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Water absorption

Physical quantity indicating the degree of water absorption of an object under normal atmospheric pressure
It means that the object is normal Atmospheric pressure Imbibitive physical quantity , expressed as a percentage.
Chinese name
Water absorption
Foreign name
coefficient of water absorption

Determination purpose

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Geological work Middle: ① Determination rock The purpose of water absorption is to evaluate some building material The quality of minerals mine Provide data basis for mining design and solving relevant engineering geological problems. Water absorption of rock Mainly determined by porosity Size of. adopt Feeding hopper Join to Glass perforated plate Start the stopwatch at the same time to record different times Glass capillary Reading of internal scale (ml). The measured time is as follows: 15 seconds, 30 seconds, 45 seconds, 1 minute, 2 minutes, 5 minutes, 10 minutes, 20 minutes, 30 minutes, 60 minutes, 90 minutes, 120 minutes.
material Water absorption Of measurement It refers to the increase of material immersed in water for a certain time at a certain temperature Weight percentage

General rock

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As follows:
Granite 0.07%~0.30% (weight%)
Marble 0.06﹪~ 0.45﹪
quartz 0.10﹪~ 2.00﹪

Stone

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Water absorption refers to Stone stay normal atmospheric pressure The ability to absorb water. with Stone The absorbed water shall be measured and percentage Indicates it. Stone The water absorption of is determined by the number and size of the voids and the way the particles are arranged. Stone It depends on whether it is easy to get wet and the condition of removing air from the gap. The smaller the water absorption Stone The denser the harder, such as igneous rock Its water absorption is often less than 1%, and some dense sedimentary rock About 3%, some loose sedimentary rock be Changda 8% or more. The greater the water absorption of stone, the worse its engineering properties.
igneous rock The water absorption rate of Stone The invasion surface of the middle capillary is transferred to the other side. We often see Stone Uneven wetting on the surface is such a phenomenon Capillary action Typical of. Generally, igneous rock The capillary system of feldspar as well as olivine pyroxene Hornblende Biotite Iron and magnesium contained in, etc mineral And the interface crack surface.
Five pieces can be prepared for measuring water absorption Stone The volume of each piece is about 50 cubic centimeters. Remove the dust first, dry it completely, and then weigh it. After the weight is obtained, put it in Measuring cylinder Scrubber Or other containers, submerge to a quarter of the height of the sample with water for two hours; Add water to the half height of the sample, and then soak for three hours; Add water to submerge the sample to a height of three fourths until the sample is completely submerged; Then place the sample in water Twenty-four hours , then take it out, wipe it gently with a cloth and weigh it, then press the following formula Stone Calculate the water absorption of: W=(B-G)/G × 100%, where W is the water absorption, expressed as a percentage, G is the weight of the sample after drying, in grams, and B is the weight of the sample after saturated with water, in grams.