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Titlebook: Aeolian Sand and Sand Dunes; Kenneth Pye,Haim Tsoar Book 2009 Springer-Verlag Berlin Heidelberg 2009 Aeolian.Dunes.Pye.Sand.geomorphology.

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期刊全称Aeolian Sand and Sand Dunes
影响因子2023Kenneth Pye,Haim Tsoar
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发行地址Almost encyclopedic in its coverage of topics.Includes supplementary material:
图书封面Titlebook: Aeolian Sand and Sand Dunes;  Kenneth Pye,Haim Tsoar Book 2009 Springer-Verlag Berlin Heidelberg 2009 Aeolian.Dunes.Pye.Sand.geomorphology.
影响因子It 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
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The Formation of Sand Seas and Dune Fields,ussed, including climate, topography, the distribution of large sand sources, and regional-scale sand transport pathways. The response of sand seas and dunefields to changes in climate and sea level is also discussed.
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Aeolian Bed Forms,tics and development of each of these bedform types, including their relationship to airflow and sand transport at different spatial and temporal scales. The effect of vegetation on dune morphology and rate of movement is considered, and the factors which control the broad-scale morphology of aeolia
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Post-Depositional Modification of Dune Sands,nudation, compaction, addition of airborne dust, weathering, soil development and cementation by carbonates, salts, iron oxides and organic matter. This chapter reviews the factors which control these changes and the nature of the resulting sediments.
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Kenneth Pye,Haim TsoarAlmost encyclopedic in its coverage of topics.Includes supplementary material:
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