Abstract

A soil microcosm experiment was carried out to quantify the transfer of cadmium (Cd) and lead (Pb) in a multi-species soil system (MS·3). Red earth from Jiangxi (S1), fluvo-aquic soil from Henan (S2), fluvo-aquic soil from Beijing (S3), and black soil from Heilongjiang (S4) were used for soil column packing with S1, S3, or S4 as the 20–50 cm layer and S2, which was Cd- and Pb-contaminated, as the top 0–20 cm layer. For each soil combination, four treatments were set up: CK (no wheat and no earthworm), W (only wheat), E (only earthworm), and E + W (earthworm and wheat). The results showed that the coexistence of earthworm with wheat reduced Cd and Pb contents in wheat plants and earthworms, and increased plant biomass, but had no significant effect on the survival rate and mean weight change rate of earthworms. Total Cd and Pb decreased remarkably in the 0–20 cm layer while increased in the 20–50 cm layer, and approximately 32.8%–51.1% of Cd and 0.35%–7.0% of Pb migrated down into the 20–50 cm soil layers from the 0–20 cm soil layers. The migration varied between the treatments from S2 to S1, S2, and S3. In S2–S1 and S2–S4 columns, the amount of Cd migration decreased when the earthworms coexisted with wheat, while in S2–S3 column, there was no significant difference on such amount regardless of the coexistence of earthworms with wheat. Taken together, the results indicated that the migration of Cd and Pb was not only associated with wheat and earthworm, but also depended on soil types.

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