Submitted by Erin Rasmussen on
Publication Type:
Journal ArticleSource:
Ecosystems (2008) 11: 726, Volume 11, p.726 (2008)URL:
http://www.css.cornell.edu/faculty/lehmann/publ/Ecosystems%2011,%20726-739,%202008%20Kimetu.pdfKeywords:
agroecosystem, chronosequence, soil degradation, soil organic matter, soil productivityAbstract:
In the highlands of Western Kenya, we investigated the reversibility of soil productivity decline with increasing length of continuous maize cultivation over 100 years (corresponding to decreasing soil organic carbon (SOC) and nutrient contents) using organic matter additions of differing quality and stability as a function of soil texture and inorganic nitrogen (N) additions. The ability of additions of labile organic matter (green and animal manure) to improve productivity primarily by enhanced nutrient availability was contrasted with the ability of stable organic matter (biochar and sawdust) to improve productivity by enhancing SOC. Maize productivity declined by 66% during the first 35 years of continuous cropping after forest clearing. Productivity remained at a low level of 3.0 t grain ha-1 across the chronosequence stretching up to 105 years of continuous cultivation despite full N
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