Depletive Water Balance and High Vulnerability Due to Conflicts over Access and Rights

Abstract

Sustainable water supply problem becomes strategic when inelastic demand levels are overhauling maximum available supplies. The situation is more acute when the groundwater recharge area is heavily populated, consist of urban, industrial and agricultural areas and above all have typical karstic morphology and extensive regions of thin or null soil cover. During winter season the infiltrated water mixed with the wastewater leaking from poorly designed cesspits and wastewater overflow from the treatment plants of the adjacent settlements. Currently, most of the recharge area is disturbed due to the ongoing urban development in Beitar Elite and Tzur Hadassah in conjunction with the planned Security Fence (apartheid wall) threatens to extend over ~70% of the aquifer recharge area. Such massive destruction in a small watershed leads to considerable decrease in springs discharge and could completely dry-out the springs at the upper part of the valley. The aim of this research is to improve understanding of the hydrologic processes controlling water quantity and quality of springs discharging small (<1E6 m3/yr) basin in the mountain aquifer.

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Shoqeir, J. (2014) Depletive Water Balance and High Vulnerability Due to Conflicts over Access and Rights. Journal of Water Resource and Protection, 6, 1011-1016. doi: 10.4236/jwarp.2014.611095.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Falkenmark, M. (2013) Growing Water Scarcity in Agriculture: Future Challenge to Global Water Security. Philosophical Transactions of the Royal Society A Mathematical, Physical & Engineering Sciences, 371, 20120410.
[2] Drew, D. and Hotzl, H. (1999) Conservation of Karst Terrains and Karst Water. International Contributions to Hydrogeology (IAH), Balkema, Rotterdam, 322p.
[3] Office for Official Publications of the European Communities (1995) Cost Action 65: Hydrogeological Aspects of Groundwater Protection in Karstic Areas: Final Report. Office for Official Publications of the European Communities, Brussels.
[4] Israel, H.So. (2005) Development and Status of Israel’s Water Resources as of Fall 2004. Hydrological Service of Israel Report from Office of National Infrastructure.
[5] Shoqeir, J. (2014) Tracing Groundwater in Karstic Aquifer: IWRM Components Implications and Challenges. LAP Lambert Academic Publishing, AV Akademikerverlag GmbH & Co. KG., Osnabrück, 264p.
[6] El-Fadel, M., Quba’a, R., El-Hougeiri, N., Hashisho, Z. and Jamali, D. (2001) The Israeli Palestinian Mountain Aquifer: A Case Study in Ground Water Conflict Resolution. Journal of Natural Resources & Life Sciences Education, 30, 50-61.
[7] Qannam, Z. (2003) A Hydrogeological, Hydrochemical and Environmental Study in Wadi Al Arroub Drainage Basin, Inst. für Geologie, South West Bank, Palestine.
[8] Fetter, C.W. (2001) Applied Hydrogeology. Prentice Hall, Upper Saddle River, NJ, xvii, 598p.
[9] Komac, B. (2001) The Karst Springs of the Kanin Massif. Acta Geographica, 41, 12.

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