Note that from 2019 onwards, new deposited material will be hosted on the Springer Nature site.
2018, vol. 66
August 2018
Solvent-kaolinite interactions investigated using the 3D-RISM-KH molecular theory of solvation
Stanislav R.Stoyanov, Feng Lin, and Yuming Xu
Tables S1, S2
2018, vol. 66
June 2018
Quantitative X-ray powder diffraction and the illite polytype analysis method for direct fault rock dating: A comparison of analytical techniques
Austin Boles, Anja Schleicher, John Solum, and Ben van der Pluijm
Appendix S5, Figure S1, Table S1, Table S2, Table S3 Table S4
2017, vol. 65
October 2017
Testing high-voltage electrical discharges in disintegrating claystone for isotopic and mineralogical studies: an example using Opaninus claystone
Horst Zwingmann, Alfons Berger, Urs Eggenberger, Andrew Todd, and Marco Herwegh
Supplementary data
2017, vol. 65
June 2017
Solid-state 1H and 27Al NMR Studies of DMSO-kaolinite Intercalates
Jonathan Fafard, Victor Terskikh and Christian Detellier
Supplementary Figures S1, S2
2017, vol. 65
April 2017
Mineralogy, Geochemistry, and Genesis of Bentonites in Miocene Volcanic-sedimentary Units of the Ankara-Çankiri Basin, Central Anatolia, Turkey
Selahattin Kadir, Tacit Külah, Nergis Önalgil, Hülya Erkoyun and W. Crawford Elliott
Supplementary Tables S1a, S1b, S1c, S1d
2017, vol. 65
April 2017
Characterization of the Second Package of the Alternative Buffer Material (ABM) Experiment – II Exchangeable Cation Population Rearrangement
R. Dohrmann and S. Kaufhold
Supplementary Table S1
2016, vol. 64
October 2016
XRD and TEM studies on nanophase manganese oxides in freshwater ferromanganese nodules from Green Bay, Lake Michigan
Seungyeol Lee and Huifang Xu
Supplementary table
2016, vol. 64
August 2016
Intercalation of ethylene glycol in smectites: Several molecular simulation models verified by X-ray diffraction data
Marek Szczerba and Andrey G. Kalinichev
2016, vol. 64
August 2016
Structure and dynamics of water–smectite interfaces: Hydrogen bonding and the origin of the sharp O–Dw/O–Hw infrared band from molecular simulations
Marek Szczerba, Artur Kuligiewicz, Arkadiusz Derkowski, Vassilis Gionis, Georgios D. Chryssikos, and Andrey G. Kalinichev
2016, vol. 64
August 2016
Molecular dynamics simulations of anion exclusion in clay interlayer nanopores
Christophe Tournassat, Ian C. Bourg, Michael Holmboe, Garrison Sposito, and Carl I. Steefel
Supplementary info
2015, vol. 63
December 2015
Formation and restacking of disordered smectite osmotic hydrates
Benjamin Gilbert, Luis R. Comolli, Ruth M. Tinnacher, Martin Kunz, and Jillian F. Banfield
2015, vol. 63
June 2015
Composition and genesis of the nickel-chrome-bearing nontronite and montmorillonite in lateritized ultramafic rocsk in the Muratdagi Region (Usak, western Anatolia), Turkey
Extended Tables 2, 3
2014, vol. 62
August 2014
Mineralogical and isotopic record of diagenesis from the Opalinus Clay Formation at Benken, Switzerland: implications for the modeling of pore-water chemistry in a clay formation
Catherine Lerouge, Sylvain Grangeon, Francis Claret, Eric Gaucher, Philippe Blanc, Catherine Guerrot, Christine Flehoc, Guillaume Wille, and Martin Mazurek
Appendix 1, Appendix 2
2014, vol. 62
August 2014
Mineralogy , geochemistry, and genesis of mudstones in the Upper Miocene Mustafapașa member of the Ürgüp formation in the Cappadocia regoin, Central Anatolia, Turkey
Tacit Külah, Selahattin Kadir, Ali Gürel, Muhsin Eren, ad Nergis Önal;gil
Extended form of Table 2
2014, vol. 62
April 2014
