THE CHEMISTRY IN 60 SECONDS
- Asphalt is a colloid - dark heavy asphaltene molecules suspended in a lighter oil called maltenes (Asphalt Institute model).
- The maltenes are the glue - they keep the asphalt flexible and bond the mineral granules to the mat.
- UV + heat drive the maltenes off - they oxidize, volatilize, and migrate to the surface where they wash away.
- What's left is brittle - the asphaltenes clump, the binder hardens, the granules lose their seat.
- Florida accelerates this 2-3x versus northern climates because UV intensity and roof-deck temperatures are both higher.
- The result is granule loss - the visible symptom homeowners see in the gutter.
- Bottom line: The chemistry is reversible up to a point. Once the mat is exposed, the clock runs different.
WHAT'S ON THIS PAGE
- What An Asphalt Shingle Actually Is
- The Colloidal Model: Asphaltenes In Maltenes
- What UV Radiation Does To The Binder
- What Florida Heat Does On Top Of That
- Why The Granules Let Go
- The Actual Oxidation Chemistry
- What The Research Says
- Where The Chemistry Is Still Reversible
- Why Florida Roofs Age Faster
- Frequently Asked Questions
What An Asphalt Shingle Actually Is
Before the chemistry makes sense, the shingle itself has to make sense. An asphalt shingle is a layered sandwich. From the bottom up:
- Release film — keeps the shingles from sticking together in the bundle.
- Back-coat asphalt — a thin layer of stabilized asphalt on the underside.
- Reinforcement mat — historically organic felt, now almost always fiberglass mat per ASTM D3462.
- Asphalt coating — the heart of the shingle. Modified or unmodified bitumen, usually 70-80% of the shingle's weight.
- Mineral granules — crushed ceramic-coated stone, the UV shield and color layer.
- Self-seal strip — heat-activated adhesive line that bonds shingles together once they're on the roof.
When a roofer talks about an "aging shingle," 95% of what they mean is happening inside that asphalt coating layer. That is where the chemistry of failure lives.
The Colloidal Model: Asphaltenes In Maltenes
Here is the part most homeowners have never been told. Asphalt is not a solid. It is not even really a liquid. Asphalt is a colloidal dispersion — heavy molecules suspended in a lighter oil, like ink in water or milk in coffee. The model has been the standard understanding of asphalt chemistry since the 1920s and is published openly by the Asphalt Institute.
The two phases:
- Asphaltenes (~15-25% by weight): Heavy, dark, complex polyaromatic molecules. Think of them as the dark heavy particles. They give the asphalt its hardness, color, and thermal resistance.
- Maltenes (~75-85% by weight): A lighter golden-brown oil phase. Maltenes are themselves a mix of saturates, aromatics, and resins. The maltenes are what keep the asphaltenes evenly dispersed and the whole binder flexible.

A useful colloidal-stability index called the Heithaus parameter measures how well the maltenes are still keeping the asphaltenes dispersed. A new shingle has a high Heithaus value. An aged shingle has a low one. The number drops as the maltenes leave.
What UV Radiation Does To The Binder
Ultraviolet radiation in the 295-to-400-nanometer range carries enough energy to break chemical bonds in organic molecules. Asphalt is full of organic molecules. Every photon that hits an exposed binder molecule can break a C-C bond, a C-H bond, or — most commonly — initiate an oxidation reaction with atmospheric oxygen.
The result over years is a long list of small chemical changes:
- Light maltenes get oxidized and converted into heavier resin compounds.
- Some maltenes volatilize directly — they evaporate off the surface.
- The resin fraction increases at the expense of the lighter aromatic and saturate fractions.
- The asphaltene fraction grows because oxidized resins eventually convert into more asphaltenes.
- The colloidal balance shifts. Asphaltenes have less maltene to swim in. They aggregate, clump, and stiffen the binder.
This is documented in the asphalt-pavement literature for decades and applies the same to roofing shingles. NREL studies on UV degradation of bituminous materials, and the long body of pavement-aging research from the Federal Highway Administration, both back the same conclusion: UV oxidation is the primary driver of asphalt aging in any exposed application.
What Florida Heat Does On Top Of That
UV alone is rough on shingles. Combine UV with the surface temperatures Florida roofs actually hit and the aging speed goes up sharply.
Measured roof-deck temperatures in Central Florida summers:
- Dark shingle, mid-afternoon June through September: 150-180F surface temperature.
- Light shingle, same conditions: 130-160F.
- Northern climate equivalent: typically 110-130F at peak.
Chemical reactions roughly double in rate for every 18-20F (10C) rise in temperature — that's the Arrhenius equation in plain English. A Florida roof running 30-40F hotter than a Pennsylvania roof is aging 2 to 3 times faster just from the temperature differential, before you even add in the higher UV intensity at lower latitude.
