| dc.contributor.author | Miardini, Arina | |
| dc.contributor.author | Harjadi, Beny | |
| dc.date.accessioned | 2012-05-01T03:55:21Z | |
| dc.date.available | 2012-05-01T03:55:21Z | |
| dc.date.issued | 2011-12 | |
| dc.identifier.citation | Arsyad, S. (1989). Konservasi Tanah dan Air. Penerbit IPB. Bogor. ________. (2000). Konservasi Tanah dan Air. Penerbit IPB. Bogor. Asdak, C. (1995). Hidrologi dan Pengelolaan Daerah Aliran Sungai. Gajah Mada University. Yogyakarta Hamilton, L.S. dan P.N.King. (1997). Daerah Aliran Sungai Hutan Tropika (Tropical Forested Watersheds). Gadjah Mada University Press. Yogyakarta Harjadi, B. (2005). Terrain Characteristic and Soil Erotion Risk Assesment for Watershed Priorization Using Remote Sensing and GIS. Tesis S2 Indian Institute of Remote Sensing Center for Space Science and Tahnology Education In Asia and The Pacific (CSSTEAP). India. Harjadi, B. (2010). Monitoring Penutupan Lahan di DAS Grindulu dengan Metode Penginderaan Jauh dan Sistem Informasi Geografi. Forum Geografi Vol. 24 No 1. Juli 2010, pp 85-91 Lillesand, T. M. and Kieffer, R. W. (1990). Penginderaan Jauh dan Interpretasi Citra. Gajah Mada University Press. Yogyakarta. Sinukaban, N. (2007). Peranan Konservasi Tanah dan Air dalam Pengelolaan Daerah Aliran Sungai. Bunga Rampai Konservasi Tanah dan Air 2004-2007. Masyarakat Konservasi Tanah dan Air. Jakarta | en_US |
| dc.identifier.issn | 0852-0682 | |
| dc.identifier.uri | http://hdl.handle.net/11617/1272 | |
| dc.description.abstract | The purpose of this study was to determine the potential erosion qualitatively by using SES by using
Remote Sensing and Geographic Information Systems in Kedung Ombo’s catchment area so it can be
determined which areas of priority should be conserved. The method used is qualitatively anaslisis
through SES method (Soil Erosion Status).) Which is calculated based on five parameters are: slope
direction (aspect), slope (slope gradient), the density of the river (drainage density), soil type (Soil types)
, and land use (landuse/landcover). The result shows that DTW Kedung Ombo has three classes of
erosion, which is very low, low and medium. Amounted to 41179.08 ha or 71.31% of the total
DTW Kedung Ombo erosion potential is still relatively mild, 13956.01 ha (24.17%), erosion potential
is very low and 2608.95 ha (4:52%) were classified as potential erosion. | en_US |
| dc.publisher | lppmums | en_US |
| dc.subject | surface erosion | en_US |
| dc.subject | kedung ombo’s cathment area | en_US |
| dc.subject | qualitative assessment | en_US |
| dc.subject | remote sensing | en_US |
| dc.subject | SIG | en_US |
| dc.title | APLIKASI PENGINDERAAN JAUH DAN SIG DALAM PENILAIAN POTENSI EROSI PERMUKAAN SECARA KUALITATIF DI DAERAH TANGKAPAN WADUK KEDUNG OMBO | en_US |
| dc.title.alternative | Application of Remote Sensing and Geographic Information System for Qualitative Assessment of Potential Surface Erosion at Kedung Ombo Catchment | en_US |
| dc.type | Article | en_US |
