DRC-2004-001043 - 0901a0688080592c

Serni-Ann ual Meteo rolo gical
Monitoring Report
For International Uranium
Blanding, Utah
January Through June 20A4
MCVEHIT-MONNETT
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Semi-Annual Meteorolo gical
Monitoring Report
For International Uranium
Blanding, Utah
January Through June 2004
Prepared for:
Intemati onal Uranium Corporation
6425 South Highway 191
P.O. Box 809
Blanding, Utah 84511
Prepared by:
McVehil-Monnett Associates, lnc.
44Inverness Drive East
Building C
Englewood, Coiorado 801 12
October 2004
MMA Project Number 1121-03
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Section
Introduction
Table of Contents
1.0
2.0
2.1
2.2
-/-.)
2.4
3.0
3.1
3.2
J.J
3.4
3.5
3.6
4.0
Monitoring Program Description .........2
Site Description............ ........2
Monitoring Instrumentation............. .......2
Data Collection And Processing ............. 3
Quality Assurance ................ 3
Analysis Results...... .............. 6
Missing Data for the January - June 2004 Monitoring period ........................ 6
Hourly Data Presentation ........................- 6
Wind Analysis By Hour Of The Day......... ................ 6
Sigma Theta And Atmospheric Stability ...................1
Precipitation Data........ ......... g
Data Recovery............. ......... 9
Conclusions................. ...... 15
List of Tables
Titie
hrstrument Specifications For The White Mesa Mill Station ..............4
10 Meter wind Data Analysis (wind Frequency Distribution By Direction
AndSpeed). . . ..................... i0
Frequencies of occurrence For Atmospheric Stability class for January -
Recorded Liquid Precipitation collected At The white Mesa Mill ..................,.. 11
Data Recovery Rates For Parameters collected At The white Mesa Mill
January- June 2004.......... ............... 11
Number
2-1
3-1
J-/.
J.J
3-4
Number
List of Figures
Titie
White Mesa Mill Monitoring Station Site Location Map
January- June 2004 Wind Rose (Graphical Annual Wind
Frequency Distribution) ................... 12
Graphical Wind Frequency Distributions By Hour Of Day
January- June 2004.......... ............... 13
Graphical Wind Frequency Distributions By Stability Class
January-June 2004.......... ............... 14
List of Appendices
Performance Audit Report
Hourly Data ln Saroad Tables
Joint Frequency Distribution of wind Speed By wind Direcrion By Hour of
The Day
Joint Frequency Distribution of wind Speed By wind Direction By stability
Class
2-1
3-1
3-2
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1.0 I1\TRODUCTION
In 1977 , meteorologrcal, air quality, and radiological monitoring was initiated at the White
Mesa Mill. The original purpose of these monitoring programs was to document the regional
atmospheric baseline and to provide adequate data to assess the potential air quality impacts resulting
from the mill. After construction of the mill, the monitoring programs were modified to address
compliance of mill operations.
McVehil-Monnett Associates, lnc. commenced work on this project in Iune of 2003, and
started to summarize the data collected since January 2003. This report describes important aspects
of the meteorological monitonng operations conducted at htemational Liraru,:m V1, hite Mesa Mill
site for data coilected from January 1 through June 30, 2004. The remainder of this report is
presented in three sections: monitoring site description (Section 2.0), analysis results (Section 3.0)
and conclusions (Section 4.0). Appendices A through D contain the semi-annual performance audit
report, hourly data listings, semi-annual joint fiequency distributions byhours ofthe day, and semi-
annual stability joint fiequency distributions by stability class.
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2.4 MOMTORTNG PROGRAM DES CRTPTION
The meteorological parameters collected for the monitoring period were wind speed, wind
direction, and standard deviation of horizontal wind direction (sigma theta), a measure of
atmospheric stability. Wind speed and wind direction were directiy measured while sigma theta and
stability class were calculated. The data were coliected and processed rlnder general site operations
protocol and quality assurance activities.
2.1 Site Description
The region encompassing the Intemational Uranium Corporation's White Mesa Mill is shown
in Figure 2-1. The mili is located on the White Mesa approximately five rniles south of Blanding,
Utah, just west of State Highw ay 191. The surrounding terain slopes up towards the north and
down to the south through southwest. The meteorological monitoring station, located on the
nofthern property boundary of the milI, is situated in the southwest corner of Section 22, Township
37 South and Range 22East at an elevation of 5,660 feet above means sea level. This location was
chosen for the purpose of compliance monitoring for operations at the mill.
2.2 Monitoring Instrumentation
The sensors, their accuracies, an<i the sampiing heights useci in the monitoring program are
shown in Table 2-1. On June 1 7,2003 the Weathertronics instrumentation was removed. A Met
One wind cup anemometer and wind vane were installed at the standard ten-meter height above
ground-level. The two Met One sensors were comected to a Campbell Scientific CR- 1 0 data logger.
The logger continuously recorded wind speed and wind direction, calculating and storing houriy
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averages of these parameters. The iogger also calculated and stored sigma theta. Data stored in the
logger were then transferred to a solid state storage module on a monthiy basis.
2.3 Data Collection and Processing
Data on storage modules were downloaded to a computer for further processing through
several program routines. These programs reform atthe data,check for anomalies, calculate stability
class (See Section 3.3), and perform other statistical summary functions.
2.4 Quality Assurance
After the meteorological data were downloaded and processed, a meteorologist checked any
anomalies flagged by the processing programs and also reviewed the data for any other anomalies not
captured by the processing programs. The project mallager was notified of any anomalies, and the
reasons for the elToneous data along with possible solutions to the problem(s) were discussed. The
Mill was then contacted and given instructions for anynecessaryrepairs. Ifrequired, personnel from
MMA were dispatched to the site to remedy the situation.
Any anomalous data in the monitoring period were coffecterl, ifpossible. If corrections were
impossible to make, available data were substituted from a nearby NOAA weather station in
Blanding. This station is operated in a cooperative effort with the University ofutah, Department of
lvleieoroiogy. iftiie etroneous daia could neither be corrected nor substituted, ii was coded as invaiid
or missing. as appropriate.
During the first six months of 2004, one semi-annual performance audit was conducted.
Performance audits of the wind speed and wind direction sensors were completed on May 27 . The
results for both audits indicated that the instrumentation audited was operating within EpA-specified
accuracies. The report for each audit is included in Appendix A.
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Table 2-1
Instrument Specifi cations
For the International Uranium Corporation
White Mesa Mill Station
Parameter Instrument Reading
Accuracy
Monitoring Height Manufacturer and
Model Number
Wind Speed 0.1 meters/second 10 meters Met One 010
Wind Direction t3.0"10 meters Met One 020
Siema Theta N/A 10 meters Calculated
Data Logger N/A N/A Campbell Scientific
CR-l0
Figure 2-l
White Mesa Mill
Monitoring Station
Site Location
630000
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0 m 2000 m 4000 m 6000 m
Mdfid frm Eehnic DRG le!, Blediry, Ud N3730w1osm&60
NAD2TUTMEastiag (m)
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3.0 ANALYSIS RESULTS
Meteorological data were collected at the White Mesa Mill and processed according to the
procedures described in Section 2.0. The stabilify class was determined for each hour (see Section
3.3 for determination methodology) and the data set was then analyzed by time of day and stability
classification.
3.1 Missing Data for the January through June 2004 Monitoring period
One section of missing data occurred for the January through June 2004 monitoring period.
Wind direction, sigma theta, and stability class data from the period of January t hour 1 through
Janr-tary 14 hotrr 10, a total of 122 hotrs, a.re missing due to a malfi:nctioning sensor. The wind
direction sensor was replaced on January 14,2004. At this time, data from the NOAA weather
station in Blanding were not available for substitution purposes.
3.2 Hourly Data Presentation
For the .Ianuary through June 2004 monitoring period, hourly averaged values ofwind speed,
wind direction, sigma theta and stability class are presented in Appendix B in the Storage and
Retrieval ofAerometric Data (SAROAD) format, including missing or invalid data. This format is a
method ofpresenting air quality and meteorological data. The SAROAD format also includes, when
applicable, average monthly values for each hour, daily averages and monthly averages.
