Study on characteristics of sediment and bed load discharge in Sungai Jemberau at Tasik Chini

This study had been carried out to identify sediment characteristics in Sungai Jemberau at Tasik Chini, and to compare their bed load dischargedata between the measured and predicted methods. It was observed that extensive uncontrolled mining activities nearby Sungai Jemberau had led to erosion and...

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Bibliographic Details
Main Authors: Adilah, A.N (Author), Nur Marhidayu, M.S.S (Author)
Format: Article
Language:English
Published: Institute of Physics Publishing 2019
Subjects:
Online Access:View Fulltext in Publisher
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020 |a 17551307 (ISSN) 
245 1 0 |a Study on characteristics of sediment and bed load discharge in Sungai Jemberau at Tasik Chini 
260 0 |b Institute of Physics Publishing  |c 2019 
650 0 4 |a Bed load 
650 0 4 |a Concrete placing 
650 0 4 |a Earthquake engineering 
650 0 4 |a Engineering geology 
650 0 4 |a Geophysics 
650 0 4 |a Median grain sizes 
650 0 4 |a Mining activities 
650 0 4 |a Rainfall event 
650 0 4 |a River bed 
650 0 4 |a Rivers 
650 0 4 |a Sediment characteristic 
650 0 4 |a Sediment size 
650 0 4 |a Sediment transport 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1088/1755-1315/244/1/012046 
856 |z View in Scopus  |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-85063461707&doi=10.1088%2f1755-1315%2f244%2f1%2f012046&partnerID=40&md5=4a0cccbdfe560648a543a2445efb78ff 
520 3 |a This study had been carried out to identify sediment characteristics in Sungai Jemberau at Tasik Chini, and to compare their bed load dischargedata between the measured and predicted methods. It was observed that extensive uncontrolled mining activities nearby Sungai Jemberau had led to erosion and hence increasing bedload discharge. This situation hadbecome worst during storm or rainfall events because of increased sedimentation process.The river depth hadbecome shallow as the river bed was filled with bedload settles on the riverbed. Due to this situation, flooding becomes more severe as the river overflows. From here, the bedload discharge can be estimated using the DuBoys and Schoklitsch equation. Sediment size was classified using the Udden Wentworth Scale. Mostly, the median grain size (d50) wasin a range of 2.0mm to 4.0mm, and was classified as Very Fine Gravel (VFG). Meanwhile, the density of sediment was in a range of 2.34g/cm3 to 2.97g/cm3. Lastly, the comparison between the measured and predicted bedload discharge shown that DuBoys equation gives better prediction of bedload discharge in Sungai Jemberau. © 2019 Published under licence by IOP Publishing Ltd. 
700 1 0 |a Adilah, A.N.  |e author  
700 1 0 |a Nur Marhidayu, M.S.S.  |e author