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Glaeser, R., Fripiat, J. J. (1976) Hydratation des smectites et demixtion des cations Li, Na en fonction de la localisation des substitutions isomorphiques. Clay Minerals, 11 (2) 93-99 doi:10.1180/claymin.1976.011.2.01

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Reference TypeJournal (article/letter/editorial)
TitleHydratation des smectites et demixtion des cations Li, Na en fonction de la localisation des substitutions isomorphiques
JournalClay Minerals
AuthorsGlaeser, R.Author
Fripiat, J. J.Author
Year1976 (June)Volume11
Issue2
PublisherMineralogical Society
DOIdoi:10.1180/claymin.1976.011.2.01Search in ResearchGate
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Mindat Ref. ID562292Long-form Identifiermindat:1:5:562292:8
GUID0
Full ReferenceGlaeser, R., Fripiat, J. J. (1976) Hydratation des smectites et demixtion des cations Li, Na en fonction de la localisation des substitutions isomorphiques. Clay Minerals, 11 (2) 93-99 doi:10.1180/claymin.1976.011.2.01
Plain TextGlaeser, R., Fripiat, J. J. (1976) Hydratation des smectites et demixtion des cations Li, Na en fonction de la localisation des substitutions isomorphiques. Clay Minerals, 11 (2) 93-99 doi:10.1180/claymin.1976.011.2.01
In(1976, June) Clay Minerals Vol. 11 (2) Mineralogical Society

See Also

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Besson, G., Glaeser, R., Tchoubar, C. (1983) Le césium, revelateur de structure des smectites. Clay Minerals, 18 (1) 11-19 doi:10.1180/claymin.1983.018.1.02
Gaultier, J.-P. (1985) Etude de la repartition des cations interfoliaires dans les phlogopites alterees-(Na, Ca) et (Na, K) Clay Minerals, 20 (1) 1-14 doi:10.1180/claymin.1985.020.1.01
Pons, C. H., Rousseaux, F., Tchoubar, D. (1982) Utilisation du rayonnement synchrotron en diffusion aux petits angles pour l'etude du gonflement des smectites: II. Etude de différents systÈmes eau-smectites en fonction de la température. Clay Minerals, 17 (3) 327-338 doi:10.1180/claymin.1982.017.3.05
Pons, C. H., Rousseaux, F., Tchoubar, D. (1981) Utilisation du rayonnement synchrotron en diffusion aux petits angles pour l'Ă©tude du gonflement des smectites: I. Etude du systeme eau-montmorillonite-Na en fonction de la temperature. Clay Minerals, 16 (1) 23-42 doi:10.1180/claymin.1981.016.1.02
Glaeser, R. (1954) Isothermes D'Hydratation Des Montmorillonites Bi-Ionigiues (Na, Ca) Clay Minerals, 2 (12) 188-193 doi:10.1180/claymin.1954.002.12.13
Desprairies, A. (1983) Relation entre le parametre b des smectites et leur contenu en fer et magnesium. Application a l'etude des sediments. Clay Minerals, 18 (2) 165-175 doi:10.1180/claymin.1983.018.2.05
Chassin, P. (1976) Influence de la stereochimie des diols sur la formation des complexes interfoliaires de la montmorillonite calcique. Clay Minerals, 11 (1) 13-22 doi:10.1180/claymin.1976.011.1.03
Chahi, A., Weber, F., Prevot, L., Lucas, J. (1993) L’Utilisation des Resines Echangeuses de Cations (Amberlite IRC-50H) dans la Dispersion et la Purification des Argiles des Roches a Carbonates, Phosphates et Sulfates. Clay Minerals, 28 (4) 585-601 doi:10.1180/claymin.1993.028.4.08
Chassin, P. (1976) Signification de la mesure des surfaces totales des argiles avec l'ethane 1·2 diol. Clay Minerals, 11 (1) 23-29 doi:10.1180/claymin.1976.011.1.04
Alcover, J-F., Gatineau, L. (1980) Facteurs determinant la structure de la couche interlamellaire des vermiculites saturees par des cations divalents. Clay Minerals, 15 (3) 239-248 doi:10.1180/claymin.1980.015.3.04
PĂ©zerat, H. (1954) Influence Des Substitutions Isomorphes Sur Les Parametres De Structure Des Phyllites. Clay Minerals, 2 (12) 156-161 doi:10.1180/claymin.1954.002.12.06
 
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