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Roadside Revegetation

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IMPLEMENTATION GUIDES<br />

first growing season. Ammonium nitrate, ammonium sulfate, potassium nitrate, and urea are<br />

several examples of fast-release fertilizers.<br />

“Water soluble” or “available” nutrients do not always remain available or soluble after they<br />

are applied to the soil. Available forms of phosphorus, for instance, react in the soil to form less<br />

soluble compounds; potassium gets bound up in soils with moderate to high proportions of<br />

clay; and many of the micronutrients (e.g., zinc, copper, manganese) become unavailable when<br />

applied to soils with low pH (see Section 5.5.5, pH and Salts). Unless soils<br />

are sandy or rocky, it can be assumed that many of the nutrients stated<br />

as “available,” except for nitrogen and sulfur, will become somewhat<br />

immobile once they are applied. Over time, however, these nutrients<br />

100<br />

will become available for plant uptake.<br />

90<br />

The advantages of fast-release fertilizers are they are relatively inexpensive,<br />

easy to handle, immediately available to the plant, and can<br />

80<br />

be applied through a range of fertilizer spreading equipment. Disadvantages<br />

are that some nutrients, such as nitrogen, will leach through<br />

70<br />

the soil profile if they are not first taken up by plants or captured by soil<br />

microorganisms in the break down of carbon. Nitrates from fast-release<br />

60<br />

fertilizers have been found to leach through sandy soils to depths that<br />

50<br />

are 4 times the rate of rainfall (Dancer 1975). For example, for sites with<br />

annual rainfalls of 12 inches, nitrate could move to a depth of four feet<br />

40<br />

if it was not taken up by plants or soil organisms. At this depth, nitrogen<br />

would be out of range of most establishing root systems.<br />

Since fast-release fertilizers are salts, they have a potential to burn foliage<br />

and roots, especially when fertilizers are applied at high concentrations<br />

or when applied during dry weather (see Section 5.5.5.2, Mitigating for<br />

Low pH Soils). High concentrations of fast-release fertilizers can also<br />

Trifolium<br />

repens<br />

affect germination rates (Figure 10-4) because of the high soluble salt levels (Brooks and Blaser<br />

1964; Carr and Ballard 1979). Salt damage can be reduced by mixing fast-release fertilizers at<br />

lower concentrations or by applying them during rainy weather.<br />

Slow-Release Fertilizers – These fertilizers are designed to release nutrients at a much slower<br />

rate. To be labeled slow-release fertilizer, some states require a specific amount of nitrogen<br />

to be in a slow-release form. Forms of nitrogen shown on the label as “slowly-available” or<br />

“water- insoluble” are good indicators that a fertilizer is in a slow-release form. The advantages of<br />

using slow-release fertilizers are (1) nutrients are supplied at a time when plants are potentially<br />

growing; (2) less frequent applications; (3) less potential for leaching into ground water; and<br />

(4) less potential to cause salt injury. The disadvantages are that many slow-release fertilizers<br />

are bulky, cost more to purchase and apply, and are limited by the type of fertilizer application<br />

equipment that can be used. On the whole, however, slow-release fertilizers have greater<br />

applicability for revegetating disturbed sites than fast-release fertilizers.<br />

Slow-release fertilizers come in either organic or inorganic forms. Organic fertilizers include<br />

animal manures (including chicken, steer, cow), bone meal, fish emulsion, composted sewage<br />

sludge, and yard waste. Unprocessed organic fertilizers are hard to apply to roadside projects<br />

because they are bulky and high in moisture. Commercially available organic fertilizers, such<br />

as Fertil-Fiber and Biosol®, have been processed to remove most moisture, which makes<br />

them easier to apply through most fertilizer spreading equipment.<br />

The agents responsible for release of nutrients from organic fertilizers are decomposing soil<br />

bacteria. When soil bacteria are active, the release of nutrients is high; when dormant, the rate is<br />

low. The release of nutrients is therefore a function of moisture and temperature, which governs<br />

the rate of bacterial growth. Warm temperatures and high moisture, conditions conducive<br />

to plant growth, are also favorable for the break down of organic fertilizers. Because of this,<br />

the release of nutrients from the decomposition of organic fertilizers often coincides with<br />

the period when plants are growing (spring and fall) and the need for nutrients is greatest.<br />

% Germination<br />

30<br />

Without Fertilizer<br />

Festuca<br />

arundinacea<br />

With Fertilizer<br />

Festuca<br />

rubra<br />

Lolium<br />

perenne<br />

Figure 10-4 | Reduced<br />

seed germination after<br />

exposure to fertilizer<br />

Germination of seeds for some species<br />

can be reduced following exposure to<br />

a 10-30-10 fertilizer solution at a rate<br />

of 750 lbs fertilizer per 1,000 gallon hydroseeder<br />

(after Carr and Ballard 1979).<br />

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

228

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