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Dating Groundwater Using Dissolved Organic Carbon and Estimating Flow Path Travel Times in Southern Nevada Aquifers.

机译:在内华达州南部含水层中使用溶解的有机碳对地下水进行定年并估算流径旅行时间。

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摘要

The study's objective was to evaluate the use of dissolved organic carbon (DOC) carbon-14 (14C) to estimate groundwater ages in southern Nevada aquifers. Hydrogeologists have traditionally used dissolved inorganic carbon (DIC) 14C to estimate groundwater ages. However, because multiple processes change DIC 14C activities in groundwater, complex corrections are often required, and the ages generated can be frustratingly inexact. The hypothesis was that DOC 14C dating is more accurate because DOC is less reactive with aquifer rocks.;Water samples were analyzed for 14C by accelerator mass spectrometry. Laboratory experiments indicated that there is no significant dilution of groundwater DOC 14C by leaching of 'dead' (no 14C) organic carbon from aquifer rocks. Similar DOC compounds were identified in both up- and down-gradient waters meaning that alterations from kerogen or bacteria likely have minimal effects on DOC 14C activities. Loss of DOC 14C through matrix diffusion is minimal because calculated diffusion coefficients were relatively small for DOC 14C compared to a conservative bromide tracer. Dissolved organic carbon 14C activity, expressed in percent modern carbon (pmc), for 14 recharge area locations ranged from 96.0 to 120.1 pmc, with an average of 105.8 pmc, yielding a recent (post-atmospheric nuclear weapons testing) age. Dissolved organic carbon 14C activity for eight down-gradient locations ranged from 45.8 to 75.2 pmc with an average of 62.3 pmc, or about 3,900 years. Flow-path travel times are thousands of years less for DOC than for both corrected and uncorrected DIC. This discrepancy likely is the result of water-rock reactions and other physical processes such as matrix diffusion that lower DIC 14C activities in groundwater. Results from this study demonstrate that the DOC 14C dating technique can be used to estimate groundwater ages in aquifers with low DOC and provides an alternative to the traditional DIC 14C dating.
机译:这项研究的目的是评估使用溶解性有机碳(DOC)碳14(14C)估算内华达州南部含水层的地下水年龄。传统上,水文地质学家使用溶解的无机碳(DIC)14C来估算地下水年龄。但是,由于多个过程改变了DIC 14C在地下水中的活动,因此经常需要进行复杂的校正,并且生成的年龄可能令人沮丧地不准确。假设是DOC 14C测年更准确,因为DOC与含水层岩石的反应性较小。;通过加速器质谱分析了水样中的14C。实验室实验表明,通过从含水层岩石中浸出“死”(无14C)有机碳,没有明显稀释地下水DOC 14C。在上坡度和下坡度水域均鉴定出相似的DOC化合物,这意味着由干酪根或细菌引起的变化可能对DOC 14C活性的影响最小。由于与保守的溴化物示踪剂相比,DOC 14C的计算扩散系数相对较小,因此通过基质扩散造成的DOC 14C损失极小。 14个补给区位置的溶解有机碳14C活性以现代碳百分比(pmc)表示,范围为96.0至120.1 pmc,平均为105.8 pmc,产生了最近的(大气后核武器试验)年龄。八个向下梯度位置的溶解有机碳14C活性范围为45.8至75.2 pmc,平均62.3 pmc,约3,900年。与修正和未修正的DIC相比,DOC的流径旅行时间要短数千年。这种差异可能是水岩石反应和其他物理过程(例如基质扩散)导致地下水中DIC 14C活性降低的结果。这项研究的结果表明,DOC 14C测年技术可用于估算DOC较低的含水层中的地下水年龄,并为传统DIC 14C测年提供了一种替代方法。

著录项

  • 作者

    Fereday, Wyatt.;

  • 作者单位

    University of Nevada, Reno.;

  • 授予单位 University of Nevada, Reno.;
  • 学科 Hydrologic sciences.
  • 学位 M.S.
  • 年度 2013
  • 页码 89 p.
  • 总页数 89
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:41:28

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