Rejani R, Rao K V, Osman M, Srinivasa Rao Ch, Reddy K Sammi, Chary G R, Samuel Josily
ICAR-Central Research Institute for Dryland Agriculture, Hyderabad, Telangana, India.
Environ Monit Assess. 2016 Mar;188(3):143. doi: 10.1007/s10661-016-5143-4. Epub 2016 Feb 4.
The ungauged wet semi-arid watershed cluster, Seethagondi, lies in the Adilabad district of Telangana in India and is prone to severe erosion and water scarcity. The runoff and soil loss data at watershed, catchment, and field level are necessary for planning soil and water conservation interventions. In this study, an attempt was made to develop a spatial soil loss estimation model for Seethagondi cluster using RUSLE coupled with ARCGIS and was used to estimate the soil loss spatially and temporally. The daily rainfall data of Aphrodite for the period from 1951 to 2007 was used, and the annual rainfall varied from 508 to 1351 mm with a mean annual rainfall of 950 mm and a mean erosivity of 6789 MJ mm ha(-1) h(-1) year(-1). Considerable variation in land use land cover especially in crop land and fallow land was observed during normal and drought years, and corresponding variation in the erosivity, C factor, and soil loss was also noted. The mean value of C factor derived from NDVI for crop land was 0.42 and 0.22 in normal year and drought years, respectively. The topography is undulating and major portion of the cluster has slope less than 10°, and 85.3% of the cluster has soil loss below 20 t ha(-1) year(-1). The soil loss from crop land varied from 2.9 to 3.6 t ha(-1) year(-1) in low rainfall years to 31.8 to 34.7 t ha(-1) year(-1) in high rainfall years with a mean annual soil loss of 12.2 t ha(-1) year(-1). The soil loss from crop land was higher in the month of August with an annual soil loss of 13.1 and 2.9 t ha(-1) year(-1) in normal and drought year, respectively. Based on the soil loss in a normal year, the interventions recommended for 85.3% of area of the watershed includes agronomic measures such as contour cultivation, graded bunds, strip cropping, mixed cropping, crop rotations, mulching, summer plowing, vegetative bunds, agri-horticultural system, and management practices such as broad bed furrow, raised sunken beds, and harvesting available water using farm ponds and percolation tanks. This methodology can be adopted for estimating the soil loss from similar ungauged watersheds with deficient data and for planning suitable soil and water conservation interventions for the sustainable management of the watersheds.
未测流的湿润半干旱流域集群Seethagondi位于印度特伦甘纳邦阿迪拉巴德区,容易发生严重侵蚀和水资源短缺。流域、集水区和田间层面的径流和土壤流失数据对于规划水土保持措施至关重要。在本研究中,尝试使用RUSLE结合ARCGIS为Seethagondi集群开发一个空间土壤流失估算模型,并用于在空间和时间上估算土壤流失。使用了1951年至2007年期间阿佛洛狄忒的日降雨数据,年降雨量在508至1351毫米之间变化,年平均降雨量为950毫米,平均侵蚀力为6789兆焦耳毫米公顷⁻¹小时⁻¹年⁻¹。在正常年份和干旱年份观察到土地利用土地覆盖有相当大的变化,特别是在农田和休耕地上,并且侵蚀力、C因子和土壤流失也有相应变化。从作物地的归一化植被指数得出的C因子在正常年份和干旱年份的平均值分别为0.42和0.22。地形起伏,集群的大部分地区坡度小于10°,85.3%的集群土壤流失低于20吨公顷⁻¹年⁻¹。作物地的土壤流失在低降雨年份从2.9至3.6吨公顷⁻¹年⁻¹变化到高降雨年份的31.8至34.7吨公顷⁻¹年⁻¹,年平均土壤流失为12.2吨公顷⁻¹年⁻¹。作物地的土壤流失在8月份较高,在正常年份和干旱年份的年土壤流失分别为13.1和2.9吨公顷⁻¹年⁻¹。根据正常年份的土壤流失情况,为该流域85.3%的面积推荐的措施包括农艺措施,如等高耕作、分级田埂、带状种植、混合作物种植、作物轮作、覆盖、夏季深耕、植被田埂、农业园艺系统,以及管理措施,如宽床深沟、高低床和利用农用池塘和渗滤池收集可用水。这种方法可用于估算数据不足的类似未测流流域的土壤流失,并为流域的可持续管理规划合适的水土保持措施。