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Field Investigation Of Aggregate Blow-off Of Spray Polyurethane Foam Roofs

May 15, 2011

ABSTRACT
The 2006 International Building Code
disallows the use of loose-laid aggregate on
roofs in hurricane-prone regions for fear of
damage caused by blow-off. This restriction
has had a significant impact on the roofing
industry, as loose-laid aggregate has historically
been used as an economical material
to increase ultraviolet, fire, hail, and traffic
resistance to roof membranes. In 2009,
under the auspices of the Asphalt Roofing
Manufacturers’ Association (ARMA) et al.,
Jay H. Crandell, PE, developed a design
methodology, based on the 1970s work of
Kind and Wardlaw, to avoid aggregate blowoff
from roofs of buildings of all heights. As
a follow-up to the development
of this methodology,
this researcher has
inspected 20 spray-applied
polyurethane foam roofs in
the Stuart, Florida, area
that were covered with
loose aggregate and subjected
to the combined
2004 wind events of hurricanes
Francis and Jeanne.
Each roof was examined
for the variables required
in Crandell’s Method (i.e.,
building height, parapet
height, aggregate size,
wind speed, surface
roughness) and the likelihood
of aggregate blow-off
back-calculated to test the
methodology; this likelihood
was then compared
to actual performance.
Background
Aggregate as a roof surfacing material
has a long track record of providing an economical
protective material for resistance to
ultraviolet radiation, hail, and surface traffic.
Additionally, aggregate can provide aesthetic
qualities and a predator-free nesting
place for certain bird species.
However, a well intended but overly
restrictive building code change in the 2006
International Building Code (IBC) severely
restricted the use of loose aggregate as a
roof surfacing material in hurricane zones.
Specifically, it stated the following:
1504.8 Aggregate. Aggregate used
as surfacing for roof coverings and
aggregate, gravel, or stone used as
ballast shall not be used on the roof
of a building located in a hurricaneprone
region as defined in Section
1609.2, or on any other building
with a mean roof height exceeding
that permitted by Table 1504.8
based on the exposure category and
basic wind speed at the site.
Section 1609.2 de fines hurricaneprone
regions as:
Hurricane-Prone Regions.
Areas vulnerable to hurricanes
defined as:
1. The U.S. At lan tic
Ocean and Gulf of
Mexico coasts where
the basic wind speed
is great er than 90 mph
(40 m/s) and
2. Hawaii, Puerto Rico,
Guam, Virgin Islands,
and American Samoa.
[Cited from the 2009
IBC.] Thus, as illustrated in Figure 1, the
IBC eliminated a historically economic
and reliable roof surfacing material from
a substantial geographical segment of
the roofing industry.
Beginning in late 2008, ARMA sponsored
Jay Crandell of ARES Consulting
to revisit the wind tunnel work of
Canadian researchers Kind and
Figure 1 – Hurricane-prone regions (Atlantic and Gulf coasts as
defined in IBC Section 1609.2)
18 • I N T E R FA C E J U LY 2011
This paper was originally presented at the RICOWI Fall Symposium, November 11, 2010, in Rock Hill, SC.
It is published for the first time here, courtesy of RICOWI.
Wardlaw (1976 and 1984). Crandell completed
his work in May 2009 and presented
his findings at several symposia (Crandell,
2009; Crandell and Fischer, 2010).
Crandell reviewed the Kind-Wardlaw
work and developed a modified design
method incorporating the effects of parapet
height and gravel size. Note that the Kind-
Wardlaw work and design methodology
were oriented primarily toward avoiding
scour on ballasted single-ply roofs, whereas
the Crandell work focuses on avoiding blowoff.
(Crandell’s Modified K-W Design Method
is reproduced in Appendix A.)
The purpose of this paper is to report
the findings of a field study of gravelcovered,
spray polyurethane foam (SPF)
roofs that experienced hurricane-force
winds during Hurricanes Francis and
Jeanne in 2004.
