Evaluation of some groundwater quality parameters using geostatistics in the urban coastal aquifer of Bosaso plain, Somalia

IF 0.7 Q3 AGRICULTURE, MULTIDISCIPLINARY Journal of Agricultural Sciences Pub Date : 2021-01-18 DOI:10.15832/ANKUTBD.611787
A. Said, R. Yurtal, M. Cetin, Muhammet Said Gölpinar
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引用次数: 4

Abstract

Groundwater is a major drinking water resource in arid coastal regions. The groundwater quality of Bosaso city experienced degradation due to rapid urbanization and industrialization. This study was carried out to delineate the spatial distribution of groundwater quality parameters and evaluate groundwater suitability for drinking and irrigation uses. The groundwater samples were collected from Bosaso Plain to determine the pH, electrical conductivity (EC), total dissolved solids (TDS), and sodium and chloride concentrations. To categorize water quality for irrigation purposes, sodium adsorption ratio (SAR) was calculated. Ordinary kriging procedure was performed in order to map the spatial distribution of groundwater quality parameters. The interpretation of laboratory analysis results revealed that the most of groundwater wells in the study area is unsafe for drinking purposes due to high salinity, except for the central area (Biyo Kulule). In terms of irrigation uses, the minor area may be under the risk of alkalinity or sodium hazard. However, all groundwater supply points are not suitable for irrigation due to the salinization risk and can be only used to irrigate high salt-tolerant crops. The final maps show that the groundwater quality decreases from southeast to the north of the plain. This indicates that the groundwater is probably subjected to the seawater intrusion. In this regard, the implementation of a groundwater monitoring program is necessary to achieve concrete results. Nevertheless, the most suitable groundwater quality is found to be at the central part of the Bosaso plain.
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用地质统计学方法评价索马里博萨索平原城市沿海含水层地下水水质参数
地下水是干旱沿海地区的主要饮用水资源。由于快速的城市化和工业化进程,博萨索市的地下水水质不断恶化。本研究旨在圈定地下水水质参数的空间分布,评价地下水的饮用和灌溉适宜性。采集博萨索平原地下水样品,测定其pH值、电导率、总溶解固形物(TDS)、钠和氯浓度。为了对灌溉水质进行分类,计算了钠吸附比(SAR)。为了绘制地下水水质参数的空间分布,采用了普通克里格法。实验室分析结果解释表明,研究区除中部地区(比约库勒)外,大部分地下水井水含盐量高,不宜饮用。在灌溉用途方面,少数地区可能面临碱化或钠危害的风险。但由于存在盐碱化风险,所有地下水供应点都不适合灌溉,只能用于灌溉高耐盐作物。最终的地图显示,地下水质量从东南向北下降。这表明地下水可能受到了海水的入侵。在这方面,实施地下水监测方案是取得具体成果的必要条件。然而,最适宜的地下水质量是在博萨索平原的中部。
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来源期刊
Journal of Agricultural Sciences
Journal of Agricultural Sciences AGRICULTURE, MULTIDISCIPLINARY-
CiteScore
1.80
自引率
0.00%
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0
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