3.3 Wind Analysis by Hour of the Day
The standard wind frequency distribution for the reporting period is presented graphically in
Figure 3-1. To show the diurnal pattems, additional wind frequency distributions were developed
graphically in 4-hour segments throughout the day (midnight to 4:00 A.M., 4:00 A.M. to 8:00 A.M.,
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etc.) and are presented in Figure 3-2. In addition, the diurnal frequency distribution tables are
presented in Appendix C.
Figure 3-1 shows the dominant flow for the period was a drainage wind out of the north-
northeast occurring i4.1 percent of the time. This flow is a result of the surrounding terrain,s
influence on the site.
Figure 3-2 confirms the downslope wind pattern seen in Figure 3-1, depicting the diurnal
pattern of this flow as well as other less predominant flows. During the nighttime hours from 2000
through 0800 Mountain Standard Time (MST), north through north-northeasterly winds were the
most prominent. During these nighttime hours, the drainage winds occurred approximat ely 46
percent of the time. For the daylight hours from 0800 through i 600 MST, the prominent winds were
from the south southeast through southwest. These are upslope or return flows and occurred on
average approximately 60 percent of the time during these daylight hours.
A tabularjoint frequency distribution is presented in Table 3-1. Themean wind speed forthe
monitoringperiodwas3.6meterspersecond(m/s). Thedirectionwiththehighestmearwindspeed
was south southwest at 5.0 m/s, while the lowest mean wind speed was from the east southeast
direction at2.3 rnls.
2 A o:--- TL ^.^ ^_ J ^ r_^__L __-!_ cJ.4 Sigii-ra i heta anri Aiil-rosphei-ic" StaL,iiiiv
Sigma theta (the standard deviation of the horizontal wind direction) is calculated using the
method listed in On-Site Meteorological Program Guidancefor Regulatory Modeling Applications
(EPA-45014-87-013). First,sineandcosineofwinddirectionarecalculatedbyaCampbellscientific
CR-10 data logger. Then, the average sine and cosine measurements for each fifteen minute period
are processed using the Yamartino method to calculate hourly sigma theta values.
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Since sigma theta is a gross measure of air turbulence, it can be used as an indirect measure
of atmospheric stability. The method used to calculate the Pasquiil-Gifford (P-G) atmospheric
stability class from sigma theta for this program is in accordance with EpA-45A14-87-013. This
method involves two steps. First, an initial estimate of stability for the hour is made based on sigma
theta values calculated from the sine and cosine of wind direction. The second step involves
modifying the initial estimate using the hourly mean rvind speed and time of day of the observation.
More specific information about this process can be found in this EPA reference"
The P-G stability class describes the dispersive nature of the atmosphere with Class A being
the most dispersive and Class F being the least dispersive. The more dispersive the atmosphere is,
the less air pollution may concentrate. As indicated above, the P-G methodoiogy allows unstable
conditions (Stability Classes A through C) to only occur during the da1,time, while stable conditions
(Stability Class E and F) can only occur at night. Neutral conditions (Class D) do not have any day
or nighttime restrictions and can occur at any time.
The P-G information is important in determining the dispersion of plumes or puffs from
releases of airborne material. For example, greater turbulence promotes dispersion and, therefore,
lowers concentrations of airbome pollutants. Thermal turbulence is dependent on vertical thermal
straiification, and ineciranical iurbuleiice is dependeni uporr wind speed arrd surface rougLrrress. lVith
light wind speeds, vertical thermal effects dominate the production of turbulence. During sunny
conditions, the temperature drops quickly with height above ground, creating unstable conditions.
Conversely, during light-wind, nighttime conditions, a surface inversion forms creating stable
conditions with relatively little vertical motions. Horizontal motions during light wind speed often
produce meandering in wind direction. Local terrain also plays an important part in the production
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of turbulence.
For the data collected during the January through June 2004 monitoring period, unstable
conditions occurred 37 .2 percent of the time, neutral conditions 37 .7 percent of the time, and stable
conditions 25.2 percent of the time,. The stability class data collected for the January through June
2004 monitoring period are presented in Table 3-2 and stability roses are presented in Figure 3-3.
The stabiiity ciass frequency distribution tables are presented in Appendix D.
3.5 Precipitation Data
Precipitation data (rain or snow) has been recorded in inches of liquid moisture received for
the White Mesa Mill. This data is collected at another location on the White Mesa Mill property.
Data for the January through June 2004 monitoring period is not available at this time, as shown in
Table 3-3.
3.6 Data Recovery
Table 3-4 summarizes the data recovery for this semiarurual reporting period. Data
recoveries for wind speed and wind direction were 99.9 and 92.5 percent, respectively.
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Tab1e 3-1
10 METER WIND DATA ANALYSIS
FROM a/a/2004 THROUGH 6/30/2004
INTERNATI ONAI, URANIT]M METEOROLOGf CAL STAT]ON
FREQUENCY OF OCCURRENCE OF WTND SPEED BY DIRECTION
+__-- _WIND SPEED CLASSES (M/S)_ ____+
0.0-DrR 1. 8
1.8- 3.3- 5_4
AVERAGE
WTNDTOTAL SPEED?2t^8.4 11.0
OA
11. 0
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N .0L44
NNE .0195
NE .0201
F\lF nl10
E .0083
ESE .0066
sE - 00'1 4
ssE .oa02
s .0089
ssw .0051
sw .0067
wsw .0054
w .0059
wNW .0069
NW .0098
NNW .0100
.0584 .0433 .0032 .0000
.o875 .0329 .001s .0000
.0292 .0089 .0027 .0000
.0115 .0054 .002s .0000
. 0069 . 0030 .0072 . 0000
.0014 " 0015 .0007 .0000
. 0171 . 0089 .0022 . 0002
.0210 .0089 .OO25 .0012
.0322 .0220 .00s9 .000s
. 0285 .0423 .0270 . 0087
.0188 .021s .0208 .0042
.0099 .0111 .0119 .0020
.0099 .0092 .0109 .0005
.0109 .0082 .0037 .0000
.0238 .02L5 .Oa24 .0032
.0213 .0385 .0198 .OO25
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0040
. o022
. oo02
.0007
.0000
.0000
.0005
0.119 3 .1
0.141 2.8
0 . 061 2 .6
0.031 2.6
0.019 2.5
0.016 2.3
0.035 2.9
o.o44 3.0
0.069 3.3
0.116 5.0
0 -o74 4.8
0.040 4.5
0.038 4.2
0.030 3.3
0.071 4.0
0.093 4 .3
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TOT: 0.159 0.394 O.287 A.129 0.023
AVG: L.4 2.6 4.2 6.6 9.5
TOTAI NL]MBER OF VA],TD READINGS FOR THIS
OUT OF 4042 TOTAI VAIID HOURS
TO:TAI NI]MBER OF MISSTNG HOURS =>TOTAL NUMBER OF CALM HOURS =>
0.008
L2 .1,
TABLE ->
326
24
1.000
3.6
4042
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Table 3-2
Frequencies of Occurrence
Table 3-3
Recorded Liquid Precipitation
Collected at the White Mesa Mill
Table 3-4
Data Recovery Rates
For Parameters Collected
At the White Mesa MilI Station
Januarv - June 2004
orA Stability Class for January - June 2004
Stability Class Time of Day Class
Can Occur
Frequency of
Occurrence (o/o)
A: Very Unstable Dayiieht Hours 14.5
B: Moderately Unstable Daylieht Hours 8.8
C: SliehtlvUnstable Davli.eht Hours t3.9
D:Neutral Anytime )t./
E: Sliehtlv Stable N ehtt me Hours 12.9
F: Moderately Unstable Niehtt me Hours 12.3
Monfh Recorded Liquid
Precipitation (inches)
January M SSINg
February M ssing
March M sslng
April Missing
Mav Missins
June Missing
- JUne
Parameter Recovery Rate (%)
Wind Speed 99.9
Wind Direction 92.5
Sigma Theta 92.s
Stabilitv Class 92.5
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WIND ROSE PLOT
White Mesa Mitl - Blanding, Utah
iSOUTH| --- ---'
WND SPEED(r/9
@ '=,, t
ffi a.s-rr r
M.- ^^w J./ - o.o
ffi a.o- s.z
[l z.r-:.0
E o.s-z.r
Calms:0.30%
DATA PERIOO:
2004
Jan 1 -Jun 30
00100 - 23:00
COMPANY-
lntemational Uran ium Corporation
PREPARED BY:
McVehil-Monnett
Associates FIGURE 3-1C[MW'NDS:
0.30%
TOTAL COUNTI
4042 hrs.
