Title: Atmospheric Stability
1Atmospheric Stability Methods
Measurements
- Robert F. Yewdall
- PSEG Nuclear LLC
2Introduction
- Overview Of Atmospheric Stability Classification
As It Relates To Commercial Nuclear Power
Stations - Not Intended To Endorse Any Specific Model Or
Atmospheric Dispersion Methodology
3Atmospheric Stability
- History
- NRC Requirement
-
- Uses Of Stability Index
4Prescriptive Requirement For NRC Licensees
- Regulatory Guide 1.111, Methods for Estimating
Atmospheric Transport and Dispersion. - Regulatory Guide 1.145, Atmospheric Dispersion
Models for Potential Accident Consequence
Assessment at Nuclear Power Plants. - Standard Review Plan (NUREG 0800)
- Standard Format and Content Guide (Reg Guide
1.70) - Draft Regulatory Guide DG-1111, Atmospheric
Relative Concentration For Control Room
Radiological Habitability Assessment At Nuclear
Power Plants
5The Paradox Tower Siting Requirements versus
Representation of Dispersion of Effluents at the
Point of Release
- 1. The need to gather climatological/
meteorological data for site characterization and
short term (accident) and long term dispersion
estimates. -
- 2. The need to determine what is happening to the
effluent (source term) released from the station.
6History - General
- Data gathering for station licensing siting
(primarily 10 CFR Part 100). - Early emergency planning
- Post TMI
- NRC Program and Instrument Requirements Still
1972 vintage (SG 23)
7History at PSEG
- Dispersion analysis originally developed from
Brookhaven model - Persuaded to estimate dispersion based on NRC
requirements
8Brookhaven Model
9Early FSAR Analysis All Hours
10Early FSAR Analysis Stable Only
11Basis
- Numerical functions, sy(x) and sz(x).
employed to describe the lateral and vertical
dispersion, were created empirically using
Gaussian statistics based on field observations
and tracer studies. - As described in numerous documents and as
identified in an article by C.W. Miller1 ..while
these Pasquill-Gifford (PG) curves have been
applied to a large variety of different
situations, they were actually intended for use
under rather limited circumstances wind speed
greater than 2 m/sec, nonbuoyant plumes, flow
over open country and downwind distances of only
a few km. In addition values generally
applied with the model were originally derived
from data gathered on over relatively flat,
smooth terrain -
- 1 An Examination of Gaussian Plume Dispersion
Parameters For Rough Terrain, Atmospheric
Environment, (1978) Vol. 12, pp 1359
12Post TMI Requirements
- RG 1.97 Instrumentation for Light-Water-Cooled
Nuclear Power Plants To Assess Plant and Environs
Conditions During and Following an Accident - NUREG 0654 Criteria for Preparation and
Evaluation of Radiological Emergency Response
Plans and Preparedness in Support of Nuclear
Power Plants, Rev Nov 1980 - NUREG 0737, Requirements For Emergency Response
Capability, Supp 1, 12/92 - NUREG 0696 Functional Criteria for Emergency
Response Facilities, 1981 - License conditions or commitments
13Calculation Structure
- Atmospheric Stability Is Index Into 7 Category
Grouping - Determination Of Stability Is Either By Delta
Temperature Or Sigma Theta - Stability Index Currently Defined In A Number Of
NRC Regulatory Guides and NUREG - Stability Class Generally Referred To As
Pasquill Gifford or P-G Class
14Calculation Structure - Cont
- Index Form Discrete Values (can create large
steps in dose projections) - NRC Regs Require Delta Temperature Index To Be
Used For Determination Of Long Term Accident
Dispersion Calculations - For Emergency Preparedness Purposes - Could Use
Sigma Theta As Substitute For Delta Temperature
Or For Sigma Y -
15What is going on at the release point
16Possible Differences Between Met Tower and
Release Point
- Land Sea Interfaces
- Valley Flows
- Elevation Difference Cliffs and Bluffs
17(No Transcript)
18Site Area
19Region
20(No Transcript)
21Sigma Theta
- Per ANSI/ANS- 2.5-1984, the standard deviation of
horizontal wind direction fluctuations shall be
determined by statistical analysis of samples
from no less than 180 instantaneous values of
lateral wind direction during the sample period
(i.e. if the sampling period is 15 minutes,
values sampled at every five-second interval or
less are acceptable) likewise, if the sampling
period is one hour, 20 second sampling intervals
or less are acceptable. Maximum sampling time is
one hour.
22Sigma Theta
- CLASSIFICATION OF ATMOSPHERIC STABILITY PER ANS
2.5-1984 -
- CATEGORY PASQUILL CLASS
SIGMA THETA (ST) -
- EXTREME UNSTABLE A STgt22.5
- MODERATE UNSTABLE B
22.5gtSTgt17.5 - SLIGHTLY UNSTABLE C
17.5gtSTgt12.5 - NEUTRAL D 12.5gtSTgt7.5
- SLIGHTLY STABLE E 7.5gtSTgt 3.8
- MODERATE STABLE F 3.8gtSTgt2.1
- EXTREMELY STABLE G 2.1gtST
23VERTICAL TEMP DIFF (DT)
- P-G Class (DEGREE C/100M)
- A DTlt-1.9
- B -1.9ltDTlt-1.7
- C -1.7ltDTlt-1.5
- D -1.5ltDTlt-0.5
- E -0.5ltDTlt1.5
- F 1.5ltDTlt4.0
- G 4.0ltDT
- Regulatory Guide 1.23 Table 2 defines the seven
stability classifications that are based on
ranges from sigma theta. Sigma Theta is a
measure of standard deviation.
24Example 15 Minute Average
25Example 15 Minute
26Stability Comparison Table
27Stability Comparison - Plot
28Where Do We Go From Here ?
29Guidance Current Status
- NRCS CURRENT POSITION ON METEOROLOGY (05/02)
- SAFETY GUIDE 23 (AKA, R.G. 1.23) IS STILL IN
EFFECT. - PROPOSED REV. 1, AND 2nd PROPOSED REV. 1 TO R.G.
1.23 WERE NEVER ADOPTED. - AT PRESENT, THERE IS NO EFFORT, ONGOING OR
PLANNED WITHIN NRC, FOR AN UPDATE OR REVISION. - NRC IS WAITING FOR AN INDUSTRY TRADE GROUP (e.g.
NUMUG) TO TAKE THE INITIATIVE TO GET
ANSI/ANS-3.11 RECOGNIZED.
30Issues
- NRC Support/ Recognition of Met Standard ANSI/ANS
3.11 - Prescriptive nature of dispersion modeling (
i.e., delta Ts) - Location of meteorological monitoring relative to
release location - No change in temporal, spatial changes in
condition for 50 miles - Met validation and quality programs requirement
inconsistent with effluent release validation
requirements - Station support following removal from Tech Specs