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  Water in the polar and nonpolar cavities of the protein interleukin-1β

Yin, H., Feng, G., Clore, G. M., Hummer, G., & Rasaiah, J. C. (2010). Water in the polar and nonpolar cavities of the protein interleukin-1β. The Journal of Physical Chemistry B, 114(49), 16290-16297. doi:10.1021/jp108731r.

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 Creators:
Yin, Hao1, Author
Feng, Guogang1, Author
Clore, G. Marius1, Author
Hummer, Gerhard2, Author                 
Rasaiah, Jayendran C.1, Author
Affiliations:
1External Organizations, ou_persistent22              
2Laboratory of Chemical Physics, National Institute of Diabetes and Digestive and Kidney Diseases, National Institutes of Health, Bethesda, USA, ou_persistent22              

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Free keywords: Computer Simulation, Crystallography, X-Ray, Hydrophobic and Hydrophilic Interactions, Interleukin-1beta, Models, Molecular, Thermodynamics, Water
 Abstract: Water in the protein interior serves important structural and functional roles and is also increasingly recognized as a relevant factor in drug binding. The nonpolar cavity in the protein interleukin-1β has been reported to be filled by water on the basis of some experiments and simulations and to be empty on the basis of others. Here we study the thermodynamics of filling the central nonpolar cavity and the four polar cavities of interleukin-1β by molecular dynamics simulation. We use different water models (TIP3P and SPC/E) and protein force fields (amber94 and amber03) to calculate the semigrand partition functions term by term that quantify the hydration equilibria. We consistently find that water in the central nonpolar cavity is thermodynamically unstable, independent of force field and water model. The apparent reason is the relatively small size of the cavity, with a volume less than ∼80 Å(3). Our results are consistent with the most recent X-ray crystallographic and simulation studies but disagree with an earlier interpretation of nuclear magnetic resonance (NMR) experiments probing protein-water interactions. We show that, at least semiquantitatively, the measured nuclear Overhauser effects indicating the proximity of water to the methyl groups lining the nonpolar cavity can, in all likelihood, be attributed to interactions with buried and surface water molecules near the cavity. The same methods applied to determine the occupancy of the polar cavities show that they are filled by the same number of water molecules observed in crystallography, thereby validating the theoretical and simulation methods used to study the water occupancy in the nonpolar protein cavity.

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Language(s): eng - English
 Dates: 2010-10-192010-09-132010-11-032010-12-16
 Publication Status: Issued
 Pages: 8
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1021/jp108731r
BibTex Citekey: yin_water_2010
 Degree: -

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Title: The Journal of Physical Chemistry B
  Other : J. Phys. Chem. B
Source Genre: Journal
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Publ. Info: Washington, D.C. : American Chemical Society
Pages: - Volume / Issue: 114 (49) Sequence Number: - Start / End Page: 16290 - 16297 Identifier: ISSN: 1520-6106
CoNE: https://pure.mpg.de/cone/journals/resource/1000000000293370_1