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马来西亚武吉美拉水库表层沉积物中砷的地累积指数和富集因子

Geoaccumulation Index and Enrichment Factor of Arsenic in Surface Sediment of Bukit Merah Reservoir, Malaysia.

作者信息

Abdullah Mohd Ilman Che, Sah Amir Shah Ruddin Md, Haris Hazzeman

机构信息

School of Biological Sciences, Universiti Sains Malaysia, 11800 USM Pulau Pinang, Malaysia.

出版信息

Trop Life Sci Res. 2020 Oct;31(3):109-125. doi: 10.21315/tlsr2020.31.3.8. Epub 2020 Oct 15.

DOI:10.21315/tlsr2020.31.3.8
PMID:33214859
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7652249/
Abstract

An investigation study was conducted in Bukit Merah Reservoir (BMR) for the assessment of arsenic concentration in the surface sediment in 23 sampling stations. The sediment samples were digested and analysed for arsenic using Inductively Coupled Plasma-Optical Emission Spectrometry (ICP-OES). Sediment parameters such as pH (4.42 ± 0.71), redox potential (121.77 ± 42.45 mV), conductivity (205.7 ± 64.07 μS cm) and organic matter (25.35 ± 9.34%) were also examined. The main objectives of this study are to determine the arsenic distribution and concentration and at the same time to assess the enrichment of arsenic using the geoaccumulation index ( ) and enrichment factor (EF). This study shows the total arsenic concentration in the surface sediment of BMR is 4.302 ± 2.43 mg kg and found to be below the threshold value of Canadian Interim Sediment Quality Guidelines (ISQG). High arsenic concentration is recorded near the southern part of the lake where anthropogenic activities are prevalent. Based on , 13% of sampling stations are categorised as moderately polluted, 52.2% as unpolluted to moderately polluted and the rest is categorised as unpolluted. EF shows 78.3% stations are classified as extremely high enrichment and the rest as very high enrichment. This finding provides important information on the status of arsenic contamination in BMR and creating awareness concerning the conservation and management of the reservoir in the future.

摘要

在武吉美拉水库(BMR)开展了一项调查研究,以评估23个采样站表层沉积物中的砷浓度。对沉积物样本进行消解,并使用电感耦合等离子体发射光谱法(ICP - OES)分析砷含量。还检测了沉积物参数,如pH值(4.42±0.71)、氧化还原电位(121.77±42.45毫伏)、电导率(205.7±64.07微西门子/厘米)和有机质(25.35±9.34%)。本研究的主要目的是确定砷的分布和浓度,同时使用地累积指数( )和富集因子(EF)评估砷的富集情况。研究表明,BMR表层沉积物中的总砷浓度为4.302±2.43毫克/千克,低于加拿大临时沉积物质量指南(ISQG)的阈值。在湖泊南部附近记录到高砷浓度,那里人类活动盛行。根据地累积指数,13%的采样站被归类为中度污染,52.2%为未污染至中度污染,其余为未污染。富集因子显示,78.3%的站点被归类为极高富集,其余为非常高富集。这一发现为BMR中砷污染状况提供了重要信息,并提高了未来对水库保护和管理的认识。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/3b58fa4b1eb8/TLSR-31-3-109-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/1542f717162d/TLSR-31-3-109-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/e82695226413/TLSR-31-3-109-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/91fc2380f448/TLSR-31-3-109-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/3b58fa4b1eb8/TLSR-31-3-109-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/1542f717162d/TLSR-31-3-109-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/e82695226413/TLSR-31-3-109-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/91fc2380f448/TLSR-31-3-109-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cc53/7652249/3b58fa4b1eb8/TLSR-31-3-109-g004.jpg

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