Rusle的模型应用程序估计在爪哇岛中部的Sub - Das Garang上失去了上游土地

Fahrudin Hanafi, D. Pamungkas
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引用次数: 2

摘要

加朗流域是流经中爪哇三宝垄市的主要河流之一。加朗上游主要是三宝垄市及周边水土资源保持的缓冲带和集水区。这项研究位于上游的加朗流域,目的是了解由于土地利用变化导致的侵蚀或土壤流失耐受水平。该侵蚀模型针对的是采用修正通用水土流失方程(RUSLE)方法建立的板蚀模型。使用的数据是(R) 7个水文站10年的地面降雨量,(K)从地形解释得出的土壤类型,(LS)从SRTM雷达数据得出的长度和坡度,(CP)利用多光谱监督分类(最大似然)得出的保护和土地覆盖。通过对输入数据的验证来保持建模的质量,例如对降雨数据的正态比方法和一致性检验,对土壤数据的土壤质地和颜色调查,对土地覆盖和坡度验证的混淆矩阵。研究结果上游加朗流域面积1191.56公顷(14.14%),发生的侵蚀仍低于允许侵蚀极限,而面积7.232.67公顷(85.86%)的侵蚀发生在允许侵蚀值以上。平均土壤流失量为222吨/公顷/年,潜在土壤流失量高达39,236吨/年或土壤流失厚度为3.8厘米。即使在阈值之内,考虑到上游加朗流域的重要性,这必须加以控制,其土地覆盖已经开始改变其功能,以农业和坡地上的种植园。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Aplikasi Model Rusle untuk Estimasi Kehilangan Tanah Bagian Hulu di Sub Das Garang, Jawa Tengah
The Garang watershed is one of the main rivers passing through Semarang City, Central Java. Garang uptream is mostly a buffer zone and a catchment area for the water and soil resources conservation of Semarang City and surroundings. This research is located in the upstream Garang watershed, with the aim of knowing the level of erosion or soil loss tolerance due to land use change.The erosion model is specific to sheet erosion which modeled with RUSLE (Revised Universal Soil Loss Equation) method. The data used are (R) ground rainfall from 7 hydrological stations for 10 years, (K) soil types derived from land form interpretation, (LS) length and slope from SRTM radar data, (CP) conservation and land cover derived using a multispectral supervised classification (maximum likelihood). The quality of modeling is maintained through validation of input data, such as the normal ratio method and consistency test of rain data, soil texture and color surveys for soil data, confusion matrices for land cover and slope validation.The research results of the upstream Garang watershed area of 1191,56 hectares (14.14%), the erosion that occurred was still below the allowable erosion limit, while the area of 7.232,67 hectares (85.86%) was erosion that occurred above the allowable erosion value. The average soil loss is 222 tonnes / ha / year with the potential for soil loss up to 39,236 tonnes per year or soil loss thickness of 3.8 cm. Even though it is within the threshold, this must be controlled considering the importance of the upstream Garang watershed, whose land cover has begun to change its function to agriculture and plantations on sloping land.
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