尼日利亚三角洲地区Aluu钻孔地下水和沉积物中有机污染物和铁的GIS分析

Davidson Egirani, Ginikanwa Chidi
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引用次数: 1

摘要

在尼日利亚的这一三角洲地区,人们在饮用地下水后出现高烧和胃肠道疾病的原因尚不清楚。通过GIS对地下水和钻孔沉积物中有机污染物的解释而获得的空间数据提供了铁和有机污染物对阿鲁乌地下水质量影响的基线数据和信息。从Aluu的10个钻孔中采集了45 m深度的10个水和沉积物样本,并分三份进行了分析。选择45米意味着深井中存在含地下水的沉积物。采用粒度分析仪对风干沉积物进行粒度分析。采用美国公共卫生协会方法(APHA)对水样进行化学分析。本研究采用液-液萃取法,以30 mL二氯甲烷(DCM)为萃取剂对样品进行萃取。结果进行了统计验证、空间数据和GIS分析。平均粒度为细砂(2.03)~中砂(4.3),分选差(1.45 ~ 2.1),偏度为近对称(0.02),中峰度为0.5 ~极平峰度为2.09。总烃含量为0.033 ~ 0.88 mg/L,总烃和铁含量分别为1.65 ~ 3.41 mg/L和2.98 mg/L ~ 0.48 mg/L。这些与沉积物和水中结合的污染物的结果超过了世界卫生组织的可接受限度。钻孔沉积物的特征对污染物进入地下水有明显的控制作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
GIS Analysis of Organo-Contaminants and Iron Linked to Groundwater and Sediment at Boreholes in Aluu, Delta Region, Nigeria
The source of high fever and gastrointestinal disorders in humans after groundwater consumption in this part of the delta region in Nigeria is unknown. Spatial data engineered by GIS interpretation of organo-contaminants bound to groundwater and borehole sediment provides baseline data and information on the impact of iron and organo-contaminants on groundwater quality in Aluu. A total of 10 water and sediment samples were collected at a depth of 45 m from 10 boreholes within Aluu and analyzed in triplicate. The choice of 45 m implies the occurrence of sediments bearing groundwater for a deep well. A particle size analyzer was used to perform particle size analyses of the air-dried sediments. The American Public Health Association Method (APHA) was used to perform the chemical analysis of the water samples. Here, a liquid-liquid extraction procedure was conducted on the samples using 30 mL dichloromethane (DCM) as the extraction agent. The results were subjected to statistical validation, spatial data and GIS analysis. The textural characteristics possessed a mean grain size from fine sand (2.03) to medium sand (4.3), poorly sorted of 1.45 to 2.1, skewness of near-symmetrical (0.02), meso-kurtic kurtosis of 0.5 to very platy-kurtic of 2.09. Total petroleum hydrocarbon was 0.033 mg/L to 0.88 mg/L, and total hydrocarbon content and iron were 1.65 mg/L to 3.41 mg/L, and 2.98 mg/L-0.48 mg/L respectively. The results of these contaminants bound to sediments and water were above the acceptable limits of the World Health Organization. The ingress of contaminants into the groundwater was significantly controlled by the characteristics of the borehole sediment.
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