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Observations of and remarks on the movement of moisture and frost-heavuig in soil.

, : Observations of and remarks on the movement of moisture and frost-heavuig in soil.. Z. Acker- u. PflBau, 108: 375-383

In a heavy soil with a low water table, the magnitude of soil-heaving was recorded during the winter season in relation to soil temperature and moisture and snow cover. Soil-heaving occurred immediately after the start of frost and reached a maximum of 23 mm at a time when the soil contained 20% moisture to a depth of 50-60 cm.

Accession: 014123663

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Related references

Feng, C.L.; Chen, L.I., 1958: Soil moisture problems of the North China plain and its associated areas. 1. The mechanism of moisture diffusion in soil and profile impedance to movement of soil moisture.. Soil-moisture problems are grouped into five categories according to the method of soil-moisture loss. The rate of moisture diffusion in soil from heavy clay horizons was correlated inversely with penetration pressure. Penetration pressure of the...

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