An Exploration of N2O Emission from Soils and the Role of Biochar in its Mitigation
Nitrous oxide (N2O) is a potent greenhouse gas (IPCC 2013) and is now the most significant contributor to the depletion of stratospheric ozone (Ravishankara et al. 2009). Its atmospheric concentration has increased by 20 % since the mid-19th century, most particularly since the production of synthetic nitrogen (N) fertilisers began, upon which modern agriculture which is highly dependent. Consequently the limiting of agricultural N2O emissions is of great importance. Biochar – charcoal made by the pyrolysis of biomass – has been shown capable of reducing N2O emissions when incorporated into soil (Cayuela et al. 2014; Lehmann and Joseph 2015). This Ph.D. study was undertaken to examine the mechanisms related to the production and movement of N2O in soil and whether, and by what means, biochar addition to soil might mitigate N2O emissions.
In all experiments the biochar (BC) used was made, at a highest treatment temperature of 550 oC, from the woody residue of oil mallee trees (E. Polybractea) after steam extraction of eucalypt oil. In each experiment the BC was mixed with soil(s) at rates of 0 %, 1 % and 5 % (w/w). One experiment used x-ray computed tomography, at a resolution of 70 μm, to examine the effect on soil structure resulting from the addition of BC to samples of an Arenosol, a Ferralsol and a Vertisol. For each soil bulk density (BD) decreased with increasing biochar content. Significant increases were found in porosity, pore connectivity and mean pore radius with addition of 5 % BC to the Vertisol and Ferralsol. The 1 % BC amendments produced no significant changes in those soils. Over a 15-month incubation at high moisture content the Ferralsol containing 5 % BC showed significant temporal changes in porosity, pore connectivity, mean pore radius and fractal dimension (FD) – the increase in FD suggesting greater pore space homogeneity. These changes suggested biochar-soil interactions, possibly related to reactive clay minerals and/or microbial activity. Amendment of the Arenosol with both 1 % and 5 % BC resulted in significant increases in pore connectivity and mean pore radius. A significant temporal increase in pore connectivity resulted from the 5 % amendment. Addition of BC significantly decreased the rate of water loss through evaporation and drainage of all incubated soils, reduced volumetric water content at field capacity in the two clay-rich soils and increased the available water content (– 0.01 to –1.5 MPa) of the Arenosol by 20 % (Chapter 2 and Quin et al. 2014).
In a laboratory experiment the Ferralsol, containing the BC as before, was repacked into PVC columns of 37 mm internal diameter (ID), sealed and incubated at 3 water regimes (12 %, 39 % and 54 % water-filled pore space (WFPS)) following gamma irradiation to render the contents abiotic. After N2O was injected at the base of the soil column, in the 0 % BC control 100 % of injected N2O was released into the headspace, declining to 67% in the 5% amendment. In a 100 % BC column at 6 % WFPS, only 16 % of the expected N2O was released. X-ray photoelectron spectroscopy identified changes in BC surface functional groups from the 5 % amendment that suggested reactions between N2O and the carbon matrix upon exposure to N2O. Scanning transmission electron microscopy showed formation of an organomineral layer coating an external surface of a BC particle from that group. With increasing rates of BC application, higher pH adjusted redox potentials were observed at the lower water contents. Evidence suggested that the BC from soil had taken part in redox reactions, reducing N2O to dinitrogen (N2), in addition to adsorption of N2O in (at least) the 100 % BC columns (Chapter 3 and Quin et al. 2015).
A field trial was established in north-eastern New South Wales, with the same Ferralsol repacked into PVC columns of 240 mm ID and 585 mm in height (Chapters 4 and 5). The columns were installed vertically in the ground, save for the top, soil-free 50 mm. The upper 100 mm of soil contained BC at dosage rates as before. Each column had a removable airtight cap for headspace gas sampling and silicone tubing installed at three depths for the sampling of soil gas content by diffusion. The columns were also fitted with ceramic cup lysimeters at two depths for the sampling of soil water, and thin tubes for the injection of liquid fertiliser at a depth of either 75 mm or 200 mm. With five replicates of each design (BC dosage rate and injection depth: 3×2×5 = 30) and five controls the central column of the 7×5 grid was fitted with soil moisture and temperature sensors. Three months after installation the trial commenced (on Day 0) when columns were injected with 62.8 % 15N potassium nitrate (1.68 g 15N-KNO3) at one of the two depths. Nine days prior to injection soil water contained mostly undetectable quantities of ammonium (all < 0.05 mg L-1 ) and those of native nitrate (NO3 -) ranged from 2.2 to 120 mg L-1 , so it was assumed that denitrification would effectively be the sole pathway of N2O production through reduction of NO3 -. Following persistent rainfall in-soil concentrations of N2O rose by approximately 2 orders of magnitude as soil WFPS increased to > 80 % on Day 10. This coincided with periods of high hydraulic conductivity, equivalent to drainage of 13.0 L m-2 h -1 . Drained at that rate the downward carriage of (calculated) dissolved excess 15N-N2O (15N2O) in 75 mm and 200 mm injected columns containing 0 % BC would be respectively 189 and 30 times the surface fluxes on that day. Such drainage of dissolved N2O suggests that offsite transport of N2O by leaching from some soils may be greatly underestimated, and could possibly explain some of the discrepancy between ‘top down’ estimates of emissions of N2O of ~ 4 % of applied N (Smith et al. 2012) and the Intergovernmental Panel on Climate Change’s (IPCC) default ‘bottom up’ estimate of ~ 1.3 %.
