OBJECTIVE :
To determine specific gravity of a given sample of fine aggregate.
APPARATUS:
Pycnometer, A 1 000-ml measuring cylinder,
well-ventilated oven, Taping rod, Filter papers and funnel, etc.
THEORY:
Sand particles composed of quartz have a specific gravity between 2.65 to 2.67. While inorganic clays generally range from 2.70 to 2.80. Soils with large amounts of organic matter or porous particles (such as diatomaceous earth) have specific gravity below 2.60 (Some range as low as 2.00).
The specific gravity of an aggregate is considered as the measure of strength or quality of the material. Specific gravity is defined as the ratio of weight of a given volume of aggregate to the weight of equal volume of water. Aggregates having low specific gravity are generally weaker than those with aggregates having high specific gravity. This property helps in a general identification of aggregates.
PROCEDURE:
1. Sample of
about 500 g shall be placed in the tray and covered with distilled water at a
temperature of 22 to 32°C.. The sample shall remain immersed for 24 ± l/2
hours.
2. The water shall then be carefully drained from the
sample. The saturated and surface-dry sample shall be weighed (weight A).
4. The contents of the Pycnometer shall be emptied into
the tray, The Pycnometer shall be refilled with distilled water to the same
level as 21 before, dried on the outside and weighed (weight C).
CALCULATIONS : Specific gravity, apparent specific gravity and water &absorption shall be calculated as follows:
Specific gravity =....................
Apparent Specific gravity...............
water absorption............
A = weight in g of saturated surface-dry sample,
B = weight in g of Pycnometer or gas jar containing sample and filled with distilled water,
C =weight in g of Pycnometer or
gas jar filled with distilled water only ,and D = weight in g of oven-dried
sample.
RESULTS :
1. The Specific Gravity of a
given sample of fine aggregate is found to be …….
2. The Water Absorption of a given sample of fine aggregate is found to be ……. %
0 Comments