Institute of Biological and Environmental Sciences, University of Aberdeen, Cruickshank Building, St. Machar Drive, Aberdeen AB24 3UU, United Kingdom; Department of Soil, Water and Environment, University of Dhaka, Dhaka 1000, Bangladesh.
Institute of Biological and Environmental Sciences, University of Aberdeen, Cruickshank Building, St. Machar Drive, Aberdeen AB24 3UU, United Kingdom.
Sci Total Environ. 2018 Jan 15;612:1365-1372. doi: 10.1016/j.scitotenv.2017.09.030. Epub 2017 Sep 25.
Rice plants grown on soils with elevated arsenic have been shown to have increased arsenic content in their grains. To gain a better understanding of the likelihood of high grain arsenic in rice grown in different soils, it is important to understand the factors affecting the bioavailability and mobility of arsenic. Paddy soils from six different physiographic regions of Bangladesh were collected, and diffusive gradients in thin-films (DGT) were used to assess the porewater and solid phase arsenic. While significant differences were identified in total soil arsenic (1.4-9.8mg/kg), porewater arsenic (C) (5.6-64.7μg/l), labile arsenic (C) (6.3-77.6μg/l), and solid phase pool of arsenic (K) (52-1057l/kg), importantly arsenic resupply capacity was not different between the physiographic regions. All soils had a high ratio of DGT to porewater arsenic (~1), this in conjunction with the porewater arsenic values and the high K values suggesting a large solid phase pool of arsenic capable of contributing towards the resupply/transport of the labile pool of arsenic in the soil porewater. This indicates that there is less difference in soil arsenic availability than might be predicted based solely on total soil arsenic content between the physiographic regions.
在砷含量较高的土壤中种植的水稻,其谷物中的砷含量会增加。为了更好地了解在不同土壤中种植的水稻中砷含量较高的可能性,了解影响砷生物利用度和迁移性的因素很重要。采集了孟加拉国六个不同地貌区域的稻田土壤,并使用扩散梯度薄膜(DGT)来评估孔隙水和固相砷。尽管总土壤砷(1.4-9.8mg/kg)、孔隙水砷(C)(5.6-64.7μg/l)、可利用砷(C)(6.3-77.6μg/l)和固相砷库(K)(52-1057l/kg)存在显著差异,但不同地貌区域的砷补给能力并无差异。所有土壤的 DGT 与孔隙水砷之比都很高(~1),这与孔隙水砷值和高 K 值表明,存在大量的固相砷库,能够补充/运输土壤孔隙水中的可利用砷库。这表明,与仅基于总土壤砷含量相比,不同地貌区域之间的土壤砷可利用性差异较小。