STUDI GERUSAN LOKAL AKIBAT SEDIMENTASI DI HULU BENDUNG
By the time the water flowing in the river, a number of basic sediment (bed load) and fine (suspended load) carried with the flow. At the time the river flow is hampered due to weir the flow rate of the river bottom will be reduced, and the ability of water to carry sediment flow will be reduced as...
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| Format: | Thesis |
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[Yogyakarta] : Universitas Gadjah Mada
2013
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