Hydrology and suspended sediment yield in Sungai Kinabatangan

The quality of many rivers today is affected by anthropogenic factors such as land use conversions and industrial developments. These activities have altered the pattern of runoff, increased the sediment loads delivered into river channels, and inadvertently affect the quality of river water. Thi...

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Main Author: Chua, Li Ying
Format: Thesis
Language:English
Published: 2016
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Online Access:https://eprints.ums.edu.my/id/eprint/17517/1/Hydrology%20and%20suspended%20sediment.pdf
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spelling my-ums-ep.175172017-11-20T02:16:20Z Hydrology and suspended sediment yield in Sungai Kinabatangan 2016 Chua, Li Ying QE Geology The quality of many rivers today is affected by anthropogenic factors such as land use conversions and industrial developments. These activities have altered the pattern of runoff, increased the sediment loads delivered into river channels, and inadvertently affect the quality of river water. This study was carried out to (a) analyse the hydrology characteristics of Sungai Kinabatangan Catchment; (b) determine the sediment yield in the Sungai Kinabatangan Catchment; (c) develop baseline hydro-geometry data of Sungai Kinabatangan and its tributaries; and (d) design flow duration curves (FOC) for ungauged rivers in the Sungai Kinabatangan Catchment. The four objectives were determined by field measurements of river geometries as well as analysis of long-term gauging station data. For the first objective, this study found that the Sungai Kinabatangan Catchment portrays hydrologic characteristics of a large catchment. It is mainly dominated by baseflow and less responsive to rainfall. The second objective determined that the sediment yield in the Sungai Kinabatangan Catchment averages about 250 to 1,250 tonjkm2fyear. The amount is deemed tolerable and the yield has been relatively the same since previous studies carried out 20 years ago. Hydro-geometry measurements (width and depth of a channel) were obtained for 17 tributaries within the Sungai Kinabatangan Catchment as well as the main river stem itself. These measurements are useful in establishing a baseline of hydro-geometry data for Sungai Kinabatangan. For the final objective, the design FOC for all the tributaries in the Sg. Kinabatangan basin was established based on the data from five existing gauging stations in the basin. Flow regime for each tributary could be extracted from the design FOC. This method is useful in the estimation of flow for small tributaries within a big catchment. It is especially practical where numerous high-order streams drain into the catchment and these streams are less accessible or are without a gauging record. 2016 Thesis https://eprints.ums.edu.my/id/eprint/17517/ https://eprints.ums.edu.my/id/eprint/17517/1/Hydrology%20and%20suspended%20sediment.pdf text en public masters Universiti Malaysia Sabah Faculty of Science and Natural Resources
institution Universiti Malaysia Sabah
collection UMS Institutional Repository
language English
topic QE Geology
spellingShingle QE Geology
Chua, Li Ying
Hydrology and suspended sediment yield in Sungai Kinabatangan
description The quality of many rivers today is affected by anthropogenic factors such as land use conversions and industrial developments. These activities have altered the pattern of runoff, increased the sediment loads delivered into river channels, and inadvertently affect the quality of river water. This study was carried out to (a) analyse the hydrology characteristics of Sungai Kinabatangan Catchment; (b) determine the sediment yield in the Sungai Kinabatangan Catchment; (c) develop baseline hydro-geometry data of Sungai Kinabatangan and its tributaries; and (d) design flow duration curves (FOC) for ungauged rivers in the Sungai Kinabatangan Catchment. The four objectives were determined by field measurements of river geometries as well as analysis of long-term gauging station data. For the first objective, this study found that the Sungai Kinabatangan Catchment portrays hydrologic characteristics of a large catchment. It is mainly dominated by baseflow and less responsive to rainfall. The second objective determined that the sediment yield in the Sungai Kinabatangan Catchment averages about 250 to 1,250 tonjkm2fyear. The amount is deemed tolerable and the yield has been relatively the same since previous studies carried out 20 years ago. Hydro-geometry measurements (width and depth of a channel) were obtained for 17 tributaries within the Sungai Kinabatangan Catchment as well as the main river stem itself. These measurements are useful in establishing a baseline of hydro-geometry data for Sungai Kinabatangan. For the final objective, the design FOC for all the tributaries in the Sg. Kinabatangan basin was established based on the data from five existing gauging stations in the basin. Flow regime for each tributary could be extracted from the design FOC. This method is useful in the estimation of flow for small tributaries within a big catchment. It is especially practical where numerous high-order streams drain into the catchment and these streams are less accessible or are without a gauging record.
format Thesis
qualification_level Master's degree
author Chua, Li Ying
author_facet Chua, Li Ying
author_sort Chua, Li Ying
title Hydrology and suspended sediment yield in Sungai Kinabatangan
title_short Hydrology and suspended sediment yield in Sungai Kinabatangan
title_full Hydrology and suspended sediment yield in Sungai Kinabatangan
title_fullStr Hydrology and suspended sediment yield in Sungai Kinabatangan
title_full_unstemmed Hydrology and suspended sediment yield in Sungai Kinabatangan
title_sort hydrology and suspended sediment yield in sungai kinabatangan
granting_institution Universiti Malaysia Sabah
granting_department Faculty of Science and Natural Resources
publishDate 2016
url https://eprints.ums.edu.my/id/eprint/17517/1/Hydrology%20and%20suspended%20sediment.pdf
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