Soluble organic carbon and carbon dioxide fluxes in maize fields receiving spring-applied manure

E.G. Gregorich, P. Rochette, S. McGuire, B.C. Liang, R. Lessard

    Research output: Contribution to journalArticleAcademicpeer-review

    90 Citations (Scopus)

    Abstract

    More than 19 million Mg of dairy manure are produced annually in the Canadian provinces of Quebec and Ontario, and most of it is spread on agricultural fields. Quantitative information on the impact of manure management practices on levels of soluble organic carbon (SOC) and emissions of CO 2 is important for assessing whether this management significantly contributes to increasing atmospheric CO 2 concentrations. The objective of this study was to measure the effects of dairy cattle manure (applied at 0, 56, and 112 Mg ha -1) on SOC levels in, and soil surface CO 2 fluxes from, a typical maize (Zea mays L.) field in central Canada, from April to October. The higher rate of manure increased both the CO 2 emissions and the SOC levels by a factor of two to three compared with the control. Fluxes of CO 2 were very low immediately after thaw, increased sharply following manure application and increased again in mid-June at the time when temperature and sort moisture increased; thereafter, fluxes declined throughout the rest of the season. Over the season, which was drier than normal, SOC was not a good predictor of CO 2 flux. Carbon dioxide flux increased proportionately less for the second 56 Mg ha -1 increment of manure added than for the first increment. Factors other than the quantity of SOC limited soil respiration at the highest manure application rate. Carbon dioxide is contributed to the atmosphere at a lower rate, and proportionately more manure C is retained in soil with increasing levels of manure applied.
    Original languageEnglish
    Pages (from-to)209-214
    JournalJournal of Environmental Quality
    Volume27
    Issue number1
    Publication statusPublished - 1998

    Fingerprint

    Manures
    Organic carbon
    manure
    Carbon dioxide
    carbon dioxide
    maize
    organic carbon
    Fluxes
    Dairies
    Soils
    soil respiration
    cattle
    management practice
    soil surface
    Moisture
    moisture
    atmosphere

    Cite this

    Gregorich, E. G., Rochette, P., McGuire, S., Liang, B. C., & Lessard, R. (1998). Soluble organic carbon and carbon dioxide fluxes in maize fields receiving spring-applied manure. Journal of Environmental Quality, 27(1), 209-214.
    Gregorich, E.G. ; Rochette, P. ; McGuire, S. ; Liang, B.C. ; Lessard, R. / Soluble organic carbon and carbon dioxide fluxes in maize fields receiving spring-applied manure. In: Journal of Environmental Quality. 1998 ; Vol. 27, No. 1. pp. 209-214.
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    abstract = "More than 19 million Mg of dairy manure are produced annually in the Canadian provinces of Quebec and Ontario, and most of it is spread on agricultural fields. Quantitative information on the impact of manure management practices on levels of soluble organic carbon (SOC) and emissions of CO 2 is important for assessing whether this management significantly contributes to increasing atmospheric CO 2 concentrations. The objective of this study was to measure the effects of dairy cattle manure (applied at 0, 56, and 112 Mg ha -1) on SOC levels in, and soil surface CO 2 fluxes from, a typical maize (Zea mays L.) field in central Canada, from April to October. The higher rate of manure increased both the CO 2 emissions and the SOC levels by a factor of two to three compared with the control. Fluxes of CO 2 were very low immediately after thaw, increased sharply following manure application and increased again in mid-June at the time when temperature and sort moisture increased; thereafter, fluxes declined throughout the rest of the season. Over the season, which was drier than normal, SOC was not a good predictor of CO 2 flux. Carbon dioxide flux increased proportionately less for the second 56 Mg ha -1 increment of manure added than for the first increment. Factors other than the quantity of SOC limited soil respiration at the highest manure application rate. Carbon dioxide is contributed to the atmosphere at a lower rate, and proportionately more manure C is retained in soil with increasing levels of manure applied.",
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    Gregorich, EG, Rochette, P, McGuire, S, Liang, BC & Lessard, R 1998, 'Soluble organic carbon and carbon dioxide fluxes in maize fields receiving spring-applied manure', Journal of Environmental Quality, vol. 27, no. 1, pp. 209-214.

    Soluble organic carbon and carbon dioxide fluxes in maize fields receiving spring-applied manure. / Gregorich, E.G.; Rochette, P.; McGuire, S.; Liang, B.C.; Lessard, R.

    In: Journal of Environmental Quality, Vol. 27, No. 1, 1998, p. 209-214.

    Research output: Contribution to journalArticleAcademicpeer-review

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    AB - More than 19 million Mg of dairy manure are produced annually in the Canadian provinces of Quebec and Ontario, and most of it is spread on agricultural fields. Quantitative information on the impact of manure management practices on levels of soluble organic carbon (SOC) and emissions of CO 2 is important for assessing whether this management significantly contributes to increasing atmospheric CO 2 concentrations. The objective of this study was to measure the effects of dairy cattle manure (applied at 0, 56, and 112 Mg ha -1) on SOC levels in, and soil surface CO 2 fluxes from, a typical maize (Zea mays L.) field in central Canada, from April to October. The higher rate of manure increased both the CO 2 emissions and the SOC levels by a factor of two to three compared with the control. Fluxes of CO 2 were very low immediately after thaw, increased sharply following manure application and increased again in mid-June at the time when temperature and sort moisture increased; thereafter, fluxes declined throughout the rest of the season. Over the season, which was drier than normal, SOC was not a good predictor of CO 2 flux. Carbon dioxide flux increased proportionately less for the second 56 Mg ha -1 increment of manure added than for the first increment. Factors other than the quantity of SOC limited soil respiration at the highest manure application rate. Carbon dioxide is contributed to the atmosphere at a lower rate, and proportionately more manure C is retained in soil with increasing levels of manure applied.

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