The importance of a careful grading of dif ferent-sized aggregates as affecting the strength of concrete, is graphically illustrated in the samples of natural bank sand and gravel and limestone screenings shown respectively in Plates 1 and 2. The samples are photographed and reproduced at actual size.
In Plate 1, both samples (A and B) were taken from the same natural bank of sand and gravel of glacial origin, at Attica, Indiana. They differ only in the size of the grains, due to screening; and give, in a general way, a fairly correct idea of the appearance of a well-graded sand. A, the finer sample, contained 34 per cent of voids; B, the coarser, 26.9 per cent. When made up into a 1 :3 mortar—that is, 1 part cement to 3 parts aggregate—the mortar from the coarser material, in one year, developed a compressive strength of 7,750 lbs. per square inch, whereas the finer material gave a mortar having a compressive strength of only 4,475 lbs. per square inch—a difference in strength of over 70 per cent in favor of the coarser material.
A similar relative superiority of coarse as compared with fine material, is shown by the samples of limestone screenings illustrated in Plate 2. Sample A was taken from a crushing plant near St. Louis, Mo., and shows a screening in which the grading is not at all uniform. Sam ple B came from a plant at Greenfield, Ohio, and represents the screenings separated from the crusher-run material by a screen; and it will be noted that, with the exception of the large proportion of fine material, the screenings are very well graded. Sample A contained 42.1 per cent of voids; B, 37.5 per cent. B gave a 1 : 3 mortar having a compressive strength, at one year, of 8,500 lbs. to the square inch, as com pared with only 4,908 lbs. per square inch for A. Here, again, the difference in strength was over 70 per cent in favor of the coarser screenings, showing that a large proportion of fine particles is detrimental to strength.
The relative percentage of voids in two mate rials, one of uniform size and shape, and the of irregular size and shape, is clearly shown by comparing the gravel of Sample B, Plate 1, with a mass of round shot of uniform size. In the irregular gravel, the voids equal 26.9 per cent, while in the shot they equal 47.6 per cent. That is to say, there will be nearly twice the space in gravel to fill with cement if the particles are round and all the same size.
Similar tests were conducted by Sanford E. Thompson in 1905, on Portland cement concrete. The aggregates were all of the same kind of material, varying merely in the sizes of the particles; and the proportion of the cement to the total aggregate by weight remained the same. The results showed a strength of the con crete in some cases two and a-half times what it was in others.