TY - JOUR
T1 - Linear solvation energy relationships regarding sorption and retention properties of hydrophobic organic compounds in soil leaching column chromatography
AU - Xu, Feng
AU - Liang, Xinmiao
AU - Lin, Bingcheng
AU - Su, Fan
AU - Schramm, Karl Werner
AU - Kettrup, Antonius
PY - 2002
Y1 - 2002
N2 - The capacity factors of a series of hydrophobic organic compounds (HOCs) were measured in soil leaching column chromatography (SLCC) on a soil column, and in reversed-phase liquid chromatography on a C18 column with different volumetric fractions (φ) of methanol in methanol-water mixtures. A general equation of linear solvation energy relationships, log(XYZ) = XYZ0 + mVI/100 +π* + bβm + aαm, was applied to analyze capacity factors (k′), soil organic partition coefficients (Koc) and octanol-water partition coefficients (P). The analyses exhibited high accuracy. The chief solute factors that control logKoc, logP, and logK′ (on soil and on C18) are the solute size (VI/100) and hydrogen-bond basicity (βm). Less important solute factors are the dipolarity/polarizability (πr*) and hydrogen-bond acidity (αm). Log k′ on soil and log Koc have similar signs in four fitting coefficients (m, s, b and a) and similar ratios (m:s:b:a), while k′ on C18 and logP have similar signs in coefficients (m, s, b and a) and similar ratios (m:s:b:a). Consequently, log k′ values on C18 have good correlations with logP (r > 0.97), while log k′ values on soil have good correlations with logKoc (r > 0.98). Two Koc estimation methods were developed, one through solute solvatochromic parameters, and the other through correlations with k′ on soil. For HOCs, a linear relationship between logarithmic capacity factor and methanol composition in methanol-water mixtures could also be derived in SLCC.
AB - The capacity factors of a series of hydrophobic organic compounds (HOCs) were measured in soil leaching column chromatography (SLCC) on a soil column, and in reversed-phase liquid chromatography on a C18 column with different volumetric fractions (φ) of methanol in methanol-water mixtures. A general equation of linear solvation energy relationships, log(XYZ) = XYZ0 + mVI/100 +π* + bβm + aαm, was applied to analyze capacity factors (k′), soil organic partition coefficients (Koc) and octanol-water partition coefficients (P). The analyses exhibited high accuracy. The chief solute factors that control logKoc, logP, and logK′ (on soil and on C18) are the solute size (VI/100) and hydrogen-bond basicity (βm). Less important solute factors are the dipolarity/polarizability (πr*) and hydrogen-bond acidity (αm). Log k′ on soil and log Koc have similar signs in four fitting coefficients (m, s, b and a) and similar ratios (m:s:b:a), while k′ on C18 and logP have similar signs in coefficients (m, s, b and a) and similar ratios (m:s:b:a). Consequently, log k′ values on C18 have good correlations with logP (r > 0.97), while log k′ values on soil have good correlations with logKoc (r > 0.98). Two Koc estimation methods were developed, one through solute solvatochromic parameters, and the other through correlations with k′ on soil. For HOCs, a linear relationship between logarithmic capacity factor and methanol composition in methanol-water mixtures could also be derived in SLCC.
KW - Capacity factor
KW - Linear solvation energy relationships
KW - Soil leaching column chromatography
KW - Soil organic partition coefficient
KW - Solvatochromic parameter
UR - http://www.scopus.com/inward/record.url?scp=0035987660&partnerID=8YFLogxK
U2 - 10.1016/S0045-6535(02)00100-5
DO - 10.1016/S0045-6535(02)00100-5
M3 - Article
C2 - 12146634
AN - SCOPUS:0035987660
SN - 0045-6535
VL - 48
SP - 553
EP - 562
JO - Chemosphere
JF - Chemosphere
IS - 5
ER -