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利用地球物理、地球化学和地质统计学技术对一个小热带岛屿的海水入侵进行综合评估。

An integrated assessment of seawater intrusion in a small tropical island using geophysical, geochemical, and geostatistical techniques.

机构信息

Faculty of Environmental Studies, Universiti Putra Malaysia, 43400, Serdang, Selangor, Malaysia,

出版信息

Environ Sci Pollut Res Int. 2014;21(11):7047-64. doi: 10.1007/s11356-014-2598-0. Epub 2014 Feb 18.

Abstract

In this study, geophysics, geochemistry, and geostatistical techniques were integrated to assess seawater intrusion in Kapas Island due to its geological complexity and multiple contamination sources. Five resistivity profiles were measured using an electric resistivity technique. The results reveal very low resistivity <1 Ωm, suggesting either marine clay deposit or seawater intrusion or both along the majority of the resistivity images. As a result, geochemistry was further employed to verify the resistivity evidence. The Chadha and Stiff diagrams classify the island groundwater into Ca-HCO3, Ca-Na-HCO3, Na-HCO3, and Na-Cl water types, with Ca-HCO3 as the dominant. The Mg(2+)/Mg(2+)+Ca(2+), HCO3 (-)/anion, Cl(-)/HCO3 (-), Na(+)/Cl(-), and SO4 (2-)/Cl(-) ratios show that some sampling sites are affected by seawater intrusion; these sampling sites fall within the same areas that show low-resistivity values. The resulting ratios and resistivity values were then used in the geographical information system (GIS) environment to create the geostatistical map of individual indicators. These maps were then overlaid to create the final map showing seawater-affected areas. The final map successfully delineates the area that is actually undergoing seawater intrusion. The proposed technique is not area specific, and hence, it can work in any place with similar completed characteristics or under the influence of multiple contaminants so as to distinguish the area that is truly affected by any targeted pollutants from the rest. This information would provide managers and policy makers with the knowledge of the current situation and will serve as a guide and standard in water research for sustainable management plan.

摘要

在这项研究中,地球物理学、地球化学和地质统计学技术被整合起来,以评估卡帕斯岛由于其地质复杂性和多个污染源而导致的海水入侵。使用电阻率技术测量了五条电阻率剖面。结果显示,电阻率非常低<1 Ωm,这表明在大多数电阻率图像中沿海水粘土沉积或海水入侵或两者都有。因此,进一步采用地球化学来验证电阻率证据。Chadha 和 Stiff 图将该岛地下水分为 Ca-HCO3、Ca-Na-HCO3、Na-HCO3 和 Na-Cl 水类型,其中 Ca-HCO3 占主导地位。Mg(2+)/Mg(2+)+Ca(2+)、HCO3 (-)/阴离子、Cl(-)/HCO3 (-)、Na(+)/Cl(-)和 SO4 (2-)/Cl(-)比值表明,一些采样点受到海水入侵的影响;这些采样点位于显示低电阻率值的相同区域内。然后将得到的比值和电阻率值用于地理信息系统(GIS)环境中,创建各个指标的地质统计地图。然后将这些地图叠加,创建显示受海水影响区域的最终地图。最终地图成功划定了实际正在发生海水入侵的区域。所提出的技术不是针对特定区域的,因此它可以在具有类似完成特征或受到多种污染物影响的任何地方使用,以便将真正受到任何目标污染物影响的区域与其他区域区分开来。这些信息将为管理者和决策者提供有关当前情况的知识,并将作为可持续管理计划中水资源研究的指导和标准。

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