'Lag time' diaporamas de présentation

Pharmacogenomics: Understanding the Host and Drug Interface

Pharmacogenomics: Understanding the Host and Drug Interface. Stephen Becker. The Treatment Triad: Defining the Interfaces. Patient. Virus. Drug. The Treatment Triad: Defining the Interfaces. Patient. Virus. Drug. U.S. Drug Approval and Safety 1975-1999. Lasser, JAMA, 2002.

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Pain Management

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Experiences with Real-Time Data Warehousing Using Oracle Database 10G

Experiences with Real-Time Data Warehousing Using Oracle Database 10G . Mike Schmitz High Performance Data Warehousing mike.schmitz@databaseperformance.com Michael Brey Principal Member Technical Staff ST/NEDC Oracle Engineering Oracle Corporation. Agenda.

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METHODS OF DETERMINING ABSORPTION RATE CONSTANT

A SEMINAR ON. METHODS OF DETERMINING ABSORPTION RATE CONSTANT. by V. Sandeep Kumar M.Pharmacy, I Sem. Department of Pharmaceutics University College Of Pharmaceutical Sciences Kakatiya University Warangal. CONTENTS. Introduction Methods To Detect Absorption Rate Constant.

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Premedication

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Ambient Air Monitoring by ECO PHYSICS

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Nutrient Removal Project Dissolved Oxygen Control Algorithms

Nutrient Removal Project Dissolved Oxygen Control Algorithms. Dale Meck Roslyn Odum Nick Wobbrock. Outline. Goals of oxygen control algorithms Explain the algorithms Constant Flow Rate Aeration On/Off Control Algorithm Linear Scalar Control Algorithm Exponential Control Algorithm

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What do you learn from binding constants and rate constants?

What do you learn from binding constants and rate constants?. Regulatory effects on RNA polymerase . Inducers Repressors Activators. lac repressor. lac repressor. nonspecific site. Operator. +. +. K B = K NS = 2x10 6 M -1. K B = K S = 2x10 13 M -1. In the presence of inducer:.

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Asbestos and Health

Asbestos and Health. Overview. Background on asbestos Uses of asbestos Health Effects Risk factors Medical tests Proper handling Standards/ guidelines. What is Asbestos?. Mineral Fibrous White/grey Indestructible Fireproof. How Long Has it Been a Problem?.

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Tutorial 2: Creating a Project Schedule

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Cezary Czaplewski Faculty of Chemistry University of Gda?sk Poland

All-atom molecular simulations of protein folding and unfolded-state dynamics and structure with accelerated calculations on GPU. Cezary Czaplewski Faculty of Chemistry University of Gda?sk Poland. The 10th Protein Folding Winter School, KIAS, February, 7-11, 2011.

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Commonwealth Biotechnologies, Inc.

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Young Streams vs. Old Streams

Young Streams vs. Old Streams. Young Streams vs. Old Streams. How river systems change from young to mature!. MATURE Wide Channels Large floodplains Lateral erosion Gentle slopes Meanders, oxbows Fine sediment. YOUNG. Narrow channels Small floodplains Downcutting Steep slopes

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Omori law

Omori law. Students present their assignments The modified Omori law Omori law for foreshocks Aftershocks of aftershocks Physical aspects of temporal clustering. Omori law: the modified Omori law. Omori law (Omori, 1894): the modified Omori law (Utsu, 1961):

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ESS 454 Hydrogeology

ESS 454 Hydrogeology. Module 1 Course Overview, Hydrogeology History, Hydrologic Cycle, Sustainability I & II. Withdrawal of groundwater faster than it is recharged (groundwater mining) is not sustainable. When the groundwater is gone, what are the alternatives?.

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NRCS Activities: Using the Monitoring Framework

NRCS Activities: Using the Monitoring Framework. Presentation for Office of Management and Budget March 26, 2003. Thomas W. Christensen, Director Animal Husbandry & Clean Water Programs Natural Resources Conservation Service. NRCS Activities: Using the Monitoring Framework.

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DES 606 : Watershed Modeling with HEC-HMS

DES 606 : Watershed Modeling with HEC-HMS. Module 9: S-Hydrographs Theodore G. Cleveland, Ph.D., P.E, M. ASCE, F. EWRI 26-28 August 2015. Module 9. Outline for Module 9. Define an S-hydrograph Advantages and Uses How to enter in HEC-HMS. Module 9. S-Hydrographs.

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What Can We Learn From Seismic Waves?

What Can We Learn From Seismic Waves?. D24. Seismograph stations can give us information about earthquakes. Time lag Is the time difference between the arrival of the two waves Tells how far away you are from the epicenter, NOT the direction of the earthquake.

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School on Surface Analytical Techniques 10.-13. April 2012

School on Surface Analytical Techniques 10.-13. April 2012 . Institute of Physical and Theoretical Chemistry University of Regensburg. Scope:

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