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Roadside Revegetation

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PLANNING PHASE TWO: ASSESS SITE<br />

Mitigating for High Rainfall Interception<br />

It is important to consider the water-holding capacities of the mulches or soil covers to be used,<br />

especially on arid sites. Highly decomposed, fine-textured composts have high water-holding<br />

capacities compared to coarser-textured composts and hold more moisture after a rainstorm.<br />

Coarser materials, such as shredded wood, bark, wood chips, and wood strands, hold less water,<br />

allowing more rainwater to enter the soil. In addition, because fine-textured composts hold<br />

more water than course mulches or soil, they are good growing media for desirable native<br />

plants as well as undesirable weed species. The question that should be asked when selecting<br />

a soil cover is whether it is to be used as a mulch or a growing media. If a mulch, then a coarse<br />

material should be used; if growing media, a fine compost should be used.<br />

5.2.3 INFILTRATION<br />

Infiltration is the ability of the soil surface to absorb water from rainfall, snowmelt, irrigation,<br />

or road drainage. When infiltration rates are slower than the amount of water applied to the<br />

surface of the soil, runoff will occur and this water will not be available for plant uptake. In<br />

addition, runoff can detach and transport soil, causing soil erosion, decreased water quality,<br />

and increased peak flows. See Section 5.6.5, Infiltration Rates, for a discussion of infiltration<br />

rates on surface stability.<br />

The size, abundance, and stability of soil aggregates in the surface soil determine the infiltration<br />

rates. Large stable pores created by worms, insects, and channels left behind from decayed<br />

roots will absorb water quickly and have high infiltration rates; soils that have been compacted,<br />

had their topsoil removed, or are low in organic matter will have poor infiltration rates.<br />

Under undisturbed conditions, infiltration rates are typically high, especially where a litter<br />

and duff cover exists. When soil cover is removed, the impact from rain splash can seal the<br />

soil surface, creating a crust that will significantly reduce infiltration rates. Infiltration rates are<br />

also reduced when the soil is compacted by heavy equipment or traffic.<br />

Rainfall Absorbed (inches)<br />

1<br />

0.9<br />

0.8<br />

0.7<br />

0.6<br />

0.5<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

3" thick<br />

2" thick<br />

1" thick<br />

0<br />

0 25 50 75<br />

Moisture Holding Capacity (% of dry weight)<br />

Figure 5-7 | Moisture holding<br />

capacity of mulch or litter<br />

The amount of rainfall intercepted by<br />

soil cover (e.g., mulch or litter) is dependent<br />

on its water- holding capacity<br />

and thickness.<br />

Infiltration – How to Assess<br />

The most accurate method to measure field infiltration rates the rainfall simulator (Figure<br />

5-50). This equipment is calibrated to simulate the appropriate drop size and impact velocity<br />

of many rainfall events (Grismer and Hogan 2004). The rainfall simulator is expensive to operate<br />

and is not routinely used by the designer. The most common application for this technology<br />

is in comparing different mitigating measures, such as mulches and tillage methods, on<br />

infiltration capacity.<br />

Without conducting rainfall simulation tests, infiltration rates must be inferred by measuring<br />

soil strength using a soil penetrometer, bulk density measurements (see Section 5.3.3, Soil<br />

Structure), and from site characteristics such as visual observation of compaction and the<br />

percentage of soil cover. For most construction activities that remove surface cover or disturb<br />

the topsoil, it can be assumed that infiltration rates will be reduced to levels that will create<br />

overland flow under most rainfall intensities.<br />

Mitigating for Low Infiltration Rates<br />

Minimize Compaction<br />

Driving heavy equipment over soils causes compaction and reduces infiltration rates. After<br />

sites have been prepared for seeding or planting, heavy equipment must not be driven over<br />

soils. Such practices that are often recommended for erosion control, such as trackwalking,<br />

can actually decrease infiltration rates and adversely affect the establishment and cover of<br />

native plants. These practices may not be appropriate on all soil types and should be assessed<br />

on a site-specific basis (Grismer and Hogan 2007).<br />

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

63

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