Titlebook: Desert Aeolian Processes; Vatche P. Tchakerian Book 1995 Vatche P. Tachakerian 1995 Mineral.North America.desert.environment.geomorphology

怪物

食料

Ibd810

Book 1995mber of papers devoted to aeolian processes and landforms indicated to me that aeolian geomorphology had come of age and the last 15 years or so had produced a plethora of papers, books, and edited volumes on all aspects of aeolian geomorphology. Chapter one is my tentative attempt to place develop­

debris

Melodrama

Malleable

Condescending

https://doi.org/10.1057/9780230355835d from about 8% to 148% of the expected dry threshold velocity, and with 4% moisture increased to 47%–206% of the dry value. Based on the predicted threshold shear velocities, the expected transport rates at a 1% moisture content under a 0.50 m s. shear velocity range from no transport to more than 100 kg m. hr..

intolerance

Modeling Seasonal Patterns of Blowing Dust on the Southern High Plains,xas, from 1947 to 1989. Predictions matched measured values well, especially considering that the measured data were not used to calibrate or obtain regression coefficients. It is concluded that the Texas Tech model is a reasonable simulator of soil movement, dust concentration, and visibility.

Pillory

A Review of the Effects of Surface Moisture Content on Aeolian Sand Transport,d from about 8% to 148% of the expected dry threshold velocity, and with 4% moisture increased to 47%–206% of the dry value. Based on the predicted threshold shear velocities, the expected transport rates at a 1% moisture content under a 0.50 m s. shear velocity range from no transport to more than 100 kg m. hr..

Communicate

The Resurgence of Aeolian Geomorphology,old in 1941 produced few significant works in aeolian geomorphology. More recently, however, the number of papers, edited volumes and conference proceedings has been phenomenal. This ‘renaissance’ in aeolian geomorphology is attributed to a number of interrelated factors including the increased desi