《solifluction》怎以读
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《solifluction》是什么意思
泥流，泥流作用；
英英释义
Solifluction
- In geomorphology, solifluction is a slow mass wasting slope process, occurring in periglacial environments. Solifluction describes the slow downslope movement of water-saturated sediment due to recurrent freezing and thawing of the ground, affected by gravity.
以上来源于:Wikipedia
学习《solifluction》怎么用
权威例句
SolifluctionSolifluction rates, processes and landforms: a global reviewMorphometric analysis of solifluction lobes and rock glaciers in the Swiss AlpsSolifluction steps and risers, Lee Ridge, Glacier National Park, Montana, USA: a scale and pattern analysisRates and processes of periglacial solifluction: an experimental approachSolifluction processes on permafrost and non‐permafrost slopes: results of a large‐scale laboratory simulationSnow cover and soil moisture controls on solifluction in an area of seasonal frost, eastern AlpsMorphometry and Late Holocene activity of solifluction landforms in the Sierra Nevada, southern Spain.Solifluction-induced modifications of archaeological levels: simulation based on experimental data from a modern periglacial slope a...Laboratory simulation of periglacial solifluction: Significance of porewater pressures, moisture contents and undrained shear streng...