Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schoolsLuquer, Lea McIlvaine
Science
Minerals in rock sections : $b The practical methods of identifying minerals in rock sections with the microscope, especially arranged for students in technical and scientific schools
Luquer, Lea McIlvaine
Petrology -- Laboratory manuals
The tests are best made upon about ½ mg. of powder with HFl (pure and
fuming). As soon as the fluorides begin to dry treat with dilute
H_{2}SO_{4} and warm until white fumes of SO_{3} appear. In this way the
HFl and SiFl_{4} are driven off and the sulphates are left. This part of
the test can conveniently be made on a piece of platinum foil. Add
excess of water and concentrate.
Transfer a drop to a clean object glass and, while still liquid, examine
it with the microscope. Do not use a cover-glass over the drop.
Crystallizations Obtained by Behrens’ Method.
_Potassium._ Add a little platinic chloride when octahedral crystals of
K_{2}PtCl_{6} (size .18 to .30 mm.) will appear, which are clear, bright
yellow in color with strong refraction.
[Illustration:
FIG. 82.—Potassium platinic chloride.[153]
]
[Illustration:
FIG. 83.—Sulphate of calcium (gypsum).[153]
]
_Sodium._ Use sulphate of cerium and allow a small amount of this
reagent to act through a capillary pipette upon a drop of the solution.
Very small aggregates of brown crystals (size .02 mm.) of the double
sulphate of cerium and sodium are formed, which are clearly visible with
600 diams. If potassium is present the double sulphate of that alkali
will appear in larger, grayish grains (size .05 to .06 mm.). An excess
of H_{2}SO_{4} is to be avoided.
_Calcium._ After a few minutes little gypsum crystals (CaSO_{4} +
2H_{2}O) will appear. In strongly acid solutions the thin acicular
crystals will be grouped in bushes or stars; in neutral solutions the
crystals will have the normal shape of selenite crystals or form
swallow-tailed twins.
_Magnesium._ Use salt of phosphorus dissolved in water and allow it to
mix with the solution (to which has been added ammonium chloride and
ammonia) through a capillary pipette. From a solution containing more
than 5 per cent. of magnesium are first deposited X-shaped skeletons and
rudimentary crystals of Mg.NH_{4}.PO_{4} + 6H_{2}O. If the solution is
more dilute beautiful, sharp, hemimorphic crystals (.10 to .20 mm. in
size) of the orthorhombic system will appear. These crystals often
resemble the roof of a house. The formation of the crystals is assisted
by heat. Iron and manganese phosphates yield crystals of the same type,
but the iron is separated on the addition of ammonia.
_Aluminium._ Use chloride of cæsium. Take a drop of the solution, with
excess of H_{2}SO_{4} driven off, and touch it with a platinum wire that
has been dipped in the melted chloride of cæsium. Large crystals
(.40-.90 mm. in size) of cæsium alum will form, which are octahedral and
cubo-octahedral in shape. Iron does not interfere, as its
crystallization would take place much more slowly. The solution should
not be too concentrated.
[Illustration:
FIG. 84.—Magnesiumammonium phosphate.[154]
]
[Illustration:
FIG. 85.—Cæsium alum.[154]
]
Special Tests.
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