Using nitrification inhibitors to mitigate agricultural N2O emission: a double-edged sword?
Abstract
Nitrification inhibitors show promise in decreasing nitrous oxide (N2O) emission from agricultural systems worldwide, but they may be much less effective than previously thought when both direct and indirect emissions are taken into account. Whilst nitrification inhibitors are effective at decreasing direct N2O emission and nitrate (NO3–) leaching, limited studies suggest that they may increase ammonia (NH3) volatilization and, subsequently, indirect N2O emission. These dual effects are typically not considered when evaluating the inhibitors as a climate change mitigation tool. Here, we collate results from the literature that simultaneously examined the effects of nitrification inhibitors on N2O and NH3 emissions. We found that nitrification inhibitors decreased direct N2O emission by 0.2–4.5 kg N2O-N ha−1 (8–57%), but generally increased NH3 emission by 0.2–18.7 kg NH3-N ha−1 (3–65%). Taking into account the estimated indirect N2O emission from deposited NH3, the overall impact of nitrification inhibitors ranged from −4.5 (reduction) to +0.5 (increase) kg N2O-N ha−1. Our results suggest that the beneficial effect of nitrification inhibitors in decreasing direct N2O emission can be undermined or even outweighed by an increase in NH3 volatilization.
Introduction
Globally, agriculture contributes about 60% of the total anthropogenic emission of nitrous oxide (N2O), a greenhouse gas approximately 300 times more potent than carbon dioxide (Ciais et al., 2013). The mitigation of N2O emission from agricultural systems is an important issue worldwide. Nitrification inhibitors are recommended by the IPCC as a potential mitigation option for agricultural N2O emission (IPCC, 2014) and have been extensively investigated and widely used across a broad range of agroecosystems (Chen et al., 2008; Qiao et al., 2015). Nitrification inhibitors temporarily suppress the microbial conversion of ammonium (NH4+) to nitrite (NO2–) in soil. This reduces substrate availability for nitrate (NO3–) formation and subsequent denitrification, thereby decreasing N2O emission and NO3– leaching (Bundy & Bremner, 1973; Chen et al., 2008). Recent meta-analyses indicated that nitrification inhibitors decreased N2O emission and NO3– leaching by 31–48% and 32–59%, respectively, across diverse agricultural ecosystems including upland, grassland and paddy fields (Akiyama et al., 2010; Qiao et al., 2015). Nitrate loss via leaching and run-off may be transported to groundwater, rivers or estuaries where part of it may be converted to N2O (Nevison, 2000). This indirect N2O emission can be estimated by the IPCC emission factor EF5 with a default value of 0.75% (De Klein et al., 2006).
The use of nitrification inhibitors, however, prolongs the retention of NH4+ in soil, which could potentially increase ammonia (NH3) emission (Zaman & Nguyen, 2012). Deposition of emitted NH3 not only poses a major threat to environmental quality and ecosystem biodiversity (Erisman et al., 2008), but indirectly it also contributes to N2O emission (Van Der Gon & Bleeker, 2005) through subsequent nitrification and denitrification. According to the IPCC guidelines (De Klein et al., 2006), about 1% (a range of 0.2–5%) of the NH3 emitted is converted to N2O after deposition to land (IPCC emission factor EF4).
Whilst the effect of nitrification inhibitors on NH3 volatilization is not as widely studied as that on N2O emission, Qiao et al. (2015) recently summarized the available studies and concluded that nitrification inhibitors increased NH3 volatilization from synthetic fertilizers and animal manures in agricultural systems by 33–67%. However, most of the studies included in the synthesis focussed on one or other of these gases, and Qiao et al. (2015) expressed the impact of the inhibitor as percentage change, not absolute difference, in nitrogen (N). The overall inhibitor effect on N2O emission (direct and indirect), which can be determined from studies that simultaneously measure N2O and NH3 emissions and NO3– leaching in the field, remains uncertain. The inclusion of indirect N2O emission is critical for evaluating the effectiveness of nitrification inhibitors in mitigating greenhouse gas emissions from agriculture. We therefore conducted a literature review to address this knowledge gap.
