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K-montmorillonite

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Journal Article
Published: 01 December 1998
Clays and Clay Minerals (1998) 46 (6): 636–648.
...K. Faisandier; C. H. Pons; D. Tchoubar; F. Thomas GeoRef, Copyright 2004, American Geological Institute. 1998 ...
Journal Article
Journal: Clay Minerals
Published: 01 April 2000
Clay Minerals (2000) 35 (2): 335–343.
...G. ROY; M. PELLETIER; F. THOMAS; C. DESPAS; J. BESSIÈRE Abstract Montmorillonite-water-cation systems were characterized using high-frequency impedance spectroscopy by studying the influence of the solid concentration and the nature of the exchangeable cation (Na + , K + , Ca 2...
FIGURES
First thumbnail for: Aggregation in Na-, <span class="search-highlight"...
Second thumbnail for: Aggregation in Na-, <span class="search-highlight"...
Third thumbnail for: Aggregation in Na-, <span class="search-highlight"...
Journal Article
Published: 01 December 1987
American Mineralogist (1987) 72 (11-12): 1170–1175.
...A. F. Koster van Groos; Stephen Guggenheim Abstract High-pressure differential thermal analysis ( hp-dta ) of the dehydroxylation of a Na-rich montmorillonite (Clay Minerals Society Source Clay SWy-1) and of the same montmorillonite after being K-exchanged was carried out at pressures to 2.5 kbar...
Journal Article
Published: 01 March 1975
Clays and Clay Minerals (1975) 23 (1): 61–69.
Journal Article
Journal: Clay Minerals
Published: 01 December 2005
Clay Minerals (2005) 40 (4): 499–510.
...G. SANJAY; S. SUGUNAN Abstract α-amylase was immobilized on acid-activated montmorillonite K-10 via adsorption and covalent linkage. The immobilized enzymes were characterized by X-ray diffraction (XRD), surface area measurements, 27 Al nuclear magnetic resonance (NMR) and scanning electron...
FIGURES
First thumbnail for: Immobilization of α-amylase onto <span class="sear...
Second thumbnail for: Immobilization of α-amylase onto <span class="sear...
Third thumbnail for: Immobilization of α-amylase onto <span class="sear...
Journal Article
Published: 01 April 2000
Mineralogical Magazine (2000) 64 (2): 337–346.
...H. J. Bray; S. A. T. Redfern Abstract The dehydroxylation of Ca-, K-, Mg- and Na-saturated Wyoming montmorillonite has been studied by thermogravimetry (TG), infrared (IR) spectroscopy and X-ray diffraction (XRD). Samples saturated with either Ca 2+ or Mg 2+ show a predominantly diffusion...
FIGURES
First thumbnail for: Influence of counterion species on the dehydroxyla...
Second thumbnail for: Influence of counterion species on the dehydroxyla...
Third thumbnail for: Influence of counterion species on the dehydroxyla...
Journal Article
Published: 01 April 1997
Clays and Clay Minerals (1997) 45 (2): 251–260.
... compensating cation, ionic strength, concentration of Cs, concentration of K and concentration of a soil-extracted fulvic acid. A Freundlich isotherm has been found to fit experimental data well for levels of adsorbed cesium in the range 10 (super -7) to 1 mol kg (super -1) . Evidence of surface heterogeneity...
Journal Article
Journal: Clay Minerals
Published: 01 June 1991
Clay Minerals (1991) 26 (2): 255–268.
Journal Article
Published: 01 August 1990
Clays and Clay Minerals (1990) 38 (4): 426–436.
Journal Article
Published: 01 June 1986
Clays and Clay Minerals (1986) 34 (3): 281–286.
Journal Article
Journal: Clay Minerals
Published: 01 September 1984
Clay Minerals (1984) 19 (4): 541–561.
Journal Article
Journal: Clay Minerals
Published: 01 April 1981
Clay Minerals (1981) 16 (2): 125–137.
Journal Article
Published: 01 December 1979
Clays and Clay Minerals (1979) 27 (6): 393–401.
Journal Article
Journal: Clay Minerals
Published: 01 June 1978
Clay Minerals (1978) 13 (2): 139–146.
Image
XRD profiles of (a) Li- and (b) K-montmorillonite from 2 to 32°2𝛉 under various RH conditions and at 70°C. The intensity scale of this part of the profiles was expanded by a factor of three.
Published: 01 April 2011
Figure 1. XRD profiles of (a) Li- and (b) K-montmorillonite from 2 to 32°2𝛉 under various RH conditions and at 70°C. The intensity scale of this part of the profiles was expanded by a factor of three.
Image
Evolution of interlayer of 1-, 2-, and 3-layer hydrated K-montmorillonite as a function of temperature.
Published: 01 October 2010
F igure 4. Evolution of interlayer of 1-, 2-, and 3-layer hydrated K-montmorillonite as a function of temperature.
Journal Article
Journal: Clay Minerals
Published: 01 May 2016
Clay Minerals (2016) 51 (2): 197–211.
... Si_soft00.usp Optimizations of the unit cells of Na- and Ca-montmorillonites were done using GGA-PBE approximation only. The pseudopotentials are presented in Table 1 , and the kinetic cut-off energy for a plane-wave expansion of the wave function was 310 eV as in the case of K-montmorillonite...
FIGURES
First thumbnail for: Effect of layer charge on the crystalline swelling...
Second thumbnail for: Effect of layer charge on the crystalline swelling...
Third thumbnail for: Effect of layer charge on the crystalline swelling...
Image
The swelling curves of Na-, Ca- and K-montmorillonites with different layer charges from MD and QM studies (note: water is forced into the interlayer) and experimental results: (a) Fu et al. (1990), (b) Cases et al. (1997), (c) Bérend et al. (1995) and MC calculations from Zheng et al. (2011).
Published: 01 May 2016
Fig. 4. The swelling curves of Na-, Ca- and K-montmorillonites with different layer charges from MD and QM studies (note: water is forced into the interlayer) and experimental results: (a) Fu et al . (1990) , (b) Cases et al . (1997) , (c) Bérend et al . (1995) and MC calculations from
Journal Article
Published: 01 April 1999
Clays and Clay Minerals (1999) 47 (2): 192–200.
... hydrates of Na- and K-montmorillonite. The simulated radial distribution functions then were used to compute the total radial distribution function for interlayer water, a physical quantity that can be determined experimentally by H/D isotopic-difference neutron diffraction. The simulated total radial...
Journal Article
Published: 01 April 2005
Clays and Clay Minerals (2005) 53 (2): 137–146.
..., where L represents aminotriazole. Sorption experiments and modeling in systems containing K-saturated Wyoming (SWy-K) montmorillonite suggest that at low concentrations the aminotriazole sorbs primarily in cationic form via an ion-exchange mechanism. Sorption isotherms for aminotriazole are ‘s’-shaped...
FIGURES
First thumbnail for: SORPTION OF 3-AMINO-1,2,4-TRIAZOLE AND Zn(II) ONTO...
Second thumbnail for: SORPTION OF 3-AMINO-1,2,4-TRIAZOLE AND Zn(II) ONTO...
Third thumbnail for: SORPTION OF 3-AMINO-1,2,4-TRIAZOLE AND Zn(II) ONTO...