Analysis of the Dynamics of Water Flow and Suspension Flow Discharge in Volcano Watershed with Settlement Land Use
Abstract
Suspension flow into the upstream of volcano watershed is sensitive to land use. In Indonesia, a settlement is a form of land use in several volcanic landscapes. There is currently no detailed study on the suspension flow sediment from the settlement land use. The purpose of this study is to investigate the characteristics of the relationship between water and suspension flow discharge. The study was conducted through the measurements at a gully outlet that produced 747 suspension load data. For each rainfall event, suspension load measurements were made in the field, followed by laboratory analysis. Additionally, field surveys were used to determine the characteristics of settlement land use and the water flow into the gully system. According to the findings, the peak flow discharge corresponds to the peak suspension discharge, the peak flow discharge comes before the peak suspension discharge, and the peak flow discharge happens after the peak suspension discharge. The average time lag between initial rainfall events and suspension flow was 10.36 minutes, and the suspension peak content varied by an average of 2.22 gl-1. The grain size was also dominated by the clay fraction, averaging 67.86% on the ascending branch and 67.82% on the descending branch.
References
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Hadini, L.O., Sartohadi, J., Setiawan, M.A., & Mardiatno, D. (2021). The Dynamics of flow
discharge and suspension flow discharge in volcano watershed with agroforestry land cover. Civil and Environmental Science Journal (Civense), 4(2), 141-153. https://doi.org/10.21776/ub.civense.2021.00402.4.
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Herschy, R.W., 2009. Streamflow Measurement Third edit. T. & Francis, ed., 2 Park Square, Milton Park, Abingdon, Oxon OX14 4RN.
Kellner, E., & Hubbart, J. A. (2018). Spatiotemporal variability of suspended sediment particle size in a mixed-land-use watershed. Science of the Total Environment, 615, 1164–1175. https://doi.org/10.1016/j.scitotenv.2017.10.040.
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Li, X., Wang, H., Zhang, L., & Wu, B. (2015). Soil erosion and sediment-yield prediction at Basin Scale in Upstream Watershed of Miyun Reservoir. J. Hydrol. Eng., 20(6), 1–7. https://doi.org/10.1061/(ASCE)HE.1943-5584.0001098.
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Mondal, A., Khare, D., Kundu, S., Meena, P. K., Mishra, P. K., & Shukla, R. (2015).impact of climate change on future soil erosion in different slope, land use, and soil-type conditions in a Part of the Narmada River Basin, India. J. Hydrol. Eng., 20(6), 1–12. https://doi.org/10.1061/(ASCE)HE.1943-5584.0001065.
Maulana, R.A., Lubis, K.S., & Marbun, P. (2014). Uji korelasi antara discharge aliran sungai dan konsentrasi sedimen melayang pada Muara Sub DAS Padang di Kota Tebing Tinggi. Jurnal Online Agroekoteknologi, 2(2337), 1518–1528.
Ma’wa, J., & Andawayanti, U. (2009). Studi pendugaan sisa usia guna waduk sengguruh dengan pendekatan erosi dan sedimentasi. Disertasi. Malang : Universitas Brawijaya.
Mbaya, L.A., Ayuba, H.K., & Abdullahi, J. (2012). An Assessment of gully erosion in Gombe Town, Gombe State. Journal of Geography and Geology, 4(3), 110–122.
Merritt, W.S., Lecther, R.A., & Jakeman, AJ. (2003). A Review of erosion and sediment transport model. Environment Model Software, 18, 761-799.
Miller, J.R., Mackin, G., & Miller, S.M.O. (2015). Application of Geochemical Tracers to Fluvial Sediment, London: Springer.
Morgan, R.P.C. (2005). Soil Erosion and Conservation: Third Edition. USA; Blackwell.
Nandini, R. & Narendra, B.H. (2012). Karakteristik lahan kritis bekas letusan gunung batur di Kabupaten Bangli, Bali. Penelitian hutan dan Konservasi Alam, 9(3), pp.199–211.
Neno, A.K., Herman, H., & Wahid, A. (2016). Hubungan discharge air dan tinggi muka air di Sungai Lambagu Kecamatan Tawaeli Kota Palu. Warta Rimba, 4 (2), 1–8.
Nicótina, L., Tarboton, D.G., Tesfa, T.K., & Rinaldo, A. (2011). Hydrologic controls on equilibrium soil depths. Water Resources Research, 47(4), 1–11. https://doi.org/10.1029/2010WR009538.
Nocoń, W. (2016). Quantitative monitoring of batch sedimentation based on fractional density changes. Powder Technology, 292, 1–6. https://doi.org/10.1016/j.powtec.2016.01.010.
Nugroho, S.H. & Basit, A. (2014). Sebaran sedimen berdasarkan analisis ukuran butir di Teluk Weda, Maluku Utara. Jurnal Ilmu dan Teknologi Kelautan Tropis, 6(1), 229–240.
Oktarina, N.R. (2005). Analisis hidrograf limpasan akibat variasi intensitas hujan dan kemiringan lahan (kajian laboratorium dengan simulator hujan). Jurnal Teknik Sipil dan Lingkungan. 3(1).
Panagos, P, Borrelli, P, Poesen, J, Ballabio, Lugato, E., Meusburger, K., Montanarella, L., & Allewl, C. (2015). The new assessment of soil loss by water erosion in Europe. Environmental Science & Policy, 54, 438–447. http://doi.org/10.1016/j.envsci.2015.08.012.
Parsons, A.J., & Wainwright, J. (2000). Modeling Surface Runoff. In Schmidt, J. (ed). Soil Erosion, Application of Physically Based Models. Germany: Springer.
Poesen, J., Nachtergaele, J., Verstraeten, G., & Valentina, C. (2003). Gully erosion and environmental change: importance and research needs. Catena, 50, 91-133. http://dx.doi.org/10.1016/S0341-8162(02)00143-1.
Rusdi, Alibasyah, M. R., & Abubakar, K. (2013). Evaluasi degradasi lahan diakibatkan erosi pada areal pertanian di Kecamatan Lembah Seulawah Kabupaten Aceh Besar. Jurnal Konservasi Sumber Daya Lahan. 1(1), 24–39.
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Published
2023-04-18
How to Cite
HADINI, La Ode et al.
Analysis of the Dynamics of Water Flow and Suspension Flow Discharge in Volcano Watershed with Settlement Land Use.
Geosfera Indonesia, [S.l.], v. 8, n. 1, p. 19-34, apr. 2023.
ISSN 2614-8528.
Available at: <https://jurnal.unej.ac.id/index.php/GEOSI/article/view/30921>. Date accessed: 23 nov. 2024.
doi: https://doi.org/10.19184/geosi.v8i1.30921.
Section
Original Research Articles
