Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu
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| internalnotes | [1] M. K. A. Kamarudin, M. E. Toriman, M. H. Rosli, H. Juahir, N. A. A. Aziz, A. Azid, S. F. M. Zainuddin and W. N. A. Sulaiman, “Analysis of meander evolution studies on effect from land use and climate change at the upstream reach of the Pahang River, Malaysia,” Mitigation and Adaptation Strategies for Global Change, vol. 20, pp. 1319-1334, Dec. 2015. [2] C. A. L. Jackson, A. A Zakaria, H. D. Johnson, Tongkul, F. and P. D. Crevello, “Sedimentology, stratigraphic occurrence and origin of linked debrites in the West Crocker Formation (Oligo-Miocene), Sabah, NW Borneo,” Marine and Petroleum Geology, vol. 10, pp. 122-134, Dec. 2009. [3] N. W. Abdullah and M. E. H. Toriman, “Ciri persekitaran hidrologi dan sedimentasi Sungai Telom, Cameron Highlands,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 2, pp. 161-172, 2011. [4] S. A. A. Rashid, M. B. Gasim, M. E. Toriman,H. Juahir, M. K. A. Kamarudin, A. Azid and N. A. A. Aziz, “Water quality deterioration of Jinjang River, Kuala Lumpur: Urban risk case water pollution,” Arab World Geographer, vol. 4, pp. 349-362, Dec. 2014. [5] M. E. Toriman, M. K. A. Kamarudin, M. Idris, N. R Jamil, M. B.Gasim and N. A. A. Aziz, “Sediment concentration and load analyses at Chini River, Pekan, Pahang Malaysia,” Research Journal of Earth Sciences, vol. 1, pp. 43-50, 2009. [6] M. K. A. Kamarudin, M. Idris and M. E. Toriman, “Analysis of Leptobarbus hoevenii in control environment at natural lakes,” American Journal of Agricultural and Biological Science, vol. 8, pp. 142-148, 2013. [7] Department of Irrigation and Drainage Malaysia. (2009) Rainfall data. [Online].Available:http://jpsweb.terengganu.gov.my/index.php/en/flo od-info/heavy-rain-station. [8] M. E. Toriman, M. K. A. Kamarudin, N. A. A. Aziz, H. M. Din, F. M. Ata, N. M. Abdullah, M. Idris, N. R. Jamil, N. S. A. Rani, M. H. Saad and N. W. Abdullah, “Pengurusan sedimen terhadap sumber air bersepadu: Satu kajian kes di Sungai Chini, Pekan, Pahang,” eBANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 1, pp. 267-283, 2012. [9] T. Felix. Sedimentologi, Selangor, Malaysia: Universiti Kebangsaan Malaysia Publisher, 2000. [10] M. E. Toriman, M. K. A. Kamarudin, M. H. Kamarudin, M. Idris, M. B Gasim and N. R Jamil, “Masalah sedimentasi dan penyelesaiannya melalui kaedah pengurusan persekitaran: Satu kajian kes di Sungai Chini, Pahang,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 3, pp. 1-14, 2008. [11] M. E. Toriman, O. A. Karim, M. Mokhtar, M. B. Gazim and M. P. Abdullah, “Use of InfoWork RS in modeling the impact of urbanisation on sediment yield in Cameron Highlands Malaysia,” Nature and Science, vol. 201, pp. 67-73, Jan. 2010. [12] Ab Rani, N. S., M. E. Toriman, M. Idris, N. R. Jamil and M. K. A. Kamarudin, “Muatan sedimen terampai dan perkaitannya dengan penghasilan muatan sedimen pada musim kering dan hujan di Tasik Chini, Pahang,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 1, pp. 70-83, 2009. [13] M. E. Toriman, F. M. Ata, M. K. A. Kamarudin and M. Idris, “Bedload sediment profile and effect of river bank erosion on river crosssection,” American Journal of Environmental Sciences, vol. 6, pp. 292-300, Jul. 2013. [14] J. Alison, A. J. Reading, R. D. Thompson and A. C. Millington, Humid Tropical Environmental, USA: Blackwell Publishers, 1995. [15] M. E. Toriman, L. Q. Yun, M. K. A. Kamarudin, N. A. A. Aziz, M. Mokhtar, R. Elfithri and K. Bhaktiku. “Applying seasonal climate trends to agricultural production in Tanjung Karang, Malaysia,” American Journal of Agricultural and Biological Sciences, vol. 1, pp. 119-126, Jan. 2014. [16] V. N. Mikhailov, V. I. Kravtsova and D. V. Magritskii, “Specific features of development of the modern Sulak River Delta,” Water Resources, vol. 31, pp. 117-132, Mar. 2004. [17] J. A. Udden, “Mechanical composition of clastic sediments,” Geological Society of America Bulletin, vol. 25, pp. 655-744, Jan. 1914. [18] V. Vipin, A. Kumar, V. Parashar and S. Tomar, “Physical habitat assessment of River Denwa using GIS techniques,” Journal of the Indian Society of Remote Sensing, vol. 13, pp. 127-139, Mar. 2012. [19] R. K. Gallon, J. Fournier, M. R. K. Gallon and T. R. U. E. LazyData, “Package ‘G2Sd’” Progress in Physical Geography, 33, pp. 378-402, Dec. 