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Soil greenhouse gas fluxes and global warming potential in four high-yielding maize systems

机译:四种高产玉米系统的土壤温室气体通量和全球变暖潜力

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Crop intensification is often thought to increase greenhouse gas (GHG) emissions, but studies in which crop management is optimized to exploit crop yield potential are rare. We conducted a field study in eastern Nebraska, USA to quantify GHG emissions, changes in soil organic carbon (SOC) and the net global warming potential (GWP) in four irrigated systems: continuous maize with recommended best management practices (CC-rec) or intensive management (CC-int) and maize-soybean rotation with recommended (CS-rec) or intensive management (CS-int). Grain yields of maize and soybean were generally within 80-100% of the estimated site yield potential. Large soil surface carbon dioxide (CO2) fluxes were mostly associated with rapid crop growth, high temperature and high soil water content. Within each crop rotation, soil CO2 efflux under intensive management was not consistently higher than with recommended management. Owing to differences in residue inputs, SOC increased in the two continuous maize systems, but decreased in CS-rec or remained unchanged in CS-int. N2O emission peaks were mainly associated with high temperature and high soil water content resulting from rainfall or irrigation events, but less clearly related to soil NO3-N levels. N2O fluxes in intensively managed systems were only occasionally greater than those measured in the CC-rec and CS-rec systems. Fertilizer-induced N2O emissions ranged from 1.9% to 3.5% in 2003, from 0.8% to 1.5% in 2004 and from 0.4% to 0.5% in 2005, with no consistent differences among the four systems. All four cropping systems where net sources of GHG. However, due to increased soil C sequestration continuous maize systems had lower GWP than maize-soybean systems and intensive management did not cause a significant increase in GWP. Converting maize grain to ethanol in the two continuous maize systems resulted in a net reduction in life cycle GHG emissions of maize ethanol relative to petrol-based gasoline by 33-38%. Our study provided evidence that net GHG emissions from agricultural systems can be kept low when management is optimized toward better exploitation of the yield potential. Major components for this included (i) choosing the right combination of adopted varieties, planting date and plant population to maximize crop biomass productivity, (ii) tactical water and nitrogen (N) management decisions that contributed to high N use efficiency and avoided extreme N2O emissions, and (iii) a deep tillage and residue management approach that favored the build-up of soil organic matter from large amounts of crop residues returned.
机译:人们通常认为,集约化种植会增加温室气体的排放量,但很少有研究对作物管理进行了优化,以利用作物的单产潜力。我们在美国内布拉斯加州东部进行了田野研究,以量化四种灌溉系统的温室气体排放量,土壤有机碳(SOC)和全球温室效应净值(GWP)的变化:采用推荐的最佳管理实践的连续玉米(CC-rec)或推荐的集约化管理(CC-int)和玉米-大豆轮作(CS-rec)或集约化管理(CS-int)。玉米和大豆的谷物单产通常在估计的单产潜力的80-100%之内。土壤表层二氧化碳(CO2)通量大与作物快速生长,高温和土壤含水量高有关。在每次轮作中,集约化管理下的土壤CO2流出量始终不高于推荐管理下的水平。由于残留物输入的差异,两个连续玉米系统中的SOC均增加,但CS-rec中的SOC降低,或CS-int中的SOC保持不变。 N2O排放峰值主要与降雨或灌溉事件导致的高温和高土壤水分有关,但与土壤NO3-N水平的关系不太明显。在集约化管理系统中,N2O通量仅偶尔大于CC-rec和CS-rec系统中测得的N2O通量。肥料引起的N2O排放量在2003年为1.9%至3.5%,在2004年为0.8%至1.5%,在2005年为0.4%至0.5%,这四个系统之间没有一致的差异。所有四个种植系统均产生温室气体。但是,由于土壤固碳增加,连续玉米系统的全球升温潜能值低于玉米-大豆系统,而集约化管理并未导致全球升温潜能值显着增加。在两个连续的玉米系统中将玉米籽粒转化为乙醇,相对于汽油汽油,玉米乙醇的生命周期温室气体排放净减少了33-38%。我们的研究提供了证据,表明当优化管理以更好地利用单产潜力时,可以将农业系统的净温室气体排放量保持在较低水平。这样做的主要组成部分包括(i)选择采用的品种,播种日期和植物种群的正确组合以最大程度地提高作物生物量生产力;(ii)战术水和氮(N)管理决策,这些决策有助于提高氮的利用效率并避免极端的N2O排放;以及(iii)深耕和残留管理方法,该方法有利于从大量返回的农作物残留物中积累土壤有机质。

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