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广西防城港地区浅层地下水pH值时空分布、成因及对生态环境的影响

张宏鑫, 余绍文, 张彦鹏, 陈雯, 黎清华, 刘怀庆, 张庆玉. 2022. 广西防城港地区浅层地下水pH值时空分布、成因及对生态环境的影响[J]. 中国地质, 49(3): 822-833. doi: 10.12029/gc20220310
引用本文: 张宏鑫, 余绍文, 张彦鹏, 陈雯, 黎清华, 刘怀庆, 张庆玉. 2022. 广西防城港地区浅层地下水pH值时空分布、成因及对生态环境的影响[J]. 中国地质, 49(3): 822-833. doi: 10.12029/gc20220310
ZHANG Hongxin, YU Shaowen, ZHANG Yanpeng, CHEN Wen, LI Qinghua, LIU Huaiqing, ZHANG Qingyu. 2022. Spatial-temporal distribution, genesis and environmental impact of the shallow groundwater pH values in the Fangchenggang, Guangxi[J]. Geology in China, 49(3): 822-833. doi: 10.12029/gc20220310
Citation: ZHANG Hongxin, YU Shaowen, ZHANG Yanpeng, CHEN Wen, LI Qinghua, LIU Huaiqing, ZHANG Qingyu. 2022. Spatial-temporal distribution, genesis and environmental impact of the shallow groundwater pH values in the Fangchenggang, Guangxi[J]. Geology in China, 49(3): 822-833. doi: 10.12029/gc20220310

广西防城港地区浅层地下水pH值时空分布、成因及对生态环境的影响

  • 基金项目:
    中国地质调查局项目(DD20189502, DD20160258, 12120113004100)资助
详细信息
    作者简介: 张宏鑫,男,1982年生,高级工程师,从事区域水工环地质调查评价研究;E-mail:whzhongxin@qq.com
    通讯作者: 张彦鹏, 男, 1985年生, 博士, 从事水工环地质调查评价研究; E-mail: 523907140@qq.com
  • 中图分类号: P641;X143

Spatial-temporal distribution, genesis and environmental impact of the shallow groundwater pH values in the Fangchenggang, Guangxi

  • Fund Project: Supported by the project of China Geological Survey (No.DD20189502, No.DD20160258, No.12120113004100)
More Information
    Author Bio: ZHANG Hongxin, male, born in 1982, engineer, mainly engaged in the investigation and research of regional hydrogeology, engineering geology and environmental geology; E-mail: Whzhongxin@qq.com .
    Corresponding author: ZHANG Yanpeng, male, born in 1985, doctor, mainly engaged in the investigation and research of regional hydrogeology, engineering geology and environmental geology; E-mail: 523907140@qq.com
  • 研究目的

    查明防城港地区浅层偏酸性地下水时空分布、成因及环境影响。

    研究方法

    于2013—2015年间进行了浅层地下水pH值现场测试,枯水期214组,丰水期168组;讨论了其时空分布特征、成因和生态影响。

    研究结果

    结果表明,丰水期和枯水期偏酸性(pH < 6.5)地下水样分别占79.3%和64.3%,pH值总体上丰水期低于枯水期。地下水pH值在低山区(均在5≤pH<5.5范围,平均值5.18,n=4)<丘陵区(大多数5≤pH<6.5,平均值5.18,n=202)<平原区(大多数6.5≤pH<8.5,平均值6.77,n=8)。

    结论

    偏酸性地下水成因主要与偏酸性大气降水有关,其次与酸性的包气带介质及硫化物矿物的氧化有关。偏酸性大气降水入渗补给是丰水期pH值低于枯水期的主要原因。相比较而言,潮汐作用使得江平地区地下水pH值升高。偏酸性地下水影响饮水安全(研究区枯水期仅20.6%的样品pH值符合生活饮用水标准),促进某些有害组分的释放,腐蚀地下管网和建筑桩基等设施。偏酸性地下水向地表水排泄亦可对地表水环境和地表生态系统产生影响。本研究有助于研究区水资源管理。

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  • 图 1  防城港地区地貌分区及浅层地下水采样点分布图

    Figure 1. 

    图 2  浅层地下水pH值的统计特征

    Figure 2. 

    图 3  防城港地区浅层地下水枯水期pH值分布特征图

    Figure 3. 

    图 4  浅层地下水pH值与主要水化学参数及ANC(酸中和能力)的关系

    Figure 4. 

    图 5  浅层地下水Na+与Cl-的关系

    Figure 5. 

    图 6  研究区地表出露地层中的褐铁矿化

    Figure 6. 

    表 1  按地貌分区浅层地下水枯水期pH值统计

    Table 1.  Statistics of pH of groundwater in different landscape

    下载: 导出CSV

    表 2  丰、枯水期地下水pH值对比统计

    Table 2.  Comparison of groundwater pH values in wet season and dry season

    下载: 导出CSV

    表 3  枯水期主要地下水水化学类型pH值统计

    Table 3.  pH statistics of major groundwater chemical types

    下载: 导出CSV

    表 4  研究区地下水主要离子及pH值相关性

    Table 4.  Correlation coefficients of ionic concentration and pH of groundwaterin study area

    下载: 导出CSV

    表 5  防城港地区降雨pH值统计

    Table 5.  pH of precipitation in the Fangchenggang area

    下载: 导出CSV

    表 6  包气带介质酸碱性统计

    Table 6.  Statistics of pH value of unsaturated zone

    下载: 导出CSV
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出版历程
收稿日期:  2020-01-02
修回日期:  2020-07-15
刊出日期:  2022-06-25

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