Observation on the sedimentation pattern based on the river features using sediment river study model
The process of settling of suspended material by the process of gravity is known as sedimentation. It was a natural process that carries the materials such as stones and sand that form layers of solid at the bottom of water flow. Particles are deposited when the velocity cannot supports the parti...
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| Format: | Undergraduates Project Papers |
| Language: | English |
| Published: |
2014
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| Subjects: | |
| Online Access: | http://umpir.ump.edu.my/id/eprint/10107/1/RAHAYU%20BINTI%20RAZALI%20%23.PDF |
| _version_ | 1796990736288186368 |
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| author | Rahayu, Razali |
| author_facet | Rahayu, Razali |
| author_sort | Rahayu, Razali |
| collection | UMP |
| description | The process of settling of suspended material by the process of gravity is known as
sedimentation. It was a natural process that carries the materials such as stones and sand
that form layers of solid at the bottom of water flow. Particles are deposited when the
velocity cannot supports the particles anymore, which removed from the flow with the
help of gravity. The main objective why this study is carried out was to determine and
o1éry'e if there was any effect of the Hver characteristic on the pattern of the sediments
deposited. The size distribution of the sediment was also determined at every river
characteristic, to prove if the river characteristic also affects the distribution of the
sediments. One river model was designed with all the characteristic to be used in this
study. The river model was not designed using the actual river scale because the study
was only based on the river features. The experiment was run in a few sets with different
sediment placement. The water flow generated the sediments and form different pattern.
The pattern is then observed and captured. The samples of sediment at selected location
in the river model were sieved to identify the size of sediment. Observation from the
captured image of the river at studied point, shown that there are different pattern of
sedimentation due to different river features. This show that the river features also affect
the procesof sedimentation. Sediment size distribution and flow strength are the factors
that effect on sediment transport rates in the rivers. From the sieve analysis, it can be
observed that the size of the sediment is different at different point of the river. |
| first_indexed | 2024-03-06T11:55:58Z |
| format | Undergraduates Project Papers |
| id | UMPir10107 |
| institution | Universiti Malaysia Pahang |
| language | English |
| last_indexed | 2024-03-06T11:55:58Z |
| publishDate | 2014 |
| record_format | dspace |
| spelling | UMPir101072021-07-22T03:43:10Z http://umpir.ump.edu.my/id/eprint/10107/ Observation on the sedimentation pattern based on the river features using sediment river study model Rahayu, Razali TC Hydraulic engineering. Ocean engineering The process of settling of suspended material by the process of gravity is known as sedimentation. It was a natural process that carries the materials such as stones and sand that form layers of solid at the bottom of water flow. Particles are deposited when the velocity cannot supports the particles anymore, which removed from the flow with the help of gravity. The main objective why this study is carried out was to determine and o1éry'e if there was any effect of the Hver characteristic on the pattern of the sediments deposited. The size distribution of the sediment was also determined at every river characteristic, to prove if the river characteristic also affects the distribution of the sediments. One river model was designed with all the characteristic to be used in this study. The river model was not designed using the actual river scale because the study was only based on the river features. The experiment was run in a few sets with different sediment placement. The water flow generated the sediments and form different pattern. The pattern is then observed and captured. The samples of sediment at selected location in the river model were sieved to identify the size of sediment. Observation from the captured image of the river at studied point, shown that there are different pattern of sedimentation due to different river features. This show that the river features also affect the procesof sedimentation. Sediment size distribution and flow strength are the factors that effect on sediment transport rates in the rivers. From the sieve analysis, it can be observed that the size of the sediment is different at different point of the river. 2014-06 Undergraduates Project Papers NonPeerReviewed application/pdf en http://umpir.ump.edu.my/id/eprint/10107/1/RAHAYU%20BINTI%20RAZALI%20%23.PDF Rahayu, Razali (2014) Observation on the sedimentation pattern based on the river features using sediment river study model. Faculty of Civil Engineering and Earth Resources, Universiti Malaysia Pahang. |
| spellingShingle | TC Hydraulic engineering. Ocean engineering Rahayu, Razali Observation on the sedimentation pattern based on the river features using sediment river study model |
| title | Observation on the sedimentation pattern based on the river features using sediment river study model |
| title_full | Observation on the sedimentation pattern based on the river features using sediment river study model |
| title_fullStr | Observation on the sedimentation pattern based on the river features using sediment river study model |
| title_full_unstemmed | Observation on the sedimentation pattern based on the river features using sediment river study model |
| title_short | Observation on the sedimentation pattern based on the river features using sediment river study model |
| title_sort | observation on the sedimentation pattern based on the river features using sediment river study model |
| topic | TC Hydraulic engineering. Ocean engineering |
| url | http://umpir.ump.edu.my/id/eprint/10107/1/RAHAYU%20BINTI%20RAZALI%20%23.PDF |
| work_keys_str_mv | AT rahayurazali observationonthesedimentationpatternbasedontheriverfeaturesusingsedimentriverstudymodel |