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首页> 外文期刊>Journal of Contaminant Hydrology >Hydrochemical and multivariate statistical interpretations of spatial controls of nitrate concentrations in a shallow alluvial aquifer around oxbow lakes (Osong area, central Korea)
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Hydrochemical and multivariate statistical interpretations of spatial controls of nitrate concentrations in a shallow alluvial aquifer around oxbow lakes (Osong area, central Korea)

机译:水化学和多变量统计解释,解释了牛b湖附近(朝鲜中部大城地区)浅冲积层中硝酸盐浓度的空间控制

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摘要

Hydrochemical and multivariate statistical interpretations of 16 physicochemical parameters of 45 groundwater samples from a riverside alluvial aquifer underneath an agricultural area in Osong, central Korea, were performed in this study to understand the spatial controls of nitrate concentrations in terms of biogeochemical processes occurring near oxbow lakes within a fluvial plain. Nitrate concentrations in groundwater showed a large variability from 0.1 to 190.6 mg/L (mean = 35.0 mg/L) with significantly lower values near oxbow lakes. The evaluation of hydrochemical data indicated that the groundwater chemistry (especially, degree of nitrate contamination) is mainly controlled by two competing processes: 1) agricultural contamination and 2) redox processes. In addition, results of factorial kriging, consisting of two steps (i.e., co-regionalization and factor analysis), reliably showed a spatial control of the concentrations of nitrate and other redox-sensitive species; in particular, significant denitrification was observed restrictedly near oxbow lakes. The results of this study indicate that sub-oxic conditions in an alluvial groundwater system are developed geologically and geochemically in and near oxbow lakes, which can effectively enhance the natural attenuation of nitrate before the groundwater discharges to nearby streams. This study also demonstrates the usefulness of multivariate statistical analysis in groundwater study as a supplementary tool for interpretation of complex hydrochemical data sets.
机译:在这项研究中,对韩国中部Osong某农业地区下方的河边冲积层中的45个地下水样品的16个物理化学参数进行了水化学和多变量统计解释,以了解在牛弓湖附近发生的生物地球化学过程中硝酸盐浓度的空间控制。在河流平原内。地下水中的硝酸盐浓度在0.1至190.6 mg / L之间变化很大(平均值= 35.0 mg / L),在牛b湖附近的浓度明显较低。对水化学数据的评估表明,地下水化学(尤其是硝酸盐污染程度)主要受两个相互竞争的过程控制:1)农业污染和2)氧化还原过程。此外,阶乘克里金法的结果包括两个步骤(即共同区域化和因子分析),可可靠地显示出对硝酸盐和其他氧化还原敏感物种的浓度的空间控制;特别是,在牛弓湖附近仅观察到明显的反硝化作用。这项研究的结果表明,冲积地下水系统中的低氧条件是在牛sub湖及其附近的地质和地球化学条件下发展的,这可以有效地增强硝酸盐在地下水排入附近河流之前的自然衰减。这项研究还证明了在地下水研究中进行多元统计分析作为解释复杂水化学数据集的补充工具的有用性。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2009年第4期|114-127|共14页
  • 作者单位

    Department of Earth and Environmental Sciences and the Environmental Geosphere Research Lab (EGRL), Korea University. Seoul 136-701, Republic of Korea;

    Department of Earth and Environmental Sciences and the Environmental Geosphere Research Lab (EGRL), Korea University. Seoul 136-701, Republic of Korea;

    Department of Earth and Environmental Sciences and the Environmental Geosphere Research Lab (EGRL), Korea University. Seoul 136-701, Republic of Korea CO_2, Sequestration Research Group, Korea Institute of Geoscience and Mineral Resources, Daejeon, Republic of Korea;

    Department of Statistics, Dongguk University, Seoul, Republic of Korea;

    Department of Environmental Engineering, Kunsan National University, Kunsan, Republic of Korea;

    Department of Alternative Energy Development, Jungwon University, Choongbuk, Republic of Korea;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    spatial variation of nitrate; shallow alluvial aquifer; hydrochemistry; factorial kriging; redox control of agricultural contaminants; oxbow lake;

    机译:硝酸盐的空间变化;浅层冲积层;水化学阶乘克里格氧化还原控制农业污染物;牛弓湖;

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