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8/11/2019 Appendix b Distress Identification Manual
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Figure B.1. Low Severity Alligator Cracking (fine longitudinal
cracks in wheel path)
Figure B.2. Low Severity Alligator Cracking (fine longitudinal
cracks in wheel path)
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Figure B.3. Low Severity Alligator Cracking (sealed longitudinal
cracks in wheel path of outer truck lane)
Figure B.4. Medium Severity Alligator Cracking in Wheel Paths
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Figure B.5. Medium Severity Alligator Cracking in Wheel Paths
Figure B.6. Medium Severity Alligator Cracking in Wheel Paths
Near Longitudinal Joint in Shoulder Due To
Encroaching Traffic and Loss of Support
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Figure B.7. Medium Severity Alligator Cracking in Wheel Paths
Figure B.8. Medium Alligator Cracking at Free Edge of Lane
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Figure B.9. Medium Alligator Cracking in Outer Wheel Path
(pumping also exists)
Figure B.10. High Severity Alligator Cracking (in portions of
picture where pieces are severely spalled)
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Figure B.11. High Severity Alligator Cracking in Center of
Photo Where Pieces Are Severely Spalled
Figure B.12. High Severity Alligator Cracking of Shoulder Where
Large Amount of Trucks Park
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Figure B.13. Bleeding in Wheel Paths
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Figure B.15. Low Severity Block Cracking
Figure B.16. Low Severity Block Cracking Near Centerline
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Figure B.17. Medium Severity Block Cracking
Figure B.18. Medium Severity Block Cracking
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Figure B.19. High Severity Block Cracking
Figure B.20. High Severity Block Cracking
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Figure B.21. Illustrative Diagram of Corrugation Profile
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Figure B.21a. High Severity Corrugation
Figure B.21b. High Severity Corrugation
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Figure B.22. Low Severity Depression (identified by oil droppings
on pavement surface)
Figure B.23. High Severity Depression in Shoulder (high severityalligator cracking also exists and would be recorded
in addition to the depression)
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Figure B.24. Low Severity Joint Reflection Cracking From
Transverse Joint in PCC Slab
Figure B.25. Low Severity Joint Reflection Cracking from
Transverse Joint in PCC Slab
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Figure B. 26. Medium Severity Joint Reflection Cracking fromLongitudinal Widening Joint in PCC Slab
Figure B.27. Medium Severity Joint Reflection Cracking from
Transverse Joint in PCC Slab
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Figure B.28. High Severity Joint Reflection Cracking from
Transverse Joint in PCC Slab
Figure B.29. High Severity Joint Reflection Cracking from
Longitudinal Widening Joint in PCC Slab
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Figure B.30. High Severity Joint Reflection Cracking from
Transverse Joint in PCC Slab
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Figure B.31. Medium Severity Lane/Shoulder Drop-off
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Figure B.32. Medium Severity Lane/Shoulder Joint Separation (note
Separation near outside of edge paint strip)
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Figure B.33. Low Severity Transverse Cracking
Figure B.34. Low Severity Longitudinal and Transverse Cracking
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Figure B.35. Low Severity Transverse Cracking Across Shoulder
Figure B.36. Medium Severity Transverse Cracking
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Figure B.37. Medium Severity Transverse Cracking
Figure B.38. Medium Severity Transverse Cracking
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Figure B.39. Medium Severity Transverse Cracking
Figure B.40. Medium Severity Transverse Cracking Across Shoulder
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Figure B.41. High Severity Transverse Cracking
Figure B.42. High Severity Longitudinal Cracking
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Figure B.43. High Severity Transverse Cracking
Figure B.44. High Severity Transverse Cracking (this crack is
Caused initially by reflection from cement
Stabilized base)
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Figure B.46. Low Severity Patch
Figure B.47. Low Severity Patch Along Shoulder Joint
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Figure B.49. Medium Severity Patch
Figure B.48. Medium Severity Patch
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Figure B.50. High Severity Patch
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Figure B.51. Polished Aggregate (photo taken in wheel path
Of 23 year old high traffic volume turnpike)
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Acceleration of None.
Polished Aggregate
Due to Moisture:
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Figure B.52. Low Severity Pothole
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Figure B.53. Low Severity Pothole
Figure B.54. Medium Severity Pothole
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Figure B.55. Medium Severity Pothole
Figure B.56. High Severity Pothole
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Figure B.57. High Severity Pothole
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Acceleration of Potholes occur due to the breakdown or disintegration
Pothole Distress of the asphalt surface material from alligator crack-
Due to Moisture: ing, linear cracking, or raveling and weathering,
all of which are accelerated by free moisture.
Once a small hole exists, free moisture will
accumulate and through freeze-thaw and/or pumping
action additional material will be broken out of the
hole and it will increase in severity.
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Figure B.58. Medium Severity (stabilized base is pumping)
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Figure B.58a. Medium Severity Pumping
Figure B.58b. Medium Severity Pumping
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Figure B.59. High Severity Pumping (stabilized base is pumping)
Figure B.60. High Severity Pumping (stabilized base is pumping
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Figure B.60. High Severity Pumping (stabilized base is pumping)
Figure B.61. Low Severity Raveling and Weathering
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Acceleration of Prolonged soaking of the asphalt stabilized materials
Raveling and causes moisture to penetrate between the asphalt and
Weathering Due aggregate surface that wets the surface of the aggregate.
To Moisture: The moisture may penetrate the asphalt films by
emulsion formation causing stripping and thus
contributing to raveling and weathering.
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Figure B.62. Medium Severity Raveling and Weathering
Figure B.63. Medium Severity Raveling and Weathering
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Figure B.63. Medium Severity Raveling and Weathering
Figure B.64. Medium Severity Raveling and Weathering
Figure B.65. Medium Severity Raveling and Weathering
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Figure B.67. High Severity Raveling and Weathering
Figure B.66. High Severity Raveling and Weathering
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Figure B.68. Low Severity Rutting
Figure B.69. Medium Severity Rutting
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Figure B.70. High Severity Rutting
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Figure B.72. Slippage Cracking
Figure B.73. Slippage Cracking
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Figure B.73. Slippage Cracking
Figure B.74. Medium Severity Swell Occurring at a Patch Due to
Buckling of Concrete Slab Beneath Asphalt Surface
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Acceleration of Free moisture between the asphalt concrete surface and
Slippage Cracking granular layer may weaken the bond between the layers.
Due to Moisture: Once this bond is lost the potential for slippage
cracking in areas of breaking or turning traffic
increases dramatically.
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Acceleration of Swells can be accelerated by moisture in two ways:
Swell Due to (1) frost heaves may occur in freeze climates,
Moisture: (2) an expansive soil will swell when exposed to
moisture, and (3) heave over culverts, when colder
soils draw in moisture and create local heaves.
Frost heave is caused by the formation of ice crystals
in a frost susceptible sub grade. The ice crystals
grow until ice lenses from which produce frost heave.
A swelling soil increases in volume when content
increases, and decreases its volume when water content
is reduced. A swelling soil has a high plasticity
index and can be determined by lab test or experience.
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Figure B.75. High Severity Swell Due to Buckling of
Concrete Slab Beneath Asphalt Surface