Field Observations of Aeolian Sand Transport Rate Using a Piezoelectric Ceramic Sensor This study conducted field observations in terms of the number

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1 Field Observations of Aeolian Sand Transport Rate Using a Piezoelectric Ceramic Sensor This study conducted field observations in terms of the number of blown sand impacts and wind velocity in the period of Jan 2005 at an open ocean beach in Japan, in order to investigate effects of meteorological change on the aeolian sand transport. A regression curve of relationship between wind velocity and impact counts during a no rainfall phase in the field coincided with wind-tunnel experimental results of Ni et al. (2002) and Hotta et al. (2006), indicating that the piezoelectric sensor measuring the impact counts is a useful tool to observe the sand flux in the field. The counts (sand flux) for wind direction in cross-shore direction decreased by one order of magnitude due to a change in the wind direction from longshore to cross-shore and then by more than one order due to an increase in the moisture content.

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5 Baas, A.C.W.(2004): Evaluation of saltation flux impact responders (Safires) for measuring instantaneous aeolian sand trans- port intensity, Geomorphology, vol.59, pp Bagnold, R.A.(1941): The Physics of Blown Sand and Desert Dunes, Methuen, London, 265p. Bauer, B.O. and Namikas, S.L.(1998): Design and field test of a continuously weighing, tipping-bucket assembly for aeolian sand traps, Earth Surface Processes and Landforms, vol.23, pp Butterfield, G.R.(1991): Grain transport rates in steady and unsteady turbulent airflows, Acta mechanica, [Supple.] 1, pp Charnock, H.(1955): Wind stress on a water surface, The Quarterly Journal of the Royal Meteorological Society, vol.81, pp Cornelis, W.M. and Gabriels, D.(2003): The effect of surface moisture on the entrainment of dune sand by wind: an evaluation of selected models, Sedimentology, vol.50, pp Dong, Z., Liu, X., Wang, X., Li, F., and Zhao, A.(2004): Experimental investigation of the velocity of a sand cloud blowing over a sandy surface, Earth Surface Processes and Landforms, vol.29, pp Gillies, J.A. and Berkofsky, L.(2004): Eolian suspension above the saltation layer, the concentration profile, Journal of Sedimentary Research, vol.74, pp Greeley, R., Blumberg, D.G. and Williams, S.H.(1996): Field measurements of the flux and speed of wind-blown sand, Sedimentology, vol.43, pp Hotta, S., S. Kubota, N. Nakamura, and K. Hosaka (2006): Wind tunnel study of vertical distribution of sand transport rate by wind, Proceedings of the 30th International Conference on Coastal Engineering, ASCE, pp.2604?2616. Iversen, J.D., and K.R. Rasmussen (1999): The effect of wind speed and bed slop.on sand transport, Sedimentology, 46, pp.723?731. Jackson, D.W.T. (1996) A new, instantaneous aeolian sand trap for field use. In: Sedimentology, 43, pp Ni, J.R., Li, Z.S. and Mendoza, C. (2002): Vertical profiles of aeolian sand mass flux, Geomorphology, vol.49, pp Owen, P.R.(1964): Saltation of uniform grains in air, Journal of Fluid Mechanics, vol.20, pp Rasmussen, K.R. and Mikkelsen, H.E.(1998): On the efficiency of vertical array aeolian field traps, Sedimentology, vol. 45, pp Raupach, M.R.(1991): Saltation layers, vegetation canopies and roughness lengths, Acta mechanica, [Supple] 1, pp Stockton, P.H. and Gillette, D.A.(1990): Field measurement of the sheltering effect of vegetation on erodible land surfaces, Land degradation & rehabilitation, vol.2, pp

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