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鄂尔多斯盆地多级次地下水流系统中硝酸盐分布特征及其成因

张晓旭 周爱国 刘运德 张俊

张晓旭, 周爱国, 刘运德, 张俊. 鄂尔多斯盆地多级次地下水流系统中硝酸盐分布特征及其成因[J]. 地质科技通报, 2022, 41(1): 231-239. doi: 10.19509/j.cnki.dzkq.2022.0022
引用本文: 张晓旭, 周爱国, 刘运德, 张俊. 鄂尔多斯盆地多级次地下水流系统中硝酸盐分布特征及其成因[J]. 地质科技通报, 2022, 41(1): 231-239. doi: 10.19509/j.cnki.dzkq.2022.0022
Zhang Xiaoxu, Zhou Aiguo, Liu Yunde, Zhang Jun. Distribution characteristics and genesis of nitrate in nested groundwater flow system in northern Ordos Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(1): 231-239. doi: 10.19509/j.cnki.dzkq.2022.0022
Citation: Zhang Xiaoxu, Zhou Aiguo, Liu Yunde, Zhang Jun. Distribution characteristics and genesis of nitrate in nested groundwater flow system in northern Ordos Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(1): 231-239. doi: 10.19509/j.cnki.dzkq.2022.0022

鄂尔多斯盆地多级次地下水流系统中硝酸盐分布特征及其成因

doi: 10.19509/j.cnki.dzkq.2022.0022
基金项目: 

国家自然科学基金项目 41772263

中国地质调查局干旱-半干旱区地下水与生态重点实验室基金项目 KLGEAS201602

详细信息
    作者简介:

    张晓旭(1997-), 女, 现正攻读水文地质学专业硕士学位, 主要从事环境地球化学方面的研究工作。E-mail: zhangxiaoxu@cug.edu.cn

    通讯作者:

    刘运德(1984-), 男, 副教授, 博士生导师, 主要从事环境同位素与环境水文地质领域的教学与研究工作。E-mail: lydcn84@126.com

  • 中图分类号: P641;X141

Distribution characteristics and genesis of nitrate in nested groundwater flow system in northern Ordos Basin

  • 摘要: 水资源短缺的鄂尔多斯盆地内地下水遭受硝酸盐(NO3-)污染等问题日益突出,识别盆地不同地下水流系统的NO3-分布规律及其成因,对地下水资源的合理利用与保护具有重要意义。选取鄂尔多斯盆地北部湖泊集中区白垩系地下水系统为研究对象,基于水化学和聚类-主成分分析划分地下水流系统级次,在此基础上对比分析不同级次地下水流系统中NO3-分布特征,综合水化学和环境同位素分析识别多级次地下水流系统中NO3-来源及其潜在过程。研究表明:研究区ρ(NO3-)超出地下水质量标准(GB/T 14848-2017)Ⅲ类水标准的地下水样品集中在局部-中间地下水流系统,其超标率达到28%;区域地下水流系统中ρ(NO3-)均值约为1 mg/L。研究区不同级次地下水流系统中ρ(NO3-)分布特征主要与人类活动影响程度有关,而地下水蒸发富集和反硝化衰减作用对ρ(NO3-)的影响可以忽略。其中,局部-中间地下水流系统受到人类活动产生的污染影响显著,其NO3-污染主要来源于无机铵肥和粪便污水等;区域地下水流系统可能尚未受到人类活动污染,其NO3-来源于天然有机氮矿化。

     

  • 图 1  研究区区位图(a)(据文献[32]修改)、采样点空间分布图(b)和A-A′剖面地下水流系统示意图(c)(据文献[33]修改)

    Figure 1.  Location of the study area(a), spatial distribution of sampling sites(b) and the schematic diagram of groundwater flow system at section A-A′(c)

    图 2  聚类分析树状图(a)和主成分得分-载荷图(b)

    Figure 2.  Dendrogram of cluster analysis(a) and diagram of principal components scores-load (b)

    图 3  不同类别地下水样的氢氧同位素组成(δ2HH2Oδ18OH2O)关系图

    Figure 3.  Relationship between δ2HH2O and δ18OH2O in different clusters of groundwater samples

    图 4  不同类别地下水样的d值与ρ(NO3-)之间的关系

    Figure 4.  Relationship between deuterium-excess value and nitrate content in different clusters of groundwater samples

    图 5  不同类别地下水样的稳定氮同位素组成(δ15NNO3)与ln(NO3-N)之间的关系

    Figure 5.  Relationship between δ15NNO3 and nitrate content in different clusters of groundwater samples

    图 6  不同类别地下水样中NO3-δ18O和δ15N关系图(图中各潜在来源NO3-δ15N和δ18O值源于文献[5, 44, 47])

    Figure 6.  Relationship between δ18ONO3 and δ15NNO3 in different clusters of groundwater samples

    表  1  不同类别地下水样的水化学组成

    Table  1.   Hydrochemical components in different clusters of groundwater samples

    地下水样品 ρ(DO)/(mg·L-1) ρ(TDS)/(mg·L-1) ρ(NO3-)/(mg·L-1) δ15NNO3/‰ δ18ONO3/‰ δ18OH2O/‰ δ2HH2O/‰ 主要水化学类型
    C1 最小值~最大值 0.1~2.5 277.0~437.5 0.7~5.3 1.9~6.4 -2.0~11.6 -10.78~-9.10 -87.7~-75.0 HCO3-Na型和HCO3·SO4-Na型
    均值 1.5 349.7 1.2 3.6 2.6 -10.18 -83.5
    C2 最小值~最大值 8.0~10.6 366.4~681.3 64.8~191.8 -0.7~4.6 -2.8~4.1 -8.87~-7.58 -67.8~59.6 HCO3-Ca型和HCO3·NO3-Ca型
    均值 9.6 496.1 123.3 2.3 -0.4 -8.21 -63.7
    C3 最小值~最大值 1.6~9.6 201.8~409.0 0.8~97.8 2.3~6.9 -4.5~6.3 -11.44~-7.38 -88.1~58.9 HCO3-Ca型和HCO3-Na型
    均值 5.7 286.3 32.1 4.4 0.6 -9.06 -70.6
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