Department of Microbial Ecology, Netherlands Institute of Ecology (NIOO-KNAW), Droevendaalsesteeg 10, 6708, PB Wageningen, The Netherlands.
Max Planck Institute for Terrestrial Microbiology, Karl-von-Frisch Straβe 10, D-35043, Marburg, Germany.
Glob Chang Biol. 2015 Oct;21(10):3864-79. doi: 10.1111/gcb.12974. Epub 2015 Jun 27.
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 2 months. 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.
为了满足全球对粮食、饲料和生物能源的需求,农业必须加强投入,将更多的碳化合物(残留物)重新投入农业系统,以防止土壤质量和肥力下降。然而,农业集约化会降低土壤对甲烷的吸收能力,从而减少甚至丧失甲烷汇的功能。与湿地农业土壤(稻田)相比,好氧农业土壤中的甲烷氧化潜能受到的关注较少,这可能是由于预计这些土壤的甲烷吸收能力较低或可以忽略不计。因此,仍然缺乏一项详细的研究来验证或反驳这一假设。作为一种典型的农业实践,我们确定了生物基残留物应用对土壤甲烷通量的影响,并确定了甲烷氧化潜能,包括对残留物添加后 2 个月内甲烷氧化菌群的定性(诊断微阵列)和定量(特定 qPCR 分析)分析。出乎意料的是,在特定残留物添加后,我们通过甲烷通量测量和甲烷氧化测定都检测到甲烷吸收的显著瞬时刺激。这种刺激显然是细胞特异性活性诱导的结果,而不是甲烷氧化菌种群的生长。尽管是短暂的,但这种增强的甲烷吸收可抵消在培养过程中排放的总气态 CO2 的 16%。甲烷氧化菌群主要由 Methylosinus 组成,有利于农业土壤中的甲烷氧化。虽然农业土壤通常被认为是甲烷的净源或相对较弱的甲烷汇,但我们的结果表明,甲烷氧化速率可以被刺激,从而导致更高的土壤甲烷吸收。因此,即使农业对土壤甲烷吸收产生不利影响,实施精心设计的管理策略(例如重复应用特定残留物)也可能补偿土地利用变化后甲烷汇功能的丧失。