Sorption of lead in soil as a function of pH: a study case in México.
Reactions of lead sorption onto soil are largely affected by properties and composition of soil and its solution. In this study, the lead sorption onto regosol eutric soil from Francisco I. Madero, Zacatecas, Mexico is evaluated at different pH values. Soil samples were suspended in lead solutions of 10, 25, 50, 100, 150, 200, 300, and 400 mg/l (as Pb(NO3)2). The pH was adjusted at 2, 3, 4, and 5.5 with nitric acid for each of the lead solution concentrations. In all the cases the ionic strength was I=0.09 M with calcium nitrate. The solid-liquid-ratios were fixed in 1:100 and 1:200 g/ml. The results show that lead sorption increases when pH increases. Experimental isotherms were adjusted by both Langmuir and Freundlich models. The Langmuir affinity parameter, K, indicates that the lead sorption capacity of Francisco I. Madero soils is largely perceptible to pH changes.
Martínez-Villegas
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N
Department of Crop and Soil Sciences, Penn State University, 116 Agricultural Sciences and Industries Building, University Park, PA 16802, USA. nvm102@psu.edu
Flores-Vélez
L Ma
LM
Domínguez
O
O
D000327:Adsorption; D006863:Hydrogen-Ion Concentration; D007854:Lead / Q000737:chemistry*; D008800:Mexico; D008956:Models, Chemical; D012987:Soil / Q000032:analysis*; D013997:Time Factors; D014961:X-Ray Diffraction
D012987:Soil; D007854:Lead