Clay Minerals Society

Interface and its Rheological Implications, Clay Minerals Society, Boulder, CO, USA (1992). 

Perez-Castells, R., Alvarez, A., Gavilanes, J., Lizarbe, M.A., Martinez del Pozo, A., Olmo, N. and Santaren, J. (1987) (eds L.G. Schultz H.vanOlphen, F.A. Mumpton ), Proceedings of the International Clay Conference, Denver, 1985, The Clay Mineral Society, Bloomington, 359—362. 

Darder, M. and Ruiz-Hitzky E. (2007) in Clay-Based Polymer Nanocomposite, Clay Minerals Society, Vol. 14... 

Boyd SA, Jaynes WF (1994) Role of layer charge in organic contaminant sorption by organo-clays. In Mermut AR (ed) Layer charge characteristics of 2 1 silicate clay minerals. CMS Workshop Lecture Series, vol 6, The Clay Minerals Society, Boulder, CO, pp 48-77... 

Madejova J, Komadel P. Baseline studies of the clay minerals society source clays infrared methods. Clays Clay Miner. 2001 49 410-432. 

Figure 2. Calculated variation of AG° (Na Cs) (kJ mol ) with the equivalent anionic radius (A) at different interlayer molalities (35). Data of Maes and Cremers (17) are also shown. (Figure supplied by D.D. Eberl). Reproduced with permission from Ref. 35. Copyright 1980, The Clay Minerals Society.

Berteau montmorillonite subjected to 2 (i), 5 ( ) and 10 ( ) wetting-drying cycles (101). Jurves re a simulation. Table VI shows these data for the (Ca - Cs ) equilibrium. Reproduced with permission from Ref. 101. Copyright 1985, The Clay Minerals Society. 

Reproduced with permission from Ref. 101. Copyright 1985 Clay Minerals Society. ... 

Fig. 9 a Experimental diffraction pattern of an Mg/Al-COs LDH and b the simulated pattern assuming a random intergrowth of 3Ri (60%) and 3R2 (40%) polytypes. Reprinted with permission from [103]. Copyright The Clay Minerals Society... 

Kloprogge JT (ed)(2005) The Application of Vibrational Spectroscopy to Clay Minerals and Layered Double Hydroxides. Clay Minerals Society, Aimora Kloprogge JT, Frost RL (1999) J Solid State Chem 146 506... 

Figure 3.9 Relation between surface charge and reduction of structural Fe in a diocta-hedral smectite. Points are experimental data lines are theoretical relations discussed in the text (Drits and Manceau, 2000). Reproduced by permission of Clay Minerals Society...

Brown, J. M. Elliott, J. J. "The Quantitative Analysis of Minerals by Fourier Transform Infrared (FT-IR) Spectroscopy", from Workshop on Application of IR Methods to the Study of Clay Minerals, Clay Mineral Society, 20th Annual Meeting, October 1, 1983, Buffalo, NY. 

N. Guven and R. M. Pollastro (eds.), Clay-Water Interface and Its Rheological Implications, Clay Minerals Society Workshop Lectures, Vol. 4 (The Clay Minerals Society, Boulder, CO, 1992). 

Zeolites to be held in Lyon in September, 1980. Also, a conference on natural zeolites was held in Tuscon, Arizona in 1976. Sessions on zeolites have become a regular feature at large technical meetings like those of the ACS and AIChE, and at smaller specialized ones like those of the Catalysis Society, the Clay Minerals Society, and the Gordon Conferences. 

Chenu, C., Pons, C. H., and Robert, M. (1987). Interaction of kaolinite and montmorillonite with neutral polysaccharides. In Proceedings, International Clay Conference, Denver 1985, Schultz, U. G, van Olphen, H., and Mumpton, F. A., eds., Clay Minerals Society Bloomington, IN, pp. 375-381. 

Lagaly, G. (1987). Clay-organic interactions Problems and recent results. In Proceedings of the International Conference, Denver 1985, The Clay Minerals Society, pp. 343-351. 

Bailey, S.W., Brindley, G.W., Johns, W.D., Martin, R.T. and Ross, M., 1971. Report of Clay Minerals Society Nomenclature Committee. Clays Clay Miner., 19 132-134. 

This work was supported by NSF grant EAR86-09277. Figures 12 and 13 are with the permission of the Clay Minerals Society. 

Figure 5. X-ray diffractogram of reduced Na-nontronite (sampe API H-33a from Wards Natural Science Establishment, Rochester, New York) when Fe2 /Fe3 88 0.64 and n 5 atm. (Reproduced with permission from Wu, J.J Low, P. F. Roth, C. B. Clays Clay Miner, in press. Copyright 1989 The Clay Minerals Society).

Figure 6. Observed relationship between specific surface area (Sm) and Fe2 content of a chemically reduced series of ferruginous smectite (sample SWa-1 from the Source Clay Minerals Repository of The Clay Minerals Society). (Reproduced with permission from Lear,...

P. R. Stucki, J. W., Clays Clay Miner, in press. Copyright 1989 The Clay Minerals Society). 

Figure 8 Vibrational potential energy vs. configurational coordinate for electron transfer via vibronic coupling betweeg two symmetric states of a single oscillator A, initial state B, vibration-ally excited state B, thermally excited state X9 vibronic coupling parameter E f optical transition energy E t thermal transition energy (Reproduced with permission from Ref 33 Copyright 1987 The Clay Minerals Society) ...

Figure 15 Layer charge of ferruginous smectite (sample SWa-1 from the Source Clay Minerals Repository of The Clay Minerals Society).

A) Predicted by Equation 1 (B) Predicted by Equation 6 (C) observed. (Reproduced with permission from Ref. 32. Copyright 1983 The Clay Minerals Society). 

Same samples as used by Stuck et al. (29) and Lear and Stucki (32). UPMsUpton (API 25) montmorilIonite CZMsCzechoslovakia 630 montmorillonite NZM New Zealand montmorilIonite GAN Garfield (API H-33a) nontronite SWa-lsferruginous smectite (Source Clay Minerals Repository, The Clay Minerals Society). 

Figure 3. Formation of surface Si-OH-Al acidic groups upon heating NH4+ beidellite (a) and leaching Na beidellite with an acid solution, followed by calcination at the indicated temperature (b). (Reprinted with permission from ref. 19. Copyright 1987 Clay Minerals Society.)...

Hectorite (H), barasym SSM-100 (BS) from the Source Clays Repository of the Clay Minerals Society and laponite B (L) from Laporte Industries were used. The clays were exchanged with 1 M NaCl solutions three times, the < 2 mm fraction was separated by centrifugation and stored in 1 M NaCl at 277 K. 

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