首页> 外文学位 >The effects of past climate change and recent agricultural irrigation recharge on the sources, ages, and quality of groundwater in the Columbia River Basalt Aquifers, Columbia Basin, Central Washington.
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The effects of past climate change and recent agricultural irrigation recharge on the sources, ages, and quality of groundwater in the Columbia River Basalt Aquifers, Columbia Basin, Central Washington.

机译:华盛顿中部哥伦比亚盆地哥伦比亚河玄武岩含水层中,过去的气候变化和最近的农业灌溉补给对地下水的来源,年龄和质量的影响。

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摘要

This study uses multiple isotopic (2H, 18O, 13C, 15NNO3, 18ONO3 , 87Sr/86Sr) and age tracers ( 3H, 14C, CFCs), in conjunction with elemental chemistry, to address the following research question: How have present day anthropogenic activities (i.e. surface water irrigation and fertilizer application) and past climatic events (i.e. cataclysmic flooding from glacial Lake Missoula and other modes of discharge from Cordilleran Ice Sheet) impacted the hydrology and geochemistry of the Columbia River Basalt Aquifers (CRBAs) in central Washington? Large-scale irrigated agriculture over the past ∼60 years has resulted in the transport of high NO3-- irrigation waters moving downward in the oxic CRBAs at rates of several meters per decade with a lack of denitrification. Deeper pristine regional groundwater in the CRBAs is Late Pleistocene in age and likely remnant Cordilleran Ice Sheet-related recharge waters (i.e. glacial Lake Missoula floodwaters).
机译:这项研究使用多种同位素(2H,18O,13C,15NNO3、18ONO3、87Sr / 86Sr)和年龄示踪剂(3H,14C,CFCs)以及元素化学,来解决以下研究问题:当今人类活动如何(即地表水灌溉和施肥)以及过去的气候事件(例如,米苏拉湖冰川的大洪水和科迪勒拉冰原的其他排放方式)影响了华盛顿市中心的哥伦比亚河玄武岩含水层(CRBA)的水文和地球化学?在过去约60年中,大规模的灌溉农业导致高NO3-灌溉水在含氧CRBA中以每十年几十米的速率向下移动,而缺乏反硝化作用。 CRBA中较深的原始区域地下水年龄是晚更新世,可能是与科迪勒拉冰原相关的补给水(即冰川米苏拉湖洪水)残留的地方。

著录项

  • 作者

    Brown, Kyle.;

  • 作者单位

    The University of Arizona.;

  • 授予单位 The University of Arizona.;
  • 学科 Hydrology.;Geochemistry.;Environmental Geology.
  • 学位 M.S.
  • 年度 2009
  • 页码 154 p.
  • 总页数 154
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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