AVG WIND SPEED
3.62 n/s
DATE:
10t5t200/
PROJECT NO.:
1721-A3
WRPLOT View - Lakes En$remental Soflwse
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Hours 05 - 08
N
Hours 09 - 12
N
Hours 17 - 20 Hours 21 - 24
Figure 3-2. Graphical Wind Frequency Distributions by Hour of Day
January - June 2004
IUC White Mesa Miil
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Stability CIass B
Stability Class C Stability CIass D
Stability Class E
Figure 3-3. Graphical Wind Frequency Distributions by Stability Class
January - June, 2004
IUC White Mesa Mill
Stability Class F
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I 4.0 cor{cLUSroNS
I Meteorological data were collected from January through June 2004 atthe White Mesa Mill
site Data recovery rates were acceptable rn'ith all recoveries greater than the required minimum ofI90 percent' The dominant feature of the winds observed at the site was a local noctumal drainage
I flow from the higher elevations to the north-northwest and northeast and a daytime upslope or return
- flow from the southeast through the southwest.I
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1-5
Appendix A
Performance Audit Report
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PERFORMANCE ATIDIT REPORT
FOR TIIE
II{TERNATIONAL I'RAI{IUM CORPORATION
WHITE MESA MILL
METEOROLOGICAL MONITORING STATION
.Iune 2004
Prepared for;
lnternati onal Uranium Colporation
White Mesa Mill
P. O. Box 809
Blanding, UT 8451 1
Prepared by:
McVehil -Monnett Associates, Inc.
44 Invemess Drive East
Building C
Englewood. Colorado 801 12
June 2004
MNIA Project Number i]21-03
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1.0 INTRODUCTION
The semi-annual performance audits for the lntemational Uranium Corporation White Mesa
Mill meteorological monitoring stationwas compieted by McVehil-Monnett Associates onMay27,
2004. Ralph Porter. a Senior Project Manager with McVehil-Monnett Associastes, Inc, performed
the audit. The \Vhite Mesa Mill is located approximateiy seven miles south of Bianding, Utah. The
meteorological air monitoring station is located northeast of the mill and approximately 1/4 mile
west of Highway 191.
This report summarizes the results ofthe performance audit that u'as conducted in accordance
rrrifh the fnllnurino mridqnce dnnrrmonfc.
- "Qualitl,4ttrt*ce Handbook for Air Pollution Measurement Systems", Vol. fV -
Meteorolo gical Measurements, (EPA-600R -9 4 I 03 8d), revised March 1 9 95 .
- "On-Site Meteorological Program Guidance forRegulatoryModelingApplications",
(EP A-450/ 4-87-0 1 3), re-issued Augusr 1 995.
The remainder of this report is divided into sections on specific auditing procedures (Section
2.0), audit resuits (Section 3.0), conclusions (Section 4.0) and recommendations (Section 5.0).
Attachment A contains the audit documents and Attachment B contains the audit iastruments'
calibration certifi cates and documentation.
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2.A SPECIF'IC AUDITING PROCEDURES
The wind direction system was audited for linearity and vane orientation by sighting the vane
at a specific target and comparing system output to the known azimuth of the target. The target
azirnuth was measured to the nearest haif degree by a precision compass. A torque watch was used to
measure the starting torque of the wind direction sensor.
The wind speed system was audited using a selectable speed anemometer drive which tums
the sensor anemometer shaft at five known rates of rotation. The values recorded by the wind speed
measurement system were then compared to the target wind speeds for these rates of rotation. The
Slarfino tnrnrrc nf the r-r-,in4i qr --eerJ qqncnr \rrac ,-aac,,--.1 ,,.;-- o rarnrra,,,^r^Lvr iij! iiriu Jpuuu iuiiiui !idJ iiisdJui trU USiiig a Lijjqijtr niituii.
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3.0 AUDIT RESULTS
Specific results for the meteorological audits are presented in Tabie 1. A brief discussion of
the results follows.
The wind direction audit results indicated that the system response was linear and coffectly
oriented. The magnetic reading of the crossann was 1.5'. The data iogger reading was 9o for audit
orientations of 11.0'. These results fall within the desired accuracy range for the wind direction
measllrement system, which is +5o. The starting torque of the wind direction sensor measured less
than 3 gram-centimeters (gm-cm) clockwise and counter-clockwise, which is below the upper
accepta:rce iimit of 6.5 gm-cm- The rryrrrd vane was oriented to onl5. one la:rdmark due tc the
instabiiity of the tower and lack of availability of a "buckettruck". I1owever, the linearity of the
system demonstrated excellent agreement between the known wind direction and the digital output
from the data acquisition system indicating that the system is accurate and recording quaiity data.
The wind speed audit results were excellent. Data logger results were identical to the known
winri speeds at the foliowing speeds, 0.268,2.9,5.6,8.3, 10.9 and 13.6.4 meters per second (mps)
corresponded very closely to their respective target wind speed values of 0.6, 6.6, 12.5,1 8.5, and
13.5 mps. The desired accurac-v range for winci speeri auciits is *(0.2 mps + 5% of observed). Starting
torque was measured at less than 0.2 gm-cm, which is below the upper acceptance limit of 0.22 gm-
cm.
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TABLE 1
AUDIT RESLTLTS
INTERNATIONAL URANILIiVI CORPORATION
W}IITE MESA MILL
METEOROLOGICAI STATION
May 27,2A04t
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Wind Directionl
Sensor starting threshold torque:
Sensor Crossarm Orientation is:
Wind Speed2
0.p*
100 rpm
200 rpm
300 rpm
400 rpm
500 rpm
Audit Value
30.0.
90.0.
180.0.
270.4"
350.0"
4 gm-cm CW and CCW
1.50
Audit Value
0.268 mps
2.9 mps
5.6 mps
8.3 mps
10.9 mps
13.6 mps
Digital Value
29.3"
gg.1 "
779.0"
274.6"
351.0'
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Digital Value
0.268 mps
2.9 mps
5.6 mps
8.3 mps
10.9 mps
13.6 mps
Sensor starting threshold torque: < 0.2 gm-cm
1) Wind ciirection system target accuracy: t5o. Sensor starting tlu'eshoid torque upper acceptancelimit: 6.S gm-cm.
2) Wind speed systern target accurac,v:+(0.5 mph + 5%o of observecl). Sensor starting torque upper
acceptance limit: 0.22 gm-cm.
lr
lr
lr
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4.0 CONCLUSIONS
The performance audit also documented the curent operating characteristics of the
meteorological instrumentation. The results of the meteorologicai performance audit indicate that
ali instrumentation was operating within EpA-specified accuracies.
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5.0 RECOMMENDATIONS
Due to the stabililv issue of the monitoring tower, it is advised that personnel no longer
climb the tower when it is fully extended. Once the tower is cranked to the lowered position
climbing is permissible. This makes testing the wind direction sensor very difficult by orienting
to known targets. The wind direction sensor should be re-oriented on the crossamr so that the
data acquisition system reads 360o, and 180' when the wind vane is pointing directly down the
crossann in each direction respectively. The crossarm should then be reoriented from magnetic
north to true north (348" magnetic) accounting fbr the 12' easterly-declination at the site.
Sighting or measuring the orientation of the crossarm relative to true north will then sirirpliff
future audits. Once the orientation is known to be correct linearitv ean be eheeked, these two
steps will verify sensor integrity and system accuracy with out the need for climbing the tower or
necessity for bucket trucks.
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ATTACI{MENT A
T AIR QUALITY PERI'ORMANCE ATIDIT D'CIIIVIENT'S
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Sensor
/-r rn e
Data Logger
Manuf a ctu:'e r /t'tode I
rud.-n,,jL o;:r^
M +b - &.vio
fr\fi *fft*
cin-^UJ LE f,t**
Form No, f,2003D.1Eevision No. Origina.lDate 1/9-?page I of l
WIND SPEED AUDIT FORM
Serial No.
t ,r 'I -[ .l :F ;.- .-
r t f r't.!-J € *
ProS eci { !} *
Sensor H,eig]nt /a vq
Auditor €n-
:br?-L,/'n- Reading Ze,L +" e,Z-3#.ds(Torque Wal-ch &J*"{-.tus
\rr1p 14 :: ? i' ll'r
;n@#4!\t.lr,)
1.
