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1860797375905267712
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INTELEK Repository
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Online Access
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https://intelek.unisza.edu.my/intelek/pages/search.php?search=!collection407072
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| date |
2015-11-05 10:23:10
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Restricted Document
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12467
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UniSZA
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1. Nasir, M. S. and Camerlengo, A. L. (1997). Response of the ocean mixed layer, off the east coast of Peninsular Malaysia during the northeast and southwest monsoons. Geoacta 22: 134-143. 2. Camerlengo, A. and Ines Demmle, M. (1997). Wind driver circulation of Peninsular Malaysia’s eastern Continetal Shelf. Scientia Marina 61(2): 2003-211. 3. Daryabor, F., Samah A. A. and S.H. Ooi. (2015). Dinamical structure of the sea off the east coast of PeninsularMalaysia. Ocean Dinamic 65: 93-106. 4. O’Brien, T. (1995). Assessment of the impact of saline drainage on key fish species. Banens, R.J. & Lehane, R. 1995 Riverine Environment Research Forum. Eds. Canberra: Murray-Darling Basin Commission. 43-46. 5. Aberle, J. and Smart, G.M., (2003).The influence of roughness structure on flow resistance on steep slopes. Journal of Hydraulic Research 41(3): 259-269. 6. Urish, D. W. and Qanbar, E. K. (1997). Hydraulic evaluation ofground water discharge, Nauset Marsh, Cape Cod National Seashore, Massachusetts. Technical Report NPS/NESO-RNR/NRT 97–07 7. McLean, R. F., Tsyban, A., Burkett, V., Codignott, J. O., Forbes, D. L., Mimura, N., Beamish, R. J., and Ittekkot. V. (2001). Coastal Zones and Marine Ecosystems. In Climate Change 2001: Impacts, Adaptation, and Vulnerability. Contribution of Working Group II to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Edited by James J. McCarthy Osvaldo F. Canziani, Neil A. Leary, David J. Dokken, and Kasey S. White, Cambridge University Press, Cambridge, UK, 343-379. 8. Hull, C. H. J., Thatcher, M. L. And Tortoriello, R.C. (1986). Salinity in the Delaware Estuary. Hull, C.H.J. & Titus,J.G. Greenhouse Effect, Sea Level Rise, and Salinity in the Delaware Estuary. Eds. Washington: Delaware River Basin Commission and US Environmental Protection Agency. p8–18. 9. Li, L., Barry, D. A., Stagnitti, F., Parlange, J. Y. and Jeng, D.S., (2000). Beach water table fluctuations due to spring– neap tides: moving boundary effects. Advances in Water Resources 23(8): 817-824. 10. Hanson, C. (2005). Review of Environment Canterbury’s groundwater quality monitoring programme. Environment Canterbury Report, U05/70. 11. Giménez, E. and Morell, I. (1997). Hydrogeochemical analysis of salinization processes in the coastal aquifer of Oropesa (Castellón, Spain). Environmental Geology 29: 118-131. 12. BERNAMA, (2012). Consultant to Study Erosion Of Sungai Paka Estuary. Bernama Media. 26 February. http://my.news.yahoo.com/consultant-study-erosion-sungai-paka-estuary-115605004.html [5 April 2013] 13. Siti Airunnisa,A. (2010). Consultant To Study Erosion Of Sungai Paka Estuary. Utusan Online. 5 May.http://www.utusan.com.my/utusan/info.asp?y=2010&dt=0505&pub=Utusan_Malaysia&sec=Timur&pg= wt_01.htm [5 April 2013] 14. APHA, (1998). Standard Methods for the Examination of Water and Wastewater. 20th edition. American. Public Health Association, Washington, DC. 15. APHA, (2005). American Public Health Association, American Water Works Association and World Environment Federation. Standard Methods for Examination of Water and Wastewater. 21st Edition. American Public Health Association, Washington DC, USA. 16. HACH, (1997). Hach Portable Turbidimeter Model 2100P Instrument and Procedure Manual, 8-25-94- 6ED,Rev. 5, Hach Company, Loveland, Colorado. 17. Mukhopadhyay, S. K., Biswas, H., De, T. K. and Jana, T. K. (2006). Fluxes of nutrients from the tropical river Hooghly at the land-ocean boundary of Sundarbans, North-east coast of Bay of Bengal, India. Journal of Marine Systems 62: 9-21.
