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  • Unknown author (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
  • Aldushin, Kirill; Jordan, Guntram; Aldushina, Elena; Schmahl, Wolfgang W. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    The kinetics of cation exchange in phlogopite have been studied in situ by hydrothermal atomic force microscopy (HAFM). The exchange of interlayer K by octylammonium ions caused an increase in the interlayer distance and ...
  • Okada, Tomohiko; Ehara, Yusuke; Ogawa, Makoto (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    The adsorption of Eu3+ from aqueous solution to natural Na+-montmorillonite (Kunipia F), synthetic saponite (Sumecton SA) and synthetic fluoro-tetrasilicic mica (Na+-TSM) clay samples was investigated. Adsorption capacities ...
  • Curtius, Hilde; Ufer, Kristian (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    From leaching experiments with metallic uranium-aluminum research reactor fuel elements in repository-relevant MgCl2-rich salt brines, a Mg-Al layered double hydroxide (LDH) with chloride as the interlayer anion was ...
  • Kawano, Motoharu; Obokata, Sumine (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Amino acids are ubiquitous in the Earth’s surface environments as reactive biological molecules produced by every living thing including bacteria. To evaluate the effects of amino acids on mineral dissolution and to reveal ...
  • Yu, G.; Saha, U. K.; Kozak, L. M.; Huang, P. M. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    The influence of organics on the crystallization of Al precipitates has been well documented. However, the effects of organics and ageing on the transformation and structural configuration of Al precipitates in relation ...
  • Meunier, Alain (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Hydroxy-interlayered minerals (HIMs) are typical of moderately acidic soils. Barnhisel and Bertsch (1989) defined the hydroxy-interlayered clay minerals as a solid-solution series between smectite, vermiculite and pedogenic ...
  • Hseu, Z. Y.; Tsai, H.; Hsi, H. C.; Chen, Y. C. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    There has been limited research on clay mineral transformation in serpentinitic soils under humid tropical conditions. In this study, four soil pedons were selected along a toposequence from the summit (Entisol), shoulder ...
  • Kadi˙r, Selahatti˙n (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Pliocene volcaniclastic lacustrine rocks of the Dog˘anbey formation in the Beysehir region (central Anatolia) are composed of organic-matter-bearing claystone, clastic units and dolomite interbeds, suggesting an anaerobic, ...
  • Bozkaya, O¨mer; Yalc¸in, Hu¨seyi˙n; Basibu¨yu¨k, Zeynel; Bozkaya, Gu¨lcan (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Hydrous Al-silicate deposits are found to the south of Pu¨tu¨rge in Malatya city, Turkey. The surrounding rocks consist of mylonitic granitic gneiss overlain by muscovite gneiss with kyanite-bearing metabasic schist lenses ...
  • Abidin, Zaenal; Matsue, Naoto; Henmi, Teruo (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Nano-ball allophane is a hydrous Al silicate with a hollow-sphere morphology that contains some defects or pores along the spherule walls. Enlargement of the pore openings by dilute alkali treatment was confirmed by cation ...
  • Unknown author (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
  • Unknown author (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
  • Kameda, Jun; Miyawaki, Ritsuro; Drits, Victor A.; Kogure, Toshihiro (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Polytypism in gu¨mbelite and its relationship to the fibrous or ribbon-like morphology exhibited by this Mg-rich illite were investigated by powder X-ray diffraction (XRD), electron back-scattered diffraction (EBSD) and ...
  • Zviagina, Bella B.; Sakharov, Boris A.; Drits, Victor A. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    To provide structural and diffraction criteria for the identification of trans-vacant (tv) a nd cisvacant (cv) mica varieties with different layer stackings, powder X-ray diffraction (XRD) patterns have been simulated for ...
  • Marti´n-marti´n, J. D.; Go´mez-gras, D.; Sanfeliu, T.; Thiry, M.; Ruiz-cruz, M. D.; Franco, F. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Diagenetic kaolin minerals are very common in the Permo-Triassic succession from the SE Iberian Range, Spain. The morphology and crystal structure of kaolin minerals has been examined in four size fractions (<1 mm, <2 mm, ...
  • Hong, Hanlie; Li, Zhaohui; Xue, Huijuan; Zhu, Yunhai; Zhang, Kexin; Xiang, Shuyuan (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    The clay mineral content of the Oligocene sediments in the Linxia Basin has been investigated using X-ray diffraction, scanning electron microscopy, and high-resolution transmission electron microscopy. The clay mineral ...
  • Aldega, Luca; Botti, Flavia; Corrado, Sveva (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Temperature-dependent clay mineral assemblages and vitrinite reflectance data have been used to investigate levels of diagenesis from the Messinian Laga Basin in the Central Apennines developed at the footwall of the ...
  • Dolinar, Bojana; Misˇicˇ, Miha; Trauner, Ludvik (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    As the water content is increased, the consistency of a fine-grained soil changes from a semisolid state to a plastic stateand finally to a liquid state. Thepl astic limit (PL) is thepoint at which the consistency, caused ...
  • Bascun˜an, Sophi´a; Kelm, Ursula; Sanhueza, Vilma; Alfaro, Guillermo (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Tuffs of the Tertiary Colbu´n Formation near Quinama´vida in central so uthern Chile have been mapped and their mineralogy analyzed. The pyroclastic rocks present a maximum outcropping thickness of 120 m and are dominated ...