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

• 主要な著者: Yuang Guo (著者), Sha Zhang (著者), Williamson Gustave (著者), Hao Liu (著者), Yujia Cai (著者), Yufei Wei (著者), Zheng Chen (著者)
• フォーマット: 図書
• 出版事項: Elsevier, 2024-02-01T00:00:00Z.
• 主題: article
• オンライン･アクセス: Connect to this object online.
• Notes: 2949-9194; 10.1016/j.seh.2023.100057
• Keywords: Moisture gradient; Dry-wet cycle; Soil pH and Eh; Soil redox potential; Water management; Soluble concentrations; Environmental sciences; GE1-350; Public aspects of medicine; RA1-1270
• Source: Soil & Environmental Health, Vol 2, Iss 1, Pp 100057- (2024)

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 are sensitive to moisture-driven changes in soil pH and Eh, which is rarely 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 to 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.