Determining completion of excess salt removal from clays. Method comparisons

E. J. Mekonnen, Ed Nater, D. A. Laird

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1 Scopus citations

Abstract

Three methods of determining the extent of excess salt removal during alcohol washing of clays were compared. Clays (<2 μm) separated from Wyoming bentonite, halloysite, and a Fargo soil (One, montmorillonitic, frigid Vertic Haplaquoll) were saturated with 0.5 M CaCl2 or 1.0 M KCl. Excess salts were removed by eight consecutive washes with 95% ethanol. Vortex and ultrasonication mixing methods were also compared. After centrifugation, the supernatants were analyzed for excess salt by (i) the AgNO3-Cl test, and by measuring (ii) electrical conductivity, and (iii) elemental concentrations. Elemental concentration and conductivity measurements indicated that substantial amounts of excess Ca and K (approximately 5 to 10% of CEC) remained in the clays when the AgNO3-Cl test was first negative. Ultrasonication reduced the number of washings required to remove excess salt from clays when compared with vortex mixing. The results demonstrate that electrical conductivity is a rapid and reliable method of determining completion of excess salt removal.

Original languageEnglish (US)
Pages (from-to)874-877
Number of pages4
JournalSoil Science Society of America Journal
Volume57
Issue number3
DOIs
StatePublished - Jan 1 1993

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