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  • Clays and Clay Minerals, Vol. 58, No. 5, 606–626, 2010. 
    Dos Anjos, Camila Wense Dias; Meunier, Alain; Guimaraes, Edi Mendes; Albani, Abderrazzak El (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Shales and claystones in the Permian Irati Formation consist of Al-rich or Fe-Mg clay minerals in its southern/central and northern parts, respectively. The constrasting compositions indicate particular geological and ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 627–643, 2010. 
    Mchenry, Lindsay J. (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The current study demonstrates how co-existing zeolite and clay minerals formed by the alteration of tephra in a closed-basin lacustrine and lake-margin environment can retain the overall composition of the original bulk ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 644–666, 2010. 
    Bozkaya, Omer; Yalcin, Huseyin (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The Antalya Unit, one of the allochthonous units of the Tauride belt, is of critical, regional tectonic importance because of the presence of rifting remnants related to the break-up of the northern margin of Gondwana ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 667–681, 2010. 
    Jodin-caumon, Marie-camille; Mosser-ruck, Regine; Rousset, Davy; Randi, Aurelien; Cathelineau, Michel; Michau, Nicolas (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Disposal facilities in deep geological formations are considered to be a possible solution for long-term management of high-level nuclear waste (HLW). The design of the repository generally consists of a multiple-barrier ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 682–690, 2010. 
    Tao, Liang; Li, Fangbai; Wang, Yongkui; Sun, Kewen (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Much attention has been paid to the adsorption of Fe(II) onto mineral surfaces as it is a crucial step in enhancing the reductive activity of Fe(II) species. The present study elucidates the role of Fe(II) adsorbed on Fe ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 691–706, 2010. 
    Mao, Changping; Chen, Jun; Yuan, Xuyin; Yang, Zhongfang; Balsam, William; Ji, Junfeng (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The source and temporal changesof mineralstrans ported by the world’slarge riversare important. In particular, clay minerals are important in evaluating the maturity of suspended sediments, weathering intensity, and source ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 707–716, 2010. 
    Kaufhold, Stephan; Ufer, Kristian; Kaufhold, Annette; Stucki, Joseph W.; Anastacio, Alexandre S.; Jahn, Reinhold; Dohrmann, Reiner (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Allophane is a very fine-grained clay mineral which is especially common in Andosols. Its importance in soils derives from its large reactive surface area. Owing to its short-range order, allophane cannot be quantified by ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 717–720, 2010. 
    Vidal, Olivier; Dubacq, Benoit; Lanari, Pierre (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The arguments of Nieto et al. (2010) in favor of the incorporation of H3O+ rather than H2O in interlayer positions of illite are disputable. Stoichiometric arguments suggest that the excess water in the Silver Hill illite ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 721–723, 2010. 
    Nieto, Fernando; Mellini, Marcello; Abad, Isabel (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The arguments of Vidal et al. (2010) against the incorporation of H3O+ rather than of H2O in the interlayer position of illite are disputable. Stoichiometric arguments do indeed suggest that the excess water in the Silver ...
  • Clays and Clay Minerals, Vol. 58, No. 5, 724, 2010. 
    Unknown author (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
  • Clays and Clay Minerals, Vol. 58, No. 5, 725, 2010. 
    Unknown author (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
  • Clays and Clay Minerals, Vol. 58, No. 6, 727–742, 2010. 
    Yuan, Hongji; Bish, David L. (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    NEWMOD#, developed by R.C. Reynolds, Jr., has been an important tool for evaluating quantitatively X-ray diffraction (XRD) patterns from interstratified clay minerals for more than 20 years. However, a significant drawback ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 743–756, 2010. 
    Srodon, Jan (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The incorporation of boron (B) and nitrogen (N) into illite is the key demand-side process responsible for the diagenetic budget of these elements in sedimentary basins, with important implications for pore-water chemistry, ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 757–765, 2010. 
    Kawano, Motoharu; Hwang, Jinyeon (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Guanidineand imidazoleareimporta nt functional molecules that constitutethe side chain of basic amino acids (arginine and histidine); these molecules are capable of interacting with mineral surfaces. However, little ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 766–771, 2010. 
    Mantovani, Marco; Becerro, Ana Isabel (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Studies of the paragenesis of authigenic illite in arkosic sandstones of various regions and ages have revealed that the illitization of kaolinite is an important reaction accounting for the formation of authigenic illite ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 772–782, 2010. 
    Baker, Leslie L.; Strawn, Daniel G.; Vaughan, Karen L.; Mcdaniel, Paul A (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The characterization of poorly crystalline minerals formed by weathering is difficult using conventional techniques. The objective of this study was to use cutting-edge spectroscopic techniques to characterize secondary ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 783–791, 2010. 
    Murphy, David M. K.; Gilkes, Robert J. (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Differentiating clay minerals that formed in a supergene environment during deep chemical weathering from those that formed during hydrothermal alteration at higher temperatures associated with a mineralizing event is ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 792–802, 2010. 
    Erkan, Ilker; Alp, Ibrahim; Celik, Mehmet Sabri (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The effects of surfactants on bentonites have been of great scientific interest for many years. Even though quaternary alkylammonium salts (QAS) have been studied, very few data are available on the comparative performance ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 803–812, 2010. 
    Barre, Pierre; Velde, Bruce (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The effect of plant species on soil-clay mineralogy has not been studied widely. In the present study, the clay mineralogy of top soils under Sequoia gigantia and grass regimes, maintained side by side for up to 150 y in ...
  • Clays and Clay Minerals, Vol. 58, No. 6, 813–820, 2010. 
    Kosoglu, Laura M.; Bickmore, Barry R.; Filz, George M.; Madden, Andrew S. (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    The coefficient of friction of clay minerals at the micro-scale has generally not been studied due to difficulties in obtaining measurements in a bulk-soil volume undergoing shear at such small scales. Information on ...