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Published online 13 September 2006
Published in J Environ Qual 35:1903-1913 (2006)
DOI: 10.2134/jeq2005.0422
© 2006 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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Theoretical Comparison of How Soil Processes Affect Uptake of Metals by Diffusive Gradients in Thinfilms and Plants

N. J. Lehto*, W. Davison, H. Zhang and W. Tych

Environmental Science Department, Lancaster University, Bailrigg, Lancaster, LA1 4YQ


Figure 1
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Fig. 1. Components of the dynamic model of a DGT soil system, (a) DIFS and (b) dynamic plant-soil system.

 

Figure 2
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Fig. 2. Total zinc uptake by DGT ({Delta}g = 0.293 cm and 0.1 cm) compared to Thlaspi arvense and Thlaspi caerulescens, when a high rate of water ingress (10–5 cm s–1) into the root is present, at different initial soil solution concentrations (mol cm–3).

 

Figure 3
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Fig. 3. Dependence of mass per unit area accumulated by DGT in 24 h on diffusion layer thickness. Diffusion layer thicknesses are shown that correspond to the flux deduced from Michaelis-Menten parameters for Zn accumulated by: Thlaspi arvense (shown by the dotted line) and Thlaspi caerulescens (shown by the solid line) (Lasat et al., 1996).

 

Figure 4
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Fig. 4. The change in solution phase Zn concentrations with distance from the DGT device after a 24 h deployment for devices with diffusion layer thicknesses that mimic uptake by T. arvense and T. caerulescens (initial equilibrium concentration of 0.1 nmol cm–3).

 

Figure 5
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Fig. 5. Modeled effect of changing the soil response time on the amount of Zn accumulated by DGT in a 24 h deployment time (diffusion layer thickness of 0.1 cm).

 

Figure 6
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Fig. 6. Effect of solid phase reservoir size, as expressed by Kd, and soil response time, Tc, on concentration of (a) metal in solution and (b) metal in solid phase with distance in the soil. The simulation is for a 24 h deployment time where the diffusion layer is 0.04 cm thick.

 





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