Systematic comparison of the hydration and dehydration of Na+-, K+-, and NH4+-saturated montmorillonite, nontronite, hectorite, saponite, and Fe-saponite by in situ X-ray diffraction measurements

Author:

Morida Koki,Fukushi Keisuke,Sakuma Hiroshi,Tamura Kenji

Funder

Japan Society for the Promotion of Science

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Water Science and Technology,Soil Science

Reference42 articles.

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2. Mechanism of adsorption and desorption of water vapor by homoionic montmorillonites: 2. The Li+, Na+, K+, Rb+, and Cs+-exchanged Forms;Bérend;Clay Clay Miner.,1995

3. Clay mineral diversity and abundance in sedimentary rocks of Gale crater;Bristow;Mars. Sci. Adv.,2018

4. Controlled-humidity XRD analyses: application to the study of smectite expansion/contraction;Chipera;Adv. X-ray Anal.,1995

5. Authigenic clay minerals from interface reactions of concrete-clay engineered barriers: a new perspective on MG-clays formation in alkaline environments;Cuevas;Minerals,2018

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