PARTICOLATO FISICA AMBIENTALE 2 Antonio Ballarin Denti

Slides:



Advertisements
Similar presentations
Plumes gaussiani nellaria FISICA AMBIENTALE 1 Antonio Ballarin Denti
Advertisements

SPETTROSCOPIA 2 FISICA AMBIENTALE 2 Antonio Ballarin Denti
Chapter 25 Electric Potential.
Particle Fall through the atmosphere
Instructor: André Bakker
Motion of particles trough fluids part 2
ES 202 Fluid and Thermal Systems Lecture 28: Drag Analysis on Flat Plates and Cross-Flow Cylinders (2/17/2003)
3. The Motion of Particles Drag force d particle diameter V flow velocity Spherical particle, Re < 1 Drag coefficient A projected area.
- Prepared by Shakil Raiman
Motion of particles trough fluids part 2
Are raindrops tear-shaped? Diameter < 2 mm Diameter 2 – 5.5 mm Diameter > 5.5 mm.
Physics 2 Chapter 14 problems Prepared by Vince Zaccone For Campus Learning Assistance Services at UCSB.
Shape of a Rain Drop. Formation of Rain The sun heats water and turns it into vapor Water condenses and falls back to the earth in form of rain. Water.
* Radius of a sphere with the same mass The Shape of Raindrops The common perception that raindrops are teardrop-shaped is wrong.
Momentum flux across the sea surface
Shape of raindr p MLIM 6323 designed by Beryl & Peon Check it out.
MITE 6323 Daphne Chan and Chris Leung Raindrop ShapeTask 4 What impacts Shape of a raindrop.
Many people will expect the rain drop size should be as follows:
Fluid Flow Pressure, momentum flux and viscosity..
Lecture #19: Fluid Dynamics I
1 The Characteristic Curves Now for the real excitement: putting the solid and fluid together! Courtesy of John Selker (Oregon State University)
Water in the atmosphere. Water content of air Mass mixing ratio, Saturated vapour pressure, equilibrium over flat surface Rate of evaporation = rate of.
Divide yourselves into groups of three (3). Write your names and your complete solution into your answer sheet, and box / encircle your final answer.
T HE C OOLING E FFECTS OF V ARYING W ATER D ROPLET V OLUME AND S URFACE C ONTACT A NGLE W ITH A M ETAL S URFACE I N A S TEADY S TATE, H IGH T EMPERATURE.
Mechanistic Modeling and CFD Simulations of Oil-Water Dispersions in Separation Components Mechanistic Modeling and CFD Simulations of Oil-Water Dispersions.
Fluids, Work and Power: Student Success Criteria I can solve problems and conduct an investigation related to the relationships between force, area, pressure,
Forces due to Static Fluids
Wind tunnel visualization of air flow AIR streamlines.
Sedimentation.
Geometry Group Summer 08 Series Toon Lenaerts, Bart Adams, and Philip Dutre Presented by Michael Su May
Chapter 03: Macroscopic interface dynamics Xiangyu Hu Technical University of Munich Part A: physical and mathematical modeling of interface.
Buoyancy forces Floating objects. Which object experiences the largest buoyancy force? 1.Box at top 2.Box in middle 3.Box at bottom 4.All same
Q14.1 The sphere on the right has twice the mass and twice the radius of the sphere on the left. Compared to the smaller sphere on the left, the larger.
Human movement through air and water
Fluid Resistance.
METR 415/715 Monday 2/4/2013. EM Radiation can be considered as particles as well as waves Small “packets” ot EM radiation that behave like particles.
Notes 11-1 Pressure. What Is Pressure? The amount of pressure you exert depends on the area over which you exert a force.
Resistance in Fluid Systems Mr. Andracke Principles of Technology.
 Anything that has mass and takes up space  Made up of tiny particles called atoms  Atoms: smallest particle of matter.
Shape of a rain drop.
Tuesday Sept 21st: Vector Calculus Derivatives of a scalar field: gradient, directional derivative, Laplacian Derivatives of a vector field: divergence,
CP502 Advanced Fluid Mechanics
1 Atmospheric Radiation – Lecture 9 PHY Lecture 9 Infrared radiation in a cloudy atmosphere.
Chapter 5.2 Notes Bernoulli’s Principle. Bernoulli’s Principle says that as the velocity of a fluid (such as air) increases, the pressure in the fluid.
Chapter 10 Fluids Pressure in Fluids Pressure is defined as the force per unit area. Pressure is a scalar; the units of pressure in the SI system.
T HE C OOLING E FFECTS OF V ARYING W ATER D ROPLET V OLUME AND S URFACE C ONTACT A NGLE W ITH A M ETAL S URFACE I N A S TEADY S TATE, H IGH T EMPERATURE.
Heat and Flow Technology I.
Date of download: 10/1/2017 Copyright © ASME. All rights reserved.
Incomplete without class notes
FLUID MECHANICS LECTURE
Part IV: Detailed Flow Structure Chap. 7: Microscopic Balances
Date of download: 11/3/2017 Copyright © ASME. All rights reserved.
GLOBAL CONSERVATION EQUATIONS
Measuring Volume Meniscus Madness
3.2 Pressure and the Buoyant Force
THERMO- AND FLUID MECHANICS LECTURE
From: Modeling of Particle-Laden Cold Flow in a Cyclone Gasifier
A light beam is incident at an angle  on the top surface of a block of plastic. The sides and bottom of the block are immersed in water. If =50, find.
Integral of a Vector Field over a Surface
Mass Transfer.
Porous Flow.
AQUARIUM DREAMS CHALLENGE ASSIGNMENT.
Chapter 3 Section 1 Pressure.
Developing relationship between ACFM vs SCFM for HEPA Filters
Today’s Lecture Objectives:
Fluids and pressure.
Properties of Fluids.
Asst. Prof. Dr. Hayder Mohammad Jaffal
Introduction to Fluid Mechanics
S.A. Shkulipa, W.K. den Otter, W.J. Briels  Biophysical Journal 
Presentation transcript:

PARTICOLATO FISICA AMBIENTALE 2 Antonio Ballarin Denti

LE PARTICELLE Volume fraction of aerosol particles in 4 quite different locations

Stages in the absorption of gaseous SO 2 ina raindrop

Cattura di SO2 da parte di una goccia di pioggia c (r > R, t = 0) = c c (r, t ) = c c (R, t) = c s (t)=0

r R r = 0, t > 0 t > 0 r R c (r, t = 0) = 0 c (R, t) = c s c (r, t ) = c s

Cattura di SO2 da parte di una goccia di pioggia Characteristic diffusion times in air and water for some drop sizes τ air τ drop 2.5 × × × R(m)10 -3 (1 mm) (10 μm) D g = m 2 s -1 D a = m 2 s -1

Fluxes at the interface air-water drop. The interface may be considered flat at x = 0

Cattura di SO2 da parte di una goccia di pioggia

Derivation of Stokeslaw Fluid is flowing from bottom to top with a non-slip condition at the surface. On the left one finds the general coordinate system, on the right the forces at the surface of the sphere. The drag is determinated by the components of the pressure force and tangential force in the direction of the flow.

LE PARTICELLE Attrito su una singola particella