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Unexpected stimulation of soil methane uptake as emergent property of agricultural soils following bio-based residue application

机译:施用生物基残留物后,土壤甲烷吸收的意外刺激成为农业土壤的发芽特性

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摘要

Intensification of agriculture to meet the global food, feed, and bioenergy demand entail increasing re-investment of carbon compounds (residues) into agro-systems to prevent decline of soil quality and fertility. However, agricultural intensification decreases soil methane uptake, reducing, and even causing the loss of the methane sink function. In contrast to wetland agricultural soils (rice paddies), the methanotrophic potential in well-aerated agricultural soils have received little attention, presumably due to the anticipated low or negligible methane uptake capacity in these soils. Consequently, a detailed study verifying or refuting this assumption is still lacking. Exemplifying a typical agricultural practice, we determined the impact of bio-based residue application on soil methane flux, and determined the methanotrophic potential, including a qualitative (diagnostic microarray) and quantitative (group-specific qPCR assays) analysis of the methanotrophic community after residue amendments over 2months. Unexpectedly, after amendments with specific residues, we detected a significant transient stimulation of methane uptake confirmed by both the methane flux measurements and methane oxidation assay. This stimulation was apparently a result of induced cell-specific activity, rather than growth of the methanotroph population. Although transient, the heightened methane uptake offsets up to 16% of total gaseous CO2 emitted during the incubation. The methanotrophic community, predominantly comprised of Methylosinus may facilitate methane oxidation in the agricultural soils. While agricultural soils are generally regarded as a net methane source or a relatively weak methane sink, our results show that methane oxidation rate can be stimulated, leading to higher soil methane uptake. Hence, even if agriculture exerts an adverse impact on soil methane uptake, implementing carefully designed management strategies (e.g. repeated application of specific residues) may compensate for the loss of the methane sink function following land-use change.
机译:为了满足全球粮食,饲料和生物能源需求,农业集约化需要增加碳化合物(残留物)对农业系统的再投资,以防止土壤质量和肥力下降。但是,农业集约化会降低土壤对甲烷的吸收,从而减少甚至导致甲烷吸收功能的丧失。与湿地农业土壤(稻田)相比,通气良好的农业土壤中的甲烷营养潜力很少受到关注,这可能是由于这些土壤中甲烷的吸收能力较低或可忽略不计。因此,仍然缺乏详细的研究来证实或驳斥这一假设。作为典型的农业实践的例证,我们确定了生物基残留物施用对土壤甲烷通量的影响,并确定了甲烷营养缺陷的潜力,包括对残留后甲烷营养缺陷群落的定性(诊断性微阵列)和定量分析(特定于组的qPCR分析)超过2个月的修订。出乎意料的是,在对特定残基进行修正后,我们检测到了甲烷吸收的显着瞬时刺激,这是通过甲烷通量测量和甲烷氧化测定来证实的。这种刺激显然是诱导的细胞特异性活性的结果,而不是甲烷营养菌种群的增长。尽管是短暂的,但提高的甲烷吸收量最多可抵消孵育过程中排放的总气态CO2的16%。甲烷营养群落主要由甲基肌苷组成,可促进农业土壤中的甲烷氧化。虽然通常将农业土壤视为甲烷的净来源或相对较弱的甲烷汇,但我们的研究结果表明,可以提高甲烷的氧化速率,从而导致更高的土壤甲烷吸收量。因此,即使农业对土壤甲烷的吸收产生不利影响,实施精心设计的管理策略(例如重复施用特定的残留物)也可以弥补土地用途变化后甲烷吸收功能的丧失。

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