Literature search
To assess the overall contribution of nitrification inhibitors to N2O emission (direct and indirect), we performed extensive keyword searches of several databases (Web of Science, Scopus, CAB Abstracts, Academic Search complete and Google Scholar) and the reference list of cited references, for studies published prior to October 2015. The keywords used in the search included nitrification inhibitors, names of the inhibitors such as DCD and DMPP, nitrous oxide/N2O emission, ammonia/NH3 emission, volatilization, direct/indirect N2O, greenhouse gas, nitrate/NO3– leaching, loss and/or mitigation, agriculture, cropping, pastures and their combinations. Only studies that simultaneously examined N2O and NH3 emissions in the same field location were included. The search resulted in 18 observations in pasture and cropping systems (Table 1).
| Agricultural system | N form | N rate kg N ha−1 | Season | Inhibitor | Effect of nitrification inhibitor (NI) | Overall NI effect on N2O emission | Country | Gas measurement technique | Reference | |||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Direct N2O emission | NH3 volatilization | (kg N ha−1) (I + II × EF4) e | N2O | NH3 | ||||||||||
| %a | Amount b (kg N ha−1) (I) | %c | Amount d (kg N ha−1) (II) | EF4 = 1% | EF4 = 5% | |||||||||
| Cropping rice | Urea | 180 | Summer | N-serve | −49.9 | −0.57 | +64.9 | +12.75 | −0.44 | +0.07 | China | CC | OC | Sun et al., 2015 |
| Cropping rice | Urea | 240 | Summer | N-serve | −19.2 | −0.27 | +37.5 | +15.80 | −0.11 | +0.52 | China | CC | OC | Sun et al., 2015 |
| Cropping maize | Slurry | 165 | Summer | DCD | −20.4 | −0.79 | −3.7 | −0.40 | −0.79 | −0.81 | Brazil | CC | CC | Aita et al., 2015 |
| Cropping wheat | Slurry | 135 | Winter | DCD | −52.3 | −1.36 | +3.1 | +0.35 | −1.35 | −1.34 | Brazil | CC | CC | Aita et al., 2015 |
| Cropping wheat/barley; pasture | Urea | 120–200 | Whole year | DCD | −46.5 | −0.52 | +6.1 | +2.20 | −0.50 | −0.41 | UK | CC | WT | Misselbrook et al., 2014 |
| Cropping wheat/barley; pasture | AN | 120–200 | Whole year | DCD | −28.7 | −0.48 | +5.4 | +0.15 | −0.48 | −0.47 | UK | CC | WT | Misselbrook et al., 2014 |
| Pasture | Urine | 365–625 | Spring–autumn | DCD | −56.8 | −1.24 | −0.8 | −0.97 | −1.25 | −1.29 | UK | CC | WT | Misselbrook et al., 2014 |
| Pasture | Urine | 365–625 | Spring–autumn | PD | −10.6 | −0.23 | +4.0 | +4.87 | −0.18 | +0.01 | UK | CC | WT | Misselbrook et al., 2014 |
| Pasture | Slurry | 106–181 | Spring–autumn | DCD | −30.1 | −0.38 | +7.7 | +2.55 | −0.36 | −0.26 | UK | CC | WT | Misselbrook et al., 2014 |
| Pasture | Urine | 600 | Autumn | DCD | −42.1 | −2.93 | +35.5 | +18.65 | −2.74 | −2.00 | New Zealand | CC | OC | Zaman et al., 2013 |
| Pasture | Urine | 600 | Spring | DCD | −40.5 | −2.15 | +13.3 | +13.87 | −2.01 | −1.46 | New Zealand | CC | OC | Zaman et al., 2013 |
| Pasture | Urine | 600 | Autumn | DCD | −37.1 | −4.47 | +43.4 | +12.60 | −4.34 | −3.84 | New Zealand | CC | OC | Zaman & Blennerhassett, 2010 |
| Pasture | Urine | 600 | Spring | DCD | −46.8 | −4.33 | +18.2 | +8.00 | −4.25 | −3.93 | New Zealand | CC | OC | Zaman & Blennerhassett, 2010 |
| Pasture | Urine | 600 | Spring | DCD | −38.6 | −4.40 | +9.1 | +2.00 | −4.38 | −4.30 | New Zealand | CC | OC | Zaman et al., 2009; |
| Pasture | Urine | 600 | Summer | DCD | −20.0 | −0.30 | +17.2 | +8.60 | −0.21 | +0.13 | New Zealand | CC | OC | Zaman et al., 2009 |
| Pasture | Slurry | 123 | Spring–summer | DMPP | −7.9 | −0.18 | +13.9 | +1.80 | −0.16 | −0.09 | Spain | CC | OC | Menéndez et al., 2009; |
| Pasture | ANS | 97 | Spring | DMPP | −8.8 | −0.39 | −51.7 | −0.15 | −0.39 | −0.40 | Spain | CC | OC | Menéndez et al., 2006 |
| Pasture | Slurry | 181 | Spring | DMPP | −29.1 | −4.51 | +42.0 | +3.16 | −4.48 | −4.35 | Spain | CC | OC | Menéndez et al., 2006 |
- AN, ammonium nitrate; ANS, ammonium nitrate sulphate; CC, closed chamber; DCD, dicyandiamide; DMPP, 3,4-dimethylpyrazole phosphate; EF4, emission factor for indirect N2O emission; NI, nitrification inhibitor; OC, open chamber; PD, pyrazole derivatives 1H-1,2,4-triazole and 3-methylpyrazole; WT, wind tunnel.
