HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Free Full Text (PDF) Free Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Similar articles in Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Wendling, L. A. Articles by Flury, M. Search for Related Content PubMed Articles by Wendling, L. A. Articles by Flury, M. GeoRef GeoRef Citation Agricola Articles by Wendling, L. A. Articles by Flury, M. Related Collections Soil Biochemistry Soil Biology Soil Chemistry Soil Mineralogy

Soil Mineralogy

Rhizosphere Effects on Cesium Fixation Sites of Soil Containing Micaceous Clays

^a USDA-ARS, P.O. Box 646120, Washington State Univ., Pullman, WA 99164-6120
^b Dep. of Crop and Soil Sciences and Center for Multiphase Environmental Research, P.O. Box 646420, Washington State Univ., Pullman, WA 99164-6420
^c Idaho National Lab., P.O. Box 1625, Idaho Falls, ID 83415
^d Los Alamos National Lab., P.O. Box 1633, Los Alamos, NM 87545

^* Corresponding author (lawendling{at}wsu.edu)

Physical and chemical weathering processes in the rhizosphere may lead to the generation of a greater density of Cs-selective frayed edge sites (FES) on rhizosphere soil as compared with bulk soil. This study was undertaken to determine if there are significant differences between bulk and rhizosphere soils from the Idaho National Laboratory (INL) with respect to their ability to bind Cs. The capacity of FES on bulk and rhizosphere soil materials and conditional Cs/K selectivity of FES were determined as a function of both soil type and initial exchanger composition. The FES capacity was significantly higher in untreated, Ca-saturated, and K-saturated rhizosphere soil materials as compared with bulk soil materials. Sorption–desorption isotherms were obtained at Cs concentrations between 5 x 10^–9 and 5 x 10^–6 M. No difference in Cs sorption was observed between bulk and rhizosphere soil materials. The composition of the exchanging solution had the greatest effect on the magnitude of Cs desorption; significantly more Cs was desorbed in the presence of KCl than in either CaCl₂ or a mixed-cation soil solution. In addition, Cs desorption was greater from rhizosphere soil materials relative to bulk soil materials. Cesium selectivity with respect to both Ca and K was significantly suppressed by weathering in the rhizosphere. We conclude that enhanced weathering in the rhizosphere increased the Cs sorption capacity of FES, but also reduced Cs selectivity on these sites. Enhanced Cs desorption from rhizosphere INL soils is likely in the presence of actively growing plants and associated microorganisms.

Abbreviations: AAS, atomic absorption spectrophotometry • FES, frayed edge sites • INL, Idaho National Laboratory • XRD, X-ray diffraction • ^cK_ex^FES, conditional Cs/K selectivity of FES • ^cK_ex, Vanselow conditional exchange coefficient