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Roadside Revegetation

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IMPLEMENTATION GUIDES<br />

Table 10.3 | Types of tillage and equipment<br />

The appropriate tillage equipment for the project depends on project objectives.<br />

Shattering Mixing Imprinting<br />

Objectives<br />

Rippers & subsoilers<br />

Disks, plows, excavator<br />

attachments<br />

Dixon imprinter, excavator<br />

attachments, trackwalking<br />

Loosen compacted soil Good Good Poor<br />

Incorporate amendments Poor Good Poor<br />

Roughen surface Good Good Good<br />

to recover its original bulk density (Wert and Thomas 1981; Froehlich and others 1983). In a<br />

review of tillage projects on rangeland soils, Gifford (1975) found that deep tillage greatly<br />

reduced runoff, while shallow tillage had little effect.<br />

Tillage alone will not return a soil to its original bulk density or hydrologic function (Figure<br />

10-7), nor will the effects of tillage last indefinitely, especially in non-cohesive soils (Onstad<br />

and others 1984). There are many factors that affect the return to bulk densities and infiltration<br />

rates typical of undisturbed reference sites. These include the type of tillage equipment used,<br />

penetration depth, soil moisture during tillage, soil texture, presence of topsoil, and organic<br />

matter content.<br />

There are two fundamentally different equipment designs for reducing compaction. One<br />

design simply lifts and drops soil in place, shattering compacted soil in the process. This type<br />

of equipment includes rock rippers, subsoilers, and “winged” subsoilers. The second design<br />

churns and mixes the soil. Equipment that falls into this category includes disk harrows, plows,<br />

spaders, and attachments to excavators. This type of equipment can also incorporate soil<br />

Inches per Hour<br />

3<br />

2<br />

1<br />

Granitic<br />

Metasedimentary<br />

1st 2nd 3rd 1st 2nd 3rd<br />

Rainfall Event<br />

Rainfall Event<br />

Ripped & Mulched<br />

Ripped<br />

Prior to Ripping<br />

Permeability rates for<br />

lightly disturbed forest soils<br />

100 year rainfall rate<br />

Snowmelt rate<br />

Figure 10-7 | Benefits of ripping<br />

and mulching vary by soil type<br />

Short-term benefits of ripping (using a winged<br />

subsoiler) and mulching road surfaces vary by soil<br />

type, as shown in rainfall simulation tests on sites in<br />

northern Idaho. Granitic soils responded to ripping<br />

and mulching with increased permeability during<br />

the first storm, but permeability rates returned to<br />

near pre-treatments rates with successive rainfall<br />

events. Metamorphic soils reacted positively to<br />

both treatments and maintained high permeability<br />

rates after three rainfall events. Mulching<br />

improved permeability in both soil types. In fact,<br />

for metamorphic soils, the combination of ripping<br />

and mulching increased permeability to rates<br />

that were typical of lightly disturbed forest soils<br />

(adapted from Luce 1997).<br />

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

234

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