Mobility of Sulfate in Forest Soils
Kinetic Modeling
H. M. Selim*,a,
G. R. Gobranb,
X. Guanb and
N. Clarkec
a Agronomy and Environmental Management Dep., Sturgis Hall, Louisiana State Univ., Baton Rouge, LA 70803
b Dep. of Ecology and Environmental Research, Swedish Univ. of Agric. Sciences, Uppsala, Sweden
c Norwegian Forest Research Inst., Høgskoleveien, Norway

View larger version (18K):
[in a new window]
|
Fig. 1. A schematic of the multireaction model for solute reactivity in soils.
|
|

View larger version (26K):
[in a new window]
|
Fig. 2. A schematic of the sequential leaching experiment through 5-cm soil columns from the E, Bs, and BC horizons (FF = forest floor).
|
|

View larger version (19K):
[in a new window]
|
Fig. 3. Experimental and simulated breakthrough results of SO4 effluent concentrations vs. pore volume (BTCs) from the E horizon [column E-I, input SO4 (Co) of 0.005 M]. The simulation is based on best-fit of the data when a linear equilibrium sorption model was assumed.
|
|

View larger version (24K):
[in a new window]
|
Fig. 4. Experimental and simulated (solid and dashed curves) BTCs of SO4 effluent concentrations from the Bs horizon [column Bs-I, input SO4 (Co) of 0.005 M]. Simulations are for a range of Kd values where a linear equilibrium sorption model was assumed.
|
|

View larger version (24K):
[in a new window]
|
Fig. 5. Experimental and simulated (solid and dashed curves) BTCs of SO4 effluent concentrations from the Bs horizon [column Bs-I, input SO4 (Co) of 0.005 M]. Simulations are for a range of n values where a nonlinear equilibrium model was assumed.
|
|

View larger version (22K):
[in a new window]
|
Fig. 6. Experimental and simulated BTCs of SO4 effluent concentrations from the Bs horizon [column Bs-I, input SO4 (Co) of 0.005 M]. Simulations are based on best-fit of the data when a linear equilibrium model (dashed curve) and a nonlinear equilibrium (solid curve) were used.
|
|

View larger version (22K):
[in a new window]
|
Fig. 7. Experimental and simulated BTCs of SO4 effluent concentrations from the Bs horizon [column Bs-I, input SO4 (Co) of 0.005 M]. Simulations are based on best-fit of the data when a kinetic model (dashed curve) and kinetic model with an irreversible reaction (solid curve) were used.
|
|

View larger version (24K):
[in a new window]
|
Fig. 8. Experimental and simulated BTCs of SO4 effluent concentrations from the Bs horizon [column Bs-II, input SO4 (Co) of 0.0005 M]. Simulations are based on best-fit of the data when a linear equilibrium model (dotted curve) and kinetic model (dashed curve) were used. The solid curve is a prediction based on the kinetic model.
|
|

View larger version (24K):
[in a new window]
|
Fig. 9. Experimental and simulated BTCs of SO4 effluent concentrations from the BC horizon [column BC-I, input SO4 (Co) of 0.005 M]. Simulations are based on best-fit of the data when linear equilibrium (dotted curve), nonlinear equilibrium (dashed curve), and kinetic models (solid curve) were used.
|
|

View larger version (21K):
[in a new window]
|
Fig. 10. Experimental and simulated BTCs of SO4 effluent concentrations from the BC horizon [column BC-II, input SO4 (Co) of 0.0005 M]. Calculations are based on the linear equilibrium model in a curve-fitting mode (solid curve) and prediction mode (dashed curve).
|
|

View larger version (21K):
[in a new window]
|
Fig. 11. Experimental and simulated BTCs of SO4 effluent concentrations from the BC horizon [column BC-II, input SO4 (Co) of 0.0005 M]. Calculations are based on the kinetic model in a curve-fitting mode (solid curve) and prediction mode (dashed curve).
|
|
Copyright © 2004 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.