Grazing-based production systems are a source of soil greenhouse gas (GHG) emissions triggered by excreta depositions. The adoption of forages (formerly known as ) with biological nitrification inhibition (BNI) capacity is a promising alternative to reduce nitrous oxide (NO) emissions from excreta patches. However, how this forage affects methane (CH) or carbon dioxide (CO) emissions from excreta patches remains unclear. This study investigated the potential effect of soils under two forages with contrasting BNI capacity on GHG emissions from cattle dung deposits. Additionally, the NO and CH emission factors (EF) for cattle dung under tropical conditions were determined. Dung from cattle grazing star grass (without BNI) was deposited on both forage plots: cv. Mulato and cv. Tully, with a respectively low and high BNI capacity. Two trials were conducted for GHG monitoring using the static chamber technique. Soil and dung properties and GHG emissions were monitored in trial 1. In trial 2, water was added to simulate rainfall and evaluate GHG emissions under wetter conditions. Our results showed that beneath dung patches, the forage genotype influenced daily CO and cumulative CH emissions during the driest conditions. However, no significant effect of the forage genotype was found on mitigating NO emissions from dung. We attribute the absence of a significant BNI effect on NO emissions to the limited incorporation of dung-N into the soil and rhizosphere where the BNI effect occurs. The average NO EFs was 0.14%, close to the IPCC 2019 uncertainty range (0.01-0.13% at 95% confidence level). Moreover, CH EFs per unit of volatile solid (VS) averaged 0.31 g CH kgVS, slightly lower than the 0.6 g CH kgVS developed by the IPCC. This implies the need to invest in studies to develop more region-specific Tier 2 EFs, including farm-level studies with animals consuming forages to consider the complete implications of forage selection on animal excreta based GHG emissions.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8609157 | PMC |
http://dx.doi.org/10.1016/j.geoderma.2021.115516 | DOI Listing |
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