2001
DOI: 10.1080/00380768.2001.10408410
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K/Ca and NH4/Ca selectivity of hydroxyaluminum-interlayered vermiculite and montmorillonite: Contribution from regular and frayed edge exchange sites

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Cited by 8 publications
(1 citation statement)
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“…-1 The findings of X-ray diffraction on clay samples indicated that Smectite, Chlorite, Kaolinite, and Illite are the order of clay minerals as shown in table 3. [12] , [24] and [25] reported comparable patterns in the Potassium -Magnesium and Potassium -Sodium exchanges. L-shaped isotherm curves are the most prevalent, figure 2, depicts three pairs of Potassium transfer isotherm curves, each representing a different amount of affinity between the two molecules being examined [26].…”
Section: Resultsmentioning
confidence: 74%
“…-1 The findings of X-ray diffraction on clay samples indicated that Smectite, Chlorite, Kaolinite, and Illite are the order of clay minerals as shown in table 3. [12] , [24] and [25] reported comparable patterns in the Potassium -Magnesium and Potassium -Sodium exchanges. L-shaped isotherm curves are the most prevalent, figure 2, depicts three pairs of Potassium transfer isotherm curves, each representing a different amount of affinity between the two molecules being examined [26].…”
Section: Resultsmentioning
confidence: 74%