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Organic matter processing and opportunities for stream mitigation in an intensively mined West Virginia watershed.

机译:在西维吉尼亚州一个集约开采的分水岭中,有机物处理和减少水流的机会。

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摘要

Mountaintop removal/valley fill mining is a controversial process that may have far-reaching impacts on central Appalachian watersheds. Our project sought to quantify spatial and temporal variation in organic matter processing within Pigeon Creek, an intensively mined sub-watershed of the Tug Fork River in southern West Virginia. Our objectives were to: (1) quantify variation in organic matter retention and decomposition among streams differing in size (drainage area), gradient, and structural complexity; and (2) quantify the effect of valley fills on stream flow, water chemistry, organic matter processing, and benthic invertebrate colonization of detritus packs in 1 st order perennial streams. Our study area consisted of 26 sites distributed across a wide range of stream sizes (ephemeral channels to large perennial streams). Four of the small perennial sites were located below large valley fills and were paired to four undisturbed sites. At each site we quantified water temperature (continuous), stream flow (continuous), habitat quality and complexity, water chemistry (seasonal), artificial leaf and stick transport (seasonal), leaf pack decomposition (seasonal), and invertebrate colonization (seasonal). Organic matter decomposition rates were variable, but unrelated to any environmental factors that we measured. Drainage area, channel complexity, and mining had a significant interactive effect on transport distance of leaves and sticks. Sites below valley fills had enhanced flow levels, but this did not result in higher transport levels. Also, sites below valley fills had significantly higher conductivity, but this did not produce a significant effect on organic matter decomposition or on benthic invertebrate colonization of leaf packs. These results add to our understanding of complex interactive effects of mining on stream ecosystem functions and our ability to compensate for lost headwater functions through restoration actions downstream.
机译:山顶清除/河谷填充开采是一个有争议的过程,可能对阿巴拉契亚中部流域产生深远影响。我们的项目旨在量化Pigeon Creek内部有机物加工的时空变化,Pigeon Creek是西维吉尼亚州南部Tug Fork河的一个密集开采的分水岭。我们的目标是:(1)量化不同尺寸(流域),坡度和结构复杂性不同的溪流中有机物保留和分解的变化; (2)量化谷粒填充对一阶多年生河流中碎屑堆积的水流,水化学,有机物加工和底栖无脊椎动物定殖的影响。我们的研究区域由26个站点组成,这些站点分布在各种溪流中(临时通道到大型多年生溪流)。多年生小型地点中的四个位于大山谷填充物下方,并与四个不受干扰的地点配对。在每个站点上,我们量化了水温(连续),水流(连续),栖息地质量和复杂性,水化学(季节性),人工叶和棒运输(季节性),叶丛分解(季节性)和无脊椎动物定居(季节性) 。有机物分解速率是可变的,但与我们测量的任何环境因素无关。流域,渠道的复杂性和采矿对树叶和树枝的运输距离具有显着的交互作用。山谷填充物以下的地点的水位有所提高,但这并未导致较高的运输量。同样,谷底填充物以下的位点具有明显更高的电导率,但这对有机物的分解或叶丛的底栖无脊椎动物定殖没有明显影响。这些结果加深了我们对采矿对河流生态系统功能的复杂互动影响的理解,以及我们通过下游的恢复行动补偿失去的源水功能的能力。

著录项

  • 作者

    Minter, Megan Stephanie.;

  • 作者单位

    West Virginia University.;

  • 授予单位 West Virginia University.;
  • 学科 Engineering Mining.;Biology Limnology.;Agriculture Fisheries and Aquaculture.;Engineering Environmental.
  • 学位 M.S.
  • 年度 2009
  • 页码 126 p.
  • 总页数 126
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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