'Time increment' diaporamas de présentation

Introduction to Work

Introduction to Work. Thursday, Jan 6, 2011! Happy New Year. Energy and Work. A body experiences a change in energy when one or more forces do work on it. A body must move under the influence of a force or forces to say work was done.

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INFILTRATION

INFILTRATION. AE 520. Infiltration Lesson Objectives. Understand the factors affecting soil water infiltration Be able to estimate infiltration rate using the Horton Equation and the Green-Ampt Equation Understand the advantages of the various infiltration functions. INFILTRATE.

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Unsteady State Heat Conduction

MODULE 5. Unsteady State Heat Conduction. UNSTEADY HEAT TRANSFER.

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You can have it right, Or you can have it now, But you cannot have it right now. (Bryan Kelly, 2002 )

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Origin of Basaltic Magma

Origin of Basaltic Magma. Today. Updates: ? Today: Different basalts from the same source Crystallization order Effect on Trace elements. Isochron method. Divide by stable 86 Sr: 87 Sr/ 86 Sr = ( 87 Sr/ 86 Sr) o + ( 87 Rb/ 86 Sr)(e l t -1) l = 1.4 x 10 -11 a -1.

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GPS based time synchronization of PC hardware

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Detention Routing

Detention Routing. www.b-e-c.com/PromoPages/GatewayBrownfields4.jpg. http://emengineers.com/images/Wh2o1lo.jpg. Objectives. Know what a detention basin is Compute a reservoir routing by hand Inflow Hydrograph Storage and Outflow versus WSE Routing Table . Detention Basins.

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E dit

Ectropic Design Navigator. F ile. E dit. C ritique. H elp. Clock system from Squeak: OODMA by Mark Guzdial. Classes. Clock. Class. Time. Collaborators. Increment time. Increment my representation of seconds. Increment my representation of minutes.

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Non-constant Forces

Non-constant Forces. Up until this time, we have mainly dealt with forces that are constant . These produce a uniform, constant acceleration. Kinematic equations can be used with these forces. However, not all forces are constant. Forces can vary with time, velocity, and with position.

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Introduction to StreamInsight

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Numerical Methods for Unsteady Heat Transfer

Numerical Methods for Unsteady Heat Transfer. Unsteady heat transfer equation, no generation, constant k, two-dimensional in Cartesian coordinate:.

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