Basalt weathering can lead to heavy metal enrichment in soils, and nickel (Ni) isotopes can served as an effective tracer for this weathering process. Water-dispersible colloids (WDCs) are ubiquitous in soil environments and can facilitate the long-range transport of sorbed pollutants. Here, we analyzed soil colloidal distribution, concentration, morphology and Ni isotopes in soil to understand the potential mobilization of WDC-bound Cr and Ni in basalt-derived paddy soils. Ultrafiltration results showed that on average > 90 % of Cr (4714.0 μg L-1) and Ni (4532.3 μg L-1) in soil solution occurring in colloid-bound form (< 1000 nm). Using AF4-UV-ICP-MS and STEM-EDS, we found that iron (Fe)-organic matter composite minerals colloids are primary carriers of Cr and Ni. Specifically, colloid-bound Cr/Ni were mainly associated with nanoparticles (1-20 nm) and fine colloid (125-350 nm) soil particle size. Notably, high weathering intensity and pH promoted the release of WDCs- Cr and Ni. Soil Ni isotopes shown light δ60Ni composition (-0.17 ‰ ∼ -0.11 ‰), primarily determined by Ni incorporation into Fe-(hydr)oxides. Ni isotopes revealed that Ni in soil and rice originates from parent rocks. These results highlighted the pivotal role of the WDCs mobilizing heavy metals in naturally high background paddy soils.
Keywords: Chromium; Colloid; Field-flow fractionation; High geochemical background; Nickel isotope.
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