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Weathering of a Metal Artifact in a Saharan Environment: Evidence for a Novel Form of Desert Varnish

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A dark-brown coating on the exterior of a World War II metal fuel can recovered in southwestern Egypt may be a variation of the desert varnish that develops on rock surfaces in arid regions. This suggestion is supported by results of infrared spectroscopic work, x-ray diffraction, scanning electron microscopic studies, and x-ray fluorescence. Exterior portions of the can resemble heavily varnished rock, differing completely in appearance and texture from rusty areas which had developed on portions of the interior surface. The coating consists principally of microscopic mineral deposits, some of which appear to be largely Fe-oxides and Fe-oxy-hydroxides. However many deposits are assemblages of Fe-oxides, clay minerals, and other elements typically occurring in forms of desert varnish often observed on the undersides of desert pavement stones in contact with the soil. Associated with the mineral matter is an organic component apparently deriving from residues of an original paint layer which had been removed by wind/sand scouring.

Keywords: Desert varnish; Infrared; Weathering of metal; World War II artifact; X-ray diffraction; X-ray fluorescence

Document Type: Research Article

DOI: http://dx.doi.org/10.1366/0003702884429111

Affiliations: 1: U.S. Army Engineer Topographic Laboratories, Ft. Belvoir, Virginia 22060-5546 2: U.S. Geological Survey, 957 National Center, Reston, Virginia 22092 3: U.S. Geological Survey, Flagstaff, Arizona 86001

Publication date: July 1, 1988

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