solifluction

听听怎么读
英 [sɒlɪ'flʌkʃən]
美 [ˌsoʊlə'flʌkʃən]
是什么意思
  • n.

    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

    学习怎么用

    权威例句

    Solifluction
    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...
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