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Roadside Revegetation

RoadsideReveg_PollinatorHabitat_DRAFTv1-1_sept2016

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PLANNING PHASE TWO: ASSESS SITE<br />

Mitigating for Road Drainage<br />

Species Selection<br />

In areas below culverts, soil moisture is typically higher than surrounding areas after rainstorms<br />

or snow melt. These areas may be suitable for more moisture-sensitive plant species that<br />

require increased soil moisture. When planted with plant species that support pollinators,<br />

these sites will increase pollinator habitat.<br />

Large Wood<br />

Obstacles, such as large wood, can be placed at the base of culverts or perpendicular to the<br />

slope to slow concentrated water and increase soil moisture in these areas. Large wood also<br />

provides nesting habitat or shelter for a number of pollinator species.<br />

Biotechnical Slope Protection<br />

Gullies can form below culvert outlets and, for this reason, these sites are often armored with<br />

rock. Moisture-loving vegetation, such as willows, sedges, and rushes, can be integrated into<br />

the hardened surfaces, such as live silt fences, as shown in Figure 5-9 and as discussed in<br />

Section 10.3.3, Installing Cuttings.<br />

Water Harvesting<br />

Road surfaces, shoulders, and to a lesser extent, cut and fill slopes are impermeable surfaces<br />

that create runoff water during precipitation. Utilizing this water for plant growth, as shown<br />

in Figure 5-5, is a form of water harvesting.<br />

5.3 AVAILABLE WATER STORAGE AND ACCESSIBILITY<br />

The previous section discussed how water enters the soil surface. This section describes how<br />

water is stored in the soil and how soil water is accessed by roots. Where precipitation is<br />

low or infrequent during the growing season, the amount of water a soil can hold between<br />

rainstorms is important from a plant survival and growth standpoint.<br />

The total available water-holding capacity (TAWHC) is the sum of all water stored in the soil<br />

profile that is available to plant roots. The amount of water that a soil can store is primarily a<br />

function of the following:<br />

◾◾<br />

Soil texture<br />

◾◾<br />

Rock fragments<br />

◾◾<br />

Soil structure<br />

◾◾<br />

Rooting depth<br />

◾◾<br />

Mycorrhizae<br />

Figure 5-9 | Live silt fence<br />

In gullies, draws, intermittent streams,<br />

or below culvert outlets, live willow<br />

stakes (see Section 10.3.3.2, Live Stakes)<br />

are placed in rows, creating what is<br />

referred to as a live silt fence, to slow<br />

water velocities and catch sediment and<br />

debris (Polster 1997). The stakes root and<br />

establish into plants over time.<br />

The amount of water a soil stores and how easily it is accessible by roots determines the types<br />

of species and the amount of vegetative cover a site can support.<br />

5.3.1 SOIL TEXTURE<br />

Soils are composed of minerals of varying sizes, ranging from clay (the smallest) to stone (the<br />

largest). Each mineral particle in a soil sample can be grouped into six categories depending on<br />

its size: clay (8 in [20 cm]). The fine soil fraction is composed of a combination of sand, silt, and clay size<br />

particles. The proportion of these size groups in a soil is called the soil texture.<br />

Figure 5-10 shows 12 soil textural classes by their proportions of sand, silt, and clay as defined by<br />

the U.S. Department of Agriculture classification system (Soil Survey Staff 1975). Two other soil<br />

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

65

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