Temperature effects on the crystallinity of synthetic nontronite and implications for nontronite formation in Columbia River Basalts
Leslie L. Baker and Daniel G. Strawn
Field maps and notes of J.A. Kittrick
2014, vol. 62
February 2014
Relative humidity-induced reversible hydration of sulfate-intercalated layered double hydroxides
S. Radha, K. Jayanthi, Josef Breu and P. Vishnu Kamath
Supporting information
2013, vol. 61
December 2013
Mineralogy of Egyptian bentonitic clays II: Geologic origin
Mohamed A. Agha, Ray E. Ferrel, George F. Hart, Mohamed S. Abu El Ghar, and A. Abdel-Motelib
2012, vol. 60
August 2012
Mineralogy of Egyptian bentonitic clays I: Discriminant Function Analysis
Mahomed A. Agha, Ray E. Ferrell, and George F. Hart
2011, vol. 59
August 2011
Interpretation of reflectance spectra of clay mineral-silica mixtures: implications for Martial clay mineralogy at Mawrth Vallis – Nancy K. McKeown, Janice L. Bishop, Javier Cuadros, Stephen Hillier, Elena Amador, Heather D. Makarewicz, Mario Parente, and Eli A. Silver
June 2011
Mineralogical and geochemical characteristics and genesis of the sepiolite deposits at Polatlı Basin (Ankara, Turkey) – Muazzez Çelik Karakaya, Necati Karakaya, and Abidin Temel
Table 4 Correlation coefficients of major and trace elements, and some element groups of dolostones, limestones, sepiolitic claystones, and detrital silicate-rich rocks.
2008, vol. 56
April 2008
Surface area and layer charge of smectite from CEC and EGME/H2O retention measurements – J. Środoń, and D. McCarty
Figure 1b-d. Figure 1. TGA-MS curves for representative Ca-smectites: (a) Wyoming montmorillonite, (b) Garfield nontronite, (c) Otay montmorillonite, (d) Ballarat saponite. Black curve = weight loss, gray curve = relative intensity of mass 18 spectrum. Weight changes from start to 110 °C, start to 200 °C, 200 °C for 20 h, and from 200 °C at 20 h to 900 °C at 1 h are shown
Figure 3 Amount of H2O released at 200 °C (WBW) compared to (a) layer charge, Q, per formula unit, (b) tetrahedral charge per formula unit.
Figure 4 Amount of H2O released above 200 °C, after 20 h of isothermal heating (TBW) compared to layer charge, Q, per formula unit.
Figure 6 H2O coverage compared with CECcorr/TSSANr ratio. The regression is used to refine the TSSANr calculation (Table 7, column 9).
Figure 7 EGME coverage compared with CECcorr/TSSANr ratio. The regression is used to refine the TSSANr calculation (Table 8, column 9).
Figure 8 Relationship between WBW/TSSAEXCH ratio and Qs (approximated by Q from Table 1). The regression is used in combination with equation 11 to calculate Qs and TSSAEXCH from WBW and CEC (Table 9, columns 7 and 9).
Table 2 Peak position data (in Å) from oriented XRD preparations of glycolated and air-dry (47%RH) <0.2 mm fractions of studied smectites. The glycolated samples demonstrate the lack of mixed-layering by the integral series of 00l reflections, and the air-dry samples – the nature of water complex (see text for details). Trace mineral contaminants are also listed.
February 2008
Pyroxene weathering to smectite: conventional and cryo-field emission scanning electron microscopy, Koua Bocca ultramafic complex, Ivory Coast – M. Velbel and W.W. Barker
February 2008
Geochemical records of a bentonitic acid-tuff succession related to a transgressive systems tract – indication of changes in the volcanic sedimentation rate – Z. Püspöki, M. Kozák, P. Kovács-Pálffy, J. Szepesi, R. McIntosh, P. Kónya, L. Vincze, and G. Gyula
Tables 1-3
2007, vol. 55
February 2007
Clay mineralogy of halloysite and alunite deposits in the Turplu area, Balikesir, Turkey – Ö. Işik Ece and Paul Schroeder