Adsorption isotherms for water vapor, basal spacing, and immersion heats and water desorption heats of Li+, Na+, Mg2+, Ca2+, Cu2+, and Fe3+ montmorillonite are measured at various relative humidities (r.h.). The amount of water adsorbed as a function of r.h. is found to increase gradually, whereas b
β¦ LIBER β¦
Adsorption of water and methanol by organic complexes of montmorillonites
β Scribed by W.H Slabaugh; G.H Kennedy
- Publisher
- Elsevier Science
- Year
- 1963
- Weight
- 306 KB
- Volume
- 18
- Category
- Article
- ISSN
- 0095-8522
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