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  1. D. S. McKinney and R. A. Friedel, J. Opt. Soc. Am. 38, 222 (1948).
    [CrossRef] [PubMed]
  2. Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
    [CrossRef]
  3. C. Corin and G. B. B. M. Sutherland, Proc. Roy. Soc. (London) A165, 43 (1938). The Hilger Instrument used was calibrated from the dispersion curve of rocksalt.
    [CrossRef]

1948 (1)

1942 (1)

Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
[CrossRef]

1938 (1)

C. Corin and G. B. B. M. Sutherland, Proc. Roy. Soc. (London) A165, 43 (1938). The Hilger Instrument used was calibrated from the dispersion curve of rocksalt.
[CrossRef]

Corin, C.

C. Corin and G. B. B. M. Sutherland, Proc. Roy. Soc. (London) A165, 43 (1938). The Hilger Instrument used was calibrated from the dispersion curve of rocksalt.
[CrossRef]

Friedel, R. A.

Kao,

Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
[CrossRef]

McKinney, D. S.

Oetjen,

Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
[CrossRef]

Randall,

Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
[CrossRef]

Sutherland, G. B. B. M.

C. Corin and G. B. B. M. Sutherland, Proc. Roy. Soc. (London) A165, 43 (1938). The Hilger Instrument used was calibrated from the dispersion curve of rocksalt.
[CrossRef]

J. Opt. Soc. Am. (1)

Proc. Roy. Soc. (London) (1)

C. Corin and G. B. B. M. Sutherland, Proc. Roy. Soc. (London) A165, 43 (1938). The Hilger Instrument used was calibrated from the dispersion curve of rocksalt.
[CrossRef]

Rev. Sci. Inst. (1)

Oetjen, Kao, and Randall, Rev. Sci. Inst. 13, 515 (1942).
[CrossRef]

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Equations (1)

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T i + T 0 = A ν i 2 + B ( ν r 2 - ν i 2 ) - 1 .