Abstract
Sub-Saharan Africa is facing food security challenges due, in part, to decades of soil nitrogen (N) depletion. Applying N fertilizer could increase crop yields and replenish soil N pools. From 2010 to 2015, field experiments conducted in Embu and Kiboko, Kenya and Harare, Zimbabwe investigated yield and N uptake response of six maize (Zea mays L.) hybrids to four N fertilizer rates (0 to 160 kg N ha−1) in continuous maize production systems. The N recovery efficiency (NRE), cumulative N balance, and soil N content in the upper 0.9 m of soil following the final harvest were determined at each N rate. Plant and soil responses to N fertilizer applications did not differ amongst hybrids. Across locations and N rates, NRE ranged from 0.4 to 1.8 kg kg−1. Higher NRE values in Kiboko and Harare occurred at lower post-harvest soil inorganic N levels. The excessively high NRE value of 1.8 kg kg−1 at 40 kg N ha−1 in Harare suggested that maize hybrids deplete soil inorganic N most at low N rates. Still, negative cumulative N balances indicated that inorganic soil N depletion occurred at all N rates in Embu and Harare (up to − 193 and − 167 kg N ha−1, respectively) and at the 40 kg N ha−1 rate in Kiboko (− 72 kg N ha−1). Overall, maize N uptake exceeded fertilizer N applied and so, while yields increased, soil N pools were not replenished, especially at low total soil N levels (< 10,000 kg N ha−1 in top 0.9 m).
Highlights
Maize cropping systems in Kenya have been reported to deplete the soil an average of 42 kg N ha-1 annually (Smaling et al 1993)
There were no significant interactions between hybrid, N rate, and/or depth effects for any of the plant–soil N dynamics reported in this paper
These 3 studies found N recovery efficiency (NRE) values ranging from 0.31 to 0.69 kg kg-1, a range consistent with the values found in Embu at all N rates and in Harare at 160 kg N ha-1
Summary
Maize cropping systems in Kenya have been reported to deplete the soil an average of 42 kg N ha-1 annually (Smaling et al 1993). In Zimbabwe, the annual depletion rates are purportedly lower than those of Kenya at around 30 kg N ha-1 (Henao and Baanante 2006). This difference in depletion is in part due to the one growing season per year in Zimbabwe yielding an average 3 t ha-1 year-1 less grain than the combined yields of 2 growing seasons per year in. Soil erosion plays a large role in soil degradation, Drechsel et al (2001) found that the average N and K balances in sub-Saharan Africa (SSA) would be negative even in scenarios where no erosion was occurring. The risk of potential negative effects has increased in conjunction with crop intensification aimed at meeting the food needs of SSA’s growing population (Drechsel et al 2001)
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