A mathematical model of the initial stage of blowing of dry equigranular soil.

Glazunov G. P.; Gendugov V. M.

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A mathematical model of the initial stage of blowing of dry equigranular soil.

机译：吹干等粒土壤初始阶段的数学模型。

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Equations describing the threshold wind velocity for a dry equigranular soil with insignificant interparticle cohesion, the minimum threshold wind velocity as a function of particle size, and the non-dimensional threshold wind velocity were developed and checked against experimental data.

机译：建立了描述颗粒间内聚力不明显的干燥等粒土壤的阈值风速，最小阈值风速随颗粒尺寸变化以及无量纲阈值风速的方程式，并根据实验数据进行了检验。

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《Moscow University Soil Science Bulletin》 |2009年第1期|共7页
作者
Glazunov G. P.; Gendugov V. M.;
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正文语种 eng
中图分类农业基础科学;
关键词
equations; erosion; mathematical models; particle size; wind erosion; wind speed;

机译：方程;侵蚀;数学模型;粒径;风蚀;风速;

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A mathematical model of the initial stage of blowing of dry equigranular soil.

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