Voids are usually referred to as a certain per centage of the whole volume. A gravel, for ex ample, with 35 per cent of voids, means that in a volume of the gravel occupying 100 cubic feet of space, 35 cubic feet consists of voids or empty spaces that have to be filled.
Having selected the available stone or gravel best adapted for the character of construction desired, any one of several different methods may be employed to determine the percentage of voids.
A gravel, for example, which on being well shaken clown weighs 110 lbs. per cubic foot, is shown by the table to contain 33 per cent of voids.
On account of the stone being measured loose, the voids shown in Table IV call for a little more of the fine material than is needed to just fill the actual voids in the concrete when tamped. They should, however, be used, as they make sufficient allowance to offset possible unevenness hi mixing.
Another method of determining the voids in coarse aggregates, is given by S. B. Newberry, substantially as follows: Use a metal box of exactly one cubic foot capacity. Fill with the material to be tested; shake down well; strike off level; and weigh. Now pour water in, at one corner, until it rises even with the surface; and weigh again. The difference in the weights will be the weight of the water that was added to fill the voids. Now, since one cubic foot of water weighs 62.5 lbs., to find the per centage of the volume occupied by the water that just filled the voids, we divide the weight of the latter by 62.5
and multiply by 100.
Suppose, for example, that the box of dry aggregate weighs 92 lbs., and, when the water is poured in, it weighs 120 lbs. Then 120-92=28 lbs., the weight of the water. The amount of the voids will therefore be (28-i-62.5) X100.44.8 per cent.
If the aggregate is dry and porous, it should be wetted before testing for voids, and then dried just enough to remove all moisture from the surface of the material. In this way the error that might occur through the absorption of water will be eliminated.
The object of pouring in the water at one point only, is to avoid entrapping bubbles of air.
Voids in gravel are seldom less than 30 per cent or more than 45 per cent. Broken stone, being angular, does not compact as readily as gravel, and hence has larger voids, though these will vary in amount, depending upon the charac ter of the stone, whether it is broken by hand or in a crusher, and whether run of crusher is taken or the material has been screened.
Table V., compiled by M. Feret, shows the percentage of voids to be found in round pebbles and broken stone of different sizes, and also in mixtures of different sizes of each of these ag gregates.