PRACTICAL USER TIPS FOR ARCON96 10 TH NUMUG MEETING Wilmington, NC June 2005 By Y. J. Lin Bechtel Power Corporation Frederick Maryland.

Slides:



Advertisements
Similar presentations
21M062007D The Shaw Group Inc. ® An Analytical Screening Technique to Estimate the Effect of Cooling Ponds on Meteorological Measurements – A Case Study.
Advertisements

CURRENT METEOROLOGICAL HAPPENINGS THE SITING AND ACCIDENT CONSEQUENCES BRANCH DIVISION OF SITE AND ENVIRONMENTAL REVIEWS OFFICE OF NEW REACTORS Brad Harvey,
Atmospheric Dispersion Modeling for Carbon-14 Emissions 14th NUMUG Conference, June 2011, Chicago, IL Theodore A. MessierMark Strum Principal ScientistAdvisory.
Prof. John Toohey-Morales, CBM, CCM
Determining a Backup Source of Meteorological Data for Dispersion Characteristics (Wind and Stability) Mark T. Carroll Heather A. McDonald Andrew J. Lotz.
Case Study: Impact of Above Ground Spent Fuel Storage on Nearby Meteorological Systems Jim Holian SAIC NUMUG Meeting Charlotte, NC June 2008.
X/Q for Releases From Area Sources 2008 RETS-REMP and NUMUG Workshop Jim Key Key Solutions, Inc.
1 DG-1247: Design-Basis Hurricane and Hurricane Missiles for Nuclear Power Plants Brad Harvey, CCM Senior Physical Scientist (Meteorology) U.S. Nuclear.
Examples of 1-Hour NO 2 and SO 2 Modeling William O’Sullivan Director, Division of Air Quality NJDEP June 14, 2011.
Introduction to SCREEN3 smokestacks image from Univ. of Waterloo Environmental Sciences Marti Blad NAU College of Engineering and Technology.
Introduction to SCREEN3 smokestacks image from Univ. of Waterloo Environmental Sciences Marti Blad.
Temporal Comparison of Atmospheric Stability Classification Methods
SO441 Synoptic Meteorology
Dispersion and Deposition Estimation Issues Presented at NUMUG San Francisco, CA 2009.
Weather and X/Q 1 Impact Of Weather Changes On TVA Nuclear Plant Chi/Q (  /Q) Kenneth G. Wastrack Doyle E. Pittman Jennifer M. Call Tennessee Valley Authority.
The ANSI/ANS 2.15 Standard for Modeling Routine Radiological Releases from Nuclear Facilities John Ciolek AlphaTRAC, Inc.
X/Q for Releases From Area Sources 2009 RETS-REMP Workshop Jim Key Key Solutions, Inc.
Using ARCON96 for Control Room Radiological Habitability Assessments
ADMS ADMS 3.3 Modelling Summary of Model Features.
1 AirWare : R elease R5.3 beta AERMOD/AERMET DDr. Kurt Fedra Environmental Software & Services GmbH A-2352 Gumpoldskirchen AUSTRIA
Introduction to the ISC Model Marti Blad NAU College of Engineering.
LiDAR analysis at a site with simple terrain Alex Clerc, Lee Cameron Tuesday 2 nd September
Strategies for the Selection of Substitute Meteorological Data Ken Sejkora Entergy Nuclear Northeast – Pilgrim Station Presented at the 14 th Annual RETS-REMP.
Air Quality Modeling.
Investigation of Meteorological Tower Siting Criteria Ken Sejkora Entergy Nuclear Northeast – Pilgrim Station Presented at the 15 th Annual RETS-REMP Workshop.
CHAPTER 5 Concentration Models: Diffusion Model.
Upper Air Charts By Tom Collow November 8, Reading Upper Air Charts Temperature (°C) Dewpoint Depression (°C) Height Wind direction and speed (knots)
EFCOG Safety Analysis Working Group May 10, 2012 Jeremy Rishel Bruce Napier Atmospheric Dispersion Modeling in Safety Analyses: GENII.
Session 4, Unit 7 Plume Rise
AMBIENT AIR CONCENTRATION MODELING Types of Pollutant Sources Point Sources e.g., stacks or vents Area Sources e.g., landfills, ponds, storage piles Volume.
Dispersion of Air Pollutants The dispersion of air pollutants is primarily determined by atmospheric conditions. If conditions are superadiabatic a great.
Section 03 - Altimetry (cont) Lesson 09
Air Dispersion Primer Deposition begins when material reaches the ground Material from the lower stack reaches the ground before that of the taller stack.
Dispersion Modeling A Brief Introduction A Brief Introduction Image from Univ. of Waterloo Environmental Sciences Marti Blad.
10.4 Projectile Motion Fort Pulaski, GA. One early use of calculus was to study projectile motion. In this section we assume ideal projectile motion:
E N G I N E E R I N G C O N S U L T I N G I N F O R M A T I O N S E R V I C E S THE TEN TIMES RULE WHERE DID IT COME FROM? IS IT REALLY VALID? T. Edward.
CHAPTER 14 Sound Doppler Effect A train passes by you with its whistle/horn blowing. You hear one pitch (tone) as the train is coming towards you and a.
BFN Sigmas1 EVALUATING METEOROLOGICAL MONITORING SITES USING SIGMA-THETA Kenneth G. Wastrack Doyle E. Pittman T ENNESSEE V ALLEY A UTHORITY.
Atmospheric boundary layers and turbulence I Wind loading and structural response Lecture 6 Dr. J.D. Holmes.
Discussion of time series and panel models
Prof. Jiakuan Yang Huazhong University of Science and Technology Air Pollution Control Engineering.
Stable Atmosphere.
Motion The symbol “Δ” means “Change in” QuantitySymbolDefinitionUnitsQuantitySymbolDefinitionUnit DistancedmDisplacementdm Speedvd/Δtm/sVelocityvd/Δtm/s.
Comparison of the AEOLUS3 Atmospheric Dispersion Computer Code with NRC Codes PAVAN and XOQDOQ 13th NUMUG Conference, October 2009, San Francisco, CA.
Transport and dispersion of air pollution
Section 9.7 – Taylor Theorem. Taylor’s Theorem Like all of the “Value Theorems,” this is an existence theorem.
Types of Models Marti Blad Northern Arizona University College of Engineering & Technology.
Energy Use Data for NCSSM – excluding petroleum-based fuel.
HF Modeling Task Mike Williams November 19, 2013.
Consequence Analysis 2.2.
NUMUG - Oct Atmospheric Stability – Methods & Measurements Robert F. Yewdall PSEG Nuclear LLC.
May 2002[NUMUG] Listening to the Wind1 of 17 LISTENING TO THE WIND TVA Experience with Installation and Operation of Ultrasonic Wind Sensors Kenneth G.
Various Methodologies for Calculating the Impacts on Delta-T From Independent Spent Fuel Storage Installations (ISFSI) Jim Holian and Steve Mirsky, SAIC.
Estimation of Maximum Temperature for Argon Gas Exiting Ullage Space in Micro-Boone K. C. Wu 11/2/11 1.
UPPER AIR FLOW The height of the atmosphere The height that the atmosphere reaches a certain pressure can tell us information about the air at a certain.
AOSC 200 Lesson 27. A Typical Day in a Pollution Episode A common severe pollution weather pattern occurs when high pressure is centered just west of.
SO441 Synoptic Meteorology
Recent Developments Regarding Control Room Habitability Assessment
Types of Models Marti Blad PhD PE
The Role of Meteorology in the Nuclear Power Industry
Air Pollution and Control (Elective- I)
Examples of 1-Hour NO2 and SO2 Modeling William O’Sullivan Director, Division of Air Quality NJDEP April 28, 2011.
PURPOSE OF AIR QUALITY MODELING Policy Analysis
Weather Stations and Weather Maps
XOQDOQ Calculation Method, Tools and Pitfalls
Wind Velocity One of the effects of wind speed is to dilute continuously released pollutants at the point of emission. Whether a source is at the surface.
Air Pressure Highs and Lows
Dispersion Models Dispersion of pollutants in the atmosphere Models
Illinois Department of Nuclear Safety
Math with MacGuyver!.
Presentation transcript:

