Orthoclase surface structure dissolution measured in situ by x-ray reflectivity and atomic force microscopy.
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.
- Research Organization:
- Argonne National Lab., IL (US)
- Sponsoring Organization:
- US Department of Energy (US)
- DOE Contract Number:
- W-31-109-ENG-38
- OSTI ID:
- 768634
- Report Number(s):
- ANL/ER/CP-103540; TRN: AH200123%%309
- Resource Relation:
- Conference: Water-Rock Interaction 10, Villasimius (IT), 06/10/2001--06/15/2001; Other Information: PBD: 28 Nov 2000
- Country of Publication:
- United States
- Language:
- English
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