Why The Granules Let Go
The granules are pressed into the asphalt coating at the factory while the asphalt is still hot and soft. The granules sit roughly two-thirds buried, one-third exposed. That one-third is the UV shield. That two-thirds is the bond.
The bond depends on the asphalt staying tacky enough to hold the granule. Tackiness is a property of the maltenes. As the maltenes leave, the binder hardens, the bond between granule and asphalt gets brittle, and the granule pops loose under any mechanical disturbance — wind, rain droplets, foot traffic, or the differential expansion-and-contraction cycle the roof goes through every day.
That's why granules in the gutter are the first visible symptom of the chemistry that's been happening invisibly inside the binder for years. The granules are the readout. By the time the gutter is full of them, the maltene loss is already significant.
The Actual Oxidation Chemistry
For the homeowner who wants the receipts. The principal oxidation reactions in aging asphalt binders are well-documented in the peer-reviewed literature. The headline transformations:
- Sulfoxide formation: Sulfur atoms in the asphalt get oxidized to sulfoxides (S=O). Detectable by FTIR at approximately 1030 cm⁻¹.
- Carbonyl formation: Carbon-hydrogen bonds oxidize to carbonyls (C=O). Detectable by FTIR at approximately 1700 cm⁻¹.
- Loss of saturates and aromatics: The lighter maltene fractions decrease over time as they oxidize or volatilize.
- Increase in resins and asphaltenes: The heavier fractions grow as lighter fractions are converted upward.
Researchers like Dr. R. Christopher Williams at Iowa State and Ohio State have published extensively on these mechanisms in bio-oil rejuvenation work. The chemistry is not in dispute. What is in dispute is how much of it is reversible.
What The Research Says
Selected references for the science above:
- Asphalt Institute (engineering publications): Colloidal model of asphalt, asphaltene-maltene dispersion, Heithaus parameter. asphaltinstitute.org
- ASTM D3462: Standard specification for asphalt shingles surfaced with mineral granules. astm.org/d3462
- ASTM D228: Standard test methods for sampling, testing, and analysis of asphalt roll roofing including mandrel bend flexibility. astm.org/d228
- FHWA aging research: Federal Highway Administration long-term oxidative aging of asphalt binders. fhwa.dot.gov
- NREL UV degradation: National Renewable Energy Laboratory studies on UV degradation of bituminous and polymer materials. nrel.gov
- Williams et al. bio-oil rejuvenation: Published research on soy-oil and other bio-derived maltene replenishers in asphalt. Iowa State / Ohio State engineering programs.
Where The Chemistry Is Still Reversible
Here is the optimistic part. Up to a point, the chemistry can be put back. Not perfectly, but meaningfully. Bio-based maltene replenishers — soybean-oil-derived treatments, plant-oil treatments, biochar-derived oils — can be introduced into an aged shingle binder. The maltene-like molecules in the rejuvenator soak into the binder, redisperse the clumped asphaltenes, and partially restore the colloidal balance.
The result, measured in independent lab testing:
- Binder flexibility recovers (mandrel bend tests passable again).
- Granule adhesion strengthens (mass-loss testing shows fewer granules released).
- The Heithaus parameter rises measurably back toward unaged values.
The full lab-data deep dive lives on the next page: Shingle Rejuvenation Science: PRI, Ohio State & Intertek Lab Results.
The limit is granule coverage. If the shingle still has a complete granule layer and the mat is not exposed, the rejuvenator has something to soak into and protect. If the mat is bare in patches, the rejuvenator cannot replace what's already gone. That's the 60% rule in chemistry terms.
Why Florida Roofs Age Faster
Putting it all together for the homeowners in Marion, Lake, Sumter, and Citrus Counties:
Florida's Aging Multipliers
- Lower latitude = higher UV intensity. Central Florida sits near 29N. UV index regularly exceeds 9-10 in summer. More photons, more bond-breaking.
- Higher temperatures = faster reactions. Arrhenius equation says ~2x reaction rate per ~18F rise. Florida deck temps run 30-40F above northern climates.
- Salt-laden coastal air (Citrus, west Marion). Adds chloride to the oxidation mix. Accelerates degradation of any exposed metal flashings and shingle edges.
- Heavy diurnal humidity cycling. Shingles wet at night, baked dry at noon. Mechanical fatigue on top of chemical aging.
- Annual hurricane impact. Even a near-miss strips a layer of already-loose granules.
The result: a Central Florida asphalt shingle roof is doing the chemistry of a roof 5 to 8 years older than it actually is. The age clock on Florida Statute 627.7011(5) does not adjust for that. It just counts calendar years. That's why the inspection matters — because the calendar lies about how the chemistry is actually doing.
The legal half of this story: The Florida 15-Year Roof Rule, Explained Straight.
Back to the hub: The Granule Truth Library.



