Experimental study of abrasion on pebbles

Authors

  • Alberto Sarmiento Alarcón Servicio Geológico Nacional

DOI:

https://doi.org/10.32685/0120-1425/bolgeol8.1-3.1960.389

Keywords:

Alteration, rotary barrel, wear, hardness, sphericity, transport

How to Cite

Sarmiento Alarcón, A. (1960). Experimental study of abrasion on pebbles. Boletín Geológico, 8(1-3), 169–226. https://doi.org/10.32685/0120-1425/bolgeol8.1-3.1960.389

Issue

Section

Articles

Published

1960-01-01

Abstract

The loading of streams is affected by two very distinct processes, namely: a) abrasion and alteration due to chemical agents during transport, including breaking up or fragmentation of the pebbles in route, and b) sorting action or selective transport. Since it is almost impossible to determine by direct observation of the material transported by water currents, which is the decrease in size due to one or the other of these processes, the sediment researcher must separate each of them in the laboratory, where they can be studied independently using experiments.

For this purpose, rotating barrels have been used to study abrasion. In this apparatus, the load is subjected to wear while retaining its identity during the experiment.

This thesis is concerned with fragments of size between 4 and 6 mm in diameter (pebble range) and is an attempt to observe the effects of abrasion as it relates to size, sphericity, and roundness.

References

A. DAUBREE. Études Synthétiques de Géologie Expérimentale, Vol. I (París: Dunod, 1879).

C. K. WENTWORTH. "A Laboratory and Field Study of Cobble Abrasion". Jour Geol., Vol. XXVII (1919), pp. 507-22; "The Shape of Pebbles", U. S. Geol. Surv. Bull. 730 (1922), pp. 103-14; "Pebble Wear on the Jarvis Island Beach", Washington University Studies Sci. and Tech. N° 5 (1931), pp. 11-37.

G. E. ANDERSON. "Experiments on the Rate of Wear of Sand Grains", Jour Geol., Vol. XXXIV (1926), pp. 144-58.

P. MARSHALL. "The Wearing of Beach Gravels", Trans. New Zealand Inst., Vol. LVIII (1927), pp. 507-32; "Collois Substances Formed by Abrasion", ibid., Vol. LX ( 1929), pp. 324-65.

ARTHUR B. COZZENS. "Rate of Wear of Common Mineral". Washington University Studies Sci. and Tech. N° 5 (1931) 71-80.

A. SCHOLITSCH. "Uber die Verkleinerung der Geschiebe in Flusslaufen", Sitzemgersber d. Akad d. Eissensch in Wien, Vol. CXLII, Part. 11 (1933), pp. 343-66. Uber Schleppkarft und Geschiebebewegung (Leipzig, 1914), p. 12.

GEORGE A. THIEL. "The Relative Resistance of Abrasion of Mineral Grains of Sand Size", Jour. Sed. Vol. X (1940), N° 3, 103-23.

B W. C. KRUMBEIN. "The Effects of Abrasion on the Size, Shape and Roundness of Rock Fragments, Jour. Geol., Vol. XLIX (1941), 482-520.

KRUMBEIN. "Measurement and Geological Significance of Shape and Roundness of Sedimentary Particles", Jour. Sed. Petr., Vol. 11, N° 2 (1941), pp. 64-72.

KRUMBEIN. "Sediments and Exponential Curves", Jour. Geol., Vol. XLV (1937), pp. 577-601.

KRUMBEIN, "The Effects of Abrasion on the Size, Shape and Roundness of Rock Fragments", op. cit., pp. 482-520.

F. J. PETTIJOHN AND A. C. LUNDAHL. "Shape and Roundness of Lake Erie Beach Sands", Jour Sed. Petr. Vol. 13, N° 2, pp. 67-78.

R. DANA RUSSELL AND R. E. TAYLOR. "Roundness and Shape of Mississipi River Sands", Jour. Geol., Vol. XLV (1937), pp. 225-67.

GEORGE A. THIEL. "The Relative Resistance to Abrasion of Mineral Crains of Sand Size", op. cit.

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