Percolation, evaporation, and condensation

Latham, B

doi:10.1002/qj.49703515104

Quart J Royal Meteoro Soc

1909

DOI: 10.1002/qj.49703515104

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Percolation, evaporation, and condensation

B Latham¹

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Drainage and evaporation from fallow soil at Rothamsted

Penman

Schofield

1941

J. Agric. Sci.

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1. Study of the automatic records shows:(a) There is a seasonal change in the drainage response after rain which can be almost wholly ascribed to viscosity changes arising from seasonal changes of soil temperature (p. 77).(b) Evaporation occurring after a fall of rain has no measurable effect on the drainage response to that rain (pp. 78, 87).(c) The maximum drainage rates for the 20 in. gauge are much larger than those for the deeper gauges. The maxima change seasonally and are again primarily dependent on viscosity (p. 78).(d) There is no marked change in the field capacity of the gauge during the year. The air-filled pore space at field capacity may change by about 15% of its average value (p. 81).

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Drainage and evaporation from fallow soil at Rothamsted

Penman

Schofield

1941

J. Agric. Sci.

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A Climatic Index for the Leaching Factor in Soil Formation

Prescott

1950

Journal of Soil Science

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Percolation, evaporation, and condensation

Cited by 2 publications

References 0 publications

Drainage and evaporation from fallow soil at Rothamsted

Drainage and evaporation from fallow soil at Rothamsted

A Climatic Index for the Leaching Factor in Soil Formation

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