
Surface Erosion Impact in Upper Serang Watershed Kemusu Municiaplity Boyolali District Centra Java
Author(s) -
Kuswaji Dwi Priyono
Publication year - 2014
Publication title -
forum geografi/forum geografi
Language(s) - English
Resource type - Journals
eISSN - 2460-3945
pISSN - 0852-0682
DOI - 10.23917/forgeo.v4i2.4854
Subject(s) - watershed , universal soil loss equation , soil loss , erosion , intensity (physics) , hydrology (agriculture) , environmental science , java , mathematics , soil science , geography , geology , physics , geomorphology , computer science , geotechnical engineering , quantum mechanics , machine learning , programming language
The aim of this reseach are two fold. The first it to clasify and evaluate the surface crosivity and the second is to map the erosivity hazard. The final yield is a map of ... - ... in 1 : 50.000. the classification of surface erosivity is based on top soil loss maximum using the Universal Soil Loss Equation (USLE) of Wischmeir and Smith Method; that is executed on every unit of land. Land unit is detected through interpretation of false colour I.R. air photograph images, shot in 1981/ 1982, scale 1 : 50.000. The classification fields the following data : erosity intensity is 6,687.5 hm (26.78 percent) is ultimate low; 2,962.5 hm (11.86 percent) is low; 5,025.0 hm (20.12 percent) is medium 5,025.0 hm (20.12 percent) is medium 287.5 hm (1.15 percent) is high, while the in habited area has 4,637 hm (18.57 percent) or classified as a very low intensity.