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首页> 外文期刊>Journal of Hydrology >Placing prairie pothole wetlands along spatial and temporal continua to improve integration of wetland function in ecological investigations
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Placing prairie pothole wetlands along spatial and temporal continua to improve integration of wetland function in ecological investigations

机译:沿空间和时间连续性放置草原坑洼湿地,以改善湿地功能在生态学研究中的整合

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摘要

We evaluated the efficacy of using chemical characteristics to rank wetland relation to surface and groundwater along a hydrologic continuum ranging from groundwater recharge to groundwater discharge. We used 27 years (1974–2002) of water chemistry data from 15 prairie pothole wetlands and known hydrologic connections of these wetlands to groundwater to evaluate spatial and temporal patterns in chemical characteristics that correspond to the unique ecosystem functions each wetland performed. Due to the mineral content and the low permeability rate of glacial till and soils, salinity of wetland waters increased along a continuum of wetland relation to groundwater recharge, flow-through or discharge. Mean inter-annual specific conductance (a proxy for salinity) increased along this continuum from wetlands that recharge groundwater being fresh to wetlands that receive groundwater discharge being the most saline, and wetlands that both recharge and discharge to groundwater (i.e., groundwater flow-through wetlands) being of intermediate salinity. The primary axis from a principal component analysis revealed that specific conductance (and major ions affecting conductance) explained 71% of the variation in wetland chemistry over the 27 years of this investigation. We found that longterm averages from this axis were useful to identify a wetland's long-term relation to surface and groundwater. Yearly or seasonal measurements of specific conductance can be less definitive because of highly dynamic inter- and intra-annual climate cycles that affect water volumes and the interaction of groundwater and geologic materials, and thereby influence the chemical composition of wetland waters. The influence of wetland relation to surface and groundwater on water chemistry has application in many scientific disciplines and is especially needed to improve ecological understanding in wetland investigations. We suggest ways that monitoring in situ wetland conditions could be linked with evolving remote sensing technology to improve our ability to better inform decisions affecting wetland sustainability and provide periodic inventories of wetland ecosystem services to document temporal trends in wetland function and how they respond to contemporary land-use change.
机译:我们评估了利用化学特征对沿从地下水补给到地下水排出的水文连续体与地表和地下水的关系进行排序的有效性。我们使用了15个草原坑洼地湿地的27年(1974–2002年)水化学数据以及这些湿地与地下水的已知水文联系来评估化学特征的时空格局,这些特征与每个湿地所具有的独特生态系统功能相对应。由于矿物质含量和冰川耕地和土壤的低渗透率,湿地水的盐度沿湿地连续性增加,与地下水的补给,流过或排出有关。在这个连续过程中,年平均比电导率(盐度的代表)从补充新鲜的地下水的湿地到接受地下水排放的盐分最多的湿地,以及补充和排放到地下水的湿地(即,地下水流)而增加。湿地)处于中等盐度。主成分分析的主轴表明,在此调查的27年中,特定的电导率(和影响电导率的主要离子)解释了71%的湿地化学变化。我们发现,从该轴获得的长期平均值有助于确定湿地与地表水和地下水的长期关系。由于高度动态的年际和年际气候周期会影响水量以及地下水与地质物质的相互作用,从而影响湿地水的化学成分,因此每年或季节性的电导率测量结果可能不太准确。湿地对地表水和地下水的关系对水化学的影响已在许多科学领域得到应用,尤其是在湿地研究中提高对生态学的认识。我们建议将监测原地湿地状况与不断发展的遥感技术联系起来的方法,以提高我们更好地为影响湿地可持续性的决策提供依据的能力,并提供定期的湿地生态系统服务清单,以记录湿地功能的时间趋势及其对当代土地的反应-使用更改。

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