Titlebook: Landslide Science for a Safer Geoenvironment; Volume 3: Targeted Kyoji Sassa,Paolo Canuti,Yueping Yin Conference proceedings 2014 Springe

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書目名稱Landslide Science for a Safer Geoenvironment影響因子(影響力)




書目名稱Landslide Science for a Safer Geoenvironment影響因子(影響力)學科排名




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書目名稱Landslide Science for a Safer Geoenvironment網(wǎng)絡公開度學科排名




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書目名稱Landslide Science for a Safer Geoenvironment被引頻次學科排名




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書目名稱Landslide Science for a Safer Geoenvironment讀者反饋學科排名

ROOF

Introduction: Debris Flowsterest in the study of debris flows, from triggering events to rheological properties determination, damages, design and efficiency of retention structures, role of vegetation, dating, hazard zonation and alarming.

花費

Dendrogeomorphic Chronologies of Debris Flows for the Crimean Mountains (Ukraine)lear signs of damage induced by past debris-flow activity. We date a total of 215 debris flows back to AD 1701 and observe a mean decadal frequency of 6.9 events, with a peak in activity during the 1940s (20 events).

軟弱

by the International Consortium on Landslides (ICL) in June 2014. The complete collection of papers from the Forum?is published in three full-color volumes and one mono-color volume. .978-3-319-38000-1978-3-319-04996-0

yohimbine

Genistein

Experimental Study on the Rheological Behaviour of Fine-Grained Soils with Sand Content and Liquidid viscosity tend to increase with increasing concentration by volume(C.) of the fluid matrix. The values of the four coefficients α., α., β., and β. were obtained by regression analysis for each fine-grained soil.

ANT

冬眠

Control Effect of Vegetation on Debris Flows: A Case Study in Batang County, Southwest Chinas means that the lower the vegetation coverage, especially forest coverage, the more frequently SDFs occur. This correspondence relationship does not exist in the GDFs. Forest coverage excludes the impacts of shrubland and meadows, thus more accurately reflects the constraining effects of vegetation

短程旅游

nurture

The Influence of Accumulated Precipitation on Debris Flow Hazard Areaea is proportional to precipitation, and the thickness of maximum debris flow accumulation is between 1.62 m and 2.13 m. The relation between accumulated precipitation and hazard area can provide officials additional information on resident evacuation.