How do vertical drains work?
When a load is applied to soft, low-permeability saturated soils, excess pore water pressures are generated because the water within the soil pores cannot immediately escape. Initially, a significant portion of the applied load is therefore carried by the pore water rather than by the soil skeleton itself. A simple analogy is a sealed drink carton without a straw. When pressure is applied to the carton, the pressure inside increases because the liquid has no easy path to escape, only when you put in the straw, the volume will change and pressure is reduced. Similarly, when soft saturated soils are loaded, pore water pressures increase until water gradually drains from the soil matrix.
As excess pore water dissipates, the load is progressively transferred from the pore water to the soil skeleton. This causes the soil to compress and adjust to the new loading conditions, a process known as consolidation. In very low-permeability soils such as clay and peat, this process can naturally take many years or even decades.
Vertical drains create artificial drainage paths through the soil. Rather than travelling the full thickness of the compressible soil layer towards a natural drainage boundary, pore water only needs to flow a relatively short horizontal distance to the nearest drain. This significantly accelerates the dissipation of excess pore water pressures and therefore the consolidation process.
The effect of shortening the drainage path can be substantial. As a general rule of thumb, the time required for consolidation is approximately proportional to the square of the drainage distance. Consequently, reducing the drainage path by half may reduce the consolidation time by approximately a factor of four, depending on the soil conditions and drainage assumptions.
Vertical drains are commonly used in combination with preload embankments, surcharge fills or vacuum consolidation systems to achieve the required degree of consolidation and strength gain within practical construction schedules.