Pengki Irawan


Water is a basic human need. The need for clean water is increasing with the increase in population. Increased water demand is not offset by the availability of surface water, where the availability of surface water decreases. Overcoming these problems, groundwater is one solution. Groundwater is below the surface of the ground in the layer of groundwater carrier. The groundwater carrier layer is called an aquifer. Groundwater exploitation must pay attention to the environmental support capacity of groundwater. Carrying capacity of groundwater is influenced by the characteristics of aquifers, these characteristics include conductivity, thickness of aquifers, width of aquifers, rocks that make up aquifers and hydraulic gradients. Based on geoelectric studies, aquifers at the location of the investigation are arranged by the sandy clay layer. Groundwater in the unconfined zones of aquifers and confined zones is composed of sandy clay and clay sand layers with potential for groundwater 86.4 - 432 m3/day, equivalent to 1 - 5 liter/second. The well discharge potential is estimated to be less than 1 liter / second. The potential of deep groundwater potential is 432 m3/day, equivalent to 5 liter/second.

Full Text:

PDF 14-22


Anonim. 2008. Pengukuran Geolistrik Untuk Menunjang Sumur Resapan KLH. Coreewell. Jakarta.

Balek, J. 1989. Groundwater Resource Assessment. Elsevier Science Publishers B.V., Amsterdam

Chow, V.T. 1964. Handbook of Applied Hydrology. Mc Graw Hill, New York

Fetter,. C. W. 1994. Applied Hydrogeology. 3rd ED. Merrill Publishing Company, Ohio

Kodoatie, R.J. 1996. Pengantar Hidrogeologi. Penerbit ANDI. Yogyakarta.

Lee, T.R. 1999. Water Management in the 21st Century. Edward Elgar Publishing: Cheltenham

Loke, M.H and Barker R.D., 1996, Rapid Least-squares Inversion of Apparent. Resistivity Pseudosection by Quasi-Newton Method. Geophysics Prospecting 44,131-152.

Irawan, Pengki. 2012. Potensi Cadangan Airtanah di DAS Ciliwung. Tesis. Sekolah Pascasarjana Institut Pertanian Bogor.

Srijatno,1980, Geofisika Terapan, Departemen fisika ITB, Bandung.

Todd, D. K. 1995. Groundwater Hydrology. Second Edition. John Wiley & Sons, Singapore.

Wagner, J. M., U. Shamir and H. R.Nemati. 1992. Groundwater quality management under urcertainty : stochastic programming approach and the value of Information. Water Resources Research 28 (5) : 1511-1530.


  • There are currently no refbacks.