2015. [20] G. Bussi, P. G. Whitehead, M. J. Bowes, D. S. Read, C. Prudhomme and S. J. Dadson, “Impacts of climate change, land-use change and phosphorus reduction on phytoplankton in the River Thames (UK),” Science of the Total Environment, Feb. 2016. [21] J. P. Brady, G. A. Ayoko, W. N. Martens and A. Goonetilleke, “Development of a hybrid pollution index for heavy metals in marine and estuarine sediments,” Environmental Monitoring and Assessment, vol. 187, pp. 1-14, May 2015. [22] J. Peryer-Fursdon, J. M. Abell, D. Clarke, D. Özkundakci, D. P. Hamilton and L. Pearson, “Spatial variability in sediment phosphorus characteristics along a hydrological gradient upstream of Lake Rotorua, New Zealand,” Environmental Earth Sciences, vol. 73, pp. 1573-1585, Feb. 2015. [23] Y. T. Spychala, D. M. Hodgson, S. S. Flint and N. P. Mountney, “Constraining the sedimentology and stratigraphy of submarine intraslope lobe deposits using exhumed examples from the Karoo Basin, South Africa,” Sedimentary Geology, vol. 322, pp. 67-81, Jun. 2015. [24] M. K. A. Kamarudin, M. E. Toriman, S. A. S. Mastura, M. Idris, N. R. Jamil and M. B. Gasim, “Temporal variability on lowland river sediment properties and yield,” American Journal of Environmental Sciences, vol. 5, pp. 657-663, 2009. [25] C. R. Townsend, The Ecology of Stream and River, London, England: Edward Arnord (Publisher) Limited, 1980. [26] X. Zhang and D. E. Walling, “Characterizing land surface erosion from cesium-137 profiles in lake and reservoir sediments,” Journal of Environmental Quality, vol. 34, pp. 514-523, Mar. 2005. [27] M. B Gasim, M. E. Toriman, M. Idris, P. I. Lun, M. K. A. Kamarudin, N. A. A. Aziz, M. Mokhtar and S. A. S. Mastura, “River flow conditions and dynamic state analysis of Pahang River,” American Journal of Applied Sciences, vol. 10, pp. 42-57, Jan. 2013. |
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| spelling | 14745 https://intelek.unisza.edu.my/intelek/pages/view.php?ref=14745 https://intelek.unisza.edu.my/intelek/pages/search.php?search=!collection407072 Restricted Document Article Journal application/pdf Adobe Acrobat Pro DC 20 Paper Capture Plug-in with ClearScan 8 1.6 Acer acer ACER 2024-08-28 21:59:04 7591-01-FH02-ESERI-16-06914.pdf UniSZA Private Access Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu International Journal on Advance Science Engineering Information Technology The amount of suspended sediment yield and the size of sediment grains an indicator of hydrological cycle, especially in the river. The sediment transportation process is one of the measurements of water resources management. Equilibrium of the river depends on the flow rate of water and by several factors such as frequency of rainfall, climate changes and land use activities that changes then effected to the river flow. Sedimentation problems occur in reservoirs, rivers, lakes, flood plains and offshore. This study was carried out in the upstream area, Lata Berangin, Hulu Keruak, Besut, Terengganu. This study was implemented to prove the sedimentation problem, especially the formation of total suspended sediment (TSS) and the bed sediment grain size. There are three important parameters were quantified in this study such as the distribution of sediment grain size (phi), TSS (mg/L) and the river discharge values (Q) (m³/s). The technique of analysis of primary data obtained which determine the bed sediment grain size according with the procedure of Gerald and Kenneth and the phi (ϕ) value in this study using the scale Udden-Wentworth that included median, mean, standard deviation, skewness, kurtosis and the Gravimetric Method used to analyze the concentration TSS is the Gravimetric Method. From the result, the highest TSS up to 6.0 mg/L which is categorized under the class I, based on the National Water Quality Standard. Overall, the estimated daily-suspended sediment load values up to 1.1649 tonne/day at Station 2. Then, from the statistics for the median, mean, standard deviation, skewness and kurtosis showed that the size of sediment falls between phi -0.30φ to phi -1.00 φ which classified as very coarse and the majority of the sediment texture and a very leptokurtic, leptokurtic texture showed sedimentation production is not so high. Overall, the sedimentation problem in Lata Berangin, Hulu Keruak still in stable level. Most of this upstream area still not developed as land use activities around the river basin. 