2.
3.
4.
5.
-+- /1)
2)
3)
4)
s)
Test WS (mph)
. Lr,?
a.c1
.; n ta
I Lr ,*1
| 3'u
0 Rpv:
IDO RtrM :
_ Lelo P_PM =
So"o RpM :
DYNAMTC WTND SPEED
(Using Sl,nchronous Motoz-s or an
Ci{ECK
Anemometer Drive)
(e m6h
mbh
lr1' fl li,
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P.PM = ID,'I
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l)cll .)
mbh
Al:soluteDifference (mph)Loqqer (mph)
Lt-Z
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D, .)
ln !^
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!
Form No. F2004D.i
Revision No. 1
Date 4/98
rage .t oi .l
Wn\ID DIRECTION ALIDIT F'ORM
Sensor
Va:re
Digital Data Acq.
ComFass
Theodoiite
Torque Watch
Solar Sighting:
Degree Wheel
(Desrees)
JU-UW
90-cw
i80-cw
270-CW
350-CW
Manufacturer/
Model No.
Wz*
t4 ab * #u -*-(*y c 4ro
S.*.L,
FJ/o' "t
Sensorlleight I # ,a+.
Serial No.
t,)tta*)tAl 4 I i 1\. " i t tlE)
t t l,l
1e, ,J) tee
", ,'1"Dare/Time S /al /c4v-+--ir ,
Auditor N,*1,,r-L FrU*:--uJde_rs 3ar,_g*. n^airg,_ j_AEs.-
Time dr} A Azimuth r* t*. Ir.cliaatiou * t\
Lanrlmafl; #1 tloi o-r fi'l-r.,e.f. P,:L
Azimuth - A.5] "i -
"
Azimuth ll o
(corrocted)
Landmark#2 8",1",q.- FcLs- - Nq,t Lr.je,nu.,.,{c
Azimuth i*J/S
Azimuth ','U/&
(corrected) i
X- f+r:+ -x-.d* i--; ;.S,. +u;.Id.i r.ig.fi.+e_ 35 ,, t) i;;3:
Slstem Linearie,Check
Digital
(Dewees)
Ar"-J
li,8
rL //) r(z
vr'l
Degree Wheel Digital
fDesrees) fDesrees)sme coslne /'//
,/*.r'\14dw,-/*:- ,/
,/
-?30-ccw
270-CCW
18O-CCW
90-ccw
30-ccw
E :..1rttt
&'li,?
:-*Y
€,1,.'*n
)a^D
Mc\Ea{IL-MONNEfi ASSOCIATES
Landmark #1
Sensor/Data Logger
Az.@eg.) Si:re Cosine
Landmark #2
Sensor,Data Logger
Az.@eg.) Sire Cosiae
ATTACIIMEI.{T B
DOCI.N{ENTATIOI{ OF'
AUDIT INSTRUMENTATION CERTIFICATION
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McVcN - Monnclt Asrgiaix Loc.
COMPASS CALIBP+.TION DO CUMENT
f 9u/Juutdu.
Caiibraliou
Location:
Magretic
Declilaiion:
N (-o)
E (-90)
SE (ru|:j)
s (- i80)
s'(-270)
le:!uic::l Siglzrui= -i
lZ-i Li,*c z i-i 5? e trnr L-
/-' r1 t-i -^ J-.=i h ,f t'{t^\'r/ )u1('Make:
Model:
SeriaI
Number:
Instrurnent(s) Used for Calibration
Comoass
Ct
I ',r - 'L
- _-,w /\ I t
1-, P- r u /'r," ,r\ ,-'- t1l 5L,:)
I : i\ r,c)
Type and l,{ake:i r rl r )rL Q i ': = 7- he od a {,tta
Mociel and Serial Number:
Cerr-ifieci:
\-^l-! I /i\s,'/'arrlr-.//r) I 1@>
^.: I l. " /i c=i 7 u, l)tt{ iLpey'
NE 1-45 _4ii rL';.- i'il? t._ = f
fll"'a , -n :! a!... ;tv.y 5_ 7g 11r €i'6"i, i,l,-.,, '*:-_,+6-\-
\'/' .l U4. L-'
rI,5 1 IJAIA
Caiibraiion Instrument Compass (Degrees)
@egrees)Acrual lCorrected
) /- >
/-^ h ..\).*
./ )'l 1\4- /.<, -
:,i7,s 3i7, /
L-, 't .) s
lt-'*'t
i'- C? /
F3;i- t.'
c,i'
xw 6*311 |
r) a)-t-,\qr-,1- V\c-"+"*
{..-<+ €oq'g 6'.,-11
br, , ]4tnq k' lL;,./i,
) \- ^i-^+i.H
l,-l ,n; 1a ,,. p;, - I
:,i S-=uJ riblita';r
Nexi Certiication Due: 'Dr. C , J crc, 3
0.0
.2
.4
.6
o.o
l_.0
7.2i.4
t-.6
r_.8
2.0
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LOW P.ANGE TOP,eLE WATC:{ DIAr_ SETTINGS
T\4ODFlT,. 1(A-"M q:;-iT Ni-114--=p z?a:
/rI t, t ) ^ ji ltq,r)<-. | \ tv /lr
vS. OUTPUT oF Lo-r; F.:ANGE ST]$[DAP.D
ir* I ! -'-n-:s - En :i-i i:tr;::a:_,_ _ :u
L--{--- - r-l-L-y! j-_u9 _--rCjl _-lT.::
0.0c . cI_
. t_3 .40.35 .50,5A .80.78 1.00i.Ot_ 1.2A1.20 t-.40
1 L-A- 1 .^
-, UJ
-L . c2 1, t 01.E4 2.C)-a n -z.u3 2.2A
T,nrrr T,i ri i
_ n 1r v!
c. 00
.2A
a-a
.80
l_. 00
t-.20i.40i. 50
t-.80
CW F,dg
o.00
a=, -)
.A
Qi
l-. 0B
1.28
1.51-
l-.70'l ea
, f) o
ivla:r r,oq FTT-T i 9- :r- \
iri=r- r a- ---t-'* /'o- F- \:_;_.- -:-4 =__!_ t,-. j:, =
To:que lry-a:ch - s a: ?-4SS
". rNrr.AL SALtEBATION tS/
vor^r-r'ro -.€tl?__f 4(_s,* I 5 [i5
CALIBHATED BY \IS ,L.'
FECOMMENDED SCHEDUI.E:
SCH=DULE BY DAT=
CA].IBRAT]ON REQU IBEMEhITS
YOUF TOnOUE WATCH GAUG= WAS CALlBRATED A; TII!4E OFsHrpM=NT, ir SHDULD BE FECALTBFATED pEHroDrcALLy. iDMAINTAIN IT'S ACSUBACY. WHILE TOFOIj= PFOOUCiS EN:-DESIGNED To HEoUIBE oNL), Y=AF:Y eAUBRATIoN, WITi HEAVYOR DAILY USAG:, CALIBHATION.IS HECOIi4MENDED EVENV SXMSNTHS, FOR HECALISF]ATION S=RVI:ES :RAN;ARI ; T' \I I < -
?_1IEl3rB llEEDS, cAHEFULLyjFACKeo: rHr ur.rriairoi:iuniiIT TO US, WE WIL. SIJBNIIT,A C5E- ESTI]\iAIE UDON HACEi;T.
\ tL 2 =- I /n^: , = r_r.J-i.3 i; at .200
SCHEDIJL= B\' DATF
ffi*,me;tryeEe
1 OO DISCOVEEY WAY, ACTON, MA 01720 USA
t' () -/- n -
I -At,4,
'i't J
T:L3.oHON= (97S) 264-9:s0 FA)l (s78) 2e3-053C
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${susiorc. @r'ecisicn, f,ftc "Ca{i6r'at'isrc @Sp*r^t
8729 €"f Freewcy
5{ouston, fX 7f0 1 f-65 01t
I
Company:
Address:
Contact:
Dept:
MCVEHILL-MONNETT ASSOCIATES
44 IN\/ERNESS DR EAST
Dln^^
ENGLEWOOD, CO 80112
RAY ROETMAN
Doc #:
Date:
pnf.
