The environmental impact on the hydrogeochemical characterization of the Kurkar aquifer system, Gaza strip, Palestine.

The Gaza strip is suffering groundwater deterioration as a result of high population density where the outflow exceeds inflow by about 20 Mm3/y. This quantity of water is believed to be replaced by deep seawater intrusion and/or upconing of deep brines in the southern areas or by anthropogenic wastewater. Large cones of depression have been formed over the last 40 years within the Gaza, Khan Younis, and Rafah governorates. The salinity increases in the northwestern and the southeastern parts of Gaza Strip. Nitrate and chloride exceed the WHO maximum permissible limits and are considered as the major pollutants of the aquifer, their high concentration values are attributed to agricultural activity and leaked wastewaters as well as the scarcity of the resource. The cluster analysis (Q-mode) classified the data into 5 clusters and 3 independent cases depending upon salinity and nitrate concentrations. The rotated factor analysis identified 3 factors. The AquaChem program clarified that the study area was supersaturated with calcite and dolomite and undersaturated with gypsum and anhydrite minerals. In general, the groundwater was unsuitable for drinking according to their TDS and NO3 contents. The groundwater can be used in permeable soils for irrigation purposes

Groundwater resources assessment using integrated geophysical techniques in the southwestern region of Peninsular Malaysia.

Combined geophysical techniques such as multi-electrode resistivity, induced polarization, and borehole geophysical techniques were carried out on volcano-sedimentary rocks in the north of Gemas as part of the groundwater resource’s investigations. The result identifies four resistivity units: the tuffaceous mudstone, tuffaceous sandstone, the tuff bed, and the shale layer. Two types of aquifer systems in terms of storage were identified within the area: one within a fracture system (tuff), which is the leaky area through which vertical flow of groundwater occurs, and an intergranular property of the sandy material of the aquifer which includes sandstone and tuffaceous sandstone. The result also reveals that the aquifer occupies a surface area of about 3,250,555 m2 with a mean depth of 43.71 m and a net volume of 9.798 × 107 m3. From the approximate volume of the porous zone (28 %) and the total aquifer volume, a usable capacity of (274.339 ± 30.177) × 107 m3 of water in the study area can be deduced. This study provides useful information that can be used to develop a much broader understanding of the nature of groundwater potential in the area and their relationship with the local geology