1946
DOI: 10.1016/0095-8522(46)90013-x
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Some aspects of the electrochemistry of clays

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Cited by 13 publications
(2 citation statements)
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“…T HE effect of gradual addition of alkali on the pH of dilute H-clay suspension has been studied 1 • 2 • Mukherjee and Mitra 1 have shown that kaolinite shows two inflections at pH 7-8 and 8-9.5 in its titration curve {pH-neutralisation curve) whereas montmorillonite manifests only one inflection between pH 7.1-8.8. The reverse character is also observed in some of these minerals 1 • 3 • 4 • This variation has been found to be primarily due to the differences in their surface area and base exchange capacity 4 • Unlike kaolinite and montmorillonite, the pH neutralization curves of illite and muscovite have three inflections 2 ; the first one is at pH 6, that of second at about pH 8 and third one is at above pH 11.…”
Section: Introductionmentioning
confidence: 99%
“…T HE effect of gradual addition of alkali on the pH of dilute H-clay suspension has been studied 1 • 2 • Mukherjee and Mitra 1 have shown that kaolinite shows two inflections at pH 7-8 and 8-9.5 in its titration curve {pH-neutralisation curve) whereas montmorillonite manifests only one inflection between pH 7.1-8.8. The reverse character is also observed in some of these minerals 1 • 3 • 4 • This variation has been found to be primarily due to the differences in their surface area and base exchange capacity 4 • Unlike kaolinite and montmorillonite, the pH neutralization curves of illite and muscovite have three inflections 2 ; the first one is at pH 6, that of second at about pH 8 and third one is at above pH 11.…”
Section: Introductionmentioning
confidence: 99%
“…The Zn retained represents about 20%, 19%, and 40% of the total exchangeable cations for these minerals. Mukherjee and Mitra (1946) have shown that a single cation may be held by a clay mineral with a wide range of bonding energies, and this is fundamentally related to the position on the silica^alumina packet at which the cation is sorbed. Accordingly, there are numerous types of energetically heterogeneous sites on these minerals.…”
Section: Ionic F'orni(s) Of Zincmentioning
confidence: 99%