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首页> 外文期刊>American Journal of Water Resources >Physico-Chemical Assessment of Water Quality in the Gidan Gulbi Shallow Floodplain Aquifer, Northwestern Nigeria
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Physico-Chemical Assessment of Water Quality in the Gidan Gulbi Shallow Floodplain Aquifer, Northwestern Nigeria

机译:尼日利亚西北地区戴丹峡谷浅洪泛省含水水质水质的理化评价

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Water quality of shallow floodplain aquifers in the Gidan Gulbi Fadama area of Gada, Sokoto State, Nigeria was assessed using water quality pollution indices for both irrigation and domestic use. Drinking water quality was assessed using pollution indices including concentration factor (CF), contamination degree (CD) and heavy metal pollution index (HPI), while irrigation water quality parameters such as sodium adsorption ratio (SAR), magnesium adsorption ratio (MAR), soluble sodium percentage (SSP), Kelly ratio (KR), residual sodium carbonate (RSC), permeability index (PI) and total hardness (TH) were used to evaluate the suitability of the water for irrigation purposes. Five heavy metals (Fe, Zn, Mn, Cr, and Cd) were selected to be assessed alongside other inorganic elements. The CF shows low intensities of contamination for Mn, Cr, and Zn while Fe and Cd have high and very high contamination intensities respectively. The results of CD and HPI indicate moderate to high contamination in the study area. The Fe most likely originates from the surrounding rocks of Taloka Formation, during fluid-rock interaction while the high degree of Cd contamination suggests an anthropogenic source. Given the land use pattern in the study area, the most likely source of the anthropogenic Cd is from pesticides, herbicides and fertilizers utilized for agricultural purposes. The areas with highest intensity of contamination (GW2, GW4 and GW7) are within or proximal to farmlands, consistent with the earlier inferred anthropogenic (agriculture) source for the major heavy metal pollutant (Cd). Furthermore, all of the water in the study area falls within the Ca-Mg/HCO3 type as revealed by the piper diagram and Schoeller plots, moreover, except for the total hardness (with a mean level of 253.13 mg/l), all other irrigation quality parameters suggest that the water is suitable for irrigation.
机译:在尼日利亚的尼日利亚佐丹峡谷富达姆地区浅泛洪叶含水层的水质,以灌溉和国内使用水质污染指数评估。使用污染指数评估饮用水质量,包括浓度因子(CF),污染程度(CD)和重金属污染指数(HPI),而灌溉水质参数如钠吸附率(SAR),镁吸附比(MAR),可溶性钠百分比(SSP),凯利比(KR),残留碳酸钠(RSC),渗透率指数(PI)和总硬度(TH)来评估水进行灌溉目的的适用性。选择五种重金属(Fe,Zn,Mn,Cr和Cd)以与其他无机元素一起评估。 CF显示Mn,Cr和Zn的低强度,而Fe和Cd分别具有高且非常高的污染强度。 CD和HPI的结果表明研究区中度至高污染。在流体岩相互作用期间,该Fe最有可能起源于塔罗帕的周围岩石,而高度的CD污染表明人为源。鉴于研究领域的土地利用模式,人为CD的最可能来源来自农药,除草剂和用于农业目的的肥料。具有最高污染强度(GW2,GW4和GW7)的区域在或近端到耕种,与主要的重金属污染物(CD)的早期推断的人类源(农业)源符合。此外,研究区域中的所有水均落入Ca-mg / hCo3类型,如吹笛式图和斯基勒图,除了总硬度(平均水平为253.13 mg / l)外,所有其他灌溉质量参数表明水适合灌溉。

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