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VIII.—The Effect of Weather Changes on Soil Temperatures

Published online by Cambridge University Press:  15 September 2014

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Extract

The temperature of the air depends on so many varying factors that its prediction is a matter of considerable difficulty, and can only be made with any degree of certainty when the minimum number of these factors is at work. Underground temperatures are dependent not only on the same factors as affect the air temperature, but, in addition, are much more affected by conductivity, rainfall, evaporation, latent heat, etc., and thus the changes in temperature beneath the surface of the soil constitute a much more complex problem.

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Proceedings
Copyright
Copyright © Royal Society of Edinburgh 1920

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References

page 58 note * The Soil, by King., F. H. The Rural Science Series. Macmillan, 1917.Google Scholar

page 59 note * “On Dew,” by John Aitken, LL.D., F.R.S., Trans. Roy. Soc. Edin., vol. xxxiii.

page 61 note * The Cooling of the Soil at Night, with special reference to Spring Frosts,” by the Author, Proc. Roy. Soc. Edin., vol. xi, 1919–20, part i, No. 2.Google Scholar

page 62 note * F. H. King, Physics of Agriculture, p. 186.

page 63 note * Meteorological Glossary, 1918Google Scholar. M.O. 225, ii, p. 230.

page 65 note * Science and Fruit Farming, by the Duke of Bedford and Spencer Pickering. Macmillan.

page 67 note * F. H. King, The Soil; A. D. Hall, The Soil.

page 77 note * The Weather at Hodsock Priory, Henry Mellish.