Humic complexing ability

Pommery, J., Ebenga, J. P., Imbenotte, M., Palavitt, G., and Erb, F. (1988). Determination of the complexing ability of a standard humic acid with cadmium ions. Water Res. 22, 185-189. 

Humic substances, which are biopolymers widely and abundantly present in natural waters and soils, also have a high complexing ability with various heavy metal ions. These compounds are formed by the random condensation of breakdown products of terrestrial and aquatic plants and extracellular metabolites of phytoplankton. Concentrations of metals in marine and fresh waters are often higher than predicted from the solubility products of corresponding hydroxide and carbonate compounds. The complexation of metal ions with dissolved humic substances is responsible for the apparent supersaturation of metals in natural waters [9-21], Water-soluble humic substances are usually divided into two fractions, humic acid (HA) and Mvic acid (FA). HA is defined in operational terms as the fraction of humic substance soluble in alkaline solutions and insoluble in acidic solutions, while FA is the fraction soluble in both alkaline and acidic solutions. A general method for the fractionation of humic substances is illustrated in Fig. 1. HA is easily obtained as a precipitate in acidic solution (pH < 1.5). Although HA appears to be an attractive adsorbent for the recovery of heavy metal ions, there is little information on its practical application as adsorbent. It is difficult to use humic acid as the adsorbent because of its high solubility in water. 

II. METAL COMPLEXING ABILITY OF HUMIC ACID A Acid-Base Properties of Humic Acid... 

Phosphorus (P) is one of the major limiting factors for plant growth in many soils. Plant availability of inorganic phosphorus (Pi) can be limited by formation of sparingly soluble Ca phosphates, particularly in alkaline and calcareous soils by adsorption to Fe- and Al-oxide surfaces in acid soils and by formation of Fe/ Al-P complexes with humic acids (94). Phosphorus deficiency can significantly alter the composition of root exudates in a way that is, at least in some plant species, related to an increased ability for mobilization of sparingly soluble P sources (29,31,71). 

Levashkevich (1968) experimentally studied the ability of specific humic acids in several types of soils to form chelated compounds with ionic forms of iron (Fe " "). It was established that in the reactions of chelate formation Fe203 is bound with humic acids into compounds in which the iron loses the properties of an independent ion, and fulvic acids have higher complexforming capability than humic. The maximum amount of Fe that can be bound with fulvic acids reaches 650-711 mg per 1 g of organic matter, with humic acids, 119-152 mg. Chelated compounds of FcjOj with fulvic acids are considerably mobile, but solution of humate complexes occurs only in alkaline environments (at pH = V.3-7.7). In acid environments these com-... 

To conclude, it is necessary to note that the reaction ability of biogenic silica depends on its structure and solubility, determined by various factors. It has been found that soluble forms of silica could be stabilized by S - 7% of glycerin and catechol. It has been determined that the amorphous part of the biogenic silica of siliceous rocks formed the complex with triethylphosphate and actively reacts with polyphenols (the simple one, catehol and complex ones, humic acids), with formation of ethers. The silicon organic derivatives and complexes formed are inert to hydrolysis. 

Humic and FULVIC acids, along with other organic colloidal materials, are fascinating substances that can have profound environmental consequences. Their abilities to complex radionuclides and toxic metals have been recognized for some time by researchers interested in the migration and mobilization of nuclear and industrial waste at contaminated sites. The micellar properties of humic and fulvic acids also give them the ability to play important roles in the solubilization and transport of hydrophobic pollutants. 

---