Abstract
IT has been shown1 that birefringent fully swollen calcium alginate fibres of 0·4 mm. diameter contract on replacing the bifunctional calcium ion by the mono-functional sodium ion. Ingersoll and Johnson suggest2, inter alia, that the contraction is due to osmotic de-swelling rather than to devulcanization brought about by ionic exchange1. This explanation is unacceptable for the reasons below.
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References
Mongar and Wassermann, Nature, 159, 746 (1947).
Ingersoll and Johnson, Nature, 162, 225 (1948).
See ref. 1, col. 2, line 21.
Mongar and Wassermann, J. Physiol., 106, 32P (1947).
Private communication from Drs. K. J. Palmer and F. T. Jones, U.S. Dept. of Agriculture.
Mongar and Wassermann, Nature, 159, 746 (1947), and MS. submitted to 11th International Congress of Pure and Applied Chemistry; Abstract No. 105/10.
Mongar and Wassermann (to be published).
MacArthur, Electronic Eng., 17, 272 (1944); 317 (1945).
MacArthur, Mongar and Wassermann (to be published elsewhere).
Astbury, Nature, 155, 667 (1945).
MacArthur and Patnaik (to be published).
MacArthur (unpublished).
Ott, “Cellulose and Cellulose Derivatives", 279 (New York, 1943).
Lloyd, Dempsey and Garrod, Trans. Farad. Soc., 42B, 228 (1946).
For example, Speakman, J. Text Inst. (Mather Lecture), 32, 183 (1944); J. Roy. Soc. Arts, 93, 603 (1945).
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MACARTHUR, I., MONGAR, J. & WASSERMANN, A. Ion Exchange and Fibre Contraction. Nature 164, 110–111 (1949). https://doi.org/10.1038/164110a0
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DOI: https://doi.org/10.1038/164110a0
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