The effect of temperature on tight metal binding by peat and soil derived solid humic acids

被引:17
作者
Ghabbour, EA [1 ]
Davies, G
Ghali, NK
Mulligan, MD
机构
[1] Northeastern Univ, Barnett Inst, Boston, MA 02115 USA
[2] Northeastern Univ, Dept Chem, Boston, MA 02115 USA
关键词
humic acids; metal binding; isotherms; thermodynamics;
D O I
10.4141/S00-065
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The brown biomaterials called humic acids (HA) in pears and soils retain water and bind metal cations and other solutes. Studies of the interactions of purified solid peat and soil-derived HA from different countries with metal cations in water probe HA microstructures and help to characterize the metal binding sites. Labile cations such as Ca-aq(2+), Co-aq(2+), Cu-aq(2+), Fe-aq(3+), Mg-aq(2+) and Mn-aq(2+) tightly bind to solid HAs in sequential steps. The isotherms A vs. c are well fitted with the Langmuir model and plots of 1/A vs. 1/c are linear for each step. Here, A is mmol bound metal g(-1) HA and c is the equilibrium cation concentration (M). This paper compares the stoichiometric site capacities v(i) and equilibrium constants K-i for tight binding of Ca-aq(2+), Co-aq(2+), Cu-aq(2+), Fe-aq(3+), Mg-aq(2+) and Mn-aq(2+) at different solid HA sites. Measurements Measurements at different temperatures give linearly correlated metal binding enthalpy and entropy changes, indicating that conformational changes and cation/HA hydration/dehydration are important factors in metal binding and release by solid HAs.
引用
收藏
页码:331 / 336
页数:6
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