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首页> 外文期刊>Marine Chemistry >Uranium and strontium isotopic evidence for strong submarine groundwater discharge in an estuary of a mountainous island: A case study in the Gaoping River Estuary, Southwestern Taiwan
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Uranium and strontium isotopic evidence for strong submarine groundwater discharge in an estuary of a mountainous island: A case study in the Gaoping River Estuary, Southwestern Taiwan

机译:山区岛屿河口海底地下水强排泄的铀和锶同位素证据:以台湾西南部高坪河口为例

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摘要

To further define the hydro-geochemical circulation in estuary from a mountainous island, over 50 river water samples were collected in three sampling schemes from the Gaoping River Estuary (GRE), the largest river catchment in southwestern Taiwan and were analyzed for major/trace elements, uranium (U) and strontium (Sr) isotopic compositions using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS). Dissolved U and Sr concentrations (0.46-13.8 nM and 2.27-86.2 μM), as well as U activity ratio (denoted as (~(234)U/~(238)U)) and ~(87)Sr/~(86)Sr (1.145-2.427 and 0.709155-0.712918), vary significantly and show strong seasonal variability. Three characteristic source waters were identified in the study region, seawater (SW). river water (RW), and groundwater (GW or evolved RW). SW has the highest U and Sr concentrations among the three end-members with low and constant (~(234)U/~(238)U) and ~(87)Sr/~(86)Sr. In contrast, RW shows the lowest U and an intermediate Sr concentration, but with medium (~(234)U/~(238)U) and the most radiogenic ~(87)Sr/~(86)Sr. GW has the medium U and lowest Sr content with rather radiogenic (~(234)U/~(238)U) and ~(87)Sr/~(86)Sr, possibly evolved from RW. The GW is most clearly identified in the vertical profile of the near estuary stations. These high (~(234)U/~(238)U) values in RW and GW reflect the outcome of intense weathering in the upper catchment, efficient leaching of α-recoil products in soils. Dissolved Sr and ~(87)Sr/~(86)Sr data confirm similar U mixing scenarios, but the index is more sensitive to water source variations. Estimated fluxes ofsubmarine groundwater discharge (SGD) in the GRE reach a maximum value of 456-2107 × 10~(11) Lyr~(-1) implying important contribution to the chemical budget in coastal regions. This study reveals that U and Sr isotopes are useful tracers for monitoring SGD in estuaries.
机译:为了进一步定义山岛上河口的水文地球化学循环,在台湾西南部最大集水区高坪河口(GRE)的三种采样方案中,收集了50多个河水样本,并对其中的主要/痕量元素进行了分析。多收集器电感耦合等离子体质谱法(MC-ICP-MS)分析铀,铀(U)和锶(Sr)同位素组成。溶解的U和Sr浓度(0.46-13.8 nM和2.27-86.2μM)以及U活性比(表示为(〜(234)U /〜(238)U))和〜(87)Sr /〜(86锶(1.145-2.427和0.709155-0.712918),变化很大,并表现出强烈的季节性变化。在研究区域中确定了三个特征性源水,即海水(SW)。河流水(RW)和地下水(GW或演变后的RW)。在具有低且恒定(〜(234)U /〜(238)U)和〜(87)Sr /〜(86)Sr的三个末端成员中,SW的U和Sr浓度最高。相反,RW显示最低的U和中等的Sr浓度,但具有中等(〜(234)U /〜(238)U)和最易放射的〜(87)Sr /〜(86)Sr。 GW具有中等的U和最低的Sr含量,具有相当的放射源(〜(234)U /〜(238)U)和〜(87)Sr /〜(86)Sr,可能是从RW演化而来的。在近河口站的垂直剖面中最清楚地确定了GW。 RW和GW中的这些高(〜(234)U /〜(238)U)值反映了上游流域强烈的风化,土壤中α-反冲产品的有效浸出的结果。溶解的Sr和〜(87)Sr /〜(86)Sr数据证实了相似的U混合情况,但该指数对水源变化更为敏感。 GRE中的海底地下水排放量(SGD)估计最大值达到456-2107×10〜(11)Lyr〜(-1),这暗示着对沿海地区化学预算的重要贡献。这项研究表明,铀和锶同位素是监测河口SGD的有用示踪剂。

著录项

  • 来源
    《Marine Chemistry》 |2013年第20期|106-116|共11页
  • 作者

    Ruo-Mei Wang; Chen-Feng You;

  • 作者单位

    Dept. of Earth Sciences, National Cheng Kung Univ.. No.l, University Road, Tainan 701, Taiwan, ROC Earth Dynamic System Research Center (EDSRC), National Cheng Kung Univ., No. I, University Road, Tainan 701, Taiwan, ROC;

    Dept. of Earth Sciences, National Cheng Kung Univ.. No.l, University Road, Tainan 701, Taiwan, ROC Earth Dynamic System Research Center (EDSRC), National Cheng Kung Univ., No. I, University Road, Tainan 701, Taiwan, ROC;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Estuary; Uranium isotopes; Strontium isotopes; MC-ICP-MS; SGD;

    机译:河口;铀同位素;锶同位素;MC-ICP-MS;新元;

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