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  • Elsevier  (1)
  • Society of Exploration Geophysicists (SEG)  (1)
  • 1
    Publication Date: 2012-07-01
    Description: The detection and localization of statistically significant spatial clustering of buried metal artifacts for applications, including archaeological, environmental site assessment, and civil infrastructure mapping, can be performed reliably, inexpensively, and noninvasively using transient electromagnetic (EM) geophysics. The local Gi*(d) statistic based on a weighted spatial autocorrelation were used to detect and localize statistically significant clustering of buried metal objects from gridded electromagnetic responses acquired at a seeded control site and at an active historical archaeological site in Paint Rock, Texas. This statistic compares the local EM millivolt response values about point i radially to the global mean and variance to calculate the Gi* statistic as a standard variate at various length scales, which can therefore be assessed for significance. Because the local Gi*(d) statistic compares local to global averages, it spatially compacts the amplitude response signal of the EM data. The resulting spatial cluster maps conformed well to the known distribution of metal targets buried at the control site, and enabled a successful excavation strategy with a significant reduction in false positives encountered at the archaeological site, when compared with more traditional methods.
    Print ISSN: 0016-8033
    Electronic ISSN: 1942-2156
    Topics: Geosciences , Physics
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  • 2
    Publication Date: 2022-01-31
    Description: Protodunes emerge from a flat sand bed at the upwind margin of White Sands Dune Field, and, over several hundred meters, transition into fully developed dunes. Here, we investigate spatial and temporal changes in topography across this transition from 2007 to 2016 using lidar-derived topography, structure-from-motion-derived topography, and RTK GPS. We characterize the deposits present in 2015 using ground penetrating radar. Symmetric protodunes give way downwind to an asymmetric protodune at the transition to slipface development. Between 2007 and 2016, protodune amplitude increased from 0.2 m to 4.0 m, migration rate increased from 3.2 m/yr to 6.1 m/yr, and wavelength increased from 76 m to 122 m. Ground-penetrating radar surveys show strata between flat and 15° make up the stratigraphic architecture of the protodunes. Strata increase in steepness commensurate with an increase in amplitude. Decimeter accumulations of low-angle strata associated with initial protodune stages give way to 4 m of accumulation composed of sets up to 1 m thick prior to slipface development. Topsets present in the thickest sets indicate near critical angles of bedform climb. Growth and slipface development occur by aerodynamic sand trapping and protodune merging. Changes in asymmetry erase initial slipfaces prior to permanent slipface development, after which efficient sand trapping and scour promotes the transition to a dune across 20 m in 5 years. Protodune stratification has hallmarks of sandsheet stratification and can be appreciated within the greater suite of processes that create low-angle eolian stratification found in modern and ancient environments.
    Type: Article , PeerReviewed
    Format: text
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