Browsing by Title

Browsing by Title

Sort by: Order: Results:

  • Clays and Clay Minerals, Vol. 57, No. 5, 513–520, 2009. 
    Zhao, Wei; Cui, Haojie; Liu, Fan; Tan, Wenfeng; Feng, Xionghan (The Clay Minerals Society, 2009)
    The relationship between vacant Mn structural sites in birnessites and heavy-metal adsorption is a current and important research topic. In this study, two series of birnessites with different average oxidation states (AOS) ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 521–530, 2009. 
    Wang, Ming Kuang; Tseng, Pao Chung; Chang, Shyun Sheng; Ray, Dah Tong; Shau, Yen Hong; Shen, Yun Wei; Chen, Ruey Chyong; Chiang, Po Neng (The Clay Minerals Society, 2009)
    The Tuluanshan Formation of the eastern Coastal Range of Taiwan overlies an andesitic core complex presumed to be the source of hydrothermal fluids responsible for the Si- and Mg-rich mineralization of sepiolite and ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 531–554, 2009. 
    Derkowski, Arkadiusz; Srodon, Jan; Franus, Wojciech; Uhlik, Peter; Banas, Michał; Zielinski, Grzegorz; Caplovicova, Maria; Franus, Małgorzata (The Clay Minerals Society, 2009)
    The K-Ar dating of glauconite has been used as an important stratigraphic tool for many decades. The application of this technique is limited to pure glauconites, free of detrital contamination by K-bearing phases, often ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 555–565, 2009. 
    Rytwo, Giora; Gonen, Yotam; Huterer-Shveky, Reuma (The Clay Minerals Society, 2009)
    Syntheticdyes in industrial effluents pose a significant risk to human health and the environment, so much effort has been expended to degrade them using various methods, including the use of clay minerals as catalysts. ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 566–577, 2009. 
    Papoulis, Dimitrios; Tsolis-Katagas, Panagiota; Kalampounias, Angelos G.; Tsikouras, Basilios (The Clay Minerals Society, 2009)
    Occurrences of halloysite-rich material in altered volcanic rocks, principally trachyandesites, dacites, and tuffs, extend over an area of ~1 km2 in the southwestern part of Limnos, Island, northeast Aegean Sea, Greece. ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 578–585, 2009. 
    Eick, Matthew J.; Luxton, Todd P.; Welsh, Holly A. (The Clay Minerals Society, 2009)
    Numerous studies have investigated the ligand-promoted dissolution of Fe (oxyhydr)oxides. In natural environments, inorganic ligands can compete with organic ligands for surface sites on (oxyhydr)oxides which may influence ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 586–601, 2009. 
    Jozefaciuk, Grzegorz (The Clay Minerals Society, 2009)
    The size, shape, and continuity of pores in mineral solids greatly influence the behavior of percolating liquids and solids in porous media, which has significant practical environmental implications. In order to expand ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 602–615, 2009. 
    Hong, Hanlie; Li, Zhaohui (The Clay Minerals Society, 2009)
    In spite of many studies of laterite origins in various parts of the world, the origin of laterite in the middle to lower reaches of the Yangtze River is still a topic of debate, thus leaving doubts about the prevailing ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 616–637, 2009. 
    Kohler, Eric; Parra, Teddy; Vidal, Olivier (The Clay Minerals Society, 2009)
    The storage of CO2 in geological reservoirs requires an understanding of the impact of CO2 on clay-rich sealing cap-rocks to identify and explore critical parameters that modify petrophysical properties such as permeability ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 638–648, 2009. 
    Letaief, Sadok; Detellier, Christian (The Clay Minerals Society, 2009)
    The objective of this studywas to design new, functional, nanostructured materials from the abundant claymineral kaolinite, in spite of development problems with the interlayer chemistry of kaolinite because of its ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 649–671, 2009. 
    Srodon, Jan; Zeelmaekers, Edwin; Derkowski, Arkadiusz (The Clay Minerals Society, 2009)
    The nature of component layers of mixed-layer illite-smectite and their possible evolution in the course of illitization have been debated since the 1960s. The present study is a new attempt to solve these problems, using ...
  • Clays and Clay Minerals, Vol. 57, No. 5, 672, 2009. 
    Unknown author (The Clay Minerals Society, 2009)
    The following are some papers that have been accepted for publication in future issues of Clays and Clay Minerals.
  • Clays and Clay Minerals, Vol. 57, No. 6, 585-586, 2009. 
    Drits, Victor (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
  • Clays and Clay Minerals, Vol. 57, No. 6, 673–685, 2009. 
    Bujnowski, Thomas J.; Guggenheim, Stephen; Brigatti, Maria Franca (The Clay Minerals Society, 2009)
    Factors controlling the crystal structure of phlogopite have been widely investigated; but the role of electrostatic interactions, for example, has received much less attention than other factors. The purpose of the present ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 686–694, 2009. 
    Dohrmann, R.; Ruping, K.B.; Kleber, M.; Ufer, K.; Jahn, R. (The Clay Minerals Society, 2009)
    In X-ray diffraction (XRD) analysis, preparation of oriented clay specimens enhances their 00l reflections by arranging basal surfaces parallel to the specimen surface. In one-dimensional modeling of XRD intensities, degree ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 695–705, 2009. 
    Ozdemir, Abdil; Keskin, Can Serkan (The Clay Minerals Society, 2009)
    An important application of clay is as a solid adsorbent for industrial dyes. The aim of the present work was to carry out an experimental-theoretical study of the adsorptionof dye mixtures, namely malachite green (MG) and ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 706–714, 2009. 
    Szabo, Tamas; Wang, Jun; Volodin, Alexander; Van Haesendonck, Chris; Dekany, Imre; Schoonheydt, Robert A. (The Clay Minerals Society, 2009)
    The sizes and shapes of single clay mineral layers are difficult to determine though they are important parameters which determine the final properties of clay polymer nanocomposites and of ultrathin clay mineral films. ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 715–724, 2009. 
    Cui, Haojie; Qiu, Guohong; Feng, Xionghan; Tan, Wenfeng; Liu, Fan (The Clay Minerals Society, 2009)
    Todorokite is a common manganese oxide mineral, with a tunnel structure, found in Earth surface environments, and is easily synthesized from layered birnessite. The aim of the current study was to prepare birnessites with ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 725–741, 2009. 
    Giorgetti, Giovanna; Monecke, Thomas; Kleeberg, Reinhard; Hannington, Mark D. (The Clay Minerals Society, 2009)
    Abstract—The conversion of volcanic glass to secondary alteration products is one of the most common mineralogical transformations during low-temperature hydrothermal alteration of submarine basalts. To better understand ...
  • Clays and Clay Minerals, Vol. 57, No. 6, 742–750, 2009. 
    Cuadros, Javier; Nieto, Fernando; Wing-dudek, Teresa (The Clay Minerals Society, 2009)
    The mechanism for the kaolinization of smectite is extremely complex. The purpose of this study was to explore this mechanism by providing more microscopic information about kaolinite-smectite (K-S) intermediate phases. ...