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Environment

N2O emissions during the freezing and thawing periods from six fields in a livestock farm, southern Hokkaido, Japan

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Pages 261-271 | Received 29 Aug 2011, Accepted 25 Feb 2012, Published online: 24 Apr 2012

Figures & data

Table 1. Nitrous oxide (N2O) emissions during the winter and cropping periods and N2O losses during the winter period for the investigated experiments

Table 2. Soil properties at 0–100 mm depth at the study site in Shizunai Experimental Livestock Farm

Table 3. Slurry and manure application after the cropping season and nitrogen (N) surplus in 2004 at the study site in Shizunai Experimental Livestock Farm. Slurry was applied on 19 October 2004 and manure was applied on 1 November 2004

Figure 1. Temporal variability of precipitation observed at the Sasayama Weather Station in the Shizunai Experimental Livestock Farm, and air temperature and snow depth observed at the Shizunai Experimental Station, from December 2004 to April 2005.

Figure 1. Temporal variability of precipitation observed at the Sasayama Weather Station in the Shizunai Experimental Livestock Farm, and air temperature and snow depth observed at the Shizunai Experimental Station, from December 2004 to April 2005.

Figure 2. Temporal variability of (a) soil temperature at 50 mm depth, (b) nitrous oxide (N2O) flux, (c) nitric oxide (NO) flux, (d) N2O-N/NO-N ratio, and (e) N2O concentration in soil with soil freezing depths at one cornfield (C2) and three grasslands (CG [converted from a cornfield in 2003], G2 [including G2s, G2c and G2n], and G3) from December 2004 to April 2005. The lines in e) indicate the edge of the frozen soil layers and the soil between the lines froze.

Figure 2. Temporal variability of (a) soil temperature at 50 mm depth, (b) nitrous oxide (N2O) flux, (c) nitric oxide (NO) flux, (d) N2O-N/NO-N ratio, and (e) N2O concentration in soil with soil freezing depths at one cornfield (C2) and three grasslands (CG [converted from a cornfield in 2003], G2 [including G2s, G2c and G2n], and G3) from December 2004 to April 2005. The lines in e) indicate the edge of the frozen soil layers and the soil between the lines froze.

Figure 3. Ammonium-nitrogen (-N), nitrate-nitrogen (-N), and dissolved organic carbon (DOC) concentrations in soil at a 0−50 mm depth at the research sites in the Shizunai Experimental Livestock Farm. Measurements were carried out on 8th (C2, CG and G3) or 18th (G2s, G2c, and G2n) December 2004 before soil freezing, on 31st March 2005 just after the start of soil thawing, and on 19th April 2005 at the end of the thawing period. Paired t-test was used to test for statistically significant differences between the data observed on 8th Dec 2004 and 19th April 2005 for each site. Levels of significance were as follows: *<0.05, **<0.01, ***<0.001.

Figure 3. Ammonium-nitrogen (-N), nitrate-nitrogen (-N), and dissolved organic carbon (DOC) concentrations in soil at a 0−50 mm depth at the research sites in the Shizunai Experimental Livestock Farm. Measurements were carried out on 8th (C2, CG and G3) or 18th (G2s, G2c, and G2n) December 2004 before soil freezing, on 31st March 2005 just after the start of soil thawing, and on 19th April 2005 at the end of the thawing period. Paired t-test was used to test for statistically significant differences between the data observed on 8th Dec 2004 and 19th April 2005 for each site. Levels of significance were as follows: *<0.05, **<0.01, ***<0.001.

Table 4. Nitrous oxide (N2O) and N2O + dinitrogen (N2) fluxes and N2O/(N2O+N2) ratio measured by denitrification enzyme activity in soils collected from the study site at Shizunai Experimental Livestock Farm just after the soil thawing on 31 March 2005

Supplemental material

tssp_a_670810_sup_25267154.pdf

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