- a The value was calculated by: (N2O emission in the treatment with NI – N2O emission in the control)/N2O emission in the control × 100%.
- b The value was calculated by: N2O emission in the treatment with NI – N2O emission in the control.
- c The value was calculated by: (NH3 volatilization in the treatment with NI – NH3 volatilization in the control)/NH3 volatilization in the control × 100%.
- d The value was calculated by: NH3 volatilization in the treatment with NI – NH3 volatilization in the control.
- e EF4 of 1% and 5% represents the mean and upper range, respectively, of the IPCC default emission factor for indirect N2O emission (De Klein et al., 2006).
Dual effects of nitrification inhibitors on N2O emission
From the literature review, we found that nitrification inhibitors consistently decreased direct N2O emission from fertilizers (urea and ammonium based) and animal wastes (slurry and urine), applied at between 97 and 625 kg N ha−1, by 0.2–4.5 kg N2O-N ha−1 (8–57%) (Table 1). On the other hand, NH3 volatilization was increased by 0.2–18.7 kg NH3-N ha−1 (3–65%) following the application of the inhibitors in all but three observations. Applying the default emission factor value of 1% (De Klein et al., 2006) for indirect N2O emission from NH3 volatilization and deposition (EF4), we found there was an overall N2O-N reduction of 0.1–4.5 kg N ha−1 from the use of nitrification inhibitors. However, when the upper range of EF4 (5%) (De Klein et al., 2006) was used, the change in N2O-N ranged from −4.4 (reduction) to +0.5 (increase) kg N ha−1 (Table 1).
We found that only two studies reported the effect of nitrification inhibitors on NO3– leaching in addition to that on N2O and NH3 emissions. This precludes the estimation of indirect N2O emission from measured NO3– leaching for the studies included in Table 1. Nonetheless, NO3– leaching is assumed to be an insignificant source of indirect N2O emission in dryland cropping systems and grassland systems where the amount of precipitation plus irrigation does not exceed 80% of the potential evapotranspiration (De Klein et al., 2006; U.S. EPA, 2014). A global process-based simulation of terrestrial N cycle estimated that the annual leaching load is around 20 kg N ha−1 for most regions with fertilizer application of >100 kg N ha−1. Based on the default EF5 value of 0.75% (De Klein et al., 2006), and an average reduction in NO3– leaching of 47% by nitrification inhibitors (Qiao et al., 2015), we estimated that the inhibitors may decrease indirect N2O emission associated with NO3– leaching by 0.07 kg N ha−1 or have no effect on the emission when NO3– leaching is negligible. This has minimal impact on the overall effect of nitrification inhibitors on N2O emission.
The results of our literature review (Table 1) indicate that nitrification inhibitors effectively and consistently decrease direct N2O emission from agricultural systems. Nonetheless, this beneficial effect can be weakened, negated or even reversed by the estimated concomitant increase in indirect N2O emission from deposited NH3. This highlights the importance of considering both gases when evaluating the use of nitrification inhibitors as a climate change mitigation option. An alternative approach would be to use a double inhibitor (a combination of a nitrification inhibitor and urease inhibitor). Urease inhibitors slow the hydrolysis of urea and consequently reduce NH3 volatilization and can be effective on urea (Chen et al., 2008). A recent study showed that both NH3 volatilization and N2O emission were decreased when urea was treated with a double inhibitor (Zaman & Blennerhassett, 2010). However, this double inhibitor approach is impractical for decreasing NH3 volatilization from N sources containing negligible urea but high NH4+ content, such as animal manure and ammonium fertilizers. In this regard, substances with a high affinity for binding onto NH4+ ions may be used as additives to mitigate NH3 volatilization. For instance, zeolite and, more recently, lignite were shown to effectively lower NH3 volatilization when mixed with animal manure (Ndegwa et al., 2008; Chen et al., 2015). Alternatively, where practical, manure should be incorporated into soil rather than being surface applied to prevent NH3 loss.
Summary and implication
Nitrification inhibitors decrease direct N2O emission and indirect N2O emission due to NO3– leaching from agroecosystems. Yet this beneficial effect is weakened by any accompanying increase in indirect N2O emission that can result from increased emission and deposition of NH3. Appropriate NH3 mitigation measures should be taken where nitrification inhibitors are being used to decrease direct N2O emissions, to enable effective and viable climate change mitigation.
Acknowledgements
This work was supported by the BIP reinvestment funds of the Faculty of Veterinary and Agricultural Sciences of the University of Melbourne, the Australia-China Joint Research Centre jointly funded by Australian Government Department of Industry and Science and the Chinese Ministry of Science and Technology.




