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巴西半干旱-沿海交界地区流域系统中土壤、水和沉积物样本及河流沉积物相关输运中的钍含量。

Thorium content in soil, water and sediment samples and fluvial sediment-associated transport in a catchment system with a semiarid-coastal interface, Brazil.

机构信息

Agronomy Department, Federal Rural University of Pernambuco (UFRPE), Dom Manuel de Medeiros Street, s/n, Dois Irmãos, Recife, PE, 52171-900, Brazil.

Agronomy Department, Federal University of Piaui (UFPI), Planalto horizonte, Bom Jesus, PI, 64900-000, Brazil.

出版信息

Environ Sci Pollut Res Int. 2019 Nov;26(32):33532-33540. doi: 10.1007/s11356-019-06499-8. Epub 2019 Oct 2.

Abstract

Thorium (Th) is one of the main sources of natural radiation to ecosystems. However, data regarding Th concentrations in rocks, soil, water and sediments are currently scarce. Accordingly, this study aimed to establish background concentrations and quality reference values (QRVs) for Th in the environmentally impacted Ipojuca River catchment in Brazil, where the weathering of granites releases Th into the environment. Additionally, the study aimed to calculate Th fluxes in water, and both bed and suspended sediment. The mean Th concentration in the study catchment soils was 28.6 mg kg. The QRV for Th was estimated to be 21 mg kg and 86.3 Bq kg. Bed and suspended sediment-associated concentrations ranged from 2.8 to 32.9 mg kg. Suspended sediment-associated discharge (3.42 t year) accounted for more than 99% of the total Th flux, while the dissolved phase transport was negligible in comparison. At the downstream cross section in the study catchment, suspended sediment samples exhibited Th concentrations similar to those observed in rivers impacted by mining activities. The discharge of sediment to the ocean from the study area is mainly triggered by soil erosion processes in the hotspot region (middle-inferior course). It is essential to identify Th hotspots before establishing environmental policies regarding human health and environmental protection.

摘要

钍 (Th) 是生态系统中天然辐射的主要来源之一。然而,目前关于岩石、土壤、水和沉积物中钍浓度的数据还很缺乏。因此,本研究旨在为巴西伊波茹卡河集水区建立背景浓度和质量参考值 (QRV),因为这里的花岗岩风化会将钍释放到环境中。此外,本研究还旨在计算水中以及河床和悬浮沉积物中的钍通量。研究流域土壤中钍的平均浓度为 28.6 毫克/千克。钍的 QRV 估计为 21 毫克/千克和 86.3 贝克/千克。河床和悬浮沉积物相关浓度范围为 2.8 至 32.9 毫克/千克。悬浮沉积物相关排放量(3.42 吨/年)占总钍通量的 99%以上,而相比之下,溶解相的传输可以忽略不计。在研究流域的下游断面,悬浮沉积物样品中的钍浓度与受采矿活动影响的河流中观察到的浓度相似。研究区域向海洋输送沉积物主要是由热点地区(中下游)的土壤侵蚀过程引发的。在制定有关人类健康和环境保护的环境政策之前,确定钍热点地区至关重要。

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