Sains Malaysiana 40(6)(2011): 537–542
Quantity and Quality of Groundwater in Fractured Metasedimentary Rocks of the West Coast of Peninsular
Malaysia
(Kualiti dan Kuantiti Air Bawah Tanah di batuan Metasedimen Terekah Pantai Barat Semenanjung Malaysia)
Nasiman Sapari*1, Raja Zainariah Raja Azie2 & Hisyam Jusoh1
1Department of Civil
Engineering, Universiti Teknologi PETRONAS
Bandar
Seri Iskandar, 31750, Tronoh,
Perak Darul Ridzuan, Malaysia
2Raja Zainariah Raja Azie
6 Jalan IB 4, Taman Iskandar Bistari
32610,
Perak Darul Ridzuan, Malaysia
Received:
1 April 2010 / Accepted: 29 September 2010
ABSTRACT
Groundwater in fractured metasedimentary rock in Malaysia is a potential source of water for drinking and industrial
uses. Industries including agricultural processing, mineral water bottling,
manufacturing and golf courses pumped the water from the underlying fractured
rocks. Fifty eight tubewells belong to private
companies operating in various places in West Coast of Peninsular Malaysia were
evaluated for their yield and quality of water. Rotary percussion methods were
used for the drilling to a maximum depth of 200 m. The productivity of the wells
and the characteristics of the aquifer were evaluated by pumping test using
both the constant discharge rate and steps drawdown methods. The average yield
of the wells at allowable drawdown of 40 m was found to be 416 m3 per
day. Results from water quality analysis indicated that the water was fresh
with an average total dissolved solids (TDS) concentration of 101 to
150 mg/L. The hardness of the water varies from as low as 13 mg/L to a maximum
of 353 mg/L. On the average, the water was moderately hard with the average
hardness value of 80 mg/L. The water facies of the
groundwater was found to be of calcium-sodium-bicarbonate water.
Keywords: Fractured metasedimentary rock; groundwater productivity; tubewell; water
quality; water supply
ABSTRAK
Air bawah tanah di dalam batuan metasedimen di Malaysia yang terekah adalah sumber air berpotensi untuk air minuman dan kegunaan industri. Industri pertanian, pembotolan mineral
air, pembuatan dan padang-padang golf adalah di antara industri yang mengambil air tersebut daripada batuan terekah. Sebanyak lima puluh lapan telaga tiub kepunyaan syarikat-syarikat swasta yang beroperasi di beberapa tempat di pantai barat Semenanjung Malaysia telah diperiksa tentang penghasilan dan kualiti airnya. Penggerudian dengan kaedah putaran tekanan udara telah digunakan untuk membina telaga sehingga kedalaman maksimum 200 m. Produktiviti telaga tiub dan ciri-ciri akuifernya telah dinilai dengan kaedah ujian pengepaman menggunakan kadar aliran dan surutan berperingkat. Purata pengeluaran air dari telaga-telaga pada surutan 40 m yang dibenarkan ialah 416 m3 sehari. Keputusan daripada analisis kualiti air menunjukkan bahawa air tersebut ialah air tawar dengan purata jumlah kepekatan pepejal-pepejal terlarut sebanyak 101 hingga 150 mg/L. Kekerasan air itu berubah daripada serendah 13 mg/L hingga ke tahap maksimum 353 mg/L. Secara purata,
air tersebut mempunyai kekerasan dengan nilai puratanya adalah 80 mg/L. Fasis air dari sumber batuan metasedimen terekah didapati tergolong dari jenis air kalsium natrium bikarbonat.
Kata kunci: Batuan metasedimen terekah; bekalan air; kualiti air; produktiviti air bawah tanah; telaga tiub
REFERENCES
Ang, N.K. 1994. Hydrologic
Framework and Groundwater Resources Utilisation in
Peninsula Malaysia. Proc. Groundwater Forum. No. 4, Geological Society
of Malaysia, 11th, January: 1.1-1.5.
APHA. 1981. Standard
Methods for the Examination of Water and Wastewater. 15th ed. Washington
D.C.: American Public Health Association.
Bouwer, H. 1979. Groundwater Hydrology. Kogakusha, Japan: McGraw-Hill.
Ellis, D., Bouchard, C. & Lantagne, G. 2000. Removal of iron and manganese from
groundwater by oxidation and microfiltration. Desalination 130: 255-264.
Geological Survey Department
of Malaysia. 1987. Groundwater Resource Study of Seri Gading Area, Johor & Rembau-Tampin-Gemas Ara, Negeri Sembilan: Fourth
Malaysian Plan (1981-1985). Project Report Department of Geological Survey.
Kuala Lumpur
Geological Survey Department
of Malaysia. 1992. Potential of Groundwater Resources in Malaysia and
Recommendation for their Planned Development. Report No. CRU 4/1992.Kuala
Lumpur.
Hall A.J., Boyce, A.J. & Fallick, A.E. 1987. Iron sulphides in metasediments: Isotopic support for a
retrogressive pyrrhotite to pyrite reaction. Chemical
Geology: Isotope Geoscience Section 65(3-4):
305-310.
Herm, J.D. 1970. Study and
Interpretation of the Chemical Characteristics of Natural Water. Second Ed.
U.S. Geol. Survey Water Supply Paper 1473.
Jusoh, A.b., Cheng,W.H., Low,W.M., Ali,
N. & Megat Mohd Noor, M.J. 2005. Study on the removal of iron and manganese
in groundwater by granular activated carbon. Desalination 182: 347-353.
Katsoyiannis, I.A., Zikoudi,
A. & Hug, S.J. 2008. Arsenic removal from groundwaters containing iron, ammonium, manganese and phosphate: A case study from treatment
unit in northern Greece. Desalination 224: 330-339.
Mohamed, A.F., Wan Yaacob, W.Z., Taha, M.R. & Samsudin, A.R. 2009. Groundwater and Soil Vulnerability in
the Langat Basin Malaysia. European Journal of Scientific Research 27(4):
628-635.
Peavy, H.S, Rowe, D.R. & Tchobanoglous, G. 1985. Environmental Engineering. Singapore:
McGraw-Hill.
Sofner, B. 1989. Groundwater
Monitoring and Groundwater Protection in North Kelantan and Perlis, Malaysia.
No. 88.2225-6, Hannover : Fed. Inst. of Geosciences and Natural Resources.
*Corresponding author; email:
nasiman@petronas.com.my
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