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Published online 5 April 2007
Published in Soil Sci Soc Am J 71:703-710 (2007)
DOI: 10.2136/sssaj2006.0206
© 2007 Soil Science Society of America
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Simultaneous Adsorption of Calcium and Sulfate and Its Effect on Their Movement

Rogerio Cichotaa,*, Iris Vogelerb, Nanthi S. Bolanc and Brent E. Clothierd

a Massey Univ., P.O. Box 11222, Palmerston North, Manawatu 4442, New Zealand
b HortResearch, Tennent Dr., Private Bag 11-030, Palmerston North 4442, New Zealand
c Massey Univ., P.O. Box 11222, Palmerston North, Manawatu 4442, New Zealand
d HortResearch, Tennent Dr., Private Bag 11-030, Palmerston North 4442, New Zealand


Figure 1
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Fig. 1. A schematic of the leaching apparatus used in the miscible displacement experiments.

 

Figure 2
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Fig. 2. Observed adsorption isotherms, where S is the adsorbed phase and C is the solution phase, for (a) SO42– and (b) Ca2+ using three different amounts of the counter ion in the added solution. Lines show adjusted Freundlich isotherms without considering ion-pair adsorption (IPA).

 

Figure 3
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Fig. 3. Adsorption isotherms, where S is the adsorbed phase and C is the solution phase, for SO42– and Ca2+, added in equimolar amounts. Dots show observed data, bold lines represent S, and thin lines show the single adsorption component, SS, as estimated using (a and b) the particle governed approach, PGA, or (c and d) solution governed approach, SGA.

 

Figure 4
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Fig. 4. Measured breakthrough curves for (a) SO42– and (b) Ca2+, for the four experimental columns (PV = pore volumes). Columns E1 and E2 leached with CaSO4, E3 leached with K2SO4, and E4 with CaCl2 (see Table 2).

 

Figure 5
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Fig. 5. Measured Cl breakthrough curves for the four experimental columns; also shown is the adjusted model. Concentration is relative to the input solution (PV = pore volumes). Columns E1 and E2 leached with CaSO4, E3 leached with K2SO4, and E4 with CaCl2 (see Table 2).

 

Figure 6
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Fig. 6. Measured (dots) and modeled (lines) breakthrough curves for SO42– and Ca2+ from (a and b) columns E1 and (c and d) E2 (leached with CaSO4). Ion-pair adsorption was described using (a and c) the particle governed approach, PGA, and (b and d) solution governed approach, SGA (PV = pore volumes).

 





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