Browsing by Author "Dong, Hailiang"

Browsing by Author "Dong, Hailiang"

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  • Clays and Clay Minerals, Vol. 54, No. 1, 67-79, 2006. 
    Seabaugh, Jennifer L.; Dong, Hailiang; Kukkadapu, Ravi K.; Eberl, Dennis D.; Morton, John P.; Kim, Jinwook (The Clay Minerals SocietyThe Clay Minerals Society, 2006)
    Shewanella putrefaciens CN32 reduces Fe(III) within two illites which have different properties: the Fithian bulk fraction and the <0.2 mm fraction of Muloorina. The Fithian illite contained 4.6% (w/w) total Fe, 81% of ...
  • Clays and Clay Minerals, Vol. 55, No. 1, 96–107, 2007. 
    Jaisi, Deb P.; Dong, Hailiang; Kim, Jinwook; He, Ziqi; Morton, John P. (The Clay Minerals SocietyThe Clay Minerals Society, 2007)
    Clay particle aggregation affects a number of environmental processes, such as contaminant sorption/desorption, particle movement/deposition, and sediment structure and stability, yet factors that control clay aggregation ...
  • Clays and Clay Minerals, Vol. 56, No. 2, 175–189, 2008. 
    Jaisi, Deb P.; Dong, Hailiang; Morton, John P. (The Clay Minerals SocietyThe Clay Minerals Society, 2008)
    Clay minerals impart important chemical properties to soils, in part, by virtue of changes in the redox state of Fe in their crystal structures. Therefore, measurement of Fe(III)/Fe(II) and partitioning of Fe(II) in different ...
  • Clays and Clay Minerals, Vol. 56, No. 4, 416–428, 2008. 
    Jaisi, Deb P.; Ji, Shanshan; Dong, Hailiang; Blake, Ruth E.; Eberl, Dennis D.; Kim, Jinwook (The Clay Minerals SocietyThe Clay Minerals Society, 2008)
    River-dominated delta areas are primary sites of active biogeochemical cycling, with productivity enhanced by terrestrial inputs of nutrients. Particle aggregation in these areas primarily controls the deposition of suspended ...
  • Clays and Clay Minerals, Vol. 57, No. 2, 213–226, 2009. 
    Yu, Bingsong; Dong, Hailiang; Jiang, Hongchen; Lv, Guo; Eberl, Dennis; Li, Shanying; Kim, Jinwook (The Clay Minerals Society, 2009)
    Abstract—The role of saline lake sediments in preserving organic matter has long been recognized. In order to further understand the preservation mechanisms, the role of clay minerals was studied. Three sediment cores, 25, ...
  • Clays and Clay Minerals, Vol. 58, No. 4, 542–557, 2010. 
    Bishop, Michael E.; Jaisi, Deb P.; Dong, Hailiang; Kukkadapu, Ravi K.; Ji, Junfeng (The Clay Minerals SocietyThe Clay Minerals Society, 2010)
    Fe-reducing micro-organisms can change the oxidation state of structural Fe in clay minerals. The interactions with complex clays and clay minerals in natural materials remain poorly understood, however. The objective of ...
  • Clays and Clay Minerals, Vol. 59, No. 1, 21–33, 2011. 
    Jaisi, Deb P.; Eberl, Dennis D.; Dong, Hailiang; Kim, Jinwook (The Clay Minerals Society, 2011)
    The formation of illite through the smectite-to-illite (S-I) reaction is considered to be one of the most important mineral reactions occurring during diagenesis. In biologically catalyzed systems, however, this transformation ...
  • Clays and Clay Minerals, Vol. 59, No. 2, 176–188, 2011. 
    Kim, Jinwook; Dong, Hailiang (The Clay Minerals Society, 2011)
    Electron energy-loss spectroscopy (EELS), energy-filtered transmission electron microscopy (EFTEM), and high-resolution transmission electron microscopy (HRTEM) have been applied in mineralogy and materials research to ...
  • Clays and Clay Minerals,Vo l. 59,No . 5,43 5–437,20 11. 
    Dong, Hailiang; Stucki, Joseph W. (The Clay Minerals Society, 2011)
    Reports of scientific investigations published in Clays and Clay Minerals address a wide range of topics covering virtually every physical and natural science and thousands of industrial products and processes worldwide. ...