Size exclusion chromatography of humic substances: Limits, perspectives and prospectives

Citation
M. De Nobili et Y. Chen, Size exclusion chromatography of humic substances: Limits, perspectives and prospectives, SOIL SCI, 164(11), 1999, pp. 825-833
Citations number
39
Categorie Soggetti
Environment/Ecology
Journal title
SOIL SCIENCE
ISSN journal
0038075X → ACNP
Volume
164
Issue
11
Year of publication
1999
Pages
825 - 833
Database
ISI
SICI code
0038-075X(199911)164:11<825:SECOHS>2.0.ZU;2-L
Abstract
The fractionation range of chromatographic media used in size exclusion chr omatography (SEC) depends strongly on the kind of substances eluted, Althou gh the fractionation range reported by the manufacturer for globular protei ns on Sephadex G-200 is 5000 to 250,000 daltons and that for dextrans 1000 to 150,000 daltons, phenolcarboxylic acids (pH = 8, 0.1 mmol/L NaOH) are el uted much earlier than would be predicted based on their molecular weight ( MW). The actual MWs for this group of compounds ranges from 200 to 500 dalt ons, whereas their MWs determined by SEC calibrated with proteins is much h igher (7200-180,000 daltons). Ion exclusion, which is the basis for this be havior, originates from residual ionized groups and limits the possibility of applying SEC to the study of conformational changes of humic substances (HS). A correct selection of experimental conditions enables the use of SEC for various applications such as the study of metal-binding equilibria and fractionation according to molecular size. To determine the MW distributio n of HS, columns should be calibrated with standard humic and fulvic acids with known MWs determined by colligative properties such as vapor pressure osmometry. It should be noted, however, that SEC studies on fractions of HS originating from various soils, result in a series of significantly differ ing calibration curves. The Linearity of the relationship between the distr ibution coefficient (K-av) values and the logarithm of the MWs implies the constancy of partial specific volumes. It also suggests that HS extracted f rom the same soil constitute a homologous series in which the structure of the larger components is formed by the repetition of structurally similar u nits and is, therefore, more regular than previously believed. The experime ntal results obtained by SEC also suggest that in regard to the sensitivity of the technique, charge density differences are small within a certain se ries compared with size differences.