Introduction
Twenty aggregate-covered, SPF roofs at
19 locations (two roofs at one location were
combined in the data set) were inspected in
the Stuart, Florida, area to determine the
degree of aggregate blow-off and scouring
following the 2004 hurricanes. The physical
characteristics of each roof were used to
determine the adjusted critical wind speeds
(Vcr’) in accordance with Crandell’s Method;
these were then compared to the estimated
actual wind speeds that occurred at the roof
(Vroof). According to Crandell, roofs where the
estimated actual wind speed exceeded the
adjusted critical wind speed (i.e., where Vcr’ >
Vroof) would be at risk for aggregate blow-off.
Determination of Estimated Wind
Speeds
Obtaining an accurate analysis of hurricane
wind speeds is not a simple task.
Hurricane Jeanne was chosen as the more
critical storm event (Jeanne was a Category
3 storm, whereas Francis was a Category 2
storm). For this study, wind speeds were
estimated using a combination of available
Hurricane Jeanne surface-wind speed
maps and adjusting those speeds to basic
wind speeds of three-second gusts at 33 ft
(10 m) above ground, Exposure C. The net
result is the wind contour map/study area
map in Figure 2.
Roof Inspection Procedures
For each roof/building location, the following
data were gathered:
• Building name, address, coordinates
• Building height
• Roof dimensions
• Parapet description
and dimensions
• Exposure category
• Aggregate sampled
• Wind effects on
aggregate
• Inspection photos
• Google Earth
overviews
Wind speeds were
estimated based on the
Figure 2 map for each
building location. The
aggregate samples were
sieved (to determine
average diameter) and
measured for specific
gravity.
The wind effects on
the aggregate were
based on observations
during the inspections
and discussions with
building owners and the roofing contractor.
Effects were classified as No Scour, Minor
Scour, Scour, and Gravel Loss.
Data Analysis
Crandell’s Method requires the following
data inputs:
Vmap: The gust speed from the ASCE 7
wind maps. For this study, the
estimated wind speeds derived
from Figure 2 were used for Vmap
values.
I: The building importance factor for
all of the buildings in this study
was 1.0, as all of the buildings
were classified as Occupancy
Category II.
h: The measured building height was
used.
hg: The gradient height for site wind
exposure was set at Exposure B,
1270 ft; Exposure C, 900 ft. All
but one building were Exposure B
(Roof No. 13 was Exp. C). Roof No.
14 could be either B or C, depending
on wind direction; Exp. B was
used for the calculations.
α: The power law terrain roughness
parameter was set at Exposure B =
6.2; Exposure C = 9.5.
Figure 2 – Study area with Hurricane Jeanne wind contours.
Yellow squares represent inspected roofs. Wind speeds are
three-second gusts, 33 ft above ground, Exposure C. (Map from
Topo North America 9.0, 2010, © DeLorme, Yarmouth, ME. Used
with permission.)
J U LY 2011 I N T E R FA C E • 1 9
H: Setting the parapet height for this
study presented a dilemma: Most
of the study building had partial
parapets or mixed parapet
heights. This is discussed further
in the Discussion section of this
report. Parapet heights ranged
from 0 to 78 inches.
d: Aggregate diameter was determined
from sieve analysis of the
samples obtained from the study
roofs. Average aggregate diameter
varied from 0.245 to 1.5 inches.
Using Crandell’s Method, Vroof was determined
according to Step 2, using the estimated
wind speed from the Figure 2 map in
place of Vmap. Next, a critical blow-off wind
speed was determined (Crandell’s Step 3)
based on parapet height. Then, using the
measured average aggregate diameter, the
adjusted critical speed was determined
(Vcr’). As a final step (corresponding to
Crandell’s Step 5), the quantity (1.1 x Vcr’) –
Vroof was calculated (labeled “X-value” for
lack of a better designation); the lower the
result (the more negative), the more likely
aggregate blow-off would occur.
