Tingkat Erodibilitas Tanah Di Daerah Aliran Sungai Bayang Sani
Abstract
The Bayang Sani Watershed has an area of 1267.97 hectares with an average rainfall of 3117 mm/ year. The topography of this watershed have varies slopes. In the rainy season, the river water is a muddy color and both soil and rocks are contained in the river’s water that causes channel damage and reduced river capacity. It is caused by the wider distribution of land erosion in the Bayang Sani Watershed. The purpose of this study was to analyze the soil erodibility. The method of this study is a quantitative study and field survey method. The data was collected by field survey and sample points were determined using purposive random sampling techniques. The sample was analyzed in the BPTP laboratory to determine the types and colors of the soil sample, depending on the quality of the soil's erosive value. The results show that soil erodibility in the Bayang Sani Watershed range 0.15-0.28. The low soil erodibility level found in land units F3.II.Kc.Qal.Lat (0.16), V2.II.Kc.Tomp.Lat (0.15) and V2.II.Sm.Tomp.Lat. (0.16) the moderate of soil erodibility was found in the land unit V3.III.Ht.Tomp.Lat (0.28).
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Arsyad, S. (2010). Konservasi Tanah Dan Air (2nd ed.). Institut Pertanian Bogor Press.
Asdak, C. (2014). Hidrologi dan Pengelolaan Daerah Aliran Sungai. In Yogyakarta. UGM Press.
Asiki, M., Maryati, S., & Akase, N. (2019). Analisis Tingkat Kerentanan Longsor Daerah Muara Sungai Bone Kota Gorontalo. Jambura Geoscience Review, 1(2), 87-101.
Dibyosaputro. (1997). Geomorfologi Dasar. Yogyakarta. UGM Press.
He, S. Q., Zheng, Z. C., & Wang, L. (2011). Land Use Patterns Effect on Soil Anti-Erodibility in Low Mountain-Hilly Region. Advanced Materials Research, 383–390, 3768–3774. https://doi.org/10.4028/www.scientific.net/AMR.383-390.3768
Hermon, D. (2012). Mitigasi Bencana Hidrometerologi. UNP Press.
Hudson N. W. (1972). Soil Conversation. New York. Cornell University Press.
Priatna, S. J. (2001). Potensi Erosi dan Indeks Erodibiitas pada Areal Perkebunan Kopi Rakyat Dengan Umur dan Lereng yang Berbeda. Jurnal Pertanian Indonesia, 3(2), 84–88.
Pujawan, M., Afandi, Novpriansyah, H., & E.S. Manik, K. (2016). Kemantapan Agregat Tanah Pada Lahan Produksi Rendah Dan Tinggi Di Pt Great Giant Pineapple. Jurnal Agrotek Tropika, 4(1), 111–115.
Putra, A., Triyatno, T., Syarief, A., & Hermon, D. (2018). Penilaian Erosi Berdasarkan Metode USLE dan Arahan Konservasi Pada DAS Air Dingin Bagian Hulu Kota Padang-Sumatera Barat. Jurnal Geografi, 10(1), 1–13. https://doi.org/10.24114/jg.v10i1.7176
Rahmayati, F. D. (2018). Summary for Policymakers. Pengaruh Kelas Kemiringan Lereng Terhadap Ketebalan Lapisan Olah, Kandungan Bahan Organik, Al Dan Fe Pada Alfisol Di Desa Gunungsari Kabupaten Tasik Malaya., 9(2), 17–27.
Sulistyaningrum, D., Susanawati, L. D., & Suharto, B. (2014). Pengaruh Karakteristik Fisika-Kimia Tanah Terhadap Nilai Indeks Erodibilitas Tanah Dan Upaya Konservasi Lahan. Jurnal Sumberdaya Alam Dan Lingkungan, 1(2), 55–62.
Tejada, M., & Gonzalez, J. L. (2006). The Relationships Between Erodibility and Erosion in a Soil Treated with Two Organic Amendments. Soil and Tillage Research, 91(1–2), 186–198. https://doi.org/10.1016/j.still.2005.12.003
Van Zuidam, & Cancelado. (1979). Terrain Analysis and Classification Using Aerial Photographs. A Geomorphological Approach. ITC. Enschede.
Wischmeier, W. H., Johnson, C. B., & Cross, B. V. (1971). Soil erodibility nomograph for farmland and construction sites. Journal of Soil and Water Conservation1.
DOI: https://doi.org/10.34312/jgeosrev.v2i1.2468
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