6 5 757-763 [1] M. K. A. Kamarudin, M. E. Toriman, M. H. Rosli, H. Juahir, N. A. A. Aziz, A. Azid, S. F. M. Zainuddin and W. N. A. Sulaiman, “Analysis of meander evolution studies on effect from land use and climate change at the upstream reach of the Pahang River, Malaysia,” Mitigation and Adaptation Strategies for Global Change, vol. 20, pp. 1319-1334, Dec. 2015. [2] C. A. L. Jackson, A. A Zakaria, H. D. Johnson, Tongkul, F. and P. D. Crevello, “Sedimentology, stratigraphic occurrence and origin of linked debrites in the West Crocker Formation (Oligo-Miocene), Sabah, NW Borneo,” Marine and Petroleum Geology, vol. 10, pp. 122-134, Dec. 2009. [3] N. W. Abdullah and M. E. H. Toriman, “Ciri persekitaran hidrologi dan sedimentasi Sungai Telom, Cameron Highlands,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 2, pp. 161-172, 2011. [4] S. A. A. Rashid, M. B. Gasim, M. E. Toriman,H. Juahir, M. K. A. Kamarudin, A. Azid and N. A. A. Aziz, “Water quality deterioration of Jinjang River, Kuala Lumpur: Urban risk case water pollution,” Arab World Geographer, vol. 4, pp. 349-362, Dec. 2014. [5] M. E. Toriman, M. K. A. Kamarudin, M. Idris, N. R Jamil, M. B.Gasim and N. A. A. Aziz, “Sediment concentration and load analyses at Chini River, Pekan, Pahang Malaysia,” Research Journal of Earth Sciences, vol. 1, pp. 43-50, 2009. [6] M. K. A. Kamarudin, M. Idris and M. E. Toriman, “Analysis of Leptobarbus hoevenii in control environment at natural lakes,” American Journal of Agricultural and Biological Science, vol. 8, pp. 142-148, 2013. [7] Department of Irrigation and Drainage Malaysia. (2009) Rainfall data. [Online].Available:http://jpsweb.terengganu.gov.my/index.php/en/flo od-info/heavy-rain-station. [8] M. E. Toriman, M. K. A. Kamarudin, N. A. A. Aziz, H. M. Din, F. M. Ata, N. M. Abdullah, M. Idris, N. R. Jamil, N. S. A. Rani, M. H. Saad and N. W. Abdullah, “Pengurusan sedimen terhadap sumber air bersepadu: Satu kajian kes di Sungai Chini, Pekan, Pahang,” eBANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 1, pp. 267-283, 2012. [9] T. Felix. Sedimentologi, Selangor, Malaysia: Universiti Kebangsaan Malaysia Publisher, 2000. [10] M. E. Toriman, M. K. A. Kamarudin, M. H. Kamarudin, M. Idris, M. B Gasim and N. R Jamil, “Masalah sedimentasi dan penyelesaiannya melalui kaedah pengurusan persekitaran: Satu kajian kes di Sungai Chini, Pahang,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 3, pp. 1-14, 2008. [11] M. E. Toriman, O. A. Karim, M. Mokhtar, M. B. Gazim and M. P. Abdullah, “Use of InfoWork RS in modeling the impact of urbanisation on sediment yield in Cameron Highlands Malaysia,” Nature and Science, vol. 201, pp. 67-73, Jan. 2010. [12] Ab Rani, N. S., M. E. Toriman, M. Idris, N. R. Jamil and M. K. A. Kamarudin, “Muatan sedimen terampai dan perkaitannya dengan penghasilan muatan sedimen pada musim kering dan hujan di Tasik Chini, Pahang,” e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, vol. 1, pp. 70-83, 2009. [13] M. E. Toriman, F. M. Ata, M. K. A. Kamarudin and M. Idris, “Bedload sediment profile and effect of river bank erosion on river crosssection,” American Journal of Environmental Sciences, vol. 6, pp. 292-300, Jul. 2013. [14] J. Alison, A. J. Reading, R. D. Thompson and A. C. Millington, Humid Tropical Environmental, USA: Blackwell Publishers, 1995. [15] M. E. Toriman, L. Q. Yun, M. K. A. Kamarudin, N. A. A. Aziz, M. Mokhtar, R. Elfithri and K. Bhaktiku. “Applying seasonal climate trends to agricultural production in Tanjung Karang, Malaysia,” American Journal of Agricultural and Biological Sciences, vol. 1, pp. 119-126, Jan. 2014. [16] V. N. Mikhailov, V. I. Kravtsova and D. V. Magritskii, “Specific features of development of the modern Sulak River Delta,” Water Resources, vol. 31, pp. 117-132, Mar. 2004. [17] J. A. Udden, “Mechanical composition of clastic sediments,” Geological Society of America Bulletin, vol. 25, pp. 655-744, Jan. 1914. [18] V. Vipin, A. Kumar, V. Parashar and S. Tomar, “Physical habitat assessment of River Denwa using GIS techniques,” Journal of the Indian Society of Remote Sensing, vol. 13, pp. 127-139, Mar. 2012. [19] R. K. Gallon, J. Fournier, M. R. K. Gallon and T. R. U. E. LazyData, “Package ‘G2Sd’” Progress in Physical Geography, 33, pp. 378-402, Dec. 2015. [20] G. Bussi, P. G. Whitehead, M. J. Bowes, D. S. Read, C. Prudhomme and S. J. Dadson, “Impacts of