'2 exchange' presentation slideshows

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746 views • 57 slides

Very Large Scale Neighborhood Search

Very Large Scale Neighborhood Search. By Jim Orlin Collaborators include: Ravi Ahuja, Ozlem Ergun, Abraham Punnen, Dushyant Sharma. Neighborhood Search. Combinatorial Optimization : minimize (f(S) : S ? F) f is typically linear, F is finite. Neighborhood Function :

706 views • 49 slides

Very Large Scale Neighborhood Search

Very Large Scale Neighborhood Search. By Jim Orlin Collaborators include: Ravi Ahuja, Ozlem Ergun, Abraham Punnen, Dushyant Sharma. Neighborhood Search. Combinatorial Optimization : minimize (f(S) : S ? F) f is typically linear, F is finite. Neighborhood Function :

612 views • 49 slides

Annual CO 2 Exchange in Irrigated and Rainfed Maize-Based Agroecosystems

Annual CO 2 Exchange in Irrigated and Rainfed Maize-Based Agroecosystems. S.B. Verma, A.E. Suyker, G.G. Burba, T.J. Arkebauer, D.T. Walters, A. Dobermann, K.G. Cassman, B. Amos, H. Yang, K.G. Hubbard, A.A. Gitelson, E.A. Walter-Shea, and D. Ginting. University of Nebraska-Lincoln.

344 views • 21 slides

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??? ???? ?????? ??????. MRI Instrumentation. MR Spectroscopy (NMRS). Statistical Maps & Time Courses. Use stat maps to pick regions. Then extract the time course. 2D ? 3D. Design Jargon: Runs. condition : one set of stimuli or one task. 4 stimulus conditions

219 views • 21 slides

Information from leading neutrons at HERA

Information from leading neutrons at HERA. V.A. K hoze, A.D. M artin, M.G. R yskin (also with A.B. Kaidalov). Alan Martin (Durham) 2 nd HERA-LHC Workshop CERN, 6-9 th June, 2006. Q 2. p exchange dominates for x L > 0.6, but absorptive effects

199 views • 13 slides

Danish Galathea 3 cruise 2006-2007

Interaction of physical, chemical and biological processes in atmosphere-ocean CO 2 exchange in the Benguela upwelling.

207 views • 13 slides

t years after death

t years after death. NO CO 2 exchange with atmosphere C12 is stable C14 decays Ratio at time t is reduced to R t with R t = C14/C12 at time t = R 0 (1/2) t/T (T = T 1/2 ) = R 0 e -t/T (T = T m )

235 views • 11 slides