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Microbial ecology and carbon and nitrogen dynamics in agroecosystems.

机译:农业生态系统中的微生物生态学和碳氮动态。

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Soil C sequestration in agricultural ecosystems is an immediate and significant option to mitigate the increase in the atmospheric CO2 concentration. The objectives of this study were to determine (1) the influence of crop and soil management practices applicable to Kansas (i.e., tillage, N fertilization, and crop rotations) on soil C and N, C sequestration rates, soil aggregation and aggregate-associated C and N; and (2) the influence of long-term tillage practices on SOC and total N, soil aggregation and aggregate-associated C and N in three soil types: an Oxisol (Brazil), a Vertisol (Argentina), and a Mollisol (Kansas, USA). The Kansas experiments included: tillage (conventional tillage (CT), reduced tillage (RT) and no-tillage (NT)) and native prairie; nitrogen (N) fertilization rates; and crop rotations comprising various combinations of winter wheat (Triticum aestivum L.), grain sorghum ( Sorghum bicolor L. Moench), and soybean (Glycine max L. Merrill ). The presence of a fallow period negatively affected C sequestration rates even under NT systems. Nitrogen fertilization generally increased C sequestration rates. Rotations that contained wheat or sorghum had the greatest C sequestration rates while continuous soybean had the lowest rates. Cultivation decreased the amount of macroaggregates with a concomitment increased in the amount of microaggregates. Wheat and sorghum increased total C in the macroaggregate fraction (>250 mum) under NT while soybean had the lowest C concentration. Cultivation reduced microbial biomass C and N and potentially mineralizable C and N. The combination of conservation tillage and rotations that produced a greater amount of residue had greater C sequestration rates. In the Oxisol, NT had greater amounts of large macroaggregates (>2000 mum) than CT, however no differences between tillage practices were detected in the Vertisol and Mollisol. Cultivation of native grassland reduced the amount of macroaggregates and the associated C and N concentration; however NT tended to be more similar to the native grassland. Overall, our results indicated that the use of conservation tillage could be an important strategy to sequester C in these agroecosystems. The adoption of management practices that enhance C sequestration would be important for reducing GHGs emissions and maintaining the sustainability of agricultural systems.
机译:农业生态系统中的固碳是减轻大气中二氧化碳浓度增加的直接而重要的选择。这项研究的目的是确定(1)适用于堪萨斯州的作物和土壤管理措施(例如耕作,氮肥和作物轮作)对土壤碳和氮,碳固存率,土壤聚集和与团聚体相关的影响C和N; (2)长期耕作对三种土壤类型的SOC和总氮,土壤团聚体以及与团聚体相关的C和N的影响:三种土壤类型:Oxisol(巴西),Vertisol(阿根廷)和Mollisol(堪萨斯州,美国)。堪萨斯州的实验包括:耕种(常规耕种(CT),减耕(RT)和免耕(NT))和本地草原;氮(N)的施肥率;作物轮作包括冬小麦(Triticum aestivum L.),高粱(Sorghum bicolor L. Moench)和大豆(Glycine max L. Merrill)的各种组合。休耕期的存在即使在NT系统下也对碳固存率产生负面影响。氮肥通常会增加固碳速率。含有小麦或高粱的轮作的固碳速率最高,而连续大豆的固碳速率最低。耕作减少了大骨料的数量,随之而来的是微骨料的数量增加。在NT下,小麦和高粱的总碳含量增加(> 250 mum),而大豆的C含量最低。耕作减少了微生物的生物量碳和氮以及可能矿化的碳和氮。保护性耕作和轮作的组合产生更多的残留物,其碳固存率更高。在Oxisol中,NT比CT具有更多的大型大团聚体(> 2000微米),但是在Vertisol和Mollisol中没有发现耕作方式之间的差异。耕种天然草原减少了大团聚体的数量以及相关的碳和氮浓度。但是新台币往往更类似于当地的草原。总体而言,我们的结果表明,保护性耕作的使用可能是在这些农业生态系统中隔离碳的重要策略。采取能够增加碳固存的管理措施,对于减少温室气体排放和维持农业系统的可持续性而言将是重要的。

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