4.7 Article

Phosphorus supply level is more important than wheat variety in safe utilization of cadmium-contaminated calcareous soil

Journal

JOURNAL OF HAZARDOUS MATERIALS
Volume 424, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jhazmat.2021.127224

Keywords

Soil remediation; Trace metals; Nutrient management; Phosphorus; Calcareous soil

Funding

  1. National Key Research and Development Program of China [2018YFC1802905]
  2. National Natural Science Foundation of China [41501337, 41401334]

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Screening and cultivating crop varieties with low Cd accumulation is an effective way to safely utilize slightly contaminated soil. However, the study found that wheat varieties in low-P soil had significantly higher grain Cd concentration than in high-P soil, exceeding safety guidelines. The difference in soil pH, nutrient levels, and Cd speciation between the two soil types influenced the Cd uptake by the plant varieties.
Screening and cultivating crop varieties with low Cd accumulation is an effective way to safely utilize the Cd slightly contaminated soil. The characteristics and mechanism of Cd uptake by 13 wheat varieties in two calcareous soils with similar Cd contamination level but different P supply level were studied. The grain Cd concentration of almost all varieties in low-P soil was significantly higher than that in high-P soil and exceeded the maximum level of 0.2 mg kg-1 recommended by the Codex Alimentarius Commission. The pH value of low-P soil was significantly lower than that of high-P soil by 0.27 units, while leaf [Mn] (proxy for rhizosphere carboxylates) and the activities of soil alkaline phosphatase and phytase were significantly higher than those of high-P soil by 35%, 55%, and 286%, respectively. The exchangeable Cd concentration in low-P soil was 2.93 times higher than that in high-P soil, while the Cd concentration of oxides and organic species was significantly lower than that in high-P soil by 21% and 64%, respectively, collectively increasing soluble Cd concentration in low-P soil by 38%. In low-P calcareous soil, P mobilization induced the change of root-zone microenvironment, resulting in the mobilization of Cd.

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