About: Effect of composition and physical properties of. natural kaolinitic clays on their strong acid weathering rates.     Goto   Sponge   NotDistinct   Permalink

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  • Two samples of pure kaolinite with a significant difference in their crystallinity, a commercial kaolin sample with 20 wt.% of illitic component and one sample of illitic clay with up to 20 wt.% of kaolinitic component were used in dissolution kinetic experiments and the results compared to data obtained from the leaching of sandstone matrix kaolinites under laboratory conditions. The mineralogical and chemical compositions of all samples were characterised using X-ray diffraction and X-ray fluorescence techniques. Specific surface area was measured by the gas adsorption (BET) method. Structural disorder of kaolinite given by the extent of the sheet translations was calculated from the X-ray diffraction data (the 'Hinckley index'). Dissolution experiments in continuously stirred suspensions (with solid/liquid ratio=1:100) were performed in 0.5 and 5 M solutions of H2SO4 at 25 and 40 degreesC, respectively, and the reaction rate was calculated from the measured concentrations of Al and Si in the soluti
  • Two samples of pure kaolinite with a significant difference in their crystallinity, a commercial kaolin sample with 20 wt.% of illitic component and one sample of illitic clay with up to 20 wt.% of kaolinitic component were used in dissolution kinetic experiments and the results compared to data obtained from the leaching of sandstone matrix kaolinites under laboratory conditions. The mineralogical and chemical compositions of all samples were characterised using X-ray diffraction and X-ray fluorescence techniques. Specific surface area was measured by the gas adsorption (BET) method. Structural disorder of kaolinite given by the extent of the sheet translations was calculated from the X-ray diffraction data (the 'Hinckley index'). Dissolution experiments in continuously stirred suspensions (with solid/liquid ratio=1:100) were performed in 0.5 and 5 M solutions of H2SO4 at 25 and 40 degreesC, respectively, and the reaction rate was calculated from the measured concentrations of Al and Si in the soluti (en)
Title
  • Effect of composition and physical properties of. natural kaolinitic clays on their strong acid weathering rates.
  • Effect of composition and physical properties of. natural kaolinitic clays on their strong acid weathering rates. (en)
skos:prefLabel
  • Effect of composition and physical properties of. natural kaolinitic clays on their strong acid weathering rates.
  • Effect of composition and physical properties of. natural kaolinitic clays on their strong acid weathering rates. (en)
skos:notation
  • RIV/61388980:_____/02:50023022!RIV/2003/GA0/A50003/N
http://linked.open.../vavai/riv/strany
  • 171;181
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA203/98/P203), Z(AV0Z4032918)
http://linked.open...iv/cisloPeriodika
  • 1-2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 644154
http://linked.open...ai/riv/idVysledku
  • RIV/61388980:_____/02:50023022
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • kaolinite; illite; dissolution (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [DE5FE0CB60B3]
http://linked.open...i/riv/nazevZdroje
  • Catena
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...ocetUcastnikuAkce
http://linked.open...nichUcastnikuAkce
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 49
http://linked.open...iv/tvurceVysledku
  • Hradil, David
  • Hostomský, Jiří
http://linked.open...n/vavai/riv/zamer
issn
  • 0341-8162
number of pages
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