DISCUSSION
Parapet Height
Parapets, partial parapets, or porous
parapets dramatically affect the wind velocities
and pressure differentials across roof
surfaces (Canon et al., 2002; Phillips,
2003). Many of the study roofs had discontinuous
parapets or variable parapet
heights. Crandell’s Method offers no suggestions
regarding mixed parapet heights.
Figure 3 – Discontinuous parapet on Roof No. 2.
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From concept to completion
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20 • I N T E R FA C E J U LY 2011
For this study, an “effective” parapet
height was used in the calculations. An
effective parapet height was defined as the
greatest parapet height at the apparent origin
of the aggregate scour. This provided the
best correlation between observations and
Crandell’s Method.
For example, Roof No. 2 (Figure 3)
drained at the back of the building. The
parapet height varied from 10 inches in
front to 36 inches (due to roof slope) at the
rear where the parapet stopped at the
draining edge. Aggregate scour originated at
the junction of the draining edge and the
36-in parapet; an effective parapet height of
36 inches was used in the calculations for
this roof.
General Findings
X-values (i.e., 1.1 x Vcr’ – Vroof) of the various
roofs varied from a low of -52 (aggregate
blow-off) to a high of +88 (no scour).
Table 1 lists the details of each roof in the
study. Of the
twenty roofs in –
spected, the overall
observations
are listed in
Table 2.
All structures
in this study
were less than 30
ft in height, and
all the roofs were
SPF with looselaid
aggregate coverings (there was no
embedment of the aggregate). All structures
were Occupancy Category II: neither an
essential facility nor a substantial hazard
(IBC, 2009: Table 1604.5).
No Scour
Some of the roofs exhibiting no scour
were completely expected.
• Roof No. 8 (X-value: +39) had a 42-
in parapet wrapping the entire roof
structure, providing ample protection
to the aggregate.
• Roof No. 19 (X-value: +88) had been
a ballasted single-ply; when this had
been converted to an aggregatecovered
SPF roof, the ballast stone
was reused. This roof had the greatest
aggregate diameter of the study
roofs (1.5 inch average). Addi tion –
ally, while this roof had a draining
edge, the 38-in-high parapet
Roof # ID City Avg. Gravel Building Parapet Ht. Exposure Est. Wind Vroof Vcr Vcr’ 1.1 x Vcr’ – Experience
Size (in) Height (ft) Eff. (in) Category Speed Vroof
(X-value)
1 Treasure Coast Stuart 0.511 20 35 B 96 68.9 121 96 37 Scour
Commerce Center
2 Treasure Coast Stuart 0.464 20 36 B 96 68.9 122 95 35 Scour
Commerce Center
3 Whiting Construction Palm City 0.508 15 0 B 98 67.2 60 48 -14 Minor Scour
4 B & A Industrial Park Stuart 0.469 21.5 0 B 100 72.6 60 47 -21 Scour
Building A
5 B & A Industrial Park Stuart 0.350 16 0 B 100 69.2 60 42 -23 Scour
Building H
6 Deggeller Building Stuart 0.496 25 0 B 100 74.4 60 48 -22 Scour
7 Arlington Electric Stuart 0.268 16 0 B 100 69.2 60 39 -27 No Scour
8 Seacoast National Bank Stuart 0.482 30 42 B 99 75.9 133 104 39 No Scour
9 Stuart Brake and Auto Stuart 0.466 15 0 B 101 69.2 60 47 -18 No Scour
10 Don Ramon’s Stuart 0.345 10 0 B 101 64.8 60 42 -19 Minor Scour
11 Wayne’s Auto Repair Stuart 0.442 15 0 B 100 68.5 60 46 -18 Scour
12 Mayfair Plaza Stuart 0.620 25 38 B 101 75.2 126 107 43 No Scour
13 Granada Plaza Stuart 0.245 14 0 C 103 93.2 60 38 -52 Gravel Loss
14 Island Village Jensen Bch 0.462 15 2 B 106 72.6 63 49 -19 Scour
15 Rent-a-Center (et al.) Fort Pierce 0.520 14 0 B 110 74.5 60 48 -21 No Scour
Strip Mall
16 Virginia Avenue Plaza Fort Pierce 0.605 15 0 B 110 75.4 60 51 -20 Minor Scour
17 Fort Pierce Business Fort Pierce 0.448 15 15 B 107 73.3 86 66 -1 Scour
Park
18 Town Center Port St. Lucie 0.458 15 18 B 104 71.3 91 70 6 No Scour
19 Blockbuster Video Port St. Lucie 1.500 14 38 B 104 70.5 126 144 88 No Scour
Table 1 – Roof inspection observations and adjusted critical wind speed (Vcr’).
