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A Comprehensive Treatise on Inorganic and Theoretical Chemistry

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PLATINUM 5<br />

§ 2. The Occurrence of the Platinum Metals<br />

The six platinum metals—platinum, iridium, osmium, ruthenium, rhodium,<br />

<strong>and</strong> palladium—form a group which occur in nature associated together as indefinite<br />

alloys, <strong>and</strong> generally uncombined. Estimates of the percentage elementary<br />

compositi<strong>on</strong> of the igneous rocks of the earth's crust are c<strong>on</strong>sidered by F. W. Clarke<br />

<strong>and</strong> H. S. Washingt<strong>on</strong> 1 to include platinum nxlO -9 , where n is an undetermined<br />

integer ; iridium <strong>and</strong> osmium, each n X 1O -10 ; <strong>and</strong> ruthenium, rhodium, <strong>and</strong><br />

palladium, each nxlO -11 . J. H. L. Vogt gave nxl0 _1 ° for platinum. I. <strong>and</strong><br />

W. Noddack's estimates are indicated below, <strong>and</strong> for a later estimate, they gave<br />

5-0 X 1O -8 . The subject was discussed by G. Berg, W. Vernadsky, F. Bernauer,<br />

A. B. Fersmann, I. <strong>and</strong> W. Noddack <strong>and</strong> O. Berg, P. Niggli, E. Herlinger,<br />

V. M. Goldschmidt <strong>and</strong> C. Peters, G. Tammann, O. E. ZvyagintzefT, <strong>and</strong> P. Vinassa.<br />

Platinum has been reported from extra-terrestrial sources. Thus, J. M. Davis<strong>on</strong> 2<br />

observed platinum <strong>and</strong> iridium in the meteoric ir<strong>on</strong> of Coahuila, <strong>and</strong> Toluca, Mexico ;<br />

H. H. Niniger, in the meteoric ir<strong>on</strong> of Ballinger, Texas ; A. Liiversidge, in the meteoric<br />

ir<strong>on</strong> of Boogaldi, New South Wales ; J. C. H. Mingaye also noted platinum in meteoric<br />

ir<strong>on</strong>. The subject was discussed by G. Osann, G. P. Merrill, <strong>and</strong> O. C Farringt<strong>on</strong>.<br />

Later they gave for platinum in meteorites 7xlO~~ 6 . G. P. Merrill reported the<br />

presence of platinum, palladium, iridium, <strong>and</strong> ruthenium in meteorites ;<br />

J. C. H. Mingaye, of platinum, palladium, <strong>and</strong> iridium. Possibly if the platinum<br />

metals had been sought in many other meteorites, they would have been found.<br />

J. IJ. Howe said that it is probable all meteorites c<strong>on</strong>tain platinum. I. <strong>and</strong><br />

W. Noddack's estimate's for percentages are as follow, atomic* distributi<strong>on</strong>s are<br />

relative to oxygen unity.<br />

1'la/tin.um<br />

Iridium<br />

Osmium<br />

Palladium<br />

lthoflium .<br />

Ruthenium<br />

Earth's<br />

crust<br />

8OxIO- 11<br />

. 3OXlO- 12<br />

6OxIO- 12<br />

8-5 vlO- 13<br />

9() x 10- 13<br />

2-3 xlO- 13<br />

Igneous<br />

rocks<br />

8-3 x IO- 8<br />

—<br />

_.<br />

—<br />

_ _<br />

—<br />

Meteoric<br />

ir<strong>on</strong><br />

1-77 x10-°<br />

2-3 X 1O- 5<br />

8-8 X I0-«<br />

1-9 xIO- 5<br />

5-Ox 10~«<br />

2-39 X 10~ a<br />

Troilite<br />

3-Ox 10-«<br />

fi-OX10~ G<br />

10XIO- 5<br />

4-5 XlO 6<br />

IO x K)- 8<br />

4-20X K)- 6<br />

Atom.<br />

distributi<strong>on</strong><br />

2-3 X 10-«<br />

3-2 X IO 7<br />

1-4 X H)-«<br />

4-6 X IO 6<br />

1-3 X 10-«<br />

61 xlO-«<br />

O. O. Hutchins <strong>and</strong> TC. L. Holden 3 observed that 16 lines of the platinum<br />

spectrum coincide with lines in the solar spectrum. H. A. Rowl<strong>and</strong>, <strong>and</strong> M. N. Saha<br />

classed platinum, iridium, osmium, <strong>and</strong> ruthenium am<strong>on</strong>gst those elements<br />

whose presence in the solar spectrum is doubtful ; <strong>and</strong> palladium <strong>and</strong> rhodium<br />

am<strong>on</strong>gst the elements present in the solar spectrum. The subject was discussed<br />

by H. M. Vern<strong>on</strong>, JE. F. Bax<strong>and</strong>all, J. N. Lockyer, <strong>and</strong> H. N. Russell. IT. v<strong>on</strong><br />

Kluber classes platinum am<strong>on</strong>gst the elements of doubtful occurrence in the fixed<br />

stars.<br />

Platinum usually occurs in nature as a native metal alloyed with <strong>on</strong>e or more<br />

members of its family, <strong>and</strong> to a less extent with ir<strong>on</strong>, nickel, chromium, etc.<br />

O. Id. Zvyagintzeff 4 studied the subject. Some of the native alloys have received<br />

special names—e.g. native platinum, native iridium, native platiniridium, native<br />

palladium, allopalladium, iridosmine—neoyanskite or osmiridium with over 40 per<br />

cent, of iridium, <strong>and</strong> siserskite, or iridosmium, with 30, or less, per cent, of iridium<br />

—palladium gold, rhodium gold, <strong>and</strong> ferroplatinum. Very few compounds of the<br />

platinum metals occur as minerals. There are <strong>on</strong>ly COOperite, represented at first<br />

by Pt( As,S)2, <strong>and</strong> later by PtS ; braggite, (Pt,Pd,Ni)S ; laurite, RuS2, or (Ru5Os)S2 ;<br />

potarite, PdHg ; sperrylite, PtAs2 ; <strong>and</strong> stibiopalladinite, Pd3Sb.<br />

In additi<strong>on</strong> to the six members of the platinum family, there may be present<br />

ir<strong>on</strong>, copper, gold, etc. C<strong>on</strong>sequently native platinum may be host to a number<br />

of guests or strangers, <strong>and</strong> the form of native platinum which is ataracted by a<br />

magnet, was named by J. F. L. Hausmann polyxenite—from rroXvs, many, <strong>and</strong><br />

£eVoy, a guest. A. Breithaupt called the latter sideroplatinwrn—from criS-qposy ir<strong>on</strong><br />

—or simply ferroplatinum. A great number of analyses of native platinum have

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