Abstract

AbstractTo quantify carbon (C) and nitrogen (N) losses in soils of West African urban and peri‐urban agriculture (UPA) we measured fluxes of CO2‐C, N2O‐N, and NH3‐N from irrigated fields in Ouagadougou, Burkina Faso, and Tamale, Ghana, under different fertilization and (waste‐)water regimes. Compared with the unamended control, application of fertilizers increased average cumulative CO2‐C emissions during eight cropping cycles in Ouagadougou by 103% and during seven cropping cycles in Tamale by 42%. Calculated total emissions measured across all cropping cycles reached 14 t C ha−1 in Ouagadougou, accounting for 73% of the C applied as organic fertilizer over a period of two years at this site, and 9 t C ha−1 in Tamale. Compared with unamended control plots, fertilizer application increased N2O‐N emissions in Ouagadougou during different cropping cycles, ranging from 37 to 360%, while average NH3‐N losses increased by 670%. Fertilizer application had no significant effects on N2O‐N losses in Tamale. While wastewater irrigation did not significantly enhance CO2‐C emissions in Ouagadougou, average CO2‐C emissions in Tamale were 71% (1.6 t C ha−1) higher on wastewater plots compared with those of the control (0.9 t C ha−1). However, no significant effects of wastewater on N2O‐N and NH3‐N emissions were observed at either location. Although biochar did not affect N2O‐N and NH3‐N losses, the addition of biochar could contribute to reducing CO2‐C emissions from urban garden soils. When related to crop production, CO2‐C emissions were higher on control than on fertilized plots, but this was not the case for absolute CO2‐C emissions.

Highlights

  • Most agricultural soils in sub-Saharan Africa (SSA) are limited in their ability to supply crops with adequate amounts of nutrients severely limiting food production

  • Mean cumulative CO2-C fluxes in Ouagadougou increased by 103% in FP1+cw (1.8 t C ha–1) compared with C+cw (0.9 t C ha–1) plots and those of FP1+ww increased by 86% compared with C+ww (Fig. 2a)

  • A total of 14 t C ha–1 was lost from fertilized plots in Ouagadougou, representing 73% of the total C applied with organic fertilizers

Read more

Summary

Introduction

Most agricultural soils in sub-Saharan Africa (SSA) are limited in their ability to supply crops with adequate amounts of nutrients severely limiting food production This is due to their inherently low fertility as a result of long weathering, leading to low cation exchange capacity and rapid turnover rates of soil organic carbon (SOC; Bationo and Buerkert, 2001). Characterized by high rates of soil amendments, year round irrigation and high temperatures, these systems are prone to rapid mineralization of organic C and N (Diogo et al, 2010; Predotova et al, 2010b; Lompo et al, 2012) via carbon dioxide (CO2), ammonia (NH3), and nitrous oxide (N2O) emissions The magnitude of these losses depends on the availability of C and N, soil management practices, and environmental conditions (Pelster et al, 2012; Kim et al, 2016)

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call