Aeolian Sand and Sand DunesIt is more than half a century since the publication of R. A. Bagnold’s classic book The physics of blown sand and desert dunes, and it is a tribute to the quality of Bagnold’s work that many of the fundamental principles which he developed - main valid today. His book continues to be essential reading for any serious s- dent of aeolian processes. However, the past two decades have seen an explosion in the scale of research dealing with aeolian transport processes, sediments, and landforms. Some of this work has been summarized in review papers and edited conference proceedings, but this book provides the rst attempt to review the whole eld of aeolian sand research. Inevitably, it has not been possible to cover all - pects in equal depth, and the balance of included material naturally re ects the - thors’ own interests to a signi cant degree. However, our aim has been to provide as broad a perspective as possible, and to provide an entry point to an extensive mul- disciplinary scienti c literature, some of which has not been given the attention it deserves in earlier textbooks and review papers. Many examples are drawn from existing published work, but the book also makes extensive use of our own research in the Middle East, Australia, Europe, and North America. The book has been written principally for use by advanced undergraduates, po- graduates, and more senior research workers in geomorphology and sedimentology. |
Contents
1 | |
8 | |
Characteristics of Windblown Sediments | 51 |
Mechanics of Aeolian Sand Transport | 99 |
The Formation of Sand Seas and Dune Fields 141 | 140 |
Aeolian Bed Forms | 175 |
Internal Sedimentary Structures of Aeolian Sand Deposits 255 | 254 |
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Common terms and phrases
accumulation active aeolian sand angle areas atmosphere average Bagnold barchan become carbonate cement changes coastal dune contain cover crest depends deposits described diameter direction distribution downwind dune sands dust effect energy equation erosion et al face fences flow force formation friction grains height higher horizontal impact important increase indicated initial known laminae larger layer less lift force linear dunes lower maximum mean measured moisture move movement nature North observed occur particles period plant Pleistocene present pressure processes quartz range regime region relatively result ridges ripple rounded saltation samples sand dunes sand sheets sand transport scale sediment shape shear showing shown slope soil sorted stress structures studies suggested surface Table temperature term threshold transverse trap Tsoar types typically vegetation weathering wide wind velocity