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Roadside Revegetation

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IMPLEMENTATION GUIDES<br />

adjacent to roads. The upper portions of steep, extensive slopes are typically not reachable<br />

by straw blowers.<br />

When straw is used as a seed mulch, it is important that the application rates are not so deep<br />

that a physical barrier is formed. A minimum depth that has been shown to control evaporation<br />

is one inch (Slick and Curtis 1985). Applying too much straw will restrict sunlight and growing<br />

space for establishing seedlings. A rule of thumb is that some surface soil (15 percent to 20<br />

percent) should be visible through the straw after application (Kay 1972, 1983; Jackson and<br />

others 1988). This equates to 1.5 to 2 tons per acre, depending on the type of straw and its<br />

moisture content.<br />

Straw is susceptible to movement with moderate to high winds. Tackifiers are often applied<br />

over the straw to keep it in place (Kay 1978). Products such as guar and plantago are used with<br />

low quantities of hydromulch to bind straw together (Manufacturers have stated application<br />

rates for this purpose). Straw can also be crimped, rolled, or punched into the soil. These<br />

measures will stabilize the straw by burying portions of the stems into the soil and can increase<br />

erosion protection because of the more intimate contact of straw with the soil surface. The<br />

potential for compaction is increased with these treatments and the tradeoffs of offsetting<br />

surface stability with long-term soil productivity should be weighed.<br />

Wood Strands and Wood Wool<br />

Wood strands and wood wool are commercially available wood products used for mulch. Wood<br />

strands are long, thin pieces of wood produced from wood waste veneer whereas, wood wool,<br />

known as excelsior, is produced from aspen wood. These products are developed as an effective<br />

erosion control alternative to straw and hay (Foltz and Dooley 2003). The advantages of wood<br />

strands over straw are that it is free of seeds, has a longer life, and is more resistant to wind.<br />

Wood strands, like straw, form a stable cover with high porosity or loft, characteristics which<br />

are important for controlling soil moisture and temperature around the germinating seeds.<br />

The large spaces or pores created by the wood strands allow space, light, and protection for<br />

young emerging seedlings (Figure 10-13). Unlike straw, these materials keep their structure<br />

or porosity over time, and do not compress with snow or lose fiber strength through decomposition.<br />

While the performance of this new product as a seed cover has not been tested, it<br />

has all the characteristics of being an excellent seed cover. The application rates for wood<br />

strands are likely to follow the guides for straw – at least 15 percent to 20 percent of the soil<br />

surface should be visible. This is likely to be greater than the recommended rates for erosion<br />

control. Installing small test plots of varying thicknesses of mulch would be a good means<br />

to determine the appropriate thickness for optimum seed germination. Wood strands are<br />

delivered in different size bales and applied by hand or through straw blowing equipment<br />

(Figure 10-23). As with straw, this product is limited by the accessibility of the site by hay<br />

transportation and blowing equipment.<br />

Litter and Duff<br />

Litter is the layer of fresh and partially decomposed needles and leaves that cover the surface<br />

of most forest and shrub plant community soils. Duff is the dark, decomposed layer directly<br />

below the litter layer (leaves and needles are not identifiable in the duff layer) that is high in<br />

nutrients and humus. In addition to providing soil protection and nutrients, litter and duff can<br />

also contain dormant, yet viable, seeds from species that make up the forest or shrub plant<br />

communities. When litter and duff are collected, they should be matched to the appropriate<br />

revegetation site. For example, litter and duff collected from cool, moist sites should not be<br />

applied on hot, dry sites.<br />

The depth that litter and duff accumulates will vary by species composition, age, and productivity<br />

of the plant community. Dense stands of ponderosa pine can produce thick layers of litter.<br />

More open forest stands on dry, less productive sites will have thinner layers of duff and litter<br />

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

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