Observation Number X-Value Range
of Roofs [1.1 (Vcr’)] – Vroof
No Scour 7 -27 to +88
Minor Scour 3 -20 to -14
Scour 9 -22 to +37
Blow-off 1 -52
Table 2 – Comparisons of roof observations.
J U LY 2011 I N T E R FA C E • 2 1
wrapped around and protected the corner (see
Figure 4).
A few of the no-scour roofs were surprises. Roof
No. 7 (X-value: -27) would have been expected to
exhibit some degree of scour: There were no parapets,
and the average gravel diameter was 0.268 in.
Why this roof, with such a low X-value, would have
performed as well as it did is not understood. The
contractor posited that this particular roof has a
gravel stop that tends to slow the drainage; during
the hurricane(s), the standing water at the roof
perimeters may have absorbed the kinetic energy of
the wind, protecting the submerged aggregate.
Scour and Minor Scour
Roofs experiencing some degree of scour ranged
in X-values from -23 to +37. Scour patterns were
not unexpected. Exposed corners exhibited the
classic “heart-shaped” or “V” pattern; corners with
partial or discontinuous parapets exhibited a
“teardrop” pattern. (See Photos 5 to 7.)
Aggregate Blow-off
Only one roof in the study was observed or reported to have had
a loss of aggregate. This particular building (Roof No. 13) had the
smallest aggregate diameter of the study (0.245 in) and was classified
as Exposure C (Figure 8). The roof has a high parapet on the
west exposure (66 inches), but the eastern side (exposure was an
open field) had no parapet. The aggregate loss apparently caused
no damage, as it was never determined where it landed (likely in
the adjoining field). The X-value for this roof was the most negative
of the study at -52.
Figure 6 – Typical scour pattern (Roof No. 4).
Figure 7 – Typical scour pattern (Roof No. 2).
Photo courtesy Google Earth.
Figure 5 – Typical minor scour (Roof No. 16).
22 • I N T E R FA C E J U LY 2011
Figure 4 – Roof No. 19 with 1.5-in aggregate and a wrap-around parapet.
Aggregate Characteristics
Samples of aggregate were removed from each of the
study roofs. The samples were sieved to determine the size
distribution from which average diameters and the size
classifications were determined. Size classifications are
shown in Table 3.
Average diameter varied from 0.245 to 1.50 in (Photo 9).
The largest size was aggregate recycled from a ballasted
single-ply roof. The smallest sizes (7, 78, and 8) were locally
described as “pea gravel.” Fines were found to be minimal
and well within ASTM D448 specification.
Aggregate was composed of various
mineral species, but the specific gravity was
remarkably uniform. Specific gravity averaged
2.59, with a range from 2.40 to 2.72.
Variation in specific gravity was insufficient
to draw any conclusions as to its effect on
scour or blow-off.
CONCLUSIONS
Crandell’s Method
The major intent of this study was to
determine the validity of Crandell’s Modified
Kind-Wardlaw Design Method for Buildings
Figure 8 – Roof No. 13 exhibited aggregate loss. The roof had no parapet
on the side facing Exposure C. Aggregate loss was from the northern half
of this roof. Photo courtesy Google Earth.
ASTM D448 Number
Size of Roofs
3 1
5 2
67 11
68 2
7 1
78 1
8 2
Table 3 – Measured aggregate sizes.
