<mods:mods version="3.3" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd" xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><mods:titleInfo><mods:title>Increased proportion of active soil N in Breton loam under cropping systems with forages and green manures</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">S P</mods:namePart><mods:namePart type="family">Wani</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">W B</mods:namePart><mods:namePart type="family">McGill</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">K L</mods:namePart><mods:namePart type="family">Haugen-Kozyra</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">N G</mods:namePart><mods:namePart type="family">Juma</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>Total soil N and N mineralization&#13;
rate partially ctririct&amp;iie the influence olvariouJcropping systems on the growth of.sequent.crop.s in a rotation' The objectives&#13;
of this study were to (1) quantify the relationship among cropping system, total N and mineralizable N, and (2) compare amount&#13;
of N mineralized under'controlled laboratory conditions-with pianl N uptake under green]ouse conditi:ns. Three cropping systems&#13;
that have been in operation between 9 and 60 yr on a Gray-Luvisol (Breton loam; were&#13;
^selected . They included: (1) an ag.lo:&#13;
ecological (lnn) d-yr rotation involving fabibeans as gr-een manure (AER1 sampled after the_first lababean crop-?nq AER?&#13;
,u-pied after 3 yr of continuous forage)l (2) continuous grain system (CG), with fertilizer N at 90 kg ha-'^yr- '; inttrated&#13;
in 1980 and considered established in f"98i; i3) a classicial Ereton iotation (CBR) involving 9]o-ng-term (ca. 1930) 5-yr rotation&#13;
with forages and cereals and no return of.ciop residues (CBR1 fertilized with P-K-S and CBR2 unfertilized). We cautio_n that&#13;
not all ohlses of each rotation were sampled: bur conclusions pertain to N-mineralization potential in soil samples immediately&#13;
preceding barley as sequent crop in each rotation. The rate ofN mineralization declined with time, but it remained greater than&#13;
iero aftei 20 wi&lt; of incirbation in all soils. Mineral-N accumulation at 20 wk followed the order AER1 &gt; AER2 &gt; &gt; CBRI &gt;&#13;
CBR2 : CG. Mineralizable soil N, following one cycle of the AER rotation, was almost double that following 60 yr of the&#13;
CBR rotation. Data for mineral-N accumulation under laboratory conditions were described best by a single-component expo-n-ential&#13;
model. Legume-based rotations were associated with increased total soil N and a greater proportional increase in active N than&#13;
in total soilN. Active N was least in soil under the CG system. The incubation-extraction procedure resulted in higher estimates&#13;
of mineralizable N than did the plant-uptake method; liowever, the ranking of N-supplying power of soils was the same.</mods:abstract><mods:classification authority="lcc">Soil Science</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">1994</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>Agricultural Institute of Canada</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mods:mods>