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Orthoclase surface structure dissolution measured in situ by x-ray reflectivity and atomic force microscopy.


DE2001768634

Publication Date 2000
Personal Author Sturchio, N. C.; Fenter, P.; Cheng, L.; Teng, H.
Page Count 7
Abstract Orthoclase (001) surface topography and interface structure were measured during dissolution by using in situ atomic force microscopy (AFM) and synchrotrons X-ray reflectivity at pH 1.1-12.9 and T = 25-84 C. Terrace roughening at low pH and step motion at high pH were the main phenomena observed, and dissolution rates were measured precisely. Contrasting dissolution mechanisms are inferred for low- and high-pH conditions. These observations clarify differences in alkali feldspar dissolution mechanisms as a function of pH, demonstrate a new in situ method for measuring face-specific dissolution rates on single crystals, and improve the fundamental basis for understanding alkali feldspar weathering processes.
Keywords
  • Atomic force microscopy
  • Dissolution
  • Monocrystals
  • Surface properties
  • Feldspars
  • Reflectivity
  • Weathering
  • Interfaces
  • Rock-fluid interactions
Source Agency
  • Technical Information Center Oak Ridge Tennessee
Corporate Authors Argonne National Lab., IL.; Department of Energy, Washington, DC.
Document Type Conference Proceedings
NTIS Issue Number 200125
Contract Number
  • W-31-109-ENG-38
Orthoclase surface structure dissolution measured in situ by x-ray reflectivity and atomic force microscopy.
Orthoclase surface structure dissolution measured in situ by x-ray reflectivity and atomic force microscopy.
DE2001768634

  • Atomic force microscopy
  • Dissolution
  • Monocrystals
  • Surface properties
  • Feldspars
  • Reflectivity
  • Weathering
  • Interfaces
  • Rock-fluid interactions
  • Technical Information Center Oak Ridge Tennessee
  • W-31-109-ENG-38
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