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Groundwater vulnerability to potential contamination in the Annapolis Valley, Nova Scotia.

机译:新斯科舍省安纳波利斯山谷的地下水容易受到潜在污染。

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摘要

The Geological Survey of Canada, in conjunction with various partners, has been undertaking a groundwater characterization project in the Annapolis Valley, Nova Scotia for the past three years. This thesis contributes towards this project through the modelling of groundwater vulnerability in the Annapolis Valley region. The groundwater vulnerability modelling utilized the concept that the degree of potential vulnerability to contamination can be mapped as a function of selected hydrologic conditions. A regional view of the vulnerability to potential contamination of groundwater resources within the Annapolis Valley was modelled using the DRASTIC methodology. This index-overlay method included the seven hydrogeologic parameters of Depth to water, net Recharge, Aquifer media, Soil media, Topography, Impact of the vadose zone, and hydraulic Conductivity, and was programmed using object modelling available in ArcGIS.; Several groundwater vulnerability scenarios were determined to take into account issues with data quality, data quantity, and potential hydrogeologic conditions variability. The resulting groundwater vulnerability for both bedrock and surficial aquifers was examined for each scenario and compared. This exercise indicated that the vulnerability model produced by the DRASTIC method can be significantly altered by seemingly minor variations in data precision and accuracy for discreet parameters. Some of those parameters that have the highest impact in the results (net recharge, depth to water, and impact of the vadose zone) commonly exhibit low dataset precision and accuracy, which is an important consideration in the establishment of groundwater protection and monitoring programs. Vulnerability results vary according to, and within, each geological unit, although generally surficial units are significantly more vulnerable than bedrock units. The bedrock (Wolfville and Blomidon formations) and surficial (sand and gravel) units believed most promising in terms of aquifer quantity and quality were found to be the units potentially most vulnerable to contamination.
机译:在过去三年中,加拿大地质调查局与各种合作伙伴一道,在新斯科舍省安纳波利斯谷地进行了地下水表征项目。本文通过对安纳波利斯山谷地区的地下水脆弱性进行建模,为该项目做出了贡献。地下水脆弱性建模利用了以下概念:潜在的污染脆弱性程度可以根据选定的水文条件进行映射。使用DRASTIC方法对安纳波利斯河谷内地下水资源可能受到污染的脆弱性的区域观点进行了建模。该索引叠加方法包括水深,净补给,含水层介质,土壤介质,地形,渗流带影响和水力传导率这七个水文地质参数,并使用ArcGIS中可用的对象建模进行了编程。确定了几种地下水脆弱性情景,以考虑到数据质量,数据量以及潜在的水文地质条件变异性等问题。针对每种情况检查并比较了基岩和表层含水层导致的地下水脆弱性。此练习表明,通过DRASTIC方法产生的漏洞模型,可以通过谨慎地对数据精度和准确性进行细微的更改来显着改变这种模型。其中一些对结果有最大影响的参数(净补给量,水深和渗流带的影响)通常显示出较低的数据集精度和准确性,这是建立地下水保护和监测程序时的重要考虑因素。脆弱性结果根据每个地质单元及其内部的不同而有所不同,尽管一般而言,表层单元比基岩单元要脆弱得多。人们认为,从含水层的数量和质量上最有前途的基岩(沃尔夫维尔和布洛米登地层)和表层(砂砾和砾石)单元是最容易受到污染的单元。

著录项

  • 作者

    Blackmore, Amanda L.;

  • 作者单位

    Acadia University (Canada).;

  • 授予单位 Acadia University (Canada).;
  • 学科 Geology.
  • 学位 M.Sc.
  • 年度 2006
  • 页码 249 p.
  • 总页数 249
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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