Biology
Scientific paper
Dec 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011agufm.p31c1719b&link_type=abstract
American Geophysical Union, Fall Meeting 2011, abstract #P31C-1719
Biology
[0406] Biogeosciences / Astrobiology And Extraterrestrial Materials, [1039] Geochemistry / Alteration And Weathering Processes
Scientific paper
Martian rocks and sediments contain weathering products including clay minerals formed as a result of interaction between rocks and water, and these materials can act as important indicators of past surface conditions on Mars. Weathering of terrestrial volcanic rocks similar to those on Mars produces nano-sized, variably hydrated aluminosilicate and iron oxide minerals, including allophane, imogolite, halloysite, hisingerite, and ferrihydrite. The nanoaluminosilicates can contain isomorphically substituted Fe, which may affect their spectral and physical properties as well as their eventual recrystallization products. Detection and quantification of such minerals in natural environments on Earth is difficult due to their variable chemical composition and lack of long-range crystalline order. Their accurate detection and quantification on Mars requires a better understanding of how composition affects their spectral properties and evolution to more crystalline phases. Aluminosilicate nanoparticles of varying composition were synthesized with isomorphically substituted Fe at Fe:Al ratios of 1:100. Allophanes were synthesized with Al:Si ratios of 2:1, 1:1, and 1:3. The substituted Fe was probed using Fe K-edge X-ray absorption fine structure spectroscopy (XAFS). The XAFS spectrum contains information about the molecular environment surrounding the target atom, and is an ideal technique for studying poorly crystalline materials that are difficult to characterize using bulk methods such as XRD. The near-edge (XANES) and extended (EXAFS) portions of the XAFS spectrum were examined, and allophane backscattering paths were fit using coordinates for a modified nanoball model (1). XANES spectra rule out ferrihydrite in the synthetic samples, suggesting all Fe was incorporated into the aluminosilicate structure. The XAFS results suggest that Fe substituted into the allophane structure is present as Fe(III) in octahedral coordination in a well-ordered sheet. Some Fe substitution in tetrahedral sites occurs in allophane with Al:Si = 2:1, but not in higher-Si compositions. These results support the nanoball model for allophane (1) based on a rolled octahedral sheet and indicate that sheet is well ordered. They do not support proposed models of an incomplete octahedral sheet in high-Si allophanes. Analysis of Fe distribution suggests considerable Fe clustering in the octahedral sheet which increases with sample aging. This clustering could lead to eventual nucleation of a separate Fe (oxyhydr)oxide phase. (1) Creton et al. (2008) J Phys Chem C 112, 358.
Baker Linda
McDaniel P.
Nickerson Ryan D.
Strawn Daniel G.
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