Mastering Roof Inspections: Asphalt Composition Shingles, Part 30
by Kenton Shepard and Nick Gromicko
The purpose of the series “Mastering Roof Inspections” is to teach home inspectors,
as well as insurance and roofing professionals, how to recognize proper and improper conditions while inspecting steep-slope,
residential roofs. This series covers roof framing, roofing materials, the attic, and the conditions that affect the roofing
materials and components, including wind and hail.
ASPHALT SHINGLE WEATHERING
"Weathering" is a general term used to describe the
effects on shingles of long-term exposure to the elements.
Weathered shingles aren’t necessarily damaged shingles, although weathering
will eventually damage shingles. Weathering is a natural process that causes shingles to deteriorate over time. The rate shingles
weather can be affected by a number of things.
Shingle Quality
Low-quality shingles will
fail before high-quality shingles. Quality can vary widely among manufacturers, and even within a single manufacturer’s
product line.
Structure Orientation
South-facing roof slopes have shorter life spans due
to increased thermal cycling and UV exposure. Some portions of the roof are affected by prevailing winds more than others.
Degree of Roof Slope
Flatter roofs have shorter life spans because they shed moisture
more slowly and are more directly exposed to UV radiation than roofs with steeper pitches.
Climate
Harsh climates shorten roof life spans. Wind, moisture and thermal cycling all contribute to deterioration
of roofing materials.
Thermal Cycling
Climates with large daily temperature swings shorten
roof life spans because they cause greater amounts of expansion and contraction. This increases the roof's rate of deterioration.
Roof Color
Darker roofs absorb more heat, which shortens shingle lifespan by accelerating the
loss of volatiles and increasing thermal cycling.
Elevation
Homes at higher elevations are exposed to more UV radiation,
which deteriorates most roof-covering materials, including asphalt shingles.
Roof
Structure Ventilation
Poor ventilation of the roof structure shortens shingle lifespan by failing to keep shingles cool, resulting
in accelerated loss of volatiles and greater amounts of thermal cycling.
Quality
of Maintenance
Failure to repair damage and keep roofs clean can result in damage and deterioration from moisture intrusion
and wind.
Now that you have a good idea of the kinds of conditions that contribute to deterioration,
let’s look at an overview of the process of deterioration.
ASPHALT SHINGLE LIFESPAN, Part 1
Asphalt shingle lifespan is strongly affected by weathering.
Even though the rate at which shingles weather varies, they still go through a generally predictable lifecycle.
The lifespan of asphalt shingles is related
to the rate at which they deteriorate. The long-term deterioration pattern of an asphalt shingle can be broken into three
parts:
- incipient
deterioration;
- accelerating deterioration; and
- decelerating deterioration.
“Incipient”
mean “early,” so incipient deterioration is the first stage. During the incipient stage, deterioration takes place
very slowly.
As time passes, deterioration starts to worsen, and shingles enter a period of accelerating
deterioration.
By the time the deterioration curve begins to flatten out and the decelerating period
begins, the shingles have reached the point of functional failure. They’re no longer protecting the roof and are
trying hard to turn back into the raw materials from which they’re manufactured.
Let's
examine the lifecycle of asphalt shingles from the time of manufacture onward. Packaging
Shingles start to age and deteriorate as soon as they’re packaged. This is the beginning of the incipient
stage. The deterioration process is very slow at first, and is mostly driven by oxidation, the chemical processes taking place
within the asphalt, and sometimes also by heat and pressure, depending on storage and transportation conditions.
Installation
Deterioration accelerates
dramatically once the shingles are installed and exposed to weather. The asphalt layer is new and hasn’t yet had a chance
to cure, so this rapid aging continues for a short time until the asphalt layer becomes tougher. This period typically includes
minor granule loss as excess granules adhered during manufacturing separate from the shingles and are washed away by runoff.
Slow, Prolonged Aging
Once the curing period is complete, shingles enter a
long period of aging at an ever-increasing rate.
At first, the pace will be so slow that it won’t
really be visible. Deterioration starts on a very minute scale with micro-cracks in the asphalt, the loss of a few granules,
dissipating volatiles, and chemical changes in the asphalt.
The rate at which aging increases
depends on a number of factors, such as shingle quality, roof orientation, slope, and other factors. This is the end
of the incipient period and the beginning of the accelerating slope.
Accelerating
Deterioration
During accelerating deterioration, these factors become more important. Multiple factors can combine to drastically
extend or shorten the service life of the shingles.
As they approach the end of
the accelerating-deterioration slope, most shingles will have common failures.
Random surface cracking, called “craze-cracking,"
can expose more asphalt to UV radiation. In cold climates, the potential for damage is increased due to the
expansion of moisture as it turns to ice. Craze-cracking will be covered in more detail in the articles to come.
Thermal cycling can cause shingles to split. Splitting may be due to:
•
contraction of the shingles themselves; or
• contraction of the roof deck.
Shingles become more brittle as volatiles, which keep them flexible,
dissipate. Loss of volatiles can degrade the bond between the asphalt and the granules, resulting in an increase in the
rate of both uniform and localized granule loss.
It
also increases the chances of creasing or splitting from flexing.
As shingles lose volatiles, they may also
become more moisture-absorbent, which can lead to distortion. Shingle distortion exposes more of the under-surface of the
shingle to moisture, and increases the chances of roof leakage because wind-driven rain can more easily penetrate the
roof.
Organic shingles are more strongly affected by the loss
of volatiles because, as the volatiles dissipate, the mat becomes more absorbent. As they deteriorate, organic shingles sometimes
delaminate, which can leave the mat directly exposed to weather.
Loss of granules increases the amount of UV radiation
reaching the asphalt. Although UV rays deteriorate asphalt, leaks from UV-caused deterioration are rare because properly
installed shingles are typically at least two layers thick.
All content copyright © 2006-2010 the International Association of Certified Home Inspectors, Inc.