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Impacts Of Peatland Drainage On The Properties Of Typical Water Flow Paths Determined From A Digital Elevation Model

机译:泥炭地排水对数字高程模型确定的典型水流路径特性的影响

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Peatland drainage enhances tree growth, changes catchment hydrology and increases export of nutrients and suspended solids to water bodies. In this study, impacts of peatland drainage on the properties of water flow paths in terrestrial parts of catchments were assessed in terms of slope, elevation, length and soil type. Three study catchments (area 31.8-153.5km~2) were delineated using a 25 m × 25 m digital elevation model (DEM). Typical water flow paths were calculated for each catchment to characterize the mean elevation above the receiving water body as a function of distance along water flow paths. The resulting two-dimensional (2D) profile also allowed calculations of horizontally distributed properties of catchments as a function of distance to the water body. Peatland drainage decreased the length and elevation of the typical water flow path, and increased the area near water bodies. Increasing drainage from 10.7% to 55.4% of the total catchment area increased the area residing close to a water body (no farther than 25 m) from 17.1% to 60.7%. This area estimate is useful for assessing the costs of water protection, arising from restricting forestry operations in the vicinity of water bodies.
机译:泥炭地的排水促进了树木的生长,改变了流域的水文状况,并增加了养分和悬浮固体向水体的出口。在这项研究中,从坡度,海拔,长度和土壤类型等方面评估了泥炭地排水对集水区陆地水流路径特性的影响。使用25 m×25 m数字高程模型(DEM)划定了三个研究流域(面积31.8-153.5km〜2)。计算每个集水区的典型水流路径,以表征接收水体上方的平均海拔高度,作为沿水流路径的距离的函数。所得的二维(2D)轮廓还允许计算流域的水平分布特性,作为与水体距离的函数。泥炭地排水减少了典型水流路径的长度和高度,并增加了水体附近的面积。排水量从总集水面积的10.7%增加到55.4%,使靠近水体(不超过25 m)的居住面积从17.1%增加到60.7%。该面积估计值可用于评估因限制水域附近的林业活动而引起的水保护成本。

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