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Figure 9 – Aggregate varied in average diameter between less than one-half
inch and 1½ inches. Most roofs had Size 67 (nominally one-half-inch
diameter).
of All Heights. All of the inspected structures
in this study were less than 30 ft
high; conclusions, therefore, are confined to
this height limitation.
An X-value calculation was determined
to compare the adjusted critical wind speed
(Vcr’) to the actual estimated wind speed
(Vroof). Per Crandell’s Method, a positive Xvalue
would be “safe” from the standpoint of
aggregate blow-off. Indeed, this was consistent
with the observations.
In fact, Crandell’s Method appears to be
quite conservative since 12 of the 20 roofs
observed had negative X-values but no
observed or reported aggregate blow-off.
The single roof that did experience blow-off
had an X-value of -52. While this might
suggest that Crandell’s Method has a “safety
factor” of about 50 mph wind speed, this
is only one sample, and there were multiple
uncertainties in this analysis.
Effects of Parapets and Edge Details
The effect of parapets on the generation
of corner wind vortices is quite profound. It
appeared from this study that discontinuous
parapets that abruptly stopped at a
draining edge had significant effects on vortices.
Several roofs exhibited scour patterns
that suggested that corner vortices, which
might otherwise lead to aggregate blow-off,
instead were disrupted with aggregate
scouring in toward the field of the roof and
away from the edge.
Roofs with mixed parapet heights or
with discontinuous parapets presented a
challenge to model under Crandell’s
Method. After trying a number of variations
on what parapet height to use, this study
found best correlation with Crandell’s
Method using an “effective” parapet height
as defined as the greatest parapet height at
the apparent origin of scour.
There may be other subtle yet significant
factors affecting the likelihood of
aggregate blow-off (and scour), including
edge details (Lin, et al., 2008). Roof No. 7
should have experienced aggregate scour to
some degree. The theory expressed by the
roofing contractor that standing water stabilized
the aggregate is speculative though
plausible. It’s apparent that the microenvironment
of the roof corner needs further
study.
ACKNOWLEDGEMENTS
The author greatly appreciates the support
and assistance of NCFI Poly urethanes,
Mount Airy, NC; and Whiting Construction,
Stuart, FL.
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REFERENCES
2009 International Building Code. Inter –
na tional Code Council: Country
Club Hills, IL.
ASTM D1863, “Standard Specification
for Mineral Aggregate Used on Built-
Up Roofs,” ASTM International, West
Conshohocken, PA.
ASTM D448, “Standard Classification
for Sizes of Aggregate for Road and
Bridge Construction,” ASTM Inter –
national, West Conshohocken, PA.
Richard P. Canon, Blake S. Joplin, and
S. Thomas Watson, “SMARF Build –
ing Cape Canaveral Air Force Sta –
tion, Florida: Seven Years Later,”
Interface, Vol. XX, No. 9, September
2002, pp. 24-36.
Jay Crandell and Michael Fischer,
“Winds of Change: Resolving Roof
Aggregate Blow-Off,” paper presented
at the RCI International Con –
vention and Trade Show, Orlando,
March 25-30, 2010.
Jay H. Crandell, “Design of Aggregate-
Surfaced Roofs to Avoid Aggregate
Blow-off: Development of a Modified
Kind-Wardlaw Design Method for
Buildings of All Heights,” paper presented
at the RICOWI Fall meeting,
Portland, Oregon, October 1, 2009.
R.J. Kind and R.L. Wardlaw, “Design of
Rooftops Against Gravel Blow-off,”
National Research Council Canada,
Ottawa, 1976.
R.J. Kind, M.G. Savage, and R.L.
Wardlaw, “Further Model Studies of
the Wind Resistance of Two Loose-
Laid Roof-Insulation Systems (High-
Rise Buildings),” National Research
Council Canada, Ottawa, 1984.
J.X. Lin, P.R. Montpellier, C.W. Tillman,
and W.I. Riker, “Aerodynamic De –
vices for Mitigation of Wind Damage
Risk,” paper presented at Advances
in Wind and Structures (AWAS) conference,
Jeju, Korea, May 29-31,
2008.
