Objective: To examine the relations of types of protein, glutamine, and glutamate to the incidence of diabetes (T2DM) among middle‐aged women. Methods: We identified incident cases of T2DM among 70,356 nurses free of T2DM and major chronic diseases at baseline, 1984–2002. Dietary habits were assessed using food frequency questionnaires. Cox proportional hazard models were used. Risk was considered significant at p for trend value<0.05. Results: During the 18‐years follow‐up (1,115,620 person‐years), we documented 3,804 new cases of T2DM. After adjusting for demographic and lifestyle variables, T2DM was not associated with total protein RR=0.88[0.78;1.00], p =0.14), animal protein (RR=0.96[0.85;1.09], p =0.77), and glutamate (RR=0.88[0.77;1.00], p =0.10). Although plant protein was inversely associated with T2DM in the multivariate model (RR=0.88 [0.78;1.00], p =0.03), this relationship appeared to be explained by cereal fiber (RR=0.97[0.85;1.11], p =0.64).Glutamine was also inversely associated with T2DM in the multivariate model (RR=0.81[0.72;0.91], p <0.001). In further analysis, glutamine was inversely related to T2DM independent of cereal fiber (RR=0.87 [0.77;0.99], p =0.02) and total protein (RR=0.79 [0.69;0.90], p =0.0002). Conclusions: Study findings suggest a significant modest inverse relation of glutamine with T2DM independent of total protein.
Based on micro-mechanical considerations, a phenomenological constitutive law is proposed for the steady creep of polycrystalline materials undergoing creep-constrained grain boundary cavitation. Singular stress and strain-rate fields at the tip of a stationary, plane strain crack are obtained revealing the role of cavitation on near-tip behavior.
ADVERTISEMENT RETURN TO ISSUEPREVArticleNEXTMechanism of formation of Grignard reagents. The rate of reaction of cyclopentyl bromide with magnesium is transport limited in diethyl etherHarold R. Rogers, John Deutch, and George M. WhitesidesCite this: J. Am. Chem. Soc. 1980, 102, 1, 226–231Publication Date (Print):January 1, 1980Publication History Published online1 May 2002Published inissue 1 January 1980https://pubs.acs.org/doi/10.1021/ja00521a035https://doi.org/10.1021/ja00521a035research-articleACS PublicationsRequest reuse permissionsArticle Views596Altmetric-Citations47LEARN ABOUT THESE METRICSArticle Views are the COUNTER-compliant sum of full text article downloads since November 2008 (both PDF and HTML) across all institutions and individuals. These metrics are regularly updated to reflect usage leading up to the last few days.Citations are the number of other articles citing this article, calculated by Crossref and updated daily. Find more information about Crossref citation counts.The Altmetric Attention Score is a quantitative measure of the attention that a research article has received online. Clicking on the donut icon will load a page at altmetric.com with additional details about the score and the social media presence for the given article. Find more information on the Altmetric Attention Score and how the score is calculated. Share Add toView InAdd Full Text with ReferenceAdd Description ExportRISCitationCitation and abstractCitation and referencesMore Options Share onFacebookTwitterWechatLinked InRedditEmail Other access optionsGet e-Alertsclose Get e-Alerts
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We present an efficient and rigorous numerical procedure for calculating the elastodynamic response of a fault subjected to slow tectonic loading processes of long duration within which there are episodes of rapid earthquake failure. This is done for a general class of rate‐ and state‐dependent friction laws with positive direct velocity effect. The algorithm allows us to treat accurately, within a single computational procedure, loading intervals of thousands of years and to calculate, for each earthquake episode, initially aseismic accelerating slip prior to dynamic rupture, the rupture propagation itself, rapid post seismic deformation which follows, and also ongoing creep slippage throughout the loading period in velocity‐strengthening fault regions. The methodology is presented using the two‐dimensional (2‐D) antiplane spectral formulation and can be readily extended to the 2‐D in‐plane and 3‐D spectral formulations and, with certain modifications, to the space‐time boundary integral formulations as well as to their discretized development using finite difference or finite element methods. The methodology can be used to address a number of important issues, such as fault operation under low overall stress, interaction of dynamic rupture propagation with pore pressure development, patterns of rupture propagation in events nucleated naturally as a part of a sequence, the earthquake nucleation process, earthquake sequences on faults with heterogeneous frictional properties and/or normal stress, and others. The procedure is illustrated for a 2‐D crustal strike‐slip fault model with depth‐variable properties. For lower values of the state‐evolution distance of the friction law, small events appear. The nucleation phases of the small and large events are very similar, suggesting that the size of an event is determined by the conditions on the fault segments the event is propagating into rather than by the nucleation process itself. We demonstrate the importance of incorporating slow tectonic loading with elastodynamics by evaluating two simplified approaches, one with the slow tectonic loading but no wave effects and the other with all dynamic effects included but much higher loading rate.