海河流域子牙河平原区地下水化学特征分析及水质评价

Hydrochemical Characteristics and Water-Quality Evaluation of Groundwater in the Ziya River Plain, Hai River Basin

  • 摘要: 海河流域子牙河平原区是河北省粮食主产区与经济发展核心区,长期依赖地下水开采导致水质咸化、硬度超标等问题突出,厘清子牙河流域平原区地下水化学特征以及水质状况,对于该区域水资源合理开发利用具有重要意义。本文聚焦该区地下水化学特征与质量评价,通过采集深层含水层组 104组水样和浅层含水层组287组水样,测试了主要阳离子(K+、Na+、Ca2+、Mg2+)和主要阴离子(Cl、\mathrmHCO_3^- 、\mathrmSO_4^2- 、\mathrmNO_3^- )以及总硬度、氨氮、铁、锰等多项指标。利用数理统计分析、Piper三线图和GIS空间插值等方法研究了水化学基本特征,引入地质累积指数修正因子载荷APCS-MLR模型,对浅层含水层组污染物的主要来源进行了解析。结果表明:研究区水化学类型呈现显著空间分异,浅层地下水由山前HCO3-Ca·Mg型过渡至滨海SO4·Cl-Na型,深层地下水以SO4·Cl-Na型、 \mathrmHCO_3^ ·Cl-Na型为主导;浅层地下水质量总体较差,Ⅴ类水占比71.25%,主要受溶解性总固体(TDS)、总硬度及\mathrmSO_4^2- 控制;深层地下水质量相对较好,F和Mn为关键限制因子;APCS-MLR模型解析显示,海水入侵、矿物溶滤及农业-工业复合污染构成主要影响因素。

     

    Abstract: The Ziya River Plain, located in the Haihe River Basin, is both a major grain-producing region and a key economic development zone in Hebei Province. Prolonged dependence on groundwater extraction has led to some issues, including water salinization and excessive hardness. Clarifying the hydrochemical characteristics and water quality status of groundwater in this region is therefore essential for the sustainable and rational utilization of local water resources. Here, a total of 104 groundwater samples were collected from deep aquifers and 287 samples from shallow aquifers. These samples were analyzed for major cations (K+, Na+, Ca2+, Mg2+), and major anions (Cl, \mathrmHCO_3^- , \mathrmSO_4^2- , \mathrmNO_3^- ), as well as additional parameters such as total hardness, ammonium nitrogen, iron, and manganese. Statistical analysis, Piper trilinear diagrams, and GIS-based spatial interpolation were employed to investigate the fundamental hydrochemical features. Additionally, an absolute principal component score–multiple linear regression (APCS-MLR) model, incorporating a modified geochemical accumulation index, was applied to identify the major pollution sources affecting the shallow aquifers. The results reveal significant spatial variation in groundwater hydrochemical types across the study area. Shallow groundwater transitions from an HCO3-Ca·Mg type in the piedmont areas to a SO4·Cl-Na type near coastal regions. Deep groundwater is mainly characterized by SO4·Cl-Na and HCO3·Cl-Na types. The overall quality of shallow groundwater is relatively poor, with Class Ⅴ water accounting for 71.25% of the samples, primarily due to elevated total dissolved solids (TDS), total hardness, and \mathrmSO_4^2- concentrations. In contrast, the quality of deep groundwater is comparatively better, although fluoride (F) and manganese (Mn) are identified as key limiting factors. The APCS-MLR model analysis indicates that the primary influencing factors include seawater intrusion, mineral dissolution, and a combination of agricultural and industrial pollution sources.

     

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