Effect of pH on the aggregation of a gray humic acid in colloidal and solid states

被引:110
作者
Alvarez-Puebla, RA [1 ]
Garrido, JJ [1 ]
机构
[1] Univ Publ Navarra, Dept Appl Chem, E-31006 Pamplona, Spain
关键词
humic substance; PCS; FT-IR; gas adsorption; porosity distributions; computational chemistry;
D O I
10.1016/j.chemosphere.2004.10.021
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Gray humic acids have a marked colloidal character, a large number of surface functional groups, and are subject to aggregation phenomena. They are able to complex soluble pollutants, and initiate flocculation processes as a function of environmental conditions. The aim of this work is to study the aggregation of a gray humic acid, which is stable in colloidal dispersion, by means of photon correlation spectroscopy, and molecular modeling. The effect of this aggregation in the solid state is also studied by means of N-2 (to 77 K) and CO2 (to 273 K) adsorption isotherms, as well as FTIR absorption. The variation of the colloid's zeta potential and size, with pH, reflects the ionization of the carboxylic and phenolic acidic groups, and a linear dependence of size on zeta potential. The decrease in the size of the colloids seems to be more affected by the ionization of the phenolic acid groups, than by that of the carboxylic acid groups, which is likely because in the case of the ionized carboxylic groups the humic colloids are still capable of generating H-bonds. In the solid state, aggregation effects are illustrated by a decrease in surface area, and a disappearance of certain micropores, with increasing pH. These features are likely due to an inhibition of aggregation in the colloidal state as a consequence of the increase in charge that results from ionization of the acidic groups, and also to an increased hindrance to H-bond formation, due to the loss of protons during the above-mentioned ionization process. (c) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:659 / 667
页数:9
相关论文
共 43 条
[11]   MOLECULAR-WEIGHT, POLYDISPERSITY, AND SPECTROSCOPIC PROPERTIES OF AQUATIC HUMIC SUBSTANCES [J].
CHIN, YP ;
AIKEN, G ;
OLOUGHLIN, E .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1994, 28 (11) :1853-1858
[12]   Tight metal binding by humic acids and its role in biomineralization [J].
Davies, G ;
Fataftah, A ;
Cherkasskiy, A ;
Ghabbour, EA ;
Radwan, A ;
Jansen, SA ;
Kolla, S ;
Paciolla, MD ;
Sein, LT ;
Buermann, W ;
Balasubramanian, M ;
Budnick, J ;
Xing, BS .
JOURNAL OF THE CHEMICAL SOCIETY-DALTON TRANSACTIONS, 1997, (21) :4047-4060
[13]   The microporous structure of organic and mineral soil materials [J].
de Jonge, H ;
de Jonge, LW ;
Mittelmeijer-Hazeleger, MC .
SOIL SCIENCE, 2000, 165 (02) :99-108
[14]   Adsorption of CO2 and n(2) on soil organic matter: Nature of porosity, surface area, and diffusion mechanisms [J].
deJonge, H ;
MittelmeijerHazeleger, MC .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1996, 30 (02) :408-413
[15]   USE OF N2 VS CO2 IN THE CHARACTERIZATION OF ACTIVATED CARBONS [J].
GARRIDO, J ;
LINARESSOLANO, A ;
MARTINMARTINEZ, JM ;
MOLINASABIO, M ;
RODRIGUEZREINOSO, F ;
TORREGROSA, R .
LANGMUIR, 1987, 3 (01) :76-81
[16]  
Gregg S.J., 1991, ADSORPTION SURFACE A, V2
[17]   Photon correlation spectroscopy investigations of proteins [J].
Gun'ko, VM ;
Klyueva, AV ;
Levchuk, YN ;
Leboda, R .
ADVANCES IN COLLOID AND INTERFACE SCIENCE, 2003, 105 :201-328
[18]   METHOD FOR THE CALCULATION OF EFFECTIVE PORE-SIZE DISTRIBUTION IN MOLECULAR-SIEVE CARBON [J].
HORVATH, G ;
KAWAZOE, K .
JOURNAL OF CHEMICAL ENGINEERING OF JAPAN, 1983, 16 (06) :470-475
[19]   Zeta potential measurements on three clays from Turkey and effects of clays on coal flotation [J].
Hussain, SA ;
Demirci, S ;
Ozbayoglu, G .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1996, 184 (02) :535-541
[20]  
Jensen F., 1999, INTRO COMPUTATIONAL