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Roadside Revegetation

RoadsideReveg_PollinatorHabitat_DRAFTv1-1_sept2016

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PLANNING PHASE TWO: ASSESS SITE<br />

5.3.4 ROOTING DEPTH<br />

Rooting depth is the distance from the surface of the soil to the lowest point that roots can<br />

penetrate. It encompasses any strata (e.g., topsoil, subsoil, and parent material) that can be<br />

accessed by plant roots. The deeper the rooting depth of a disturbed site, the greater the total<br />

available water storage and the higher the productivity of the site.<br />

Rooting depth is affected by restrictive layers that block root penetration to lower strata (see<br />

Section 5.7.2, Restrictive Layer). For example, the rooting depth of a post-construction site is<br />

estimated at 6 feet deep. However, further investigation finds that there is a highly compacted<br />

layer at 12 inches, which would limit most, if not all, root penetration below that point. The<br />

rooting depth under these conditions has been reduced to only 1 foot of soil instead of 6<br />

feet. Restrictive layers also include soils with very high or very low pH, toxic materials, or a<br />

high water table.<br />

Rooting depths vary by plant species and age of the vegetation. Most mature tree species<br />

have deep root systems that access subsoil and parent material; roots of grasses and forbs<br />

are predominantly limited to surface soils. Annual grasses and forbs require less rooting<br />

depth than perennial grasses and forbs, with the roots of these species growing in the upper<br />

surfaces of the soil. The age of the vegetation also determines the abundance and location of<br />

roots. Newly established seedlings have shallow roots but, as the plants mature, root systems<br />

expand to access moisture deeper in the soil.<br />

Rooting patterns and root morphology play a role in how plants access soil water. Some<br />

species have finer-textured root systems that access tightly held soil moisture; other species<br />

have aggressive root systems that can penetrate deeply into cracks between rock fragments.<br />

Grasses, for instance, have shallower root systems than trees and shrubs, but their small size<br />

and high density in the surface soil gives them an advantage in shallow soils.<br />

Rooting Depth – How to Assess<br />

Rooting depth should be estimated from reference sites during planning and post-construction,<br />

but it is not always an easy parameter to measure. Observing road cuts is often the best means<br />

to determine rooting depth. Rock type (e.g., granite, sandstone, and schist), fracturing patterns,<br />

rock weathering, and the degree of rock fracturing will provide an indication of rooting depth.<br />

Observing the amount and type of roots in the fractures of existing road cuts will give a good<br />

idea of rooting depth.<br />

Fracturing and weathering of rock can also be determined from geotechnical analysis. If the<br />

bedrock has been drilled, the drill log report can provide an indication of degree and depth of<br />

rock fracturing and weathering. One way that rock quality is assessed is through a classification<br />

called the Rock Quality Designation Index (RQD). This system rates the bedrock by how much<br />

fracturing is observed in the cores. It is calculated by measuring the pieces of rock in the core<br />

sample that are longer than 10 cm, summing the length of these pieces, and dividing by the<br />

total length of the core (Deere and Deere 1988). A small RQD means that the bedrock is highly<br />

fractured whereas a high RQD means the bedrock is massive. A RQD may be poor from an<br />

engineering standpoint because of the high fractures, but favorable from a revegetation<br />

standpoint because cracks will hold some moisture and allow root penetration. A RQD rated<br />

as “very poor,” “poor,” and even “fair” should be somewhat favorable to root penetration.<br />

Rooting depth is also affected by the presence of a restrictive layer caused either naturally<br />

or by compaction. How to determine the presence of these layers is addressed in Section<br />

5.3.3.1, Soil Structure – How to Assess, and Section 5.7.2.1, Restrictive Layer – How to Assess.<br />

The literature contains many references to defining the depth of soil needed to support<br />

different plant communities. For example, 18 inches of soil has been shown to support simple<br />

grassland ecosystems, but more diverse native grassland communities are reported to require<br />

up to 4 feet or more (Munshower 1994). These figures can be misleading if they are not put in<br />

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

73

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