首页> 外文会议>1st International Conference on Sustainable Planning and Development 2003 Skiathos, Greece >Application of GIS for soil erosion and nutrient loss modelling in a small river catchment
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Application of GIS for soil erosion and nutrient loss modelling in a small river catchment

机译:GIS在小流域水土流失与养分流失建模中的应用。

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This paper aims to describe and compare different possibilities to model soil loss in Sipe River catchment (8.87 km~2) based on GIS (Geographical Information Systems) application and principles of USLE (Universal Soil Loss Equation) model. The Sipe River catchment is situated in Northern Europe in South Estonia. Different methods and equations were used to calculate USLE factors and soil loss. Nutrient losses are partly determined by the erosion process, an especially strong correlation is found between soil loss and phosphorus runoff. A significant part of nitrogen lies in topsoil and therefore besides leaching erosion also has a major influence on organic nitrogen loss. Nutrient loss due to erosion leads to lowered soil fertility rate and eutrophication of streams and lakes. Calculated erosion amounts in Sipe catchment reached 5 t ha~(-1) yr~(-1). Average potential soil loss calculated by different methods remained between 0,04 ― 0.08 t ha~(-1) yr~(-1). Modelling results were compared with each other and evaluated by soil-loss measurement results carried out at nine locations with different land use and slope. Calculated and measured erosion values were similar. For grasslands, pastures and forests average differences between measured and calculated erosion rates did not exceed 0.1 t ha~(-1) yr~(-1) r. Differences between measured and calculated soil loss rates were small also for croplands but variability between different fields was higher than in grasslands. The main differences between measured and calculated erosion were found in fields where potatoes and vegetables were cultivated (up to 1 t ha~(-1) yr~(-1)). Soil samples were taken in each measurement plot to determine soil properties, phosphorus and nitrogen content. It was calculated that the average phosphorus loss due to erosion in Sipe catchment is 4.5 g ha~(-1) yr~(-1) and nitrogen loss is 0.1 kg ha~(-1) yr~(-1).
机译:本文旨在描述和比较基于GIS(地理信息系统)应用和USLE(通用土壤流失方程)模型原理的Sipe河流域(8.87 km〜2)土壤流失建模的各种可能性。 Sipe河集水区位于南爱沙尼亚的北欧。使用了不同的方法和方程式来计算USLE因子和土壤流失。养分流失部分取决于侵蚀过程,土壤流失与磷径流之间存在特别强烈的相关性。氮的很大一部分存在于表层土壤中,因此,除了淋溶作用外,侵蚀还对有机氮的流失产生重大影响。侵蚀造成的养分流失导致土壤肥力降低,溪流和湖泊富营养化。刀耕地流域的侵蚀量计算值达到5 t ha〜(-1)yr〜(-1)。不同方法计算得出的平均潜在土壤流失量在0.04〜0.08 t ha〜(-1)yr〜(-1)之间。将模型结果相互比较,并通过在9个不同土地利用和坡度的地点进行的土壤流失测量结果进行评估。计算和测得的侵蚀值相似。对于草地,牧场和森林,测得和计算出的侵蚀率之间的平均差异不超过0.1 t ha〜(-1)yr〜(-1)r。农田的土壤流失率的测量值与计算值之间的差异也很小,但不同田间的变异性高于草地。在种植马铃薯和蔬菜的田地(高达1 t ha〜(-1)yr〜(-1))中,测得的侵蚀量与计算得出的侵蚀量之间存在主要差异。在每个测量区中采集土壤样品,以确定土壤性质,磷和氮含量。据计算,刀鞘流域因侵蚀造成的平均磷损失为4.5 g ha〜(-1)yr〜(-1),氮损失为0.1 kg ha〜(-1)yr〜(-1)。

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