1991•Soil ScienceRequires access

EFFECTS OF AUTOCLAVING ON SURFACE PROPERTIES AND SORPTION OF PHOSPHATE AND ZINC IN PHOSPHATE-TREATED SOILS

R. J. XIE, A. F. MacKenzie

Open publisher page 10 citations

Abstract

Autoclaving, commonly used in soil microbiological studies, may alter soil surface properties and influence subsequent reactions. Adsorption and desorption of added P or Zn and changes in Zn fractions were studied using autoclaved and nonautoclaved soil samples. Changes in surface tension with autoclaving were estimated by fitting the Gibb's surface excess isotherm to P adsorption data. Autoclaving reduced P adsorption but increased P and Zn desorption. Reduced P adsorption or increased P desorption was associated with the decreases in extractable Fe and Al and with increases in cation exchange capacity and surface tension. Autoclaving reduced the rate of gain of surface tension with adsorbed P. Increased surface tension in terms of each mol of adsorbed or desorbed P was greater for coarse- than for finetextured soils, suggesting that energy released for every mol of adsorbed P was greater in coarse- than in fine-textured soils. Increased Zn desorption was a result of reduced specific Zn adsorption, which was associated with autoclaving. Autoclaving was less effective in changing Zn adsorption or Zn fractions in fine than in coarse textured soil. Decreased Zn adsorption by autoclaving may have been due to a balance between increased nonspecific and reduced specific Zn adsorption in that both Zn desorption and KNO3-extractable Zn were increased. In terms of charge, the increased negative charge was consistent with decreases in P adsorption and increases in KNO3-extractable Zn.

About this research paper

What this paper is about

Autoclaving, commonly used in soil microbiological studies, may alter soil surface properties and influence subsequent reactions. Adsorption and desorption of added P or Zn and changes in Zn fractions were studied using autoclaved and nonautoclaved soil samples. Changes in surface tension with autoclaving were estimated by fitting the Gibb's surface excess isotherm to P adsorption data. Autoclaving reduced P adsorption but increased P and Zn desorption. Reduced P adsorption or increased P desorption was associated with the decreases in extractable Fe and Al and with increases in cation exchange capacity and surface tension. Autoclaving reduced the rate of gain of surface tension with adsorbed P. Increased surface tension in terms of each mol of adsorbed or desorbed P was greater for coarse- than for finetextured soils, suggesting that energy released for every mol of adsorbed P was greater in coarse- than in fine-textured soils. Increased Zn desorption was a result of reduced specific Zn adsorption, which was associated with autoclaving. Autoclaving was less effective in changing Zn adsorption or Zn fractions in fine than in coarse textured soil. Decreased Zn adsorption by autoclaving may have been due to a balance between increased nonspecific and reduced specific Zn adsorption in that both Zn desorption and KNO3-extractable Zn were increased. In terms of charge, the increased negative charge was consistent with decreases in P adsorption and increases in KNO3-extractable Zn.

Why it matters

OpenAlex reports 10 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Autoclaving, commonly used in soil microbiological studies, may alter soil surface properties and influence subsequent reactions. Adsorption and desorption of added P or Zn and changes in Zn fractions were studied using autoclaved and nonautoclaved soil samples. Changes in surface tension with autoclaving were estimated by fitting the Gibb's surface excess isotherm to P adsorption data. Autoclaving reduced P adsorption but increased P and Zn desorption. Reduced P adsorption or increased P desorption was associated with the decreases in extractable Fe and Al and with increases in cation exchange capacity and surface tension. Autoclaving reduced the rate of gain of surface tension with adsorbed P. Increased surface tension in terms of each mol of adsorbed or desorbed P was greater for coarse- than for finetextured soils, suggesting that energy released for every mol of adsorbed P was greater in coarse- than in fine-textured soils. Increased Zn desorption was a result of reduced specific Zn adsorption, which was associated with autoclaving. Autoclaving was less effective in changing Zn adsorption or Zn fractions in fine than in coarse textured soil. Decreased Zn adsorption by autoclaving may have been due to a balance between increased nonspecific and reduced specific Zn adsorption in that both Zn desorption and KNO3-extractable Zn were increased. In terms of charge, the increased negative charge was consistent with decreases in P adsorption and increases in KNO3-extractable Zn.

Key concepts: Adsorption, Desorption, Chemistry, Sorption, Soil water, Zinc, Phosphate, Surface tension

Related papers

Back to paper searchBrowse research topicsOriginal source
EFFECTS OF AUTOCLAVING ON SURFACE PROPERTIES AND SORPTION OF PHOSPHATE AND ZINC IN PHOSPHATE-TREATED SOILS — Research Paper | ScholarLens