Throughout the trial no emitted excess 15N2 was detected, although some was detected within the soil, indicating that some full denitrification had occurred. For each depth of NO3 - injection there were no significant differences in relation to biochar content of surface fluxes of N2O on any day of measurement, nor of their cumulative emissions during the 89 day period of the trial. Total emissions of 15N2O for all biochar contents (0, 1 and 5 %, n = 15) of 75 mm and 200 mm injected columns for Days 1–23 (after which emissions were minimal) were respectively 9.74 mg 15N-N2O m-2 and a significantly lower (p = 0.0002) 1.60 mg 15N-N2O m-2 – corresponding to 0.46 % and 0.075 % respectively of total N denitrified from 14+15NO3 - injected and below the IPCC default of 1 % for direct emissions. The effect of deeper fertiliser placement on indirect emissions remains unclear as, while there was considerable leaching of 15NO3 -from all columns, it was greater from those injected at 200 mm and its fate undetermined.
In summary, the possible and hitherto unrecognised drainage of significant quantities of dissolved N2O from some soils would seem to warrant further study. Overall, amendment with the eucalypt BC clearly affected soil structure. While the BC lowered N2O emissions from Ferralsol in the laboratory, through both adsorption and redox reactions, it was plainly ineffective in lowering emissions in the field. It is apparent that there may not be a single explanation for this outcome – the activity of field soil biota, the acidity of the Ferralsol, the weathering of the BC and greater variability of conditions in the field being factors possibly contributing to the difference. This emphasises the need for further field trials of biochars to determine their effectiveness in mitigating N2O emissions, their effect on N cycling in soil, and the longevity of any effects prior to their widespread use.
Oil mallee biochar improves soil structural properties - A study with x-ray micro-CT
Employing x-ray computed tomography (μ-CT), we examined the impact of an oil mallee (OM) biochar, at concentrations of 0%, 1% and 5% (w/w), on soil structural traits in three soil types (Vertisol, Ferralsol and Arenosol). The biochar was pyrolysed at a maximum temperature of 550°C, sieved to between 250 μm and 2 mm prior to amending the soils, had an internal porosity of 75% (v/v) and an organic carbon (Corg) content of 60%. Soil structure was quantified, at a resolution of 70 μm, by measuring μ-CT porosity, mean pore radius, fractal dimension and connectivity of the pore space. Addition of 5% OM biochar resulted in higher μ-CT porosity (i.e. ≥70 μm) in the Vertisol (p < 0.001), averaging 7.5, 9.1 and 13.4%, respectively, for 0, 1 and 5% biochar, with the Ferralsol having corresponding μ-CT porosities of 6.2, 6.5 and 10.9%, the difference also being significant (p = 0.03) for 5% OM biochar amendment. Significant increases (p < 0.05) in connectivity of the largest pore and mean pore radius were observed in all three soils containing 5% OM biochar and also in the Arenosol with 1% OM biochar. Over a 15-month incubation the Ferralsol containing 5% OM biochar showed increased μ-CT porosity (p < 0.05) and fractal dimension (p < 0.05), the latter indicating greater homogeneity of pore space distribution. Addition of OM biochar significantly decreased the rate of water loss through evaporation and drainage of all incubated soils (p < 0.05) and reduced volumetric water content at field capacity in the two clay-rich soils. Soil with 1% OM biochar showed an increase in the rate of drainage in the Vertisol (p < 0.05 at −0.02 MPa) and a 20% increase in the available water content of the Arenosol (p < 0.05). It is hypothesised that the highly porous structure of biochar may have contributed to the changed water retention characteristics of the soils. This study highlights the potential for OM biochar to modify the structural characteristics of contrasting soils.