Page:
J+JOJ
9116/2003
90C-l\4ET-238
1
I Gage:
Mfg;
Location:
Torque Watch
Waters
Control:
Mociel:
Serial #:
+JA1
JOD- llvl
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+,/ - Tolerances:
Graph Scale:-tcO -75 -50 -?5
+2.000000 / -2.000000
+0.005000
t-) la 50 75 100Clcclrwise Torgue = Vattsesnr- -- -l",as -=f -q-Jg D=r.i=.rlo:.:+3.000000 +2.980000 _0.020000
19.000000 +9.990000 -C.01000Cr'l 'l nnnnnn t1 ) t,- . J00000 r3.00000C+15,000000 +15. Ot00c0 _0.010000+18.000000 +is.01000c +0.010000
Comments:
Reference HPI, SiO# 10671
Itle ceftiiv the eouipment lsed for lhis calibmtion is tnceable lo ,A//s7 through one or more of the following numbers\'-e978074: CDI DtGtTtrST TOROUE WATCH CALIBRATOR
Gage status: PASS i /,1 Ne4.t caiibration Due: gf 16rz0a4
cerliiled 3v: Satvador Gon-aiez Signature: i,O l'..,1y.1iir - -/frp?{:tJc-..'
Tiis:=rtiircat=isncivaiiountessaIl,ioaoe(s)u,.pr"=
"Laboratorv Environmenlal condiiions: Temperature: Zoc +l- 2c, Relative Humiditv: betwe-n +o*1ns ooo/o"calibraticn msasurements are perform=d jn accordance wiih quideiines setforth in ANSj/NCSL 7540-.1-.1 994, Iso10012_1the 1SO 9000/as9000 seiies of quality standaros and Houston Preclsion's euality manual cjated: 6ij5/01, Rev. j."lf addiiional informaticn regarding ihis calibraiion is required, please con.iaci ihis Iaboi-arcry.*All caiibrat)ons irave be=n penormeo'under the supervision ano authoriry of p,yan D. oliphant, Lab Manaoei.--This Repori of Test may only be reproduc=d in fullwith the expr=ssec1 wrilien p=rmission of Housion precision, inc.
lqn/ tra tTnrx
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ftfi e'tea ro lo g i ca ! I n stru rnents
Certiflcaie of Calibration and Testing
R.lt4. Young Conrpany certifies that the aborre
calibrated using stanciards whose accuracies are
Siandards and Technologies (NIST).
equipment has been inspected and
iraceable to ihe National Insiitute of
(1)
(2)
\r.)
Measured at the optical encocier ouiput
Frequency output produces 320 pulses per revoluiion of the motor shaft
Indicaieci on the conirol Unii LCD display - Note: Divide displayed rpm by 10 toe rlnr tia*a nnir rcl ma*nr '^-
*lndicates oui of ioierance
ffi trto CaiiUration Adjusiments Required L l As l-ound
|-tDr aar
I-l a" I ofi1 I / rv !e'L
Traceable frequency
Date of inspeciion
meter used in caiibraiion
'10 January 20C3
Tesieci By
R.M. YOUNG COMPANY 2801 Aero Park Drive, Traverse City, Michioan 49686 U;A
Te l: 2l 1 -946-3980 Fax: Z3i -946-47 72 Email; met.sal es@vouno usa-com
Test Unit:Modei: 'lBB10
Description: Anemometer Drive -
- iomprised of Mooels
Serial
10 to 1,000 Rpm
18820 Control Unii &1 8831 Motor Assemblv
Nominal
li,4 oror
Rpm
Output
Frequency (1)
iz
Calculated
Rpm (2)
Indicated
Rpnr (3)
60
t.
120 d+o tZc I /iJ( )
24A Z4x>
420 ZZlo 1?-o ALoe
A5n ZZw>bw (aOnr>
llzi il^^t-.n,ioo anrt f-^,,n{ -F^r^^r..".D v,vv,\ rleru,rur-lv
I3to i g ic:
IQao I Q*cc
i^^ -^+-+i^^.,--:il-rlDtr ruLoLrul|\,Elilt=u
Appendix B
Hourly Data
in
SAROAD Tables
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Appendix C
Joint Frequency Distribution
Of Wind Speed by Wind Direction
By Hour of the Day
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1O METEP. WIND DATA ANALYSIS
FROM !/ L/20A4 THROUGH 6/_30/2AA4
INTERNATIONAL URANIUM METECROLOGICAL STATTON
FREQUENCY OE OCCURRENCE OF WIND SPEED BY DIRECTION
HOUR OF THE DAY OO_04
+----------WIND SPEED CLASSES (M/S)---,------+
0.0- 1.8- 3.3-DrR 1. B 3.3 5.4 8.4 11.0 11.0 TOTAL
AVERAGE
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.0041
.0428
.0010
" 0013
.0005
.0008
. 0010
.0003
.000s
.0008
.0005
.0008
.0028
.0031
a2tB
0285
0111
0099
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
,0000
.0000
.0000
.0000
.0000
,0099 .00lc
0017 .00c7
0010 .000s
. 0005 .0000
.0005 .0000
.0000 .0000
.0000 ,0000
.0000 . 0000
.0000 .0000
.0000 .0000
.0000 . 0000
. 0005 .0000
.0005 .0005
. 0000 - 0002
.00c0 .0000
.0005 .0000
.0000 . 0000
.0005 . 0002
,00c7 .0000
0.038 2.9
4.044 2.8
0.015 2.3
0.005 2.2
0 . 002 2.6
0.003 1. 9
0.003 2.3
0.002 2.7
0.005 3.3
0.006 4.4
0. 003 3.6
0.002 2.4
0.004 3.1
0.003 2.5
0.017 3 "2
0.015 3.0
0 015
0025
0 010
0 017
0 017
0005
0 010
0420
0 017
0082
0057
0c00
00c0
0002
0 017
a02t
0015
0005
001c
0002
0052
0052
T
I
I
I
I
TOT: 0. 030
AVG: 1.4
TOTAL
0.442 0. 004
4.7 6.3
0.000
0.0
TABLE ->
326
0.090
2.6
0.001
9.6
0 .1 €,1
2.9
NUMBER OF VALJD READINGS FOR THIS
OUT OF 4042 TOTAL VALID HOURS
TO?AL NUMBER OF MISSING HOURS :>
6"7 2
I
I
I
I
t
I
I
I
T
T
I
t
I
I
t
I
T
t
I
1O },JETER WIND DATA ANALYSTS
FROM I/ l/2004 THROUGH 6/3A/20A4
INTERNATIONAL URANIUM I"{ETEOROLOGICAL STATION
EREQUENCY OF OCCURRENCtr OF WiND SPEED BY DIRECTION
HOUR OF THE DAY 04_08
+--------*-hrrND sPEED CLASSES (M/S)_________*+
DIR
0"0- 1.8-1.8 3.3
N .0054 .0a92 .0A41 .0000 .0000
NNtr .0081 .0309 .0082 .0002 .ooo0
NE .0091 .0115 .0017 .0005 .0000
ENE .0033 .0035 .0002 .00c5 .00c0
E . 0038 . 0025 .0a02 . 0000 . 0000
ESE .0023 .0010 .00c2 _ 000c .0000
sE .0016 .00s2 .0025 .0005 .0000
ssE .0025 .0037 .0010 .0000 .0000
s " 0003 .0017 .0007 .0005 .0000
ssw .0003 .0012 .0012 .0017 .0002
s!{ .0005 .0010 .0010 .0000 .0000
l{sw .0003 " 0005 . 0000 . 0002 . o0o0
!{ .0018 .0015 .0000 .0000 . o0oo
r/\iNW .0423 . 0c:7 . 0000 . 0002 . 0000
NW .0018 -0030 .0030 .0005 .0000
NNW .0028 .0045 .0054 .0010 .0000
3.3- 5.4 8.45.4 8.4 11.0 11. 0
AVERAGE
WTND
SPEEDTOTAL
0.019
o .041
n nr"
0. 007
0. 006
0. 003
0.010
0. 007
0. 003
0. 005
o .002
0. 001
0. 003
0. 004
0. 008
0.014
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
. c000
.0000
2.1
2.6
)')
2.2
7.9
1.9
2.1
atr
3.5
4.6
2.6
3.6
to
2.2
3.1
3.3
ToT: 4.046 0.083 0.030 0.00G 0.000 0.000
AVG: 1.4 2.5 4.i 6.0 10.1 0.0
TOTAL NUMBER OF VALID READINGS EOR THIS TABLE
OUT OF 4042 TOTAL VALID HOI]RS
TOTAL NUMBER OF MISSING HOURS :> 326
0.165
2.6
-2 0 / I
t
I
I
t
!
