Relationship between respiratory quotient, nitrification, and nitrous oxide emissions in a forced aerated composting process
Introduction
The spreading of livestock excrement can contribute to nitrate contamination of groundwater and eutrophication of surface waters. To mitigate these issues, a decentralized differentiable treatment system for livestock excreta that discharges minimum pollutants, produces minimal greenhouse gas (GHG) emissions, and more effectively recovers nutrients has been proposed (Fujiwara, 2012). Producing compost of better quality and less GHG emission is one of the key technologies in this innovative system, through preventing environmental pollution and enhancing resource recycling in agricultural areas. To achieve these outcomes, it is necessary to understand changes of the material during the composting process. In particular, the emission of nitrous oxide (N2O), which is a GHG and has a reported global warming potential 298 times greater than that of carbon dioxide (CO2) (IPCC, 2007), has become a problem in agricultural areas. Controls are needed to reduce N2O emissions produced during the composting process.
Compost stability is an important component of the composting process, because it has implications for compost use as a fertilizer. Stability is related to the types of organic compounds that remain following composting and the microbial activity of composted materials (California Compost Quality Council, 2001). The primary goal of composting is to produce a stabilized end-product (Komilis and Kanellos, 2012). Some of the most common compost stability tests are based on quantification of microbial respiration (Komilis et al., 2011a). Microbial respiration activity indices based on oxygen (O2) uptake rate (OUR) such as AT4 (static respiration index for 4 days) and specific OUR (SOUR) (Lasaridi et al., 2006), and on CO2 evolution (Bernal et al., 2009), are commonly used to test compost stability (Gómez et al., 2006). By coupling data of OUR and CO2 evolution rates, the respiratory quotient (RQ) can be calculated. The RQ is the ratio of the number of moles of CO2 generated to the number of moles of O2 consumed. The value of RQ is known to reflect not only microbial respiration but also the biochemical composition of organic material (Gea et al., 2004), and is widely used in the study of soil environments (Dilly, 2003). Previous studies have reported that RQ is a useful index for composting processes (Atkinson et al., 1997), although others reported that RQ did not change significantly throughout those processes (Gea et al., 2004, Gómez et al., 2006). The applicability of RQ as an index of compost stability requires further study.
Stability indices are not only important measures of compost characteristics, but can also be used for process performance monitoring (Gómez et al., 2006). It is important to establish useful indices for both measuring compost stability and monitoring microbial reactions during composting, to identify appropriate conditions that will produce high-quality compost while lowering GHG emissions. To reduce N2O emissions from the composting process, microbial activity in the nitrogen cycle during nitrogen transformation should be monitored. Previous studies of respiration indices such as RQ in composting processes have only focused on the biochemical composition of organic material (Gea et al., 2004, Komilis and Kanellos, 2012). In an earlier study, we constructed experimental devices for continuous monitoring of emitted gases from a composting reactor, indicating that N2O emissions occurred simultaneously with an RQ decrease (Tsutsui et al., 2013). However, we could not obtain information about potential mechanisms responsible for this relationship, because we did not conduct either microbial community or mass balance analyses.
In this study, we took a two-step approach to examine RQ usefulness as an indicator, for both compost stability and monitoring of nitrification and N2O emissions. In the first step, we performed a detailed gas-phase analysis to clarify the relationship between the RQ decrease and N2O emissions. We used lab-scale forced aerated composting reactors to continuously measure gas components, toward evaluating the suitability of RQ as an indicator. In this experiment, we did not conduct sampling campaigns to avoid the variation of gas components triggered by sample mixing for clarifying the relationship between the RQ decrease and N2O emissions. In the second step, we investigated mechanisms responsible for the simultaneous occurrence of nitrification and N2O emissions with the RQ decrease in the forced aerated composting process. This was done by conducting gas phase, sample composition, microbial community, and mass balance analyses. In addition, temporally and spatially complex environment conditions (such as temperature, oxygen concentration, and water content) make us difficult to clear the mechanism of N2O emission in actual composting process. To achieve the objective of our study, we conducted the forced aerated composting process under isothermal condition and maintained the water content at constant to prevent the effect of large fluctuation in environmental conditions.
Section snippets
Composting reactors and experimental devices
Composting reactors and experimental devices used were described in detail by Tsutsui et al. (2013). Briefly, we used three 1.63-L forced aerated composting reactors equipped with a porous stainless steel plate at the bottom. Inlet gas was humidified to maintain water content of the samples at ∼60%. Outlet gas was bubbled into a 5 mM sulfuric acid solution to trap ammonia gas. To express the measured gas concentration in the inlet and outlet as the molar flow rate (mmol/h) at standard conditions
Relationship between RQ value and N2O emission in Experiment I
Profiles of the OUR and CO2 emissions from the triplicate composting reactors are shown in Fig. 1(A) and (B), respectively. Small standard deviations of the OUR or CO2 emission profiles throughout the experiment demonstrate good reproducibility of organic matter decomposition in this experiment. Additionally, the profile of CO2 emission rates was similar to that of OUR in all reactors, with relatively low values. In the first hour of the experiment, OUR and CO2 emission rates were maxima; they
Conclusion
We assessed the relationship between RQ, nitrification, and N2O emission in a forced aerated composting process using lab-scale reactors. Continuous emissions of N2O were observed during a decrease in RQ. Mass balance calculations demonstrated that nitrification occurrence caused the latter decrease. Correlation between nitrification and N2O emission shows that nitrification triggered that emission. Our results indicate that RQ is a useful index, predicting the occurrence of nitrification and N2
Acknowledgements
This research was financially supported by the Core Research for Evolutionary Science and Technology (CREST) of the Japan Science and Technology Agency. The authors wish to thank Dr. Nowaki Hijikata of Hokkaido University for his assistance with the instrumental analyses.
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