Building Stone(1)
Durability
Durability of rock will be depend on its capacity to stand the attack of the agents of
weathering . Resistance to weathering will be determined by the chemical
stability of constituent mineral which varies within wide limit.
Some minerals being more easily decomposed than others. The
common rock forming minerals when arranged in the order of increasing
resistance to weathering . ( nepheline, lecute, olivine , augite hornblende,
plagioclase, orthoclase, biotite , muscovite, quartz,.) Acid rocks are more durable than the basic
rocks.
Porosity
The shape , size, nature of packing of the grains of a rock
give rise to the property of porosity.
It is expressed as ratio between the total volume of pores spaces and total
volume of rock sample. It expressed in percentage.
Porosity is an important
engineering property in the sense that it accounts for absorption values
of stones. i. e. capacity of stone to absorb moisture when immersed in water
for 72 hours.
Presence of interlocking crystals angular grains abundant
cementing material are responsible for low porosity of stone .highly porous if
composed of spherical or rounded grains
eg. granite quartzite basalts .1 to .5 percent
Sand stone , lime stone 5 to 25 percent
Density
Weight per unit volume of substance 1) Dry density 2) bulk density 3) saturated
density 4) true density
Engineering significance of this is denser rock are stronger
than lighter rock of same composition. Density of stone being known , load
imposed by it at any level in the stone.
Granite 2.7 Basalt 2.9
Sandstone 2.6 Limestone 2.6
Abrasive Resistance
It is more qualitative than quantitative property. It is
defined as resistance which a stone offers to rubbing action. This test is
carried for stones used in along paving road, in flooring, in building and as lining
in tunnels. The safe value for coefficient of wear is 20 . Abrasive resistance is determined with the
help of Dorrys Abrasion testing machine.
Frost and Fire
resistance
Many building stones shows quick disintegration when used in
situation involving frost formation or heating. Frost causes disintegration by
expansion of water , on freezing within the rock pores.
In case of fire it is
unequal expansion in different minerals and also at different depth from
surface inward. This effect becomes more pronounced when rock is first heated
and then suddenly cooled by water. Stone may crumble to pieces under such a
treatment. Rock which are found porous and weak in strength are easily affected
in cold climates by frost action.
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