climate change, land-use change and phosphorus reduction on phytoplankton in the River Thames (UK),” Science of the Total Environment, Feb. 2016. [21] J. P. Brady, G. A. Ayoko, W. N. Martens and A. Goonetilleke, “Development of a hybrid pollution index for heavy metals in marine and estuarine sediments,” Environmental Monitoring and Assessment, vol. 187, pp. 1-14, May 2015. [22] J. Peryer-Fursdon, J. M. Abell, D. Clarke, D. Özkundakci, D. P. Hamilton and L. Pearson, “Spatial variability in sediment phosphorus characteristics along a hydrological gradient upstream of Lake Rotorua, New Zealand,” Environmental Earth Sciences, vol. 73, pp. 1573-1585, Feb. 2015. [23] Y. T. Spychala, D. M. Hodgson, S. S. Flint and N. P. Mountney, “Constraining the sedimentology and stratigraphy of submarine intraslope lobe deposits using exhumed examples from the Karoo Basin, South Africa,” Sedimentary Geology, vol. 322, pp. 67-81, Jun. 2015. [24] M. K. A. Kamarudin, M. E. Toriman, S. A. S. Mastura, M. Idris, N. R. Jamil and M. B. Gasim, “Temporal variability on lowland river sediment properties and yield,” American Journal of Environmental Sciences, vol. 5, pp. 657-663, 2009. [25] C. R. Townsend, The Ecology of Stream and River, London, England: Edward Arnord (Publisher) Limited, 1980. [26] X. Zhang and D. E. Walling, “Characterizing land surface erosion from cesium-137 profiles in lake and reservoir sediments,” Journal of Environmental Quality, vol. 34, pp. 514-523, Mar. 2005. [27] M. B Gasim, M. E. Toriman, M. Idris, P. I. Lun, M. K. A. Kamarudin, N. A. A. Aziz, M. Mokhtar and S. A. S. Mastura, “River flow conditions and dynamic state analysis of Pahang River,” American Journal of Applied Sciences, vol. 10, pp. 42-57, Jan. 2013. |
| spellingShingle | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| summary | The amount of suspended sediment yield and the size of sediment grains an indicator of hydrological cycle, especially in the river. The sediment transportation process is one of the measurements of water resources management. Equilibrium of the river depends on the flow rate of water and by several factors such as frequency of rainfall, climate changes and land use activities that changes then effected to the river flow. Sedimentation problems occur in reservoirs, rivers, lakes, flood plains and offshore. This study was carried out in the upstream area, Lata Berangin, Hulu Keruak, Besut, Terengganu. This study was implemented to prove the sedimentation problem, especially the formation of total suspended sediment (TSS) and the bed sediment grain size. There are three important parameters were quantified in this study such as the distribution of sediment grain size (phi), TSS (mg/L) and the river discharge values (Q) (m³/s). The technique of analysis of primary data obtained which determine the bed sediment grain size according with the procedure of Gerald and Kenneth and the phi (ϕ) value in this study using the scale Udden-Wentworth that included median, mean, standard deviation, skewness, kurtosis and the Gravimetric Method used to analyze the concentration TSS is the Gravimetric Method. From the result, the highest TSS up to 6.0 mg/L which is categorized under the class I, based on the National Water Quality Standard. Overall, the estimated daily-suspended sediment load values up to 1.1649 tonne/day at Station 2. Then, from the statistics for the median, mean, standard deviation, skewness and kurtosis showed that the size of sediment falls between phi -0.30φ to phi -1.00 φ which classified as very coarse and the majority of the sediment texture and a very leptokurtic, leptokurtic texture showed sedimentation production is not so high. Overall, the sedimentation problem in Lata Berangin, Hulu Keruak still in stable level. Most of this upstream area still not developed as land use activities around the river basin. |
| title | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| title_full | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| title_fullStr | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| title_full_unstemmed | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| title_short | Assessment of Total Suspended Sediment and Bed Sediment Grains in Upstream Areas of Lata Berangin, Terengganu |
| title_sort | assessment of total suspended sediment and bed sediment grains in upstream areas of lata berangin, terengganu |