Dynamics of cadmium and arsenic at the capillary fringe of paddy soils: A microcosm study based on high-resolution porewater analysis

Yuang Guo , Sha Zhang , Williamson Gustave , Hao Liu , Yujia Cai , Yufei Wei , Zheng Chen
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Abstract

Arsenic (As) and cadmium (Cd) are prevalent in paddy soils, posing potential threats to food safety and public health. The concentrations of soluble ​As and Cd is sensitive to moisture-driven changes in soil pH and Eh, which is barely described at the critical dry-wet interface. Here, tempo-spatial changes of soluble As and Cd were captured by In-situ Porewater Iterative samplers at the capillary fringe that extended from saturated to unsaturated moisture gradient at the millimeter scale (60 ​mm profile in depth) through two episodic dry-wet cycles (55 days in total). The As and Cd concentrations showed less significant fluctuation in second cycle compared to the initial dry-wet cycle. The study also revealed at the capillary fringe profile (20–40 ​mm), the As concentrations increased from 4.6 μg L−1 in unsaturated soils to 13.5 μg L−1 in saturated soils, while Cd decreased from 3.3 to 0.2 μg L−1. This observed correlation was aligned with the vertical changes in soil Eh (+287 to +381 ​mV) and pH (3.42–6.07). This study found a distinct zone characterized by low As and low Cd concentrations, typically situated approximately 10–30 ​mm beneath the capillary fringe. Upon further analysis, it was determined that soil with an Eh of 249 ​mV and a pH of 4.3 potentially serves as an optimal environment for decreasing As and Cd levels in porewater. These findings suggest that it is feasible to reduce As and Cd concentration in the soil by implementing appropriate depth-controlled water management techniques.

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稻田土壤毛细管边缘镉和砷的动态:利用高分辨率孔隙水分析进行的微观世界研究
砷(As)和镉(Cd)在水稻田土壤中普遍存在,对食品安全和公众健康构成潜在威胁。可溶性砷和镉的浓度对湿度驱动的土壤 pH 值和 Eh 值的变化非常敏感,而这在关键的干湿界面上几乎没有描述。在这里,原位孔隙水迭代采样器在毛细管边缘捕捉到了可溶性砷和镉的时空变化,毛细管边缘从饱和湿度梯度延伸到非饱和湿度梯度的毫米尺度(剖面深度为 60 毫米),经历了两个偶发的干湿循环(共 55 天)。与最初的干湿周期相比,第二个周期的砷和镉浓度波动较小。研究还发现,在毛细管边缘剖面(20-40 毫米),砷浓度从非饱和土壤中的 4.6 μg L-1 增加到饱和土壤中的 13.5 μg L-1,而镉浓度则从 3.3 μg L-1 降低到 0.2 μg L-1。观察到的这种相关性与土壤 Eh 值(+287 至 +381 mV)和 pH 值(3.42-6.07)的垂直变化一致。这项研究发现了一个以低砷和低镉浓度为特征的独特区域,通常位于毛细管边缘下约 10-30 毫米处。经过进一步分析,确定土壤的 Eh 值为 249 mV,pH 值为 4.3,这可能是降低孔隙水中砷和镉含量的最佳环境。这些研究结果表明,通过实施适当的深度控制水管理技术,降低土壤中的砷和镉浓度是可行的。
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