I
1O MtrTER WIND DATA ANALYSIS
FROM Li 7/2A04 THROUGH 6/3A/2A04
INTERNATTONAL URANIUM METEOROLOGICAL STATION
FREQUE,NCY OF OCCURRENCE OF WIND SPEED BY DIRECTION
HOUR OE THE DAY OB_I2
+----------wrND spEED CLASSES (M/S)----------+
DIR
0.0- 1.8- 3.3- 5.41.8 3.3 5.4 8.4 11.0 11.0 TOTAL
AVERAGE
WIND
SPEED
t
t
t
t
I
I
I
T
N
NNE
NE
ENE
E
L5L
JI,
S
SSW
SW
WSW
W
.0013
.0018
.0023
.0025
. 001E
.0018
.0020
.0031
.0032
.0023
.0011
.0015
.0018
.0005
.0005
.0008
0007
0021
00r2
0c25
004 5
0106
015 1
008 9
00 41
0a21
aa22
0012
0 015
0005
0015
0015
00L2
0000
ac32
0054
0099
011 6
004 0
0007
0007
0002
0020
0020
.0000
.0000
.0000
" 0000
.0000
.0000
.0000
- 0000
.0000
.0002
.0000
.0000
.0000
.0000
.0000
.0000
WNW
NW
NNW
.0000 .0007
.0020 .0010
.0002 .0000
. c000 .0000
.0007 .0000
. 000r .0000
.0000 .0000
.0002 .0000
.0c72 . c000
" 0015 .0002
.4422 .0002
.0084 .4025
.0032 .0005
.0005 .0007
.0007 .0000
.0005 .0000
.0022 . 0000
.0c37 .0000
a .002 2 .1
0.005 2.2
0.005 3.0
0.007 2.8
0.004 2.5
0.004 2.2
0.011 2.1
o.021 3.2
0.031 3.4
0. 034 4.1
0.013 4 .4
0.006 3.5
0.005 2.8
0. 002 3.2
0.006 4"6
0. 007 5 .3I
T
T
T
I
TOT: 0.028
AVG: I.4
TOTAL
0.061 0.04 6
2,6 4.2
0.000
11.3
TABLE :>
326
0 .425
6.4
0.004
9.5
0. 166
3.6
NUMBER OF VALID READINGS FOR THIS
OUT OF 4042 TOTAL VALID HOI]RS
TOTAL NUMBER OE MISSING HOURS :>
61 \
T
I
I
I
t
I
1O METtrR WIND DATA ANALYSIS
FROM l/ 7/2004 rHRouGH 6/3A/2004
INTERNATIONAL URANiUM METEOROLOGICAL STATION
DIR
FREQUENCY OF OCCURRENCE
HOUR OF
+_____----_WIND SPEED CLASSES
0.0- 1. B* 3.3- 5.4
1.8 3.3 5.4 8.4
OF I^]IND SPEED BY DIRECTION
THE DAY 12_76
(M/S ) ----------+
11.0 11.0 TOTAL
AVERAGE
WIND
S PEED
I
I
t
I
I
T
I
I
N
NNE
\lr
ENE
E
ESE
SE
JJL
s
SSW
SW
WSW
W
WNW
NW
NNW
.0005
.0003
.0010
.0008
.0000
" 0003
.0018
.0015
.0013
.0021
.0013
.0010
.0005
.0008
.0003
" 0008
0005
0007
0005
0005
00c7
0000
0000
000c
0000
0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0020
.0005
.0002
.00c5
.0000
.0000
.0005
a0L2 .0010
0472 .00r 2
0010 .0010
001 2. . o0a2
0.003 3.1
0.002 3.8
0.004 3.2
0.004 3.2
0.003 4 " 1
0.002 2.9
0.006 3.3
0.008 3.6
0.017 3. 6
0"045 5.0
0.031 5.0
0.010 5.3
0.005 5.5
0.007 4 .7
0.011 5.5
0.008 6 "2
.0012
.00i5
.0030
.0032
.0069
.0114
" 007 4
.0015
.0010
.0017
.0017
.0005
UUU /
00c5
0 010
aal2
0067
0168
0104
0020
0015
an?,
0032
oo??
ao22
0094
0094
a0 41
4021
0 012
005 9
0032
0000
0032
0 017
00c5
0000
0000
00c2
0 012
0002 .0000
0002 .00c2
0010 .0007
t
I
I
I
I
TOT: 0 " 014
AVG: 1.5
TOTAL
0.04 6
2.6
0.053
4.3
0.043
6.8
0.0c8
9.4
0.004
11. B
TABLE :>
326
0.168
4.6
NUMBER OF'VALID READINGS FOR THIS
OUT OI' 4C42 TOTAL VALID HOURS
TOTAL NUMBER OF MISSING HOURS =>
61 6
I
I
t
I
I
T
1O P]ETER IdIND DATA ANALYSIS
FROM L/ t/2004 THROUGH 5i30/2004
INTERNATIONAL URANIUM METEOROLOGICAL STATICN
FREQUENCY OF OCCURRENCE OF V;IND SPEED BY DIRECTION
HOUR OF THE DAY 16-20
+__----_**-WIND SPEED CLASSES (M/S)_______--_+
DIR
0.0- 1.8- 3.3-1.8 3.3 5.4 8.4 11.0 11.0 TOTAL
AVERAGE
WIND
S PEED
t
I
I
t
I
t
I
t
N
NNE
NE
ENE
E
SE
S
SSW
SW
WSW
W
I{NW
NW
NNW
.0001
.0015
.0425
.0018
.0008
" 0008
.0010
.0015
.0026
.0011
.0026
" 0015
.0013
.0013
.0008
oa22
0072
0005
001c
00c7
0 017
0057
00 41
004 7
4022
0 017
0 010
t)iri_\',
0005
0 015
0007
0024
0452
0035
0067
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0017
.0007
.0000
.0002
.0000
.0000
.0000
0052 . 004 9
0040 .0015
0015 .0000
0000 .0000
0002 .0000
0005 .0000
0005 .0000
0002 .00cc
0002 .0000
000c . a0a2
0002 .0002
0042 .0015
0069 .0015
0064 .0005
0054 " 0005
0015 .0c00
0025 .0017
0c12 .0010
4.072 3.8
0.007 2.1
0.007 2.6
0.004 2.8
0.002 3.1
0.002 3.0
0. 003 3. 6
0.004 3.1
0.011 2.8
0.018 5.5
0.020 5.2
0.017 4.8
0.01s 4.9
n nn? / i
0.015 4. B
4.022 -5.1
0020 .0054
0 011
0035
0030
0059
0035 .0092I
I
t
I
I
TOT: 0.422
AVG: 1.3
TOTAL
0.053 0. 038
4.4 €).1
0.003
12 .6
TABLE :>
326
0.04 5
2.6
0.007
9.4
0.167
NUMBER OF VALID READINGS FOR THIS
OUT OF' 4042 TOTAL VALID HOURS
TOTAL NUMBER OF MISSING HOURS :>
51 6
t
I
I
t
I
I
I
I
I
I
I
I
T
t
I
I
I
I
I
1O METER WIND DATA ANALYSIS
FROM i/ 7/2A04 THROUGH 6/3A/2004
INTtrR.NATIONAL URANIUM METEOROLOGICAL STATION
EREQUENCY OF OCCURRENCE OF' WIND SPEED BY DIRECTION
HCUR OF THE DAY 2A_24
+----------WIND SPEED CLASSES (M/S)--*---*---+
nn_
D]R 1. B
1.8- 3.3- 5.4 B-4
CA 8.4 11.0 11.0 TOTAL
AVERAGE
WiND
SPEED
N
NNE
\lr
-LL\ -L
E
ESE
SE
ear
c
SSW
SW
WSW
W
WNW
NW
NNW
" 0025
.0025
.0010
.0008
. 0010
.0003
" 0005
" 0008
.0005
.0000
.0008
.0003
" 0010
.0015
.0031
.0018
.4273
.0210
.0035
.0012
.000r5
.0000
" 00i2
" 0007
.0010
.0005
.0005
.0020
" 0012
.0021
.0059
. ao61
0208
a72L
0020
0007
UOL)O
0002
0007
aac2
0 010
0047
0012
0 012
0005
0 015
cc22
014 6
.00c0
.0000
.0000
.0000
. u0ut)
.0000
.0000
. c000
.0000
.0000
.0c10
.0000
.0000
.0000
.0000
.0000
0005 .0000
0000 .0000
0007 .0000
0002 .0000
UUL) U . OOOO
0000 .0000
0000 .0000
0000 .0000
0002 .0000
aa21 .0007
oal2 .0002
0000 .0aa2
