'Absorption cross' presentation slideshows

Fundamentals of Neutronics : Reactivity Coefficients in Nuclear Reactors

900 views • 37 slides

Reflection from Layered Surfaces due to Subsurface Scattering

Reflection from Layered Surfaces due to Subsurface Scattering. Pat Hanrahan Wolfgang Krueger SIGGRAPH 1993 Andrea Rowan March 2, 2001. Outline. Problem description Previous Work Reflection / Transmission formulas Results Successes / Problems Related Recent Work. Problem Description.

562 views • 36 slides

Weighting functions (Box AMFs) for Limb measurements of stratospheric trace species

380 views • 32 slides

The Finite Reactor in One Energy Group

The Finite Reactor in One Energy Group. B. Rouben McMaster University EP 4D03/6D03 Nuclear Reactor Analysis 2008 Sept-Dec. Contents. We analyze the criticality or degree of non-criticality of a finite reactor in 1 energy group. . The Reactor Equation.

624 views • 28 slides

Natural Nuclear Fission Reactor

Natural Nuclear Fission Reactor. Physics h190. Fission. Discovery and implementation of fission is arguably one of the more important and controversial scientific and technological discoveries in physics in the 20 th century Surprisingly this may just been a naturally occurring phenomenon

556 views • 22 slides

TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY

TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY. The many faces of atmospheric ozone:. In stratosphere: UV shield. Stratosphere: 90% of total. In middle/upper troposphere: greenhouse gas. Troposphere. In lower/middle troposphere: precursor of OH, main atmospheric oxidant.

375 views • 15 slides

Background :

An Optimized Evaluation of Isotopic Fractionation of N 2 O in the Atmosphere Yuk L. Yung 1 , Jason D. Weibel 2 , and Run-Lie Shia 1 1 Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena CA 2 Chemistry Department, Shenandoah University, Winchester VA.

127 views • 1 slides