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XIII.—On the Size of the Particles in Deep-sea Deposits

Published online by Cambridge University Press:  15 September 2014

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Summary

A new method for the mechanical analysis of soils and deposits has been developed. It consists in weighing, from time to time, on a specially constructed balance, the amount of sediment accumulated on a circular disc suspended from the balance near the bottom of a vessel containing an aqueous suspension of the sample. From the “accumulation-curve” thus obtained one finds by a series of mathematical operations a “distribution-curve,” i.e. a curve showing how the amount of particles of a certain size varies with the latter quantity.

This method has been applied to the study of some deep-sea deposits from the Challenger Office. The distribution-curves thus obtained show marked differences for the different samples, and reveal a surprising lack of very fine particles in the deposits from the largest depths, besides suggesting interesting problems for new research.

Type
Proceedings
Copyright
Copyright © Royal Society of Edinburgh 1917

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References

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page 219 note † Résultats des campagnes scientifiques, etc., par Albert I, fasc. xix, “Etude des fonds marins, etc.,” par J. Thoulet, Monaco, 1901. See also J. Thoulet, “Analyse mécanique des sols sous-marines,” Annales des Mines, avril 1900.

page 220 note * Bodenkunde, Berlin, 1905, S. 56.

page 220 note † For further particulars see Internat. Reports on Pedology, vol. v, 257–312 (1915).

page 221 note * This term is used in the Maxwellian sense, i.e. to represent how the number of particles of a certain size varies with that quantity, or rather how the particles are distributed amongst the different sizes.

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page 233 note * Observe that log r = 0 and log r = −∞ correspond respectively to r = 1μμ and r = 0.

page 234 note * The printing having been delayed by the fire at Messrs Neill & Co.'s printing works.