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Roadside Revegetation

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PLANNING PHASE TWO: ASSESS SITE<br />

the long vertical roots (taproots) that can cross failure planes and bind the soil<br />

strata together (Figure 5-62).<br />

Soil Strength – How to Assess<br />

The designer will probably not perform engineering tests for soil strength, yet<br />

knowing a little about these tests could be important, especially if the designer<br />

is making recommendations that soils on potentially unstable sites be deeply<br />

tilled or amended with organic matter.<br />

A common method engineers use to estimate soil strength is to correlate soil<br />

classification (from sieve analysis and the characteristics of clay particles) with<br />

published literature values. Shear vanes or cone penetrometers are good<br />

methods to approximate the strength of fine-grained soils in the field, and<br />

published research is used to correlate these readings with laboratory shear<br />

strength test results.<br />

The triaxial shear test is a more precise laboratory method to determine shear<br />

strength of soils. In this test, a long cylinder of the soil is placed in a latex<br />

membrane and submerged in a clear plastic cylinder filled with water. A vertical<br />

pressure is applied to the cylinder at a slow rate until the soil sample shears. Very<br />

sensitive strain gauges measure the soil displacement, applied forces, and any<br />

pore water pressures that develop. Various water pressures are applied to the<br />

cylinder to simulate the confining pressure of soil depth (Brunsden and Prior<br />

1984). This test can be used to determine the shear strength of soils that have<br />

been amended with organic materials.<br />

Mitigating for Low Soil Strength<br />

Biotechnical Engineering Techniques<br />

Many biotechnical slope stabilization techniques use vegetative cuttings from willows or other<br />

easy-to-root species to structurally reinforce the soil. As these materials root, they add further<br />

stabilization to slopes through interconnecting root systems and soil moisture withdrawal.<br />

These practices include stake planting, pole planting, joint planting, brush layers, and branch<br />

packing (see Section 10.3.3, Installing Cuttings).<br />

Shrub and Tree Seedlings<br />

On drier sites, where willow cuttings are less likely to survive and grow, shrub and tree seedlings<br />

can be used. While these species are slower growing, they usually have deeper root systems<br />

and persist longer once they are established. Grass and forb species can quickly establish on<br />

Figure 5-62 | Plant roots<br />

and slope stability<br />

Plant roots and stems increase slope<br />

stability by (A) reinforcing the surface<br />

horizon through a matrix of roots, (B)<br />

anchoring surface horizons to rock or<br />

subsoils, and (C) stems supporting the<br />

soil upslope.<br />

Figure 5-63 | Effects of roots<br />

on slope stability<br />

This debris slide (noted by its shallow, steep<br />

appearance) took place two years after construction<br />

when the grass and forbs were fully<br />

established. Establishing shrub species, rather<br />

than grass and forb species, on steep, potentially<br />

unstable slopes, would be better for long<br />

term stability because shrub species are deeper<br />

rooting and have higher root tensile strength.<br />

<strong>Roadside</strong> <strong>Revegetation</strong>: An Integrated Approach to Establishing Native Plants and Pollinator Habitat<br />

119

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