Groundwater In Kelantan
The public water supply in Kelantan is handled by Air Kelantan Sdn. The results show that the ground water of the first top aquifer is fresh with resistivities ranging from 47 Ohm-m to 164 Ohm-m except in an area along the coast where the water is brackish.
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Bulletin of the Geological Society of Malaysia.
Groundwater in kelantan. Northern Kelantan is covered by Quaternary alluvium of marine and fluviatile origin which has a large potential for groundwater sources. Many Kelantanese people use groundwater. Samples of untreated groundwater from 454 drinking water wells provided under Water Supply And Sanitation Programme BAKAS were analyzed between Mac and December 2013.
They normally get their water supply. Groundwater type in Melor Kelantan is considered as unconfined aquifer. In Kelantan groundwater supplies more than 40 of the public water supply of the state.
Kelantan population 1 666 000. Groundwater has been abstracted from shallow and deep aquifers. In 2012 about 160 million liters per day MLD or 40 of the total state water usage came from groundwater sources.
The major potential area for groundwater in Kelantan is the northern Kelantan which is underlain by Quaternary alluvium as shown in Fig22. Full PDF Package Download Full PDF Package. The demand on groundwater for potable use has risen steadily over the last 30 years.
Presently fresh groundwater supply is obtained from 82 numbers of production wells located at 13 well-fields at North Kelantan. Distribution pattern of nitrate and fluoride in shallow domestic groundwater wells in northern parts of kelantan malaysia In Pakistan groundwater is the second largest source of irrigated agriculture because of the arid climatic conditions 12. Salinity study of coastal groundwater aquifers in north Kelantan Malaysia.
Estimation of recharge by whatever method is normally subject to large uncertainties and errors. GROUNDWATER USAGE 10 11 Less than 3 of the present water use in Malaysia is developed from groundwater resources The use of groundwater for domestic purposes is mainly confined to rural and remote areas where there is no piped water supply Exception. No samples positive for Vibrio Cholera were.
Kelantan River basin has been carried out in order to estimate and understand groundwater recharge processes. Made available by US. The maintenance and protection of groundwater ecosystems should.
Thus the suggested location for production well is located at 30 m from the centre line Profile B and at depth of 60 75 m beneath ground surface. There is no piped water supply. Khairul Nizar et al.
PhD thesis University of domestic use. Department of Energy Office of Scientific and Technical Information. This also include h ousehold that use 2 source of water supply from public utilities and also alternative source of water suppl y.
The chemical and isotopic composition of groundwater from 52 sites in the London UK area was determined as part of a project aimed at assessing th. Approximately 75 of the Lower Kelantan Basin population relies on groundwater to meet their daily needs. This alluvium region covers area of about 1500 km2 from total area of Kelantan state of 14922 km2 which is approximately 10 of the State area.
However the rate of aquifer recharge is one of the most difficult factors to measure in the evaluation of ground water resources. Groundwater is the main source of drinking water in the northern Kelantan area of Malaysia Wan et al. In Malaysia especially in Kelantan there are nearly 70 of the populations using groundwater for public and domestic supplies 2.
Groundwater has supported 70 of the water supply at the Lower Kelantan River Basin LKRB since the 1930s and demand for groundwater increases annually. However despite their importance the groundwater resources are under stress of exploitation and contamination. Acknowledgements This research was funded by the National Research Institute of Malaysia NAHRIM.
There were 49 221454 samples positive for Total Coliform 14 65454 positive for Ecoli and 3 13454 positive for Salmonella spp respectively. A short summary of this paper. The people dig private wells and draw water from a shallow aquifer while the Water Supply Department takes the groundwater from 101 130 102i W 102 130 8 lor 102-I 20 L Study area 0 20 J L South China Sea 40 60 80 kilometres -J Scale 101 30 102 100 Fig.
However groundwater is being significantly utilised for public water supply in Kelantan and Perlis. The ground water of the second aquifer generally has resistivity lower than 45 Ohm-m and has been classified as brackish water. 1 A description of the study area.
The groundwater geochemistry of Lower Kelantan Basin was evaluated based on major ions characteristic to determine its suitability for drinking domestic use and irrigation. However a comprehensive study on groundwater recharge estimation has never been reported. Mesozoic granitic and sedimentary or metasedimentary bedrock underlay the alluvium layer which mainly consists of shale sandstone phyllite and slate.
Environ Geosci 13239 The groundwater within the second aquifer in north Noor IM 1979 Prefeasibility study of potential groundwater Kelantan is brackish and therefore it is not suitable for development in Kelantan Malaysia. Groundwater samples from different aquifer layers shallow intermediate and deep were collected and analysed for pH electrical conductivity EC total dissolved solid TDS Ca Mg Na K Cl SO4. The other states which supplement the water supply systems groundwater are Terengganu Pahang Sarawak and Sabah.
The groundwater is naturally recharged by meteoric water and streams that maintain the resource in the aquifers Daud and Roslan 1981. Generally the groundwater of the Lower Kelantan Basin is suitable for drinking domestic and agriculture irrigation use except from intermediate aquifer which located less than 8 km from the coastal area. The groundwater resources of the SgKelantan river basin are the main sources of fresh water and also are vitally needed to supplement surface water sources.
The suggested area is considered as the possible location of potential groundwater zone. Therefore groundwater is one. 37 Full PDFs related to this paper.
In Kelantan groundwater plays a very important role in the public water supply system. INTRODUCTION The people of north Kelantan especially those living in villages use groundwater for domestic purposes. Content in the third aquifer is generally low with values ranging from 2 to 210 mgl and thus the ground water in this aquifer is considered fresh and good for domestic use.
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