0015 .0000
0002 . c000
000? .0010
0040 .0002
0.04s 3.3
0.036 3.0
0.007 3.3
0.003 3.0
0.002 1. B
0.000 2.5
0.002 2.8
0.002 2.L
0.003 3.5
0.009 5.5
0.005 6.7
0.004 3.5
0.004 4.0
0.005 2"9
0.013 3 " 4
0.421 4.7
TOT: 0.018
AVG: \ .4
TOTAL
a.ai2 0.002
6.6 9.8
0. 001
11.9
TABLE :>
?,2 €,
0.070
2.1
'..t. t.rb4
4.2
0.168
3.6
NUMBER OF VALID READINGS FOR TI']IS
OUT OF 4042 TOTAL VALID HOURS
TOTAL NUI'4BER OF 14]SSIN.G HCURS =>
616
Appendix D
Joint Frequency Distribution
Of Wind Speed by Wind Direction
By Stability Class
t
I
I
I
I
t
10 METER W]ND DATA ANALYSIS
FROM 1/ t/20A4 THROUGH 6/30 /20A4
INTERNATIONAL URANIUM METECROLOGICAL STATION
FREQUENCY OF OCCURRENCE OF WIND SPEED BY DIRECTION
STABILITY CLASS A
+----------WIND SPEED CLASSES (M/S)----------+
DTR
CA
8.4
0.0- 1.8- 3.3-1.8 3.3 5.4 11.0 11.0 TOTAL
AVERAGE
WIND
SPEEI)
I
t
I
I
t
t
I
I
N .0030
NNE .0030
NE .0062
ENE .0045
E .0047
ESE .0030
sE .0050
ssE .0065
s .0048
ssw .0040
sl1] " 0030
wsw .0035
!f .0028
I,/NW .0025
Nr{ .0015
NNW .0030
.4025 .0000
.0025 .0000
.0017 .0000
. oa42 . 0000
" 0037 " 0000
.0035 .0000
.0412 .0000
.0099 .0000
.0134 .0000
.012L .0000
.0064 " 0000
.0035 .0000
.0045 .0000
.0025 .0000
.0432 . 0000
.0030 . 0000
0000 .0000 0.00s 1. B
0. 005 1. B
0. 008 1. 5
0.009 )_.1
0.008 1. B
0. 0c6 7.9
o .012 2 .0
0.016 2.0
0.018 2.2
0.015 2.2
0. 009 2.2
0.007 7.9
0.007 7.9
0.005 1.9
0. 005 2.t
0.005 1. B
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
" 0000
.0000
0000
000c
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.00c0
" 0000
T
I
I
I
T
ToT: 0.061 0.084 0.000 0.000 0. 000AVG: 1.4 2.4 0.C 0.0 0.0
TOTAL NUMBER OF VALID RE,ADINGS FOR THIS
OUT OF 4042 TOTAL VALID HOURS
TOTAL NUMBER O!- MISSING HOURS :>
0.000
0.0
TABLE :>
325
0.145
583
2"4
I
I
I
I
t
I
1O METER WIND DATA ANALYSIS
FROM L/ L/20A4 THROUGH 6/3A/2004
INTERNATIONAL URANTUIV METEOROLOGICAL STATION
FREQUENCY OF OCCURRENCE OF V\]IND SPEED BY DIRECTION
STABILITY CLASS B
+_-----_-__WTND SPEED CLASSES (M/S)__---.___-+
DIR
0.0-
1.8
1. B-
?l
3.3- 5.4 8.4
5.4 8.4 11.0 11.0
AVERAGE
WIND
TOTAL SPEED
t
t
I
I
I
I
I
t
N .0005
NNE . OOOB
NE "0012
ENE .0005
E .0000
ESE .0005
sE .0000
ssE .0003
s " 0001
ssw .0003
sw .0005
wsw .0000
!1I .0007
WL]W , COO3
NW .0003
NNW " 0000
.0000 .0000
.0000 " 0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
.0000 .0000
. 0000 .0000
. 0000 .000c
" c000 .0000
.0000 .0000
o .002 2 .9
0.004 2.1
0. 003 2.4
0.003 3.0
c. 002 3. 4
0.002 2.3
0.005 3.2
0.008 3.2
0.017 3.2
0.018 3.3
0.009 3.1
0.003 3.4
0. 003 3. 0
t. vvz L " a
0.003 3.2
0.003 3.3
.0007
" 0015
" 0at2
. o012
.0007
.0015
.0030
.0045
.0114
.0082
. 004 9
" 00L2
.0007
.0c10
" 0012
- AC)12
0007
0 015
0007
0012
0 010
0002
0025
0032
0059
0094
004 0
0022
0 017
c00s
0 015
0 015
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000I
I
I
I
t
TOT: 0.006
AVG: 1.5
TOTAL
0.000 0.0000.0 0.0
0.000
0.0
TABLE :>
326
0.044
2.9
0. 038
3.6
O.OBB
355
3.1
NUMBER OE VALID READINGS FCR THIS
OUT CF 4042 TOTAL VALID HOURS
TOTAL NUMBER OF II{ISSING HoIIRS :>
I
I
t
I
I
I
10 METER WIND DATA ANALYSIS
FROM t/ L/20A4 THROUGH 5/3A/2004
INTERNATIONAL URANIUM METEOROLOGICAL STATION
FREQUENCY OE OCCURRENCE OF WiND SPEED BY DIRtrCTION
STABILITY CLASS C
+----------WIND SPEED CLASSES (MiS)---------*+
DIR
0.0- 1.8- 3.3- 5.41.8 3.3 5.4 8.4 11.0 11.0 1U.t AL
AVERAGE
WIND
SPEED
I
I
I
I
T
T
t
I
N .0007
NNE " OOOB
NE " 0015
ENE ,OOT2
E .0000
ESE .0002
sE .0000
ssE .0000
s " 0000
ssw " 0003
sw .0000
ll]sw .0000
w .0002
YII\VV . UUT]/
NW .0000
NNW .0000 0002 .0057
.0000 .0000
.00a2 .0000
.0000 .0000
.0005 .0000
.0002 .0000
.0002 .0000
.0000 .0000
.0002 .0000
.0015 .0000
.0037 .0000
.4452 .0000
.0025 .0000
.0015 .0000
.00i2 .0000
.001r .0000
.0017 .0000
0.004 3.3
0.005 2.6
0.007 2.8
0.004 3. 6
0. 002 4 .4
0.001 4.0
0.005 3.1
0.006 3. B
0.015 4 .4
0 .029 4 .5
0.022 4.1
0.009 4.9
0.005 4.6
0.006 4. B
0.010 4.9
0.008 4 . B
. 0010
.0045
" 0432
.0005
.0002
.0000
" 0017
.0025
.0015
.0032
.0030
.0007
.0002
" 0002
.0005
0020
0007
002 0
0022
0 012
0 010
0030
0037
011 6
0223
aI29
005 9
0032
0040
0074
.0000
.0000
.0000
.000c
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
. U U rll.l
.0000
.0000
TOT:t
I
T
I
t
0.005 0.023 0.089 A.A22 0.000t.4 2.6 4.6 5.'t 0.0
TOTAL NUMBER OF VALID READINGS FOR TIiIS
OUT OF 4042 TOTAL VALID HOURS
TOTAL NUMBER OF MISSING IiOURS ->
0.000
0.0
TABLE :>
326
0.139
551
4.3
I
I
I
I
I
I
10 METER WiND DATA ANALYSIS
FROM L/ 7/2004 THROUGH 6/3A/2004
INTERNATIONAL URANIUM METEORCLOGICAL STATION
EREQUENCY OF OCCURRENCE OF WIND SPEED BY DIRECTTON
STABILITY CLASS D
+----------wrND spEED CLASSES (M/S)*---------+
D]R 1.8 3.3 5.4 8.4 11.0 11"0 TOTAL
AVERAGE
WIND
SPEED
I
t
I
t
T
I
I
I
N
NNE
NE
ENE
tr
ner
S
SSW
SW
WSW
W
WNW
NW
NNW
.0013
.0032
.0020
.0000
.0000
.0000
.0005
.0005
.0008
.0005
.0005
.0003
.0008
.0010
.0003
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0040
" 0022
.00c2
