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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Main Authors: , Suhada Arief, , Prof. Dr. Ir. Bambang Yulistyanto
格式: Theses and Dissertations NonPeerReviewed
出版: [Yogyakarta] : Universitas Gadjah Mada 2013
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在線閱讀:https://repository.ugm.ac.id/126046/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=66236
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機構: Universitas Gadjah Mada