Soil Science Society of America Journal · 1970 · 42 citations · 0 references
AgricultureEarth SciencesSoil SciencesSoil ChemistrySoil MineralogySoil ScienceDiffusion In SolidsHeavy Metal BioaccumulationConcentrationDiffusion Coefficient EstimationDiffusion MeasurementsMicronutrient ImmobilizationNutrient Diffusion In SoilSoil Metal MobilityZinc DistributionZinc Immobilization In Soils
Abstract Self‐diffusion coefficients for Zn and ZnEDTA (zinc ethylenediaminetetraacetic acid) were determined in aqueous solution and in soil. Those in solution were estimated from diffusion measurements in agar‐agar gel and were found to be 8.8 × 10 ‐6 cm 2 sec ‐1 for Zn and 6.8 × 10 ‐6 cm 2 sec ‐1 for ZnEDTA. The apparent diffusion coefficient of Zn in soil increased from 0.36 × 10 ‐9 cm 2 sec ‐1 to 3.0 × 10 ‐9 cm 2 sec ‐1 with addition of 1.53 × 10 ‐8 mole of EDTA/g soil and to 9.0 × 10 ‐9 cm 2 sec ‐1 with addition of 1.53 × 10 ‐8 mole of ZnEDTA/g soil. The true diffusion coefficient D p of Zn in soil was fairly constant at different levels of EDTA, averaging 1.81 × 10 ‐7 cm 2 sec ‐1 . Addition of EDTA to soils increased the diffusion of Zn; this increase was explained by the transformation of the solid phase soil Zn into soluble ZnEDTA complexes, thereby increasing the concentration gradient of total diffusible Zn. Chelating agents were shown to play an important role in overcoming the rate‐limiting steps of solution and diffusion which are largely responsible for the movement of micronutrient cations in soils.