solifluction

solifluction怎么读

英式音标：[sɒlɪ\'flʌkʃən]

美式音标：[ˌsoʊlə\'flʌkʃən]

solifluction的意思释义

n.

泥流，泥流作用；

英英释义

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.

solifluction用法及例句

例句参考

Solifluction rates, processes and landforms: a global review

Morphometric analysis of solifluction lobes and rock glaciers in the Swiss Alps

Solifluction steps and risers, Lee Ridge, Glacier National Park, Montana, USA: a scale and pattern analysis

Rates and processes of periglacial solifluction: an experimental approach

Solifluction processes on permafrost and non‐permafrost slopes: results of a large‐scale laboratory simulation

Snow cover and soil moisture controls on solifluction in an area of seasonal frost, eastern Alps

Morphometry 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...