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Assessment of the spring water quality in The Shoubak area, Jordan

机译:约旦Shoubak地区的泉水水质评估

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The present study investigates the physical, chemical, and biological characteristics of spring water samples in Shoubak area in the southern Jordan. The samples were collected from May 2004 to May 2005. All samples were analyzed for temperature, conductivity, dissolved oxygen, pH, major cations (Ca~(2+), Mg~(2+), K~+, Na~+), major anions (Cl~-, NO_3~-, HCO_3~-, SO_4~(2-), PO_4~(3-), F~-), and trace metals (Fe~(2+), Al~(3+), Mn~(2+), Cu~(2+), Cr~(3+), Ni~(2+), Zn~(2+), Pb~(2+), Cd~(2+)). Water quality for available springs showed high salinity through long period of contact with rocks. The ion concentrations in the water samples were from dissolution of carbonate rocks and ion exchange processes in clay. The general chemistry of water samples was typically of alkaline earth waters with prevailing bicarbonate chloride. Some springs showed elevated nitrate and sulfate contents which could reflect to percolation from septic tanks, cesspools, and agricultural practices. The infiltration of wastewater from cesspools and septic tanks into ground-water is considered the major source of water pollution. The results showed that there were great variations among the analyzed samples with respect to their physical, chemical and biological parameters, which lie below the maximum permissible levels of the Jordanian and WHO drinking water standards. The results indicate that the trace metals of spring's water of Shoubak area do not generally pose any health or environmental problems. Factor analysis was used to identify the contributers to water quality. The first factor represents major contribution from anthropogenic activities, while the second one represents major contribution from natural processes.
机译:本研究调查了约旦南部Shoubak地区的泉水样品的物理,化学和生物学特性。从2004年5月至2005年5月收集样品。分析所有样品的温度,电导率,溶解氧,pH,主要阳离子(Ca〜(2 +),Mg〜(2 +),K〜+,Na〜+)。 ,主要阴离子(Cl〜-,NO_3〜-,HCO_3〜-,SO_4〜(2-),PO_4〜(3-),F〜-)和痕量金属(Fe〜(2 +),Al〜(3 +),Mn〜(2 +),Cu〜(2 +),Cr〜(3 +),Ni〜(2 +),Zn〜(2 +),Pb〜(2 +),Cd〜(2+) ))。长期接触岩石后,可用温泉的水质显示出较高的盐度。水样品中的离子浓度来自碳酸盐岩石的溶解和粘土中的离子交换过程。水样的一般化学成分通常是碱土水和盛行的碳酸氢盐。一些泉水的硝酸盐和硫酸盐含量升高,可能反映出化粪池,污水池和农业实践的渗漏。来自污水池和化粪池的废水渗入地下水被认为是水污染的主要来源。结果表明,分析样品之间的物理,化学和生物学参数差异很大,低于约旦和世卫组织饮用水标准的最大允许水平。结果表明,Shoubak地区泉水中的微量金属一般不会对健康或环境造成任何影响。因子分析被用来确定水质的贡献者。第一个因素代表人为活动的主要贡献,而第二个因素代表自然过程的主要贡献。

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