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Dinitrogen fixation

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The incorporation of trees and crops that are able to biologically fix N2 is fairly common and well researched in tropical agroforestry systems (Nair, Buresh, Mugendi, & Latt, 1999). In temperate systems, similar accounts of incorporating N2–fixing trees into agroforestry are rare, perhaps because of the abundance and historically low cost of N fertilizer and the low value of N2–fixing trees. Despite the infrequent use of biological N2 fixation by trees in temperate agroforestry systems, there is potential for using N2–fixing tree species native to temperate environments. Species from the genera Robinia, Prosopis, and Alnus have the potential to provide N2 fixation benefits in temperate agroforestry systems (Boring & Swank, 1984; Seiter, Ingham, William, & Hibbs, 1995). Seiter et al. (1995) demonstrated this potential in a red alder (Alnus rubra Bong.)–maize alley‐cropping system in Oregon. They observed, using a 15N injection technique, that 32–58% of the total N in maize was obtained from N2 fixed by red alder and that N transfer increased by shortening the distance between the trees and crops.

There are also several leguminous herbaceous plant species capable of fixing atmospheric N2 in temperate agroforestry systems, including alfalfa, clover, hairy vetch (Vicia villosa Roth), and soybean (Troeh & Thompson, 1993). Although multiple studies have incorporated leguminous herbaceous species capable of biological N2 fixation into temperate agroforestry systems (Alley et al., 1998; Delate et al., 2005; Gakis et al., 2004; Silva‐Pando, Gonzalez‐Hernandez, & Rozados‐Lorenzo, 2002), few studies have actually quantified the effects that these species have on soil N (Dupraz et al., 1998; Waring & Snowdon, 1985). Nitrogen buildup in the soil is possible from leguminous herbaceous understory species; however, this is a slow process that does not occur immediately after herbaceous plant establishment. In a radiata pine–subterranean clover (Trifolium subterraneum L.) silvopasture in Australia, Waring and Snowdon (1985) observed a 36% increase in soil N at the end of seven growing seasons in the silvopasture, which corresponded to a 14% increase in tree diameter compared with pines growing in a monoculture without a subterranean clover understory.

North American Agroforestry

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