阿尔文地区d z河流域土壤侵蚀状况预测

Esin Erdoğan Yüksel, M. Özalp, Saim Yıldırımer
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引用次数: 1

摘要

研究目的:本研究的主要目的是借助WEPP(水蚀预测项目)模型预测与土壤侵蚀有关的一些过程(土壤流失、径流量和产沙量)。研究区域:将WEPP模型应用于Duz Creek流域(1059公顷)。它是Artvin Borcka区附近流入大科鲁赫河流域的一个子流域。材料和方法:根据WEPP模型的要求,利用现场采样(土壤)、实验室分析和GIS(地理信息系统)评估收集的数据,为流域创建了四个关于土壤、气候、坡度和植物覆盖/管理的大型数据文件。为了便于运行和详细调查研究区的土壤侵蚀过程,将研究流域划分为八个小型水文单元(SHU),并在这些SHU上运行该程序。主要结果:在GeoWEPP运行结束时,结果显示,研究区域内的年降水量总计约735毫米。该模型还预测,这一降水量产生的径流约为207毫米,进而产生的年总土壤损失和泥沙量分别为2815.2吨和2720.9吨。此外,单位面积产沙量估计约为2.57吨/公顷/年,而输沙率(SDR)为0.977。最后,该模型预测,侵蚀沉积物的颗粒分布分别为粘土、淤泥和沙子的20%、25%和55%,而流失沉积物的平均有机质含量约为5%。亮点:可以在短时间内计算出大面积的水土流失和产沙量,而且成本很低。
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Predicting Soil Erosion Status of the Düz Creek Watershed in Artvin
Aim of study: Main objective of this research was to predict some of the processes (soil loss, runoff and sediment yield) related to soil erosion with the help of WEPP (Water Erosion Prediction Project) model. Area of study: The WEPP model was applied to the Duz Creek Watershed (1059 ha in size). It is a sub-watershed flowing into the greater Coruh River Basin near the district of Borcka, Artvin. Material and methods: As required by the WEPP model, four large-data files of soil, climate, slope and plant cover/management were created for the watershed using the data gathered from in-field samplings (soil), laboratory analyses and GIS (Geographical Information Systems) assessments. For easier run and detailed investigation of soil erosion process of the research area, the studied watershed was divided into eight small hydrological units (SHUs) and the program was run on these SHUs. Main results: At the end of GeoWEPP’s run, the results revealed that a total of about 735 mm annual precipitation was fell within the study area. The model also predicted that there was approximately 207 mm as runoff out of this amount of precipitation, which, in turn, generated an annual total soil loss and sediment amounts as 2815.2 t and 2720.9 t, respectively. In addition, the sediment yield per unit area was estimated to be around 2.57 ton/ha/yr while the sediment delivery ratio (SDR) was found to be as 0.977. Lastly, the model predicted that the particle distribution of eroded sediment were 20%, 25% and 55% of clay, silt and sand, respectively, while the mean organic matter (OM) amount of the lost sediment was about 5% for the studied watershed. Highlights: Soil loss and sediment yield can be calculated for large areas in a short time and with little cost.
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