.0007
.0000
.0000
.0005
.0205 .0223
.0465 .0190
.0119 .0042
.0024 " 0017
"0072 .0007
.0010 .0002
.0017 .003s
.0420 .0020
.0020 .0442
.0035 .0077
.0021 .0040
.0020 .0a21
"0022 .0040
.0c37 . 003r
.0064 .0096
" 0037 .0242
.0032 . 0000
.0012 .0000
.0021 .0000
.0020 .0000
.0010 .0000
.0005 .0000
.0422 .0002
.0022 .0012
. 004 5 . 0005
.0233 .0087
.0145 .0042
.0094 .0a20
.0094 .0005
.0025 .0000
.0105 .0032
.0181 .0025
a .041 3.1
0.0?0 3.1
0.027 3.4
0.006 4. s
0.003 4.4
0.002 3.9
0.008 4.3
0.008 5. 1
0 .072 4 .9
0.048 1.0
0.028 6.9
0.017 6.2
0.018 5.1
U. U-LU 4 . Z
0.031 5.3
0.04 9 5. 5I
I
T
I
I
TOT: 0.0L2 0.113 0.114 0.107 0.023AVG: L.4 2.1 4.2 5.8 9.5
TOTAL NUMBER OF VALID READINGS FOR TI]IS
OUT OF 4042 TOTAL VALID HOURS
TOTAL NUMBER OE MISSING HOURS :>
0.008
L2 .l
TABLE :>
326
0.371
1523
4.9
t
I
I
t
t
I DIR
1O METER WIND DATA ANALYSIS
FROM t/ r/2A04 THROUGH 6/30/20A4
INTERNATIONAL URANIUM IVIETEOROLCGICAL STATION
FREQUENCY OF OCCURRENCE OE WIND SPEED BY DIRECTION
STABILITY CLASS E
+----------wrND sPEED CLASSES (M/S)----------+
AVERAGE0.0- 1.8- 3.3- 5.4 8.4 > i/irND
1. B 3.3 5.4 B. 4 11.0 11 .0 TOTAL SPEED
I
I
T
I
I
I
T
I
N
NNE
NE
ENE
E
ESE
SE
S
SSW
SW
WSW
W
WNW
NW
NNW
.0008
.0033
.0010
.0005
.0005
.0002
" 0003
.0000
.0008
.0000
.0005
.0000
.0003
.0005
. 0010
.0005
" 0198
.0235
.4061
.0005
.0002
.0002
" 00r2
.0017
.0020
.0005
.0007
" 0007
.0a12
.0a2a
" 0054
.004 9
- 01E3
. 0116
.0020
.0002
.0000
.0000
.0000
.0000
. a0c2
.0030
.0007
.0002
.0002
.0000
" 0030
.0a7 2
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
" 0000
.0000
.0000
.0000
.000c
" 0000
.0000
.0000 .0000
.0000 .0000
. 0000 .0000
.0000 .0000
0.039 3.3
0.038 2.9
0.010 2.1
0.001 2.5
0.001 1.9
0.000 2.4
0.001 2.4
c.002 2.4
0.003 2.3
0.003 4.2
0.002 3.0
0.001 2.6
0 .ao2 2 .6
0.0c2 2.6
0.009 3.1
0.013 3.5
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .000c
0000 .0000
0000 .0000I
I
I
I
I
ToT: 0.010 0.071 0.047 0.000 0.000
AVG: 1.5 2.1 4.A 0.0 0.0
TOTAL NUMBER OF VALID READINGS FOR THIS
OUT OF 4042 TOTAL VALID HOURS
TOTAL NUMBER OF MISSING HOURS :>
0. 000
0.0
TABLE :>
326
4.L29
tran
3.1
T
t
I
t
t
I
1O METER W]ND DATA ANALYS]S
EROM L/ L/2004 THROUGH 6/30/2004
INTERNATTONAL URANIUM METEOROLOGICAL STATION
EREQUENCY OF OCCURRENCE OE W]ND SPEED BY DIRECTION
STABILITY CLASS F
+----------WIND SPEED CLASSES (MiS)----------+
DIR 1.8 3.3 5.4 8.4 11.0 11.0 TOTAL
AVERAGE
WIND
SPEED
I
T
I
I
I
T
I
T
N
NNE
NE
r\tr
E
Fer
QT
SSE
S
SSW
SW
WSW
W
WNTJ
NW
NNW
.0078
.0080
" 0080
.0052
.0030
" 0021
.0017
.0021
.0421
,0007
.0022
.0017
.0025
.0030
.0060
. ao62
013 9
0492
004 5
0032
0007
0 012
0022
0005
0020
0 010
0 010
0 017
0 010
0c15
0059
0082
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.0000
.c000
.0000
. c000
0000 .0000
0000 .0000
0000 .00c0
0000 .0000
00c0 .0000
000c .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0000
0000 .0c00
0000 .0c00
0000 .0000
0.022 2.0
0.017 1. B
0 .012 I .1
0.008 1.5
0.004 1. 6
0.004 1.5
0.004 1 " B
0.003 1.5
0.005 7.1
0.002 1. B
0.003 1.5
0.003 1.5
0.003 1.5
0.004 7.1
0.013 1. B
0.014 2.0I
I
I
t
T
TOT: 0.064 0.059 0.000 0.00C 0.00C
AVG: 1.3 2.3 0.0 0.0 0.0
TOTAL NUMBER OF VALID READINGS FOR THIS
OUT OF 4042 TOTAL VALID HOUB.S
TOTAL NUMBER OE MISSII{G HOURS =>
0. 000
0.0
TABLE :>
326
0.123
500
l.B
I
I
I
I
I
I
t
T
T
I
I
I
I
I
T
!
I
I
I
Addendun to the Semi-Annuel Monitoring Report, July ThrougL Deceuber 2(X14,
aad Annual Moteorological Srmnily Report For 2fit4 For Intcrnstional Urrnium,
Blanding; Utah
2004 Precipitation Deta
Precipitation data (rain or snow) has been recorded in inches of liquid moisnre
received tbr the White Mesa Mill. This data is coUected at another localion on the Whire
Mesa Mill property. Table A-l presents the ?004 rnonthiy and annual totals as well as
monthly and annual climatological normals. The annual precipitarion total at the White
Mesa Mill for 2004 was 11.50 inches. This total is below the climatological normal of
I 1.80 inches. The wettest month in 2004 was September with 2.69 inches, well above the
september climatological normal of 0.90". May was the driest month with no
precipitation measured (0.00 inches).
I
t
T
I
T
I
I
I
T
I
T
I
T
I
I
I
I
I
T
Addendum to the Semi-Amual Monitoring R"port, JuIy Thrcugh December 2004,
and Annual Meteorologicel Snrnmary Report For2fil4 For Intemational Uranium,
Blanding,Utrh
TableA-l
2m4 Annugl Frecipitation Record
\ilhiteMesaMill
Month Noranal
Precipitrtion
(Inches)
Yeuty
Accumulatcd
Nornal
(Inehes)
2001
Precipitation
(Incles)
2{X}4 Monthly
Accumulated
Precipitation
(Inchee)
January 1.10 l. l0 0.69 0.69
Februarv 0.80 1.90 1.90 2.59
March 0.70 2.64 0.06 2.6s
Aoril 0.70 3.30 0.88 3.53
May 0.60 3.90 0.00 3.53
June 0.40 4.30 0.04 3.s7
Julv 1.10 5.40 0-17 3.74
Aupust 1_70 7. l0 0.63 4.37
Sentember 0.90 8.00 2.69 74.6
October 1-60 9.60 0.73 7.79
November 0.90 10.50 1.70 9.49
December i.30 l 1.80 z.at I1.50