Short term N2O, CH4 and CO2 production from soil sampled at different depths and amended with a fine sized slurry fraction

Seasonal and soil-type dependent emissions of nitrous oxide from irrigated desert soils amended with digested poultry manures

Expansion of dryland agriculture requires intensive supplement of organic fertilizers to improve the fertility of nutrient-poor desert soils. The environmental impact of organic supplements in hot desert climates is not well understood. We report on seasonal emissions of nitrous oxide (N₂O) from sand and loess soils, amended with limed and non-limed anaerobic digestate of poultry manure in the Israeli Negev desert. All amended soils had substantially higher N₂O emissions, particularly during winter applications, compared to unammended soils. Winter emissions from amended loess (10-175mgN₂Om^-2day^-1) were markedly higher than winter emissions from amended sand (2-7mgN₂Om^-2day^-1). Enumeration of marker genes for nitrification and denitrification suggested that both have contributed to N₂O emissions according to prevailing environmental conditions. Lime treatment of digested manure inhibited N₂O emissions regardless of season or soil type, thus reducing the environmental impact of amending desert soils with manure digestate.

Priming of soil carbon decomposition in two Inner Mongolia grassland soils following sheep dung addition: a study using ¹³C natural abundance approach

To investigate the effect of sheep dung on soil carbon (C) sequestration, a 152 days incubation experiment was conducted with soils from two different Inner Mongolian grasslands, i.e. a Leymus chinensis dominated grassland representing the climax community (2.1% organic matter content) and a heavily degraded Artemisia frigida dominated community (1.3% organic matter content). Dung was collected from sheep either fed on L. chinensis (C₃ plant with δ¹³C = −26.8‰; dung δ¹³C = −26.2‰) or Cleistogenes squarrosa (C₄ plant with δ¹³C = −14.6‰; dung δ¹³C = −15.7‰). Fresh C₃ and C₄ sheep dung was mixed with the two grassland soils and incubated under controlled conditions for analysis of ¹³C-CO₂ emissions. Soil samples were taken at days 17, 43, 86, 127 and 152 after sheep dung addition to detect the δ¹³C signal in soil and dung components. Analysis revealed that 16.9% and 16.6% of the sheep dung C had decomposed, of which 3.5% and 2.8% was sequestrated in the soils of L. chinensis and A. frigida grasslands, respectively, while the remaining decomposed sheep dung was emitted as CO₂. The cumulative amounts of C respired from dung treated soils during 152 days were 7–8 times higher than in the un-amended controls. In both grassland soils, ca. 60% of the evolved CO₂ originated from the decomposing sheep dung and 40% from the native soil C. Priming effects of soil C decomposition were observed in both soils, i.e. 1.4 g and 1.6 g additional soil C kg⁻¹ dry soil had been emitted as CO₂ for the L. chinensis and A. frigida soils, respectively. Hence, the net C losses from L. chinensis and A. frigida soils were 0.6 g and 0.9 g C kg⁻¹ soil, which was 2.6% and 7.0% of the total C in L. chinensis and A. frigida grasslands soils, respectively. Our results suggest that grazing of degraded Inner Mongolian pastures may cause a net soil C loss due to the positive priming effect, thereby accelerating soil deterioration.

Greenhouse gas (GHG) emissions from soils amended with digestate derived from anaerobic treatment of food waste

RATIONALE

The application of organic materials to agricultural lands is considered good practice to improve soil organic matter content and recycle nutrients for crop growth. The anaerobic treatment of food waste may have environmental benefits, particularly with regard to greenhouse gases (GHGs) mitigation and enhancement of carbon sequestration.

METHODS

This work presents the results from a field experiment to evaluate CO(2) , CH(4) and N(2) O emissions from grassland amended with digestate produced by anaerobic fermentation of food waste. Experimental plots, located close to Rothamsted Research-North Wyke, were established using a randomized block design with three replicates and two treatments, added digestate (DG) and the unamended control (CNT). The digestate was applied on three occasions at an equivalent rate of 80 kg N ha(-1) .

RESULTS

The application of digestate led to an increase in CO(2) emissions, especially after the 2(nd) application (74.1 kg CO(2) -C ha(-1)  day(-1) ) compared with the CNT soil (36.4 kg CO(2) -C ha(-1)  day(-1) ), whereas DG treatment did not affect the overall CH(4) and N(2) O emissions. The total grass yield harvested on a dry matter basis was greater in the DG treated plots (0.565 kg m(-2) ) than in the CNT plots (0.282 kg m(-2) ), as was the (15)  N content in the harvest collected from the DG plots.

CONCLUSIONS

The results suggest that the digestate can be applied to agricultural land as a fertilizer to grow crops. Our study was conducted in an exceptionally dry growing season, so conclusions about the effect of digestate on GHG emissions should take this into account, and further field trials conducted under more typical growing seasons are needed.