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Interannual variability in net ecosystem carbon production in a rain-fed maize ecosystem and its climatic and biotic controls during 2005–2018

机译:2005 - 2018年雨喂养玉米生态系统中净生态系统碳生产的依赖变异性及其气候和生物控制

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摘要

Interannual variability (IAV) in net ecosystem carbon production (NEP) plays an important role in the processes of the carbon cycle, but the long-term trends in NEP and the climatic and biotic control of IAV in NEP still remain unclear in agroecosystems. We investigated interannual variability in NEP, expressed as annual values and anomalies, and its climatic and biotic controls using an eddy-covariance dataset for 2005-2018 for rain-fed spring maize in northeastern China. Average annual NEP was 270±31 g C m-2yr -1, with no significant changes over time. The effects on interannual variability in NEP of gross ecosystem productivity (GEP) that was mainly controlled by soil water content (SWC) and leaf area index (LAI), were more than those of respiration (RE) that was controlled by temperature and LAI. Further, maximum daily NEP (NEPmax) that was dominated by summer vapor pressure deficit explained the largest fraction of annual anomalies in NEP, followed by carbon dioxide uptake period (CUP) that was defined by the beginning date (BDOY) and the end date (EDOY) of CUP. The variability in BDOY was mainly determined by spring precipitation and the effective accumulated temperature, and the variability in EDOY was determined by autumn precipitation, SWC and LAI. NEP may decrease with declining precipitation in the future due to decreasing GEP, NEPmax, or CUP, and irrigation and residues cover may be useful in efforts to maintain current NEP levels. Our results indicate that interannual variability in NEP in agroecosystems may be more sensitive to changes in water conditions (such as precipitation, SWC and VPD) induced by climate changes, while temperature may be an important indirect factor when VPD is dominated.
机译:净生态系统碳生产(NEP)中的际变化(IAV)在碳循环过程中起重要作用,但NEP的长期趋势和NEP中IAV的气候和生物控制仍然不清楚在农业系统中仍然不清楚。我们调查了NEP的际变量,表示为年度值和异常,以及使用2005-2018的涡流和生物控制,2005 - 2018年在中国东北雨喂养春季玉米。年平均每年的NEP为270±31 G C m-2yr -1,随着时间的推移没有显着变化。主要由土壤含水量(SWC)和叶面积指数(LAI)控制的生态系统生产率(GEP)中纳皮的持续变异性的影响比温度和赖温控的呼吸(RE)的效果。此外,由夏季蒸汽压力缺陷主导的最大每日NEP(NEPMAX)解释了NEP中最大的一半大部分,其次是由开始日期(BDOY)和结束日期所定义的二氧化碳摄取期(杯)(杯子)的杯子。 BDOY的变异主要是由弹簧沉淀和有效累积温度决定的,并且通过秋天沉淀,SWC和Lai测定了Edoy的变异性。由于降低GEP,NepMax或杯子,未来降水可能会随着灌溉和残留物覆盖而减少未来降水可能在努力维持当前NEP水平的努力中。我们的研究结果表明,农业重组中NEP的续变性对气候变化引起的水状况(如沉淀,SWC和VPD)的变化更敏感,而当VPD主导时,温度可能是重要的间接因素。

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