{"refrec":{"BRefID":59042,"RR":"<b>Vincent, P.</b> (1996). Variation in particle size distribution on the beach and windward side of a large coastal dune, southwest France. <i>Sediment. Geol. 103(3-4)</i>: 273-280. <a href=\"http://dx.doi.org/10.1016/0037-0738(95)00110-7\" target=\"_blank\">http://dx.doi.org/10.1016/0037-0738(95)00110-7</a>","BEntID":56637,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Sediment. Geol. 103(3-4)</i>: 273-280. <a href=\"http://dx.doi.org/10.1016/0037-0738(95)00110-7\" target=\"_blank\">http://dx.doi.org/10.1016/0037-0738(95)00110-7</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vincent, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vincent, P.","Englishabstract":"Variation in particle size on the beach and windward slope of Europe's largest coastal dune—the dune du Pilat, southwest France—is studied by means of the log-hyperbolic distribution. Grain size tends to coarsen up the dune as a result of progressive deflation of fines. The dune sands are well-sorted but there is no significant spatial variation in t2. Twenty-one out of twenty-five sand samples have positive p values (negative phi skewness) and there is a weak but significant decline in p towards the beach. 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