollution source verification data of the study area, the DRASTIC model combined with ArcGIS spatial analysis technology was adopted to quantitatively evaluate the vulnerability of shallow porous groundwater. Single−parameter sensitivity analysis was further applied to identify the main controlling factors of groundwater vulnerability.
      Results The vulnerability of shallow porous groundwater in Tianjin can be classified into three grades: low−moderate, moderate and high. Areas including Jizhou, Ninghe and the central urban area fall into the moderate−vulnerability category, whereas northern Jizhou (Yuqiao Reservoir), Baodi, western Jinghai and the southeastern Binhai New Area represent high−vulnerability zones. Sensitivity analysis indicates that groundwater depth is the primary controlling factor, while the hydraulic conductivity of aquifers exerts the weakest influence.
      Conclusions The shallow groundwater in Tianjin is generally characterized by moderate to high vulnerability, and groundwater table depth is the decisive factor affecting regional groundwater vulnerability. The traditional DRASTIC model has limitations in local regional adaptation, which can be optimized through targeted corrections to fit the regional hydrogeological conditions. The research findings can provide theoretical support for refined zonal management, pollution prevention, and sustainable utilization of shallow groundwater resources in Tianjin.

       

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