Southwestern Saudi Arabia is enriched with fractured and highly-weathered igneous and metamorphic rocks that function as the limited aquifer and supply significant quantities of water for household use and agriculture in this area. Twenty-seven groundwater samples were collected from shallow-dug wells and physio-chemically examined. It is displayed that, however the average value of total dissolved solids (792.67 mg/l) is not curiously high, the ionic component moved toward anthropogenic origin of pollution. The water in the area fits SO4–Cl type facies. The aquifer fractured properties and the existence of groundwater at near-surface depths affecting the groundwater hydrochemistry for the investigated area. Decision and policymakers must consider these results to minimize the environmental impact of local pollutants in the region.

沙特阿拉伯西南部充斥着破裂的，高度风化的火成岩和变质岩，这些岩石起有限的含水层的作用，并为该地区的家庭和农业提供大量的水。从浅挖井中收集了27个地下水样品，并进行了物理化学检查。结果表明，总溶解固体的平均值（792.67 mg / l）并不高，离子成分向人为污染源转移。该地区的水适合SO4-Cl型相。研究区的含水层破裂特性和近地表深度地下水的存在影响着地下水的水化学。决策者和决策者必须考虑这些结果，以最大程度地减少该地区当地污染物对环境的影响。