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6773-01-FH02-ESERI-15-04082.jpg
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norman
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oai_dc
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https://intelek.unisza.edu.my/intelek/pages/view.php?ref=12467
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12467 https://intelek.unisza.edu.my/intelek/pages/view.php?ref=12467 https://intelek.unisza.edu.my/intelek/pages/search.php?search=!collection407072 Restricted Document Article Journal image/jpeg inches 96 96 norman 1422 761 47 47 2015-11-05 10:23:10 1422x761 6773-01-FH02-ESERI-15-04082.jpg UniSZA Private Access The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia] Malaysian Journal of Analytical Sciences A study to determine the water quality at seven stations was carried out on the Paka River, Terengganu between two tides. Sampling begins from the estuary of the Paka River, and ended about 14 km from the mouth by a distance 2 km for each station. Sampling was carried out between two tides (high and low tides) and within two variations of time representing the first sampling (wet period) and the second sampling (dries period). Water quality parameters such as temperature, dissolved oxygen, conductivity, salinity, pH and total dissolved solids (TDS) were measured directly in the field using multiparameter the YSI 556. Analysis of sodium, magnesium sulfate was carried out according to the APHA and HACH methods. Determination of primary data and physicochemical characteristics of the River Paka are measured and analyzed for each sampling station. Physicochemical parameters such as temperature, pH, dissolved oxygen, total dissolved solids, salinity, electrical conductivity, sodium, and magnesium sulphate concentration were used to determine its relationship of the movement of tides and other factors that affect water quality. Station 1 shows the highest reading physicochemical parameters than station 7 during the first and second samplings. The higher reading most of physicochemical parameters was also observed during the dry season, this is because the river flow from upstream was decline due to low rainfall intensity. 19 5 Malaysian Society of Analytical Sciences Malaysian Society of Analytical Sciences 979-990 1. Nasir, M. S. and Camerlengo, A. L. (1997). Response of the ocean mixed layer, off the east coast of Peninsular Malaysia during the northeast and southwest monsoons. Geoacta 22: 134-143. 2. Camerlengo, A. and Ines Demmle, M. (1997). Wind driver circulation of Peninsular Malaysia’s eastern Continetal Shelf. Scientia Marina 61(2): 2003-211. 3. Daryabor, F., Samah A. A. and S.H. Ooi. (2015). Dinamical structure of the sea off the east coast of PeninsularMalaysia. Ocean Dinamic 65: 93-106. 4. O’Brien, T. (1995). Assessment of the impact of saline drainage on key fish species. Banens, R.J. & Lehane, R. 1995 Riverine Environment Research Forum. Eds. Canberra: Murray-Darling Basin Commission. 43-46. 5. Aberle, J. and Smart, G.M., (2003).The influence of roughness structure on flow resistance on steep slopes. Journal of Hydraulic Research 41(3): 259-269. 6. Urish, D. W. and Qanbar, E. K. (1997). Hydraulic evaluation ofground water discharge, Nauset Marsh, Cape Cod National Seashore, Massachusetts. Technical Report NPS/NESO-RNR/NRT 97–07 7. McLean, R. F., Tsyban, A., Burkett, V., Codignott, J. O., Forbes, D. L., Mimura, N., Beamish, R. J., and Ittekkot. V. (2001). Coastal Zones and Marine Ecosystems. In Climate Change 2001: Impacts, Adaptation, and Vulnerability. Contribution of Working Group II to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Edited by James J. McCarthy Osvaldo F. Canziani, Neil A. Leary, David J. Dokken, and Kasey S. White, Cambridge University Press, Cambridge, UK, 343-379. 8. Hull, C. H. J., Thatcher, M. L. And Tortoriello, R.C. (1986). Salinity in the Delaware Estuary. Hull, C.H.J. & Titus,J.G. Greenhouse Effect, Sea Level Rise, and Salinity in the Delaware Estuary. Eds. Washington: Delaware River Basin Commission and US Environmental Protection Agency. p8–18. 