Effect of Soil Physical Properties on Surface Runoff in Lukulo Upstream Watershed
Abstract
Lukulo upstream watershed is one of the watersheds in Central Java Province, which passes through 3 districts; Kebumen, Wonosobo, and Banjarnegara. Lukulo upstream watershed has eight sub-watersheds located in areas with diverse topography and lithology. The diversity of topography and lithology affects the characteristics of the area, as does the physical condition of the soil. The physical condition of this soil affects the runoff. Soil’s physical properties control rainwater to run off and have important effects on runoff behavior in watersheds. This study aims to determine the physical properties of the soil against runoff in each sub-watershed and each part of the watershed. The method used uses a laboratory, studio, and field approach. The results obtained show that the physical properties of the soil in the Lukulo upstream watershed affect the amount of runoff resistance in the upstream area; in the downstream area the runoff is relatively good. The study also shows two different results. In the Loning watershed, the velocity of downstream runoff is higher than the upstream, while in the Lokidang and Medana watershed, level of surface water flow is lower in the downstream area.
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Chai, H., Rao, S., Wang, R., Liu, J., Huang, Q., & Mou, X. (2015). The Effect of the Geomorphologic Type as Surrogate to the Time Factor on Digital Soil Mapping. Open Journal of Soil Science, 5(June), 123–134. https://doi.org/http://dx.doi.org/10.4236/ojss.2015.56012
Davie, T. (2008). Fundamentals of hydrology. In Southeastern Geographer (Second, Vol. 44, Issue 1). Taylor & Francis e-Library.
Miller, B. A., & Schaetzl, R. J. (2016). Geoderma History of soil geography in the context of scale. Geoderma, 264, 284–300. https://doi.org/10.1016/j.geoderma.2015.08.041
Mockus, V., Werner, J., Woodward, D. E., Nielsen, R., Dobos, R., Hjelmfelt, A., & Hoeft, C. C. (2009). Hydrologic Soil Groups. In National Engineering Handbook. Natural Resources Conservation Service.
Raharjo, P. D. (2010a). Penggunaan Data Penginderaan Jauh dalam Analisis Bentukan Lahan Asal Proses Fluvial di Wilayah Karangsambung. Jurnal Geografi, 7(2), 146–152. https://doi.org/https://doi.org/10.15294/jg.v7i2.85
Raharjo, P. D. (2010b). Penggunaan data penginderaan jauh dan SIG untuk pemantauan kekritisan di DAS Lukulo Jawa Tengah. Jurnal Manusia Dan Lingkungan, 17(l), 37–45. https://doi.org/doi.org/10.22146/jml.18524
Raharjo, P. D. (2014). Aplikasi teknik penginderaan jauh multi-temporal untuk kajian limpasan permukaan akibat perubahan Penutup lahan, kasus di DAS Grompol Jawa Tengah [Universitas Gadjah Mada]. https://repository.ugm.ac.id/133236/
Raharjo, P. D., Ansori, C., Widitanto, K., & Winduhutomo, S. (2018). Kemampuan tanah dalam mempengaruhi aliran air permukaan di DAS Lukulo Hulu.
Raharjo, P. D., & Haryono, E. (2020). Sintesa Geomorfologi Antroposen Kawasan Cagar Alam Geologi Karangsambung Bagian Selatan. Jurnal Geografi Gea, 20(2), 141–150. https://doi.org/10.17509/gea.v20i2.27727
Raharjo, P. D., & Nur, A. M. (2013). Pemetaan gerakan tanah Kawasan Cagar Alam Geologi Karangsambung dengan menggunakan data penginderaan jauh dan SIG. Forum Geografi, 27(2), 99–114.
Raharjo, P. D., Nur, A. M., & Hidayat, E. (2011). Aplikasi sistem informasi geografis dalam identifikasi kerentanan bencana alam di kawasan cagar alam geologi karangsambung. Buletin Geologi Tata Lingkungan, 21(1), 23–33. https://doi.org/https://doi.org/10.5072/FK2/JLK8PZ
Raharjo, P. D., & Saifudin. (2008). Pemetaan Erosi DAS Lukulo Hulu dengan Menggunakan Data Penginderaan Jauh dan Sistem Informasi Geografi. Jurnal Ilmu Tanah Dan Lingkungan, 8(2), 103–113. https://doi.org/https://doi.org/10.5072/FK2/1KXZCT
Raharjo, P. D., Widiyanto, K., Winduhutomo, S., & Purnami, D. N. (2016). Morfometri dan Lingkungan Fisik DAS Lukulo Hulu Ditinjau dari Pengaruhnya Terhadap Aliran Air Permukaan , runoff.
Raharjo, P. D., Widiyanto, K., Winduhutomo, S., & Yudaputra, A. (2019). The role of geomorphology for analysis of landscape ecology in The Loning Watershed, Karangsambung-Karangbolong National Geopark. Prosiding Nasional Kebumian Ke-12, 615–628. https://repository.ugm.ac.id/id/eprint/275744
Raharjo, P. D., Winduhutomo, S., Widayanto, K., & Puswanto, E. (2016). Analisa Hidrologi Permukaan dalam Hubungannya dengan Debit Banjir DAS Lukulo Hulu dengan Menggunakan Data Penginderaan Jauh. Jurnal Geografi, 13(2), 163–178. https://doi.org/https://doi.org/10.15294/jg.v13i2.7974
Saifudin, & Raharjo, P. D. (2009). Perencanaan DAS Welaran sebagai daerah pengujian hidrologi. Prosiding Simposium Sains Geoinformasi I, November, 191–196.
Schaetzl, R. J., & Anderson, S. (2005). Soils: Genesis and Geomorphology. Cambridge University Press.
Scipal, K., Scheffler, C., & Wagner, W. (2005). Soil moisture-runoff relation at the catchment scale as observed with coarse resolution microwave remote sensing. Hydrology and Earth System Sciences, 9(3), 173–183. https://doi.org/10.5194/hess-9-173-2005
Seyhan, E. (1977). Fundamentals of Hydrology. Geografisch Instituut der Rijksuniversiteit.
Sosrodarsono, S., & Takeda, K. (1978). Hidrologi Untuk Pengairan. Pradnya Paramita.
Zinck, J. A. (2013). Geopedology, Elements of geomorphology for soil and geohazard studies. ITC Faculty of Geo-Information Science and Earth Observation.
Zuidam, V., & Cancelado, V. Z. (1978). Terrain Analisys and Classification Uisng Aerial Photography, A Geomorphological Approach. In ITC textbook of Photo-Interpretation. ITC Faculty of Geo-Information Science and Earth Observation.
DOI: https://doi.org/10.17509/gea.v22i1.39470
DOI (PDF): https://doi.org/10.17509/gea.v22i1.39470.g18940
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