TY - JOUR
T1 - Dynamics of cadmium and arsenic at the capillary fringe of paddy soils
T2 - A microcosm study based on high-resolution porewater analysis
AU - Guo, Yuang
AU - Zhang, Sha
AU - Gustave, Williamson
AU - Liu, Hao
AU - Cai, Yujia
AU - Wei, Yufei
AU - Chen, Zheng
N1 - Publisher Copyright:
© 2024 The Authors
PY - 2024/2
Y1 - 2024/2
N2 - 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.
AB - 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.
KW - Dry-wet cycle
KW - Moisture gradient
KW - Saturated soils
KW - Soil pH and Eh
KW - Soil redox potential
KW - Soluble concentrations
KW - Unsaturated soils
KW - Water management
UR - http://www.scopus.com/inward/record.url?scp=85182876316&partnerID=8YFLogxK
U2 - 10.1016/j.seh.2023.100057
DO - 10.1016/j.seh.2023.100057
M3 - Article
AN - SCOPUS:85182876316
SN - 2949-9194
VL - 2
JO - Soil and Environmental Health
JF - Soil and Environmental Health
IS - 1
M1 - 100057
ER -