Institute of Nuclear Science & Technology, Bangladesh Atomic Energy Commission, Savar, Dhaka, 1349, Bangladesh.
Institute of Nuclear Science & Technology, Bangladesh Atomic Energy Commission, Savar, Dhaka, 1349, Bangladesh; Department of Environmental Science, Bangladesh University of Professionals (BUP), Mirpur-12, Cantonment, Dhaka, 1216, Bangladesh.
Chemosphere. 2023 Oct;339:139733. doi: 10.1016/j.chemosphere.2023.139733. Epub 2023 Aug 4.
This study utilized surface sediments from a potentially less polluted transboundary Himalayan River (Brahmaputra: China-India-Bangladesh) to investigate the abundance of 15 geochemically and ecologically significant elements and to predict their sources and ecological consequences. INAA was applied to determine the elemental concentrations. The average abundances (μg.g) of Rb (94.20), Cs (4.49), Th (20.31), & U (2.73) were 1.12-2.26 folds elevated than shale. Environmental indices disclosed a pollution status ranging from "uncontaminated to moderately contaminated," with minimal Rb, U, and Th enrichment in the downstream zone. Consensus-based sediment quality guideline (SQG) threshold values suggested that only Cr (60% samples > TEL) may impose rare biological effects. Ecological risk indices suggested "minor to no" possible eco-toxicological risks for the accounted elements (Cr, Co, Mn, Zn, Sb, & As). The positive matrix factorization (PMF) model predicated the predominance of geogenic or crustal contributions (∼72.69%) for Al, K, Na, Ti, Co, Zn, Ba, Cs, As, Rb, Th, & U derived from elemental fractionations, mineral weathering, and bio-geo-chemical mobilization. The relative contributions of anthropogenic sources (∼27.31%; such as the construction of roads, settlement expansion, litter disposal, municipal waste discharge, mining activities, agricultural encroachment, etc.) on elemental distribution were significantly lower. The abundance of Cr and Mn was mainly influenced by anthropogenic sources. This study demonstrated the effectiveness of utilizing geo-environmental guidelines and receptor models in discriminating the natural & anthropogenic origins of metals in the complex riverine sediments of a less anthropogenically affected river.
本研究利用源自一条潜在污染较少的跨界喜马拉雅河流(雅鲁藏布江:中国-印度-孟加拉国)的表层沉积物,调查了 15 种地球化学和生态意义重大的元素的丰度,并预测了它们的来源和生态后果。应用 INAA 测定元素浓度。Rb(94.20)、Cs(4.49)、Th(20.31)和 U(2.73)的平均丰度(μg.g)比页岩高 1.12-2.26 倍。环境指数揭示了污染状况,范围从“无污染到中度污染”,下游区仅存在 Rb、U 和 Th 的轻微富集。基于共识的沉积物质量指导值(SQG)阈值表明,只有 Cr(60%的样品> TEL)可能会产生罕见的生物效应。生态风险指数表明,对于所考虑的元素(Cr、Co、Mn、Zn、Sb 和 As),可能存在“轻微到无”的生态毒性风险。正矩阵因子分解(PMF)模型预测,源自元素分馏、矿物风化和生物地球化学迁移的地球成因或地壳来源(约 72.69%)对 Al、K、Na、Ti、Co、Zn、Ba、Cs、As、Rb、Th 和 U 的主导作用。人为来源(约 27.31%;如道路建设、居住点扩张、垃圾处理、城市废物排放、采矿活动、农业侵占等)对元素分布的相对贡献要低得多。Cr 和 Mn 的丰度主要受人为源的影响。本研究表明,利用地球环境准则和受体模型可以有效地区分受人为影响较小的河流复杂河流水体沉积物中金属的自然和人为来源。