Trace Metal Mobility in Post-mining Soils: An Integrated Risk Assessment

Date Received: Nov 10, 2025

Date Accepted: Mar 10, 2026

Date Published: Jun 30, 2026

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NATURAL RESOURCES AND ENVIRONMENT

How to Cite:

Arne, R., Marlena, B., Fabian, S., Lan, C., & Son, N. (2026). Trace Metal Mobility in Post-mining Soils: An Integrated Risk Assessment. Vietnam Journal of Agricultural Sciences, 9(2), 3010–3018. https://doi.org/10.31817/vjas.2026.9.2.08

Trace Metal Mobility in Post-mining Soils: An Integrated Risk Assessment

Arne Reck (*) 1 , Marlena Bodewein 2 , Fabian Stolpe 1 , Cao Thin Lan 3   , Ngo Thanh Son 4

  • Corresponding author: [email protected]
  • 1 Independent Institute of Environmental Issues, Berlin 10119, German
  • 2 Institute of Geography, University of Cologne, Kölln 50923, Germany
  • 3 Faculty of Agriculture and Forestry, University of Da Lat, Lam Dong Province 670000, Vietnam
  • 4 Faculty of Natural Resources and Environment, Vietnam National University of Agriculture, Hanoi 12400, Vietnam Introduction
  • Keywords

    In situ soil solution sampling, trace metal mobility, soil water balance simulations, HYDRUS 1-D, Lam Dong province

    Abstract


    Trace metal (TM) contamination in post-mining soils represents a long-term environmental risk due to potential leaching into groundwater. This study applied an integrated risk assessment approach—combining sequential extraction, in situ soil solution sampling, and HYDRUS-1D modelling—to evaluate TM behaviour along the soil–groundwater pathway at a recently abandoned bauxite mining site in the Central Highlands of Vietnam, currently used for cassava cultivation. Our results revealed that less than 1% of the total TM concentrations (As, Cu, Zn, Pb) are mobilizable, indicating a negligible risk of groundwater contamination under the current conditions. This low mobility is primarily attributed to strong sorption by Fe- and Al-(hydr)oxides, despite the moderately acidic soil pH (5.3 ± 0.2). With the exception of Pb, the in situ soil solution samples showed consistently higher TM concentrations than predicted by sequential extraction (1.1–4.9-fold higher). This trend suggests that natural complexation with dissolved organic matter and minor redox fluctuations may enhance TM mobility more than estimated by lab experiments under controlled conditions. Simulation of the soil water balance indicated an annual infiltration of 3,654mm, evapotranspiration of 845mm, and seepage of 2,809mm, with TM loads far below admissible regulatory limits. However, continuous monitoring is recommended, as potential changes in pH, organic matter, or precipitation patterns could alter TM solubility and increase leaching risks in the future. These findings demonstrate that total TM concentrations may serve as valid first-order approximation for risk assessments in similar tropical post-mining soils, though site-specific conditions should always be considered.

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