Abstract:The adsorption of Zn by soils which are different in their major cationexchange materials was measured at equilibrium Zn concentrations up to lo-' M in lo-' to l O -' M CaCl,. The results are interpreted on K$;-[Zn],,il plots, where KE; is the selectivity coefficient defined by the equation All natural samples except those containing halloysite exhibited no or very small specific Zn adsorption. AU Ca-saturated samples exhibited specific Zn adsorption dependent oncation-exchange materials. The cationexchange si… Show more
“…The values of K and b constants for pH and ionic strength values are shown in Table 2. [24] Maximum zinc adsorption was always higher in the surface soil than in the subsoil ( Table 2). A good fit of adsorption data by Langmuir and Freundlich equations for soils of the State of Sa˜o Paulo, Brazil, was also observed by others.…”
Ionic strength and pH influence the adsorption of cations due to the variation of the electric charge in soils rich in iron (Fe) and aluminum (Al) oxides and hydroxides. The objective of this study was to investigate the influence of pH and ionic strength on zinc (Zn) sorption in a highly weathered Brazilian soil. The equations of Langmuir and Freundlich were adjusted to describe the adsorption.
ORDER
REPRINTSZinc adsorption increased with the elevation of the pH and with the decrease of the ionic strength. The pH effect, however, surpassed the effect of the ionic strength. The largest variation of adsorption with pH suggests the presence of high-affinity adsorption sites. Langmuir and Freundlich equations were well fitted to zinc adsorption at all pH and ionic strength values. At all ionic strength and pH values, maximum adsorption in the surface layer, with negative balance of charge, was higher than in the subsoil, wherein the zero point of salt effect was higher than the soil pH in CaCl 2 .
“…The values of K and b constants for pH and ionic strength values are shown in Table 2. [24] Maximum zinc adsorption was always higher in the surface soil than in the subsoil ( Table 2). A good fit of adsorption data by Langmuir and Freundlich equations for soils of the State of Sa˜o Paulo, Brazil, was also observed by others.…”
Ionic strength and pH influence the adsorption of cations due to the variation of the electric charge in soils rich in iron (Fe) and aluminum (Al) oxides and hydroxides. The objective of this study was to investigate the influence of pH and ionic strength on zinc (Zn) sorption in a highly weathered Brazilian soil. The equations of Langmuir and Freundlich were adjusted to describe the adsorption.
ORDER
REPRINTSZinc adsorption increased with the elevation of the pH and with the decrease of the ionic strength. The pH effect, however, surpassed the effect of the ionic strength. The largest variation of adsorption with pH suggests the presence of high-affinity adsorption sites. Langmuir and Freundlich equations were well fitted to zinc adsorption at all pH and ionic strength values. At all ionic strength and pH values, maximum adsorption in the surface layer, with negative balance of charge, was higher than in the subsoil, wherein the zero point of salt effect was higher than the soil pH in CaCl 2 .
“…It is considered that Zn is adsorbed at first on sites with "higher selectivity" and then on sites with "lower selectivity." The proportion of "high" and "low" selectivity sites differ from clay to clay, and their differences broadly parallel those between the soils containing these clays as major cation-exchange materials (Wada and Abd-Elfattah, 1979). However, some soils tend to adsorb Zn more q I000 I , The K~vs.…”
Section: Resultsmentioning
confidence: 99%
“…In an earlier study (Wada and Abd-Elfattah, 1979) on Zn adsorption by soils which differ in their major cation-exchange materials, halloysite was found to be a very selective adsorbent for Zn. Halloysite and kaolinite are widespread products of hydrothermal alteration and weathering and are common constituents of soils and sediments.…”
Abstract--Zn-and Ca-adsorption equilibria of five Ca-saturated halloysite samples were measured at equilibrium Zn concentrations up to 10 -2 M in 10 4 to 10 -z M CaCI2. The results were interpreted on K zn vs.[Zn]/CEC (%) plots, where KZ~ is the selectivity coefficient (= [Zn][Ca]/ [Ca][Zn]), Zn and Ca represent the adsorbed species, and CEC is the cation-exchange capacity. All Zn adsorption occurred at cationexchange sites, and 0.77 to 36.0 meq Zn/100 g clay, which constitutes 9 to 83% of the CEC, was adsorbed with "high selectivities" (KZ~ > 10). The higher values were found for two spherical and one "filmy" halloysites, whereas the lower values were found for two tubular halloysites. The magnitude of their 001 intensity, hydration in interlayer space, CEC, and "free" iron oxide content did not correlate with the selective Zn adsorption, but a good correlation was found between the proportion of "high selectivity" sites for Zn and proportion of "high affinity" sites for H +. The adsorption of Zn at the "high selectivity" sites was not completely reversible, and KZ~, values > 1000 were recorded in 0.5 M CaC12 for Zn which occupied 10-40% of the exchange sites. Selective Zn adsorption decreased with decreasing pH, and all adsorbed Zn was extracted with 0.1 M HC1.
“…For example, weakly bound outer-sphere adsorption complex are more rapidly exchangeable than more strongly bound inner-sphere adsorption complexes. This explains socalled specific adsortpion, which suggests alumina can adsorb heavy metal ions 1,000 to 10,000 times more readily than alkaline or alkaline earth metal ions (Wada & Abd-Elfattah, 1979).…”
Section: Adsorption Of Heavy Metal Ions Onto Aluminamentioning
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