Mary Katherine Phillips, “Evaluation of
Mitigation Measures for Reducing
High Suction Pressures on Roof
Corners,” masters thesis, Clemson
University, Clemson, SC, 2003.
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J U LY 2011 I N T E R FA C E • 2 5
Based on the evaluation in the previous section, the modified
K-W design method is presented as follows for aggregate-surfaced
BUR and SPF:
STEP 1: Determine mapped basic (design) wind speed (mph, gust)
for standard conditions (33-ft elevation and flat, open terrain –
Exposure C) using the ASCE 7-05 wind map (ASCE 2005).
STEP 2: Adjust mapped wind speed (Step 1) to a design wind
speed at roof height using the following equation and terrain
roughness parameters:
Vroof = {[h/hg](1/α)/[33/900](1/9.5)} x Vmap • I x Kd
= 1.4 x [h/hg](1/α) x Vmap x I x Kd
where,
Vroof = gust wind speed at roof height (mph).
Vmap = gust wind speed from ASCE 7 wind map (mph).
I = building importance factor (use 0.75 for Category I
buildings; 1.0 for Category II; and 1.1 for Categories
III and IV).*
h = building roof height (ft).
hg = gradient height for site wind exposure (Exp. B use
1270 ft; Exp. C use 900 ft; Exp. D use 700 ft).**
α = power law terrain roughness parameter (Exp B – 6.2;
Exp. C – 9.5; Exp. D – 11.5).**
Kd = 0.9 = wind speed directionality factor consistent with
ASCE 7 wind load directionality factor.***
*Importance factors per ASCE 7-05 have been modified to apply to wind speed in
lieu of wind load.
**Parameters for Exposure B are based on “typical” values per ASCE 7
commentary.
***For a discussion of the inclusion of the directionality factor, see Kind and
Wardlaw, 1976, Appendix A.2.6, page 28.
STEP 3: Determine critical (blow-off) wind speed for roof system
design as follows:
Vcr = 20.8 (H) + 60
where,
Vcr = critical wind speed (mph, gust).
H = parapet height above roof
surface (feet).
STEP 4: Adjust critical wind speed (Step 3) for aggregate size when
different than 1-in nominal diameter as follows:
Vcr´ = Vcr x (d)1/3
where,
Vcr´ = aggregate size-adjusted critical wind speed (mph, gust)
d = aggregate nominal diameter (inches)
(Nominal aggregate diameter is based on mean aggregate size –
see examples below.)
*ASTM D1863 #7 aggregate has a mean size similar to #67 aggregate, but with a
maximum aggregate size of ½ in instead of 3/8 in.
**ASTM D448 aggregate is not typically specified for BUR and SPF roof systems.
STEP 5: Verify that Vroof ≤ (1.1 x Vcr´).
If the above design check is not satisfied, increase aggregate
size or parapet height and reevaluate starting at Step 3.
(Note: The 1.1 factor is a calibration factor derived and justified
in Crandell, 2009.)
Roger V. Morrison, RRC, PE, is the president of Deer Ridge
Consulting, Inc., Ararat, VA, specializing in issues related to
construction uses of spray-applied polyurethane foam. Prior
to that, he served as senior staff engineer with NCFI
Polyurethanes for 21 years. Roger currently chairs the
Technical Committee and the Roofing Committee of the Spray
Polyurethane Foam Alliance. Roger may be contacted at
roger@deer-ridge-consulting.com.
Roger V. Morrison, RRC, PE
26 • I N T E R FA C E J U LY 2011
APPENDIX A
MODIFIED K-W DESIGN METHOD
(Reproduced with permission from Jay Crandell, ARES Consulting, West River, MD.)
ASTM Nominal
D1863 Size Diameter (in)
#7 3/8*
#67 3/8
#6 ½
ASTM
D448 Size**
#4 1
#24 1½
#2 2