Hostname: page-component-7479d7b7d-q6k6v Total loading time: 0 Render date: 2024-07-10T06:23:48.919Z Has data issue: false hasContentIssue false

A graphical method for the rapid correction of specific gravity determinations

Published online by Cambridge University Press:  14 March 2018

A. Hutchinson*
Affiliation:
University of Cambridge

Extract

It has long been recognized that if specific gravity determinations are to be accurate to a unit or two of the third decimal place corrections must be applied for the error due to the circumstances (i) that the weighings are made in air instead of in a vacuum, and (ii) that the temperature at which the determinations are made usually differs considerably from the standard temperature of 4° C.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1924

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Note

1 The method of arriving at this formula is discussed in the text-books, e. g. W. Watson, ‘A text-book of Practical Physics’, or F. Kohlrausch, ‘Leitfaden der praktischen Physik’. For an account of the precautions necessary in accurate work reference should be made to A. E. H. Tutton, ‘Crystallography and Practical Crystal Measurement’, 2nd edit, 1922, vol. 1, chap. xxxii, and also to a recent paper by A. C. Egerton and W. B. Lee, Prec. R. Soc. London, 1928, ser. A, vol. 103, p. 487, where other references will be found. The values of D have been taken from the tables of Landolt and Börnstein, 2rid edit, 1894, p. 39.