PPT-Particle QM Lecture 2 1 Finish Rutherford scattering

Quiz Stability of atoms Ultraviolet catastrophe Bohr Model bootcamp PHYS274 Midterm I and related announcements Midterm I on Oct 16 th Monday Professor Pui Lam will substitute for me Oct 618 while I am away at KEK. Zhibo (. zippo. ) Zhang. 03/29/2010. ESSIC. Outline. Background. Importance of ice cloud. Ice particle model and ice cloud retrieval. Influence of ice particle model on . t. retrieval. Comparison of MODIS and POLDER ice . Bryan Baum. 1. , Ping Yang. 2. , Andy Heymsfield. 3. ,. . Carl Schmitt. 3. , Aaron Bansemer. 3. , Yu Xie. 2. , Yong-Xiang Hu. 4. , Zhibo . Zhang. 5. Bob Holz. 1. , Andy Heidinger. 6. MODIS Science Team Meeting. Nanoparticle. Dispersions”. By. : PD Dr. Wolfgang . Schaertl. Institut für Physikalische Chemie, Universität Mainz, . Welderweg. 11, 55099 Mainz, Germany. schaertl@uni-mainz.de. Parts from the new book of the same title, published by Springer in July 2007. “. Lightscattering. ”. 1. Light Scattering – Theoretical Background. 1.1. Introduction. Light-wave interacts with the charges constituting a given molecule in remodelling . the spatial charge distribution:. Edan Bainglass. Jose Chavez. Kennedy Izuagbe. After his discovery of alpha particle emissions from a radioactive isotope of Radon gas, for which he was awarded the 1898 Nobel prize in Chemistry, Rutherford spent a considerable amount of time and effort into their investigation. CM34 @ RAL. Timothy Carlisle. 1. Intro.. MICE performance predicted using the cooling formula (. CF. ):. G4MICE . ≠. CF. (see . prev. CMs). Simulation disagrees with C.F by up to 20%.. MS calc. typically approx.: . goals. streaming analysis concepts. automated . approaches. sedimentation, laser light, and other techniques. contrast and compare techniques. examine particle size distributions, data. 2. Automated Particle Size Analysis. 18 . August . 2015. Scott Sieron, . Fuqing. Zhang,. Eugene . Clothiaux. , Lu . Yinghui. COLD. WARM. 270. 250. 230. 210. 190. Hurricane Karl 09/17/10 0113Z. SSMIS (image courtesy NRL). COLD. WARM. 260. Green’s Function: . The Green function will be used in Born. approximation of scattering amplitude and therefore. first we try to understand a little about Green function.. The Green’s function of an operator . 1. PHYS. 3313 . – Section 001. Lecture . #8. Monday, Sept. 24, . 2012. Dr. . Jae. hoon . Yu. Atomic Model of Thomson . Rutherford Scattering Experiment and Rutherford Atomic Model. The Classic Atomic Model. 17. Atmospheric Aerosols. a. mmonium sulfate. o. rganic carbon. All PM2.5, 2011 average. a. mmonium nitrate. s. oil (“dust”). FORMATION OF SULFATE-NITRATE-AMMONIUM AEROSOLS. Sulfate always forms an aqueous aerosol. Optical Properties of Aerosols. ENVR 416. Aerosol Technology. Topics. Definitions. Extinction. . Scattering. . Visibility. 2. Introduction. Aerosol scattering is responsible for many atmospheric events. Air Pollution and Global Warming:. History, Science, and. Solutions. . Chapter. 7: Effects of Pollution on Visibility, UV Radiation, and Colors in the Sky. . By Mark Z. Jacobson. Cambridge University . Chapter 7. What ranges do we need to measure. Particle Characterization: Light Scattering Methods. Principles for different methods. 1. Visual methods (e.g., optical, electron, and scanning electron microscopy combined with image analysis).