9. Li, L., Barry, D. A., Stagnitti, F., Parlange, J. Y. and Jeng, D.S., (2000). Beach water table fluctuations due to spring– neap tides: moving boundary effects. Advances in Water Resources 23(8): 817-824. 10. Hanson, C. (2005). Review of Environment Canterbury’s groundwater quality monitoring programme. Environment Canterbury Report, U05/70. 11. Giménez, E. and Morell, I. (1997). Hydrogeochemical analysis of salinization processes in the coastal aquifer of Oropesa (Castellón, Spain). Environmental Geology 29: 118-131. 12. BERNAMA, (2012). Consultant to Study Erosion Of Sungai Paka Estuary. Bernama Media. 26 February. http://my.news.yahoo.com/consultant-study-erosion-sungai-paka-estuary-115605004.html [5 April 2013] 13. Siti Airunnisa,A. (2010). Consultant To Study Erosion Of Sungai Paka Estuary. Utusan Online. 5 May.http://www.utusan.com.my/utusan/info.asp?y=2010&dt=0505&pub=Utusan_Malaysia&sec=Timur&pg= wt_01.htm [5 April 2013] 14. APHA, (1998). Standard Methods for the Examination of Water and Wastewater. 20th edition. American. Public Health Association, Washington, DC. 15. APHA, (2005). American Public Health Association, American Water Works Association and World Environment Federation. Standard Methods for Examination of Water and Wastewater. 21st Edition. American Public Health Association, Washington DC, USA. 16. HACH, (1997). Hach Portable Turbidimeter Model 2100P Instrument and Procedure Manual, 8-25-94- 6ED,Rev. 5, Hach Company, Loveland, Colorado. 17. Mukhopadhyay, S. K., Biswas, H., De, T. K. and Jana, T. K. (2006). Fluxes of nutrients from the tropical river Hooghly at the land-ocean boundary of Sundarbans, North-east coast of Bay of Bengal, India. Journal of Marine Systems 62: 9-21.
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| spellingShingle |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| summary |
A study to determine the water quality at seven stations was carried out on the Paka River, Terengganu between two tides. Sampling begins from the estuary of the Paka River, and ended about 14 km from the mouth by a distance 2 km for each station. Sampling was carried out between two tides (high and low tides) and within two variations of time representing the first sampling (wet period) and the second sampling (dries period). Water quality parameters such as temperature, dissolved oxygen, conductivity, salinity, pH and total dissolved solids (TDS) were measured directly in the field using multiparameter the YSI 556. Analysis of sodium, magnesium sulfate was carried out according to the APHA and HACH methods. Determination of primary data and physicochemical characteristics of the River Paka are measured and analyzed for each sampling station. Physicochemical parameters such as temperature, pH, dissolved oxygen, total dissolved solids, salinity, electrical conductivity, sodium, and magnesium sulphate concentration were used to determine its relationship of the movement of tides and other factors that affect water quality. Station 1 shows the highest reading physicochemical parameters than station 7 during the first and second samplings. The higher reading most of physicochemical parameters was also observed during the dry season, this is because the river flow from upstream was decline due to low rainfall intensity.
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| title |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| title_full |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| title_fullStr |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| title_full_unstemmed |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| title_short |
The influence of tidal activities on water quality of paka river Terengganu, Malaysia [Pengaruh aktiviti pasang surut kepada kualiti air sungai paka Terengganu, Malaysia]
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| title_sort |
influence of tidal activities on water quality of paka river terengganu, malaysia [pengaruh aktiviti pasang surut kepada kualiti air sungai paka terengganu, malaysia]
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