首页> 外文期刊>American Journal of Water Resources >Physico-Chemical Analysis of Water Quality of Springs in Bafia-Muyuka, North-Eastern Flank of Mount Cameroon (South West Region, Cameroon Volcanic Line)
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Physico-Chemical Analysis of Water Quality of Springs in Bafia-Muyuka, North-Eastern Flank of Mount Cameroon (South West Region, Cameroon Volcanic Line)

机译:喀麦隆山(西南地区,喀麦隆火山线)东北侧巴菲亚-穆尤卡泉水水质的理化分析

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Bafia-Muyuka is situated at the foot of the North Eastern flank of Mount Cameroon. The rock types of this area are mainly basaltic with minerals such as; pyroxene, olivine, plagioclase and opaque minerals. Samples collected from five (5) different springs during the rainy and dry seasons were analysed. The Physico-chemical analysis for both seasons were compared with WHO (2004) standard and were found to fall within the acceptable limit but for the exception of high temperature values in all the spring waters and NH4+ during the rainy season. All the spring waters yielded pH values above 6.5 and were classified as barely acidic to neutral water. Electrical conductivity ranged between 180-302μs/cm. The relative abundance of major ions (mg/l) were as follows; Ca2+> Mg2+> K+> Na+> NH4+ for cations and HCO3 ̄ > Cl ̄ > NO3 ̄ > SO42 ̄> HPO42 ̄ for anions. These results suggested an influence of natural processes mainly from rock weathering. The Piper’s plot showed that, these springs are characterized by the Calcium-Magnesium Bicarbonate facie (Ca-Mg-HCO3 water type). The results indicate that the springs are non-polluted chemically and are fairly portable and suitable for domestic purposes.
机译:巴菲亚-穆尤卡(Bafia-Muyuka)位于喀麦隆山的东北侧脚下。该地区的岩石类型主要是玄武岩,其中包括矿物质。辉石,橄榄石,斜长石和不透明矿物。分析了在雨季和旱季从五(5)个不同的春季采集的样品。将两个季节的理化分析与WHO(2004)标准进行比较,发现其均在可接受的范围内,但所有春季水和雨季中的NH4 +的高温值除外。所有的泉水的pH值均超过6.5,被归类为对中性水几乎没有酸性。电导率在180-302μs/ cm之间。主要离子的相对丰度(mg / l)如下: Ca2 +> Mg2 +> K +> Na +> NH4 +用于阳离子,而HCO3 ̄> Cl ̄> NO3 ̄> SO42 ̄> HPO42 ̄用于阴离子。这些结果表明自然过程的影响主要来自岩石的风化作用。派珀(Piper)的图表明,这些温泉的特征是钙镁碳酸氢盐相(Ca-Mg-HCO3水类型)。结果表明,这些弹簧在化学上没有污染,并且非常便于携带,适合家庭使用。

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