PRACTICAL USER TIPS FOR ARCON96 10 TH NUMUG MEETING Wilmington, NC June 2005 By Y. J. Lin Bechtel Power Corporation Frederick Maryland

2 History ARCON96, Rev. 1 was issued by the NRC in 1997 to calculate X/Qs in building wakes. NRC conducted a panel discussion for control room habitability analysis in March 2000 and suggested improvements to be made for ARCON96 RG was issued in 2003 to provide guidance on the proper use of ARCON96

3 Area of Interest Release Mode Release Height Wind Direction Building Area Wind Speed

4 Release Mode ARCON96 offers 3 release modes (ground, vent, stack) but NRC only recognizes ground and stack releases; ARCON96 does not calculate plume rise; User could add plume rise to release height, but clear guidance was not provided - exactly what plume rise to be used? NRC suggests to treat vent releases as ground- level releases

5 Release Height ARCON96 calculates a “midpoint height” between the lower and upper wind instrument heights. The “midpoint height” is used to determine which level of the wind data are to be used in calculating X/Qs. Do not enter absolute heights even if you have treated a vent release as a ground-level release; the “midpoint height” approach could cause unexpected error. Suggest to always enter the actual release and receptor elevations. Both RG and Users Guide (NUREG/CR- 6331) do not discuss the use of the “midpoint height” approach.

6 Figure A. Actual release and intake heights are used (Vent Release Height > Tower Midpoint Height 33 ft 197 ft 300 ft > 115 ft 200 ft 100 ft Vent Met Tower CR Bldg Air Intake 115 ft

7 Figure B. Absolute release and intake heights are used (Vent Release Height < Tower Midpoint Height 33 ft 197 ft Vent Met Tower Air Intake 115 ft 100 ft 100 ft < 115 ft

8 Wind Direction ARCON96 defines valid wind directions as between 1 and 360 degrees; this approach is not the way meteorologists commonly used. ARCON96 treats 0-deg wind as calm. Users might need to change all the north wind direction to 360 degrees in their meteorological input data.

9 Building Area In general, ARCON96 is not sensitive to the size building area. The worst case X/Qs usually occur under 3 to 4 m/s winds, instead of the 0.5 or 1 m/s winds when using the conventional Gaussian models.

10 Wind Speed For a vent release (even if treated as a ground-level release as suggested by RG 1.194), ARCON96 assumes the wind speed at the release point is higher than that at the ground- level even the release point is located within the wake region. The above approach assumes that within the wake, higher level wind speeds are greater than the lower level winds. This assumption is questionable. The above issue is the consequence of using the “midpoint height” approach. The Users Guide or RG needs to provide further explanation.

11 Velocity Profiles In front and behind a Building

12 SUMMARY Always treat vent releases as ground-level releases, unless sound justification could be made; Always enter actual above grade heights for the vent release height and receptor height in modeling, instead of entering absolute heights; Make sure north winds are recorded as 360 degrees, instead of 0 degree in the input meteorological data set; The worst case ARCON96 calculated X/Qs usually occur under 3 to 4 m/s winds; ARCON96 is not sensitive to the building area when the wind speeds are low.