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Greenhouse gas emissions from intensive pasture on ferrosol in Northern NSW, Australia: Impact of biochar amendment

机译:澳大利亚北北方北约斯北部菲克兰强烈牧场的温室气体排放:生物炭修正案的影响

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An intensive field campaign was performed from April to June 2009 to assess the effect of biochar amendment on the emission of soil-borne GHGs from a sub-tropical pasture on acidic ferrosol. Over the whole measurement period high emissions of N_2O andhigh fluxes of CO_2 could be observed, whereas a net uptake of CH_4 was measured. Only small differences in the fluxes of N_2O and CH4 from the biochar amended plots (35.33 ± 4.83 mug N_2O-N/m~2/h, -6.76 ± 0.20 ug CH4 -C/m~2/h) vs. the control plots (31.08 ± 3.50 mug N_2O-N/m~2/h, -7.30 ± 0.19 ug CHU-C/m~2/h) could be observed, while there was no significant difference in the fluxes of CO_2. However, it could be observed that N_2O emissions were significantly lower from the biochar amended plots during periods with low emission rates (< 50 mug N_2O-N/m~2/h). Only during an extremely high emission event following heavy rainfall N_2O emissions from the biochar amended plots were higher than from the control plots. Our results demonstrate that pastures on ferrosols in Northern NSW are a significant source of GHG and that the amendment of biochar can alter those emissions. However, more field and laboratory incubation studies covering prolonged observation periods are needed to clarify the impact ofbiochar amendment on soil microbial processes and the emission of soil-borne GHGs.
机译:从四月进行,以2009年6月的密集领域活动,以评估生物炭修正土传温室气体从酸性ferrosol亚热带牧草排放的效果。过N_2O andhigh CO_2的通量的整个测量周期高排放,可观察到,而CH_4的净吸收进行测定。仅在N_2O和CH4的通量小的差异从所述生物炭修正图(35.33±4.83杯N_2O-N /米〜2 /小时,-6.76±0.20微克CH4 -C /米〜2 /小时)相对于对照地块(31.08±3.50杯N_2O-N /米〜2 /小时,-7.30±0.19微克CHU-C /米〜2 /小时),可以观察到,虽然有在CO_2的磁通没有显著差异。然而,可以观察到,N_2O排放量显著从生物炭修正曲线中具有低发射率(<50杯N_2O-N /米〜2 / h)的周期降低。只有遵循来自生物炭修改地块暴雨N_2O排放量极高的发射活动期间比从对照地块高。我们的研究结果表明,在新南威尔士州北部牧场红壤温室气体是一个显著源,生物炭的修正可以改变这些排放。然而,需要覆盖延长观察期多个现场和实验室培养研究阐明ofbiochar修正案对土壤微生物流程的影响和土壤传播的温室气体的排放。

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