2004, Ottawa, Canada August 1 - 4, 2004 2004
DOI: 10.13031/2013.16187
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Modeling Phosphorus Transport in Soil and Water

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Cited by 4 publications
(2 citation statements)
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“…The theoretical treatment accepted here differs from the other often used approaches such as the NICA (nonideal competitive adsorption) model ,,, or application of the multicomponent Langmuir (Markham−Benton) equation ,,, N e = N s K L c e 1 + K L c e + K H 10 pH in which the monolayer capacity for metal ions is treated as pH-independent and equal to N s . The influence of pH on the equilibrium adsorption isotherm in our treatment is restricted to the regulation of the monolayer capacity Q value as expressed by eq .…”
Section: Theorymentioning
confidence: 99%
“…The theoretical treatment accepted here differs from the other often used approaches such as the NICA (nonideal competitive adsorption) model ,,, or application of the multicomponent Langmuir (Markham−Benton) equation ,,, N e = N s K L c e 1 + K L c e + K H 10 pH in which the monolayer capacity for metal ions is treated as pH-independent and equal to N s . The influence of pH on the equilibrium adsorption isotherm in our treatment is restricted to the regulation of the monolayer capacity Q value as expressed by eq .…”
Section: Theorymentioning
confidence: 99%
“…Both soils are characterized by a granular structure. Saturated hydraulic conductivity values were obtained from the regional soil quality inventory (MAPAQ 1990) and verified by a physicochemical analysis of soil samples (Abou Nohra 2006). Soil characteristics are presented in Table 1.…”
Section: Site Descriptionmentioning
confidence: 99%