卡诺州kumbotso市sa 'adatu rimi教育学院地下水样本的评估

Sadiq Abdurrahman Abubakar Shawai, Muhammad Sani Nahannu, H. Mukhtar, I. M. Isma'il
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引用次数: 0

摘要

人类活动是通过大气污染、废水排放、农用化学品的使用、土壤侵蚀和土地利用来决定地表水和地下水质量的一个主要因素。这项研究的目的是确定从Kumbotso Kano Sa 'adatu Rimi教育学院收集的水样的物理化学参数,并与世界卫生组织(世卫组织)和尼日利亚饮用水质量标准(NSDWQ)给出的标准进行比较。四个样本从学院内的不同地点收集进行分析。分析的参数有pH、温度、总溶解固体、总悬浮固体、悬浮固体、电导率、碱度、Mg2+、Ca2+、氨、硫酸盐、硝酸盐、亚硝酸盐、浊度、盐度、总硬度、游离二氧化碳、铁和氯化物。结果表明,除A采样点浊度、B、C、D采样点pH浓度和C、D采样点亚硝酸盐浓度外,分析参数均在who和nsdwq推荐的允许范围内。结果还表明,总硬度浓度略高于NSDWQ推荐的最大允许限值(MPL)。本文还建议,为高校管理部门定期监测水质状况提供依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ASSESMENT OF GROUNDWATER SAMPLES FROM SA'ADATU RIMI COLLEGE OF EDUCATION, KUMBOTSO, KANO
Human activities are a major factor determining the quality of surface and groundwater through atmospheric pollution, effluent discharges, use of agricultural chemicals, eroded soil and land use.The purpose of this research was to determine the physicochemical parameters of water samples collected from Sa’adatu Rimi College of Education, Kumbotso Kano and to compare with the standards given by World Health Organization (WHO) and Nigeria Standard for Drinking Water Quality (NSDWQ). Four samples were collected from different locations within the college premises for the analysis. The analyzed parameters are pH, temperature, Total dissolved solids, Total suspended solids, Suspended solid, Electrical conductivity, Alkalinity, Mg2+,Ca2+, ammonia, sulphate,Nitrate, Nitrite,Turbidity, Salinity, Total hardness, free carbon dioxide, Iron and Chloride. The results indicated that all the analyzed parameters are within the permissible limits recommended byWHO and NSDWQwith exception of turbidity level at A sampling station, pH concentration at B, C, and D sampling point and nitriteconcentrations at C and D sampling point. The results also showed that, the concentration of total hardness were slightly above the maximum permissible limit (MPL) recommended by NSDWQ. This paper also recommended that, the college management should provide a basis for the regular monitoring of water quality status.
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CiteScore
1.80
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