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  • Clays and Clay Minerals, Vol. 54, No. 2, 230-239, 2006. 
    Galan, Emilio; Aparicio, Patricia; Iglesia, Angel La; Gonzalez, Isabel (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Well ordered kaolinite was isostatically and uniaxially pressurized up to 13,200 kg/cm2 for 10 min in dry conditions and the effects of pressure on kaolinite order were determined by analyzing the shapes of two-dimensional ...
  • Clays and Clay Minerals, Vol. 54, No. 2, 240-251, 2006. 
    Giorgetti, Giovanna; Monecke, Thomas; Kleeberg, Reinhard; Hannington, Mark D. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Dacitic lava recovered from the immediate subsurface of the submarine PACMANUS hydrothermal vent field exhibits variable degrees of hydrothermal alteration resulting from the interaction of the glassy volcanic rocks with ...
  • Clays and Clay Minerals, Vol. 54, No. 2, 252-265, 2006. 
    Zazzi, Asa; Hirsch, Tomas K.; Leonova, Ekaterina; Kaikkonen, Andrei; Grins, Jekabs; Annersten, Hans; Eden, Mattias (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The structures of one synthetic and two natural chlorites of the chlinochlore type were explored using X-ray diffraction, magic-angle spinning nuclear magnetic resonance (NMR) and MoÈssbauer spectroscopy. Rietveld refinements ...
  • Clays and Clay Minerals, Vol. 54, No. 2, 266-273, 2006. 
    Ji, Junfeng; Zhao, Liang; Balsam, William; Chen, Jun; Wu, Tao; Liu, Lianwen (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Chlorite is one of the most common Fe-bearing minerals and is susceptible to weathering in loess and soils. The conventional method for analyzing chlorite, based on XRD with the Rietveld technique, is quantitative, but ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 275-294, 2006. 
    Laverret, Emmanuel; Mas, Patricia Patrier; Beaufort, Daniel; Kister, Philippe; Quirt, David; Bruneton, Patrice; Clauer, Norbert (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Unconformity-related uranium deposits, which represent a significant high-grade uranium resource, are systematically surrounded by a host-rock alteration halo enriched in clay minerals. Illite is often the major clay mineral ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 295-313, 2006. 
    Kister, Philippe; Laverret, Emmanuel; Quirt, David; Cuney, Michel; Mas, Patricia Patrier; Beaufort, Daniel; Bruneton, Patrice (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The spatial distribution of the dominant matrix minerals present in the middle-Proterozoic Athabasca Group sandstone (kaolin, illite, sudoite, dravite, hematite) was studied at a regional scale in the Shea Creek region ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 314-323, 2006. 
    Elliott, W. Crawford; Basu, Ankan; Wampler, J. Marion; Elmore, R. Douglas; Grathoff, Georg H. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The clay fractions of Jurassic marls in the Great Estuarine Group in southern Isle of Skye are composed of mixed-layered illite-smectite (I-S) with large percentages (>85%) of illite layers, kaolinite, and generally smaller ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 324-332, 2006. 
    Garcia-Romero, E.; Suarez, M.; Oyarzun, R.; Lopez-Garcia, J.A.; Regueiro, M. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Palygorskite fibers growing along fault planes in the outcrops of a large fault zone in SE Spain (Carboneras Fault Zone: CFZ; Serrata de NõÂjar) were studied by X-ray diffraction, scanning electron microscopy-energy ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 333-350, 2006. 
    Yalcin, Huseyin; Bozkay, Omer (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Talc deposits, located mainly in three areas of north-central Turkey, are present in the ophiolitic series of the Cretaceous and in siliciclastic rocks of the Paleocene. Talc deposits related to ophiolites are between ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 351-362, 2006. 
    Proust, D.; Caillaud, J.; Fontaine, C. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The early stages of amphibole weathering result in the crystallization of several clay mineral species: tri- and dioctahedral smectites, interstratified dioctahedral kaolinite-smectite (K-S), and halloysite. Each clay ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 363-374, 2006. 
    Bourg, Ian C.; Sposito, Garrison; Bourg, Alain C.M. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Compacted Na-bentonite clay barriers, widely used in the isolation of solid-waste landfills and other contaminated sites, have been proposed for a similar use in the disposal of high-level radioactive waste. Molecular ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 375-381, 2006. 
    Noyan, Hulya; Onal, Muserref; Sarikaya, Yuksel (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The Hancili bentonite from Turkey shows significant changes in surface area, micro- and mesoporosity, surface acidity and acid strength with heating from 100 to 900C for 2 h. The specific surface area (S) and specific ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 382-389, 2006. 
    Kayano, Mihoko; Ogawa, Makoto (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Cobalt (II) and Al (III) layered double hydroxides were precipitated from homogeneous solutions using urea hydrolysis under hydrothermal conditions. The particle sizes were controlled successfully by changing the reaction ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 390-401, 2006. 
    Bastida, Joaquin; Kojdecki, Marek A.; Pardo, Pablo; Amoros, Pedro (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    A reference sample of sepiolite and products of its comminution by vibrating dry-milling have been studied using X-ray diffraction (XRD) line-broadening analysis, complementary field emission scanning electron microscopy ...
  • Clays and Clay Minerals, Vol. 54, No. 3, 402-407, 2006. 
    Rakhmatkariev, Gairat (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Adsorption isotherms and differential heats of adsorption of water vapor by muscovite were measured at 303 K. The heats of adsorption are stepwise and each step corresponds to the stoichiometric formation of adsorption ...
  • Clays and Clay Minerals, Vol. 54, No. 4, 409-417, 2006. 
    Allada, Rama Kumar; Peltier, Edward; Navrotsky, Alexandra; Casey, William H.; Johnson, C. Annette; Berbeco, Hillary Thompson; Sparks, Donald L. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Interest in hydrotalcite-like compounds has grown due to their role in controlling the mobility of aqueous metals in the environment as well as their use as catalysts, catalyst precursors and specialty chemicals. Although ...
  • Clays and Clay Minerals, Vol. 54, No. 4, 418-425, 2006. 
    Tian, Xiaofei; Wei, Min; Evans, David G.; Rao, Guoying; Yang, Heli (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The controlled chemical oxidative polymerization of metanilic anion (m-NH2C6H4SO3 ÿ) within the interlayer of NiAl layered double hydroxide was performed using, for the first time, ammonium persulfate as the oxidizing ...
  • Clays and Clay Minerals, Vol. 54, No. 4, 426-434, 2006. 
    Roberts, Michael G.; Li, Hui; Teppen, Brian J.; Boyd, Stephen A. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Nitroaromatic compounds (NACs) are components of munitions commonly found as soil contaminants at military training sites and elsewhere. These compounds pose possible threats to human health and ecological systems. Recent ...
  • Clays and Clay Minerals, Vol. 54, No. 4, 435-448, 2006. 
    Harris, Rodney G.; Johnson, Bruce B.; Wells, John D. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The strong adsorption to kaolinite of four polyaromatic, cationic dyes (9-aminoacridine, 3,6- diaminoacridine, azure A and safranin O), which adsorb much less to alumina or silica, was investigated by means of acid-base ...
  • Clays and Clay Minerals, Vol. 54, No. 4, 449-455, 2006. 
    Harris, Rodney G.; Johnson, Bruce B.; Wells, John D. (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    The competitive adsorption to kaolinite between Cd(II) and four polyaromatic dyes (9- aminoacridine, 3,6-diaminoacridine, azure A and safranin O) was studied in 5 mM KNO3 at 25ëC. Under these conditions, Cd adsorbs to the ...