| Major Topics on this Page | ||
| 5.1 | Surface Drainage | |
| 5.2 | Subsurface Drainage | |
Proper drainage is important to ensure a high quality long lived pavement; moisture accumulation in any pavement structural layer can cause problems. Moisture in the subgrade and aggregate base layer can weaken these materials by increasing pore pressure and reducing the materials' resistance to shear. Additionally, some soils expand when moist, causing differential heaving. Moisture in the HMA layers can cause stripping because it, instead of the asphalt binder, will adhere to aggregate particles.
Moisture sources are typically rainwater, runoff and high groundwater. These sources are prevented from entering the pavement structure or accumulating in the subgrade through surface drainage and subsurface drainage. Usually, it is more cost effective and less risky to prevent moisture entry and accumulation using surface drainage than to effect moisture removal using subsurface drainage.
Surface drainage is concerned with removing all water that is present on the pavement surface, shoulder surface or any other surface from which it may flow onto the pavement. If not systematically removed, this water can accumulate underneath and weaken the pavement structure. There are three primary means used to prevent water infiltration and accumulation:
Figure 4.27: Sheet Flow
Subsurface drainage is concerned with removing water that percolates through or is contained in the underlying subgrade. This water, typically the result of a high water table or exceptionally wet weather, can accumulate under the pavement structure by two chief means:
Gravity flow. Water from surrounding areas can be absorbed by the soil then flow by gravity to areas underneath the pavement structure. In pavement with high air voids (above 8 - 9 percent), water can percolate down through the pavement structure itself.
Capillary rise. Capillary rise is the rise in a liquid above the level of zero pressure due to a net upward force produced by the attraction of the water molecules to a solid surface (e.g., soil). Capillary rise can be substantial, up to 6 m (20 ft.) or more. In general, the smaller the soil grain size, the greater the potential for capillary rise. Often, capillary rise is a problem in areas of high groundwater tables.
Most pavements have performed adequately without considering these effects. However, HMA pavements can fail because of subgrade support deterioration as a result of excessive moisture or other water-related problems. While the best solution is usually to prevent water infiltration with surface drainage measures, subsurface drainage can be useful, however it needs to be done judiciously, because it may be somewhat akin to treating the symptom rather than the problem. Subsurface drainage consists of three basic elements (see Figures 4.28, 4.29 and 4.30):
A permeable base to provide for rapid removal of water which enters the pavement structure. Based on recent research from California, asphalt treated permeable base layers may strip and become clogged with fines thus weakening the overall pavement structure.
A method of conveying the removed water away from the pavement structure. At the least, this may consist of a base sloped towards a drainage ditch. At the most, this may consist of a pipe collector system.

Figure 4.28: Flexible Pavement Subsurface Drainage

Figure 4.29: Rigid Pavement Subsurface Drainage with PCC Tied Shoulder

Figure 4.30: Rigid Pavement Subsurface Drainage with HMA Shoulder