Energy regimes for aeolian sand grain surface textures

Abstract An experimental study of aeolian sand grain surface texture development was undertaken with an air-driven grain-recirculating desktop apparatus. Scanning electron microscope analysis of resulting textures indicated that different texture types can be associated with distinct zones in a grain-shape/grain speed matrix. In particular, for subrounded and rounded grains, low and high energy transport can be unequivocally distinguished by the occurrence of upturned plates and Hertzian frustra respectively. Textural development does not have a simple relationship to grain velocity, but appears to relate to the energy expended per unit area within the contact zone generated by elastic deformation during impact. Hertzian theory was adapted to irregular sand grain shapes and close agreement was found between experimental results and theoretical predictions for textural development. Results of this study improve our ability to reconstruct palaeoaeolian environments and therefore our ability to determine grain provenance; in particular, the latter is shown to have direct relevance to forensic inquiries and terrorism investigations.

[1]  D. Krinsley,et al.  Eolian transport textures on the surfaces of sand grains of Early Triassic age , 1976 .

[2]  B. Bhushan,et al.  Introduction to Tribology , 2002 .

[3]  B. Lawn Fracture of Brittle Solids by Brian Lawn , 1993 .

[4]  E. Rabinowicz,et al.  Friction and Wear of Materials , 1966 .

[5]  J. Robertson,et al.  Quartz grain surface textures of soils and sediments from Canberra, Australia: A forensic reconstruction tool , 2010 .

[6]  J. C. Doornkamp,et al.  Atlas of Quartz Sand Surface Textures , 1973 .

[7]  R M Morgan,et al.  Sediment fingerprints: a forensic technique using quartz sand grains. , 2006, Science & justice : journal of the Forensic Science Society.

[8]  I. Finnie,et al.  The Mechanism of Material Removal in the Erosive Cutting of Brittle Materials , 1966 .

[9]  Andrew Warren,et al.  Geomorphology in deserts , 1973 .

[10]  D. Krinsley,et al.  The relation between the crystallography of quartz, and upturned aeolian cleavage plates , 1980 .

[11]  D. Krinsley,et al.  Wind velocities determined from the surface textures of sand grains , 1980, Nature.

[12]  Michael V. Swain,et al.  Indentation fracture in brittle rocks and glasses , 1976 .

[13]  D. B. Smith,et al.  A selective SEM study of grains from the Permian Yellow Sands of north- east England , 1981 .

[14]  Adhesion and abrasion of surface materials in the Venusian aeolian environment , 1991 .

[15]  B. Lawn,et al.  Indentation fracture: principles and applications , 1975 .

[16]  D. Campbell Percussion marks on quartz grains , 1963 .

[17]  M. Clarke,et al.  Late-Holocene sand invasion and North Atlantic storminess along the Aquitaine Coast, southwest France , 2002 .

[18]  J. J. O'Connor,et al.  The effect of the indenter elasticity on the Hertzian fracture of brittle materials , 1973, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

[19]  A. Arbogast Stratigraphic evidence for late-holocene aeolian sand mobilization and soil formation in south-central Kansas, U.S.A. , 1996 .

[20]  P. Miller,et al.  Sub-surface mechanical damage distributions during grinding of fused silica , 2005 .

[21]  K. Pye Aeolian dust and dust deposits , 1987 .

[22]  Andrew Warren,et al.  Aeolian Geomorphology: An Introduction , 1996 .

[23]  Michael V. Swain,et al.  Impact of small steel spheres on glass surfaces , 1977 .

[24]  Peter A. Bull,et al.  Environmental reconstruction by electron microscopy , 1981 .

[25]  W. Mahaney Atlas of Sand Grain Surface Textures and Applications , 2002 .