Hydrophobic Organization of Membrane Proteins Author(s): D. C. Rees, L. DeAntonio and D. Eisenberg Source: Science, New Series, Vol. 245, No. 4917 (Aug. 4, 1989), pp. 510-513 Published by: American Association for the Advancement of Science Stable URL: http://www.jstor.org/stable/1704082 . Accessed: 13/11/2014 00:37 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact
[email protected]. American Association for the Advancement of Science is collaborating with JSTOR to digitize, preserve and extend access to Science. http://www.jstor.org This content downloaded from 131.215.248.20 on Thu, 13 Nov 2014 00:37:53 AM All use subject to JSTOR Terms and Conditions cally, although it is favored thermodynami- amorphous sediment for the volume frac- 6. D. Frenkel and J. P. McTague, Annu. Rev. Phys. Chem, 31, 491 (1980). cally. However, x-ray scanning reveals that tions reported here and crystallization does 7. W. Stober, A. Fink, E. Bohn, J. ColloidInterface Sci. the volume fraction in the fan above the not occur. Thus, for these initial volume 26, 62 (1968). sediment increases smoothly with depth, fractions there exists a maximum size above 8.