abrasives ©2009 dr b c paul acknowledgement is given to the following sources sme industrial...
TRANSCRIPT
Abrasives
©2009 Dr B C Paul
Acknowledgement is given to the following sources SME Industrial Minerals, mcrocks.com, geology.com, webmineral.com, mindat.org, USGS, cs.cmu.edu,
yuprocks.com, gc.maricopa.edu
Good Abrasives
• They are cheap
• They last a long time
• They cut or wear surfaces that you want cut or worn quickly
• They don’t cut things you don’t want them to
• Hardness is an obvious important factor
• Size and shape also are important
Diamonds
• Hardness of the diamond is unmatched and for many applications they are irreplaceable for cutting– Industrial diamonds lack the color and
perfection of jewlery
• Major uses– Diamond bits for rock and concrete– Diamond dies for wire drawing– Diamond tipped tools and wheels
Diamond Locations
• Diamonds are typically found in Kimberlite and Lamproite intrusions
• The intrusions can be as recent as the Cenozoic– Diamonds themselves are usually older
• Most are 3,200,000,000 to 990,000,000 years old• A few have been found back to 4,200,000,000
• All seem to be associated with Archean basement (maybe a few younger)
Roots of Continents Deeper than Crust
At these depths stable form of carbon switches from graphite to Diamond
Melts Coming Up from Depth Drag Diamonds to the Surface
Kimberlite does not make diamondsIt drags them
The Missing Crust Problem
• Stabilization of the Mantle Composition relative to earth’s crust appears to happen around 2,700,000,000 years ago– We should have 70 to 80% of the continental
crust by then
Industrial DiamondsC S.G. 3.5 - 3.53 Hardness 10Color Colourless, yellowish to yellow, brown, black, blue, green or red, pink, champagne-tan, cognac-brown, lilac (very rare)
How Diamonds are Processed
• Crushing and Grinding– (if the deposit is weathered or a placer this may not
be needed)
• Gravity Concentration– Diamonds are heavier than surrounding minerals– some unique designs produce a concentrate of
heavy minerals
Rotary washing panMake mud and theHeavies settle
Heavy MediaThis diagram shows how cones (left) and cyclones (right) use heavy-media separation. Diamond-bearing concentrate is mixed with a fluid near the density of diamond. Separation occurs in cones and cyclones by swirling the mixture at low and high velocities respectively. In the cone, rotational mixing permits lighter minerals to float to the top and run out as overflow, while diamonds and dense minerals sink to the bottom and are sucked out with a compressed air siphon. In the cyclone, fast rotation of the suspension drives heavy minerals to the conical wall, where they sink to the bottom and are extracted, while float waste minerals are sucked from the center of the vortex. Cyclones are about 99.999% efficient at concentrating diamonds and similarly dense minerals from the original ore. Adapted from Bruton (1978)
Other Minerals Besides Diamonds are Heavy
• The grease method– Freshly exposed
diamonds grab onto axle grease
– Use greased shaking tables to pull out diamond
Reserves and Production
Industrial Diamond Reserves
0
10
20
30
40
50
60
70
80
90
Production Reserves/7
Mil
lio
ns
of
Ca
rra
ts
Other
South Africa
Russia
Congo
China
Botswana
Australia
Catch – 88% of industrial diamonds are now synthetic
What are Diamonds Worth
Ability to make synthetic diamonds has brought down the price but they areStill over $1,000,000 per ton (of course they are sold by carrots)
Corundum/ Emery
• Lots of gems are corundum
• Much of abrasive market has been taken by synthetic minerals– Get more uniform material without random
natural weaknesses– Still used for super heavy duty concrete and
durable anti-skid material
Corundum
Al2O3
S.G. 3.98 - 4.1 Hardness 9Color Colourless, blue, red, pink, yellow, grey, golden-brown
Gem forms include Rubies and Sapphires, Emery
Garnet
• Use as a grinding and polishing agent– Garnet papers still common abrasive– Also used as a “sand blasting agent”
• It does not cause silicosis
– Filtering material– A lot of natural sharpening rocks in fact get
their properties from well distributed small garnet crystals
Almandite
Fe3Al2(SiO4)3 S.G. 4.09 - 4.31, Average = 4.19 Hardness 7-8 Color Brown, Brownish red, Red, Black, Black red. Fluorescence None
Grossularite
Ca3Al2(SiO4)3
S.G. 3.42 - 3.72, Average = 3.57 Hardness 6.5-7.5 Color Brown, Colorless, Green, Gray, Yellow. Fluorescence None
Pyrope
Mg3Al2[SiO4]3
S.G. 3.5 - 3.6 Hardness 7.5Color Blood red, orange red, purple red, pink, or black red Fluorescence not reported
Andradite
Ca3Fe2(SiO4)3
S.G. 3.8 - 3.9 Hardness 6½ - 7½ Color Green, yellow, orange, reddish-brown, brown, black Fluorescence not reported
Staurolite
(Fe,Mg)2Al9(Si,Al)4O20(O,OH)4 S.G. 3.65 - 3.77, Average = 3.71 Hardness 7-7.5 Color Brownish yellow, Brownish black, Yellow brown, Dark brown, Reddish brown. Fluorescence not reported
Silica
• Sand is still dominant material for “Sand Blasting”
• Carefully graded and sized sand is used for “flint” sandpapers– Dominant market is home use
• Fine pure sands are an important raw material for glass, ceramics, and synthetic abrasives
• Naturally fine almost amorphous material that breaks up easily is called Tripoli
Sand
SiO2
S.G. 2.6 - 2.65, Average = 2.62 Hardness 7Color Brown, Colorless, Violet, Gray, Yellow. Fluorescence not reported
Soft Scrubbing Powders
• Diatomite– Used in silver polishes– More common use is filtering media
• Pumice– Main ingrediant in polishing powders and
household cleaners• Including tooth paste
– Used in hard rubbers– Used for washing stones for blue jeans
Pumice
Pumice is about 60-70% silicaIt has no crystal structure – it is a frothy glassS.G. < 1
Other Soft Abrasives
• Ground Feldspar in window cleaners
• Chalk for fine soft metal polishes
• Kaolin