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  • Perthitic feldspar weathered in batch reactor (weight ratio feldspar/water ~ 4/15) during long-term (300 day) laboratory experiments at ambient conditions. During first 50 days of the experiment, aqueous concentrations of Si, Al, K, Na, and Ca reached limiting values 3.4x10-4, 9.2x10-5, 1.5x10-4, 1.2x10-4, 1.1x10-4 mol/l, respectively. Despite the fact, the studied system was still far away from equilibrium. High supersaturation with respect to secondary minerals (gibbsite, pyrophyllite, Ca-beidellite, K-beidellite, Na-beidellite, and kaolinite) and to primary minerals (albite and K-feldspar) was reached in the solution. Reaction paths on predominant stability diagrams crossed the stability field of gibbsite and kaolinite, and points to the Na-beidelite and K-feldspar stability fields. Based on X-ray diffraction, only muscovite and illite were proved. Electron microprobe analyses showed decreasing Al/Si stoichiometry of secondary phases during time.
  • Perthitic feldspar weathered in batch reactor (weight ratio feldspar/water ~ 4/15) during long-term (300 day) laboratory experiments at ambient conditions. During first 50 days of the experiment, aqueous concentrations of Si, Al, K, Na, and Ca reached limiting values 3.4x10-4, 9.2x10-5, 1.5x10-4, 1.2x10-4, 1.1x10-4 mol/l, respectively. Despite the fact, the studied system was still far away from equilibrium. High supersaturation with respect to secondary minerals (gibbsite, pyrophyllite, Ca-beidellite, K-beidellite, Na-beidellite, and kaolinite) and to primary minerals (albite and K-feldspar) was reached in the solution. Reaction paths on predominant stability diagrams crossed the stability field of gibbsite and kaolinite, and points to the Na-beidelite and K-feldspar stability fields. Based on X-ray diffraction, only muscovite and illite were proved. Electron microprobe analyses showed decreasing Al/Si stoichiometry of secondary phases during time. (en)
  • Perthitic feldspar weathered in batch reactor (weight ratio feldspar/water ~ 4/15) during long-term (300 day) laboratory experiments at ambient conditions. During first 50 days of the experiment, aqueous concentrations of Si, Al, K, Na, and Ca reached limiting values 3.4x10-4, 9.2x10-5, 1.5x10-4, 1.2x10-4, 1.1x10-4 mol/l, respectively. Despite the fact, the studied system was still far away from equilibrium. High supersaturation with respect to secondary minerals (gibbsite, pyrophyllite, Ca-beidellite, K-beidellite, Na-beidellite, and kaolinite) and to primary minerals (albite and K-feldspar) was reached in the solution. Reaction paths on predominant stability diagrams crossed the stability field of gibbsite and kaolinite, and points to the Na-beidelite and K-feldspar stability fields. Based on X-ray diffraction, only muscovite and illite were proved. Electron microprobe analyses showed decreasing Al/Si stoichiometry of secondary phases during time. (cs)
Title
  • Experimentální zvětrávání perthitického živce
  • Experimentální zvětrávání perthitického živce (cs)
  • Experimental weathering of perthitic feldspar (en)
skos:prefLabel
  • Experimentální zvětrávání perthitického živce
  • Experimentální zvětrávání perthitického živce (cs)
  • Experimental weathering of perthitic feldspar (en)
skos:notation
  • RIV/00216224:14310/04:00030680!RIV10-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • S, Z(MSM 143100004)
http://linked.open...iv/cisloPeriodika
  • 1
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
  • 563850
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/04:00030680
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • experiment; modeling; perthitic feldspar; saturation; secondary phase; weathering (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [678D832F4DC8]
http://linked.open...i/riv/nazevZdroje
  • Geologické výzkumy na Moravě a ve Slezsku v r. 2003
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • XI
http://linked.open...iv/tvurceVysledku
  • Faimon, Jiří
  • Vybíhal, Karel
http://linked.open...n/vavai/riv/zamer
issn
  • 1212-6209
number of pages
http://localhost/t...ganizacniJednotka
  • 14310
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