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Published in Soil Sci Soc Am J 62:1604-1609 (1998)
© 1998 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Relating Preseason Soil Nitrogen to Maize Yield in Tree Legume-Maize Rotations

E. Barrios

CIAT, Apartado Aereo 6713, Cali, Colombia

F. Kwesiga

SADC/ICRAF Agroforestry Project, Makoka Agricultural Research Station, P.O. Box 134, Zomba, Malawi

R. J. Buresh* and R. Coe

International Centre for Research in Agroforestry (ICRAF), P.O. Box 30677, Nairobi, Kenya

J. I. Sprent

Dep. of Biological Sciences, Univ. of Dundee, Dundee DD1 4HN, UK

*Corresponding author (r.buresh{at}cgiar.com).

ABSTRACT

Legumes can be an important source of N for cereals in tropical, subsistence farming systems that use little or no fertilizers. Our objective was to identify measures of soil N availability, following growth of diverse legumes, that correlated with yield of a subsequent unfertilized maize (Zea mays L.) crop. Unfertilized maize followed nine 3-yr-old systems (six monocultures of planted trees legumes, a groundnut [Arachis hypogea L.]-maize-soybean [Glycine max (L.) Merr.] rotation, an uncultivated fallow with natural regrowth of vegetation, and unfertilized maize monoculture) in two experiments on a Ustic Rhodustalf in eastern Zambia. Total soil C and N before maize planting were not related to grain yield of maize. Preseason soil inorganic N (NO3 + NH4), aerobic N mineralization, and light-fraction N (N in macroorganic matter, 150–2000 µm and <1.37 Mg m-3) at 0- to 15- cm depth correlated (P < 0.01) with maize grain yield. Preseason inorganic N combined with light-fraction N accounted for 59% of the variance in maize grain yield. The predictability of maize yield was slightly improved (64% of the variance) by including the population of the parasitic weed striga [Striga asiatica (L.) Kuntze] with preseason inorganic N and light-fraction N. The results suggest that yield of unfertilized, rain-fed maize following different rotational systems on a N-limiting soil in an area with monomodal rainfall was strongly related to the additive effects of preseason soil inorganic N and a soil N fraction related to N mineralization.

Received for publication October 16, 1997.


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C. Shang and H. Tiessen
Carbon Turnover and Carbon-13 Natural Abundance in Organo-Mineral Fractions of a Tropical Dry Forest Soil under Cultivation
Soil Sci. Soc. Am. J., November 1, 2000; 64(6): 2149 - 2155.
[Abstract] [Full Text]




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