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Year-round observations of the net ecosystem exchange of carbon dioxide ina native tallgrass prairie

机译:原生高草草原中二氧化碳的净生态系统交换的全年观测

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An Ameriflux site was established in mid 1996 to study the exchange of CO2 in a native tallgrass prairie of north-central Oklahoma, USA. Approximately the first 20 months of measurements (using eddy covariance) are described here. This prairie, dominated by warm season C4 grasses, is typical of the central Kansasorthern Oklahoma region. During the first three weeks of the measurement period (mid-July-early August 1996), moisture-stress conditions prevailed. For the remainder of the period (until March 1998), however, soil moisture was nonlimiting. Mid-day net ecosystem CO2 exchange (NEE), under well-watered conditions, reached a maximum magnitude of 1.4 mg CO2 m(-2) s(-1) (flux toward the surface is positive) during peak growth (mid-July 1997), with green leaf area index of 2.8. In contrast, under moisture-stress conditions in the same growth stage in 1996, mid-day NEE was reduced to near-zero. Average night NEE ranged from near-zero, during winter dormancy, to -0.50 mg CO2 m(-2) s(-1), during peak growth. Most of the variance in average night NEE was explained by changes in soil temperature (0.1 m depth) and green leaf area. The daytime NEE measurements were examined in terms of a rectangular hyperbolic relationship with incident photosynthetically active radiation. The analysis showed that the quantum yield during peak growth was similar to those measured in other prairies and the y-intercept, so obtained, can be potentially used as an estimate of night-time CO2 emissions when eddy covariance data are unavailable. Daily integrated NEE reached its peak magnitude of 30.8 g CO2 m(-2) d(-1) (8.4 g C m(-2) d(-1)) in mid-July when the green LAI was the largest (about 2.8). In general, the seasonal trend of daily NEE I:on relatively clear days) followed that of green LAI. Annually integrated carbon exchange, between prescribed burns in 1997 and 1998, was 268 g C m(-2) y(-1). After incorporating carbon loss during the prescribed burn, the net annual carbon exchange in this prairie was near-zero in 1998.
机译:1996年年中建立了一个Ameriflux站点,以研究美国俄克拉荷马州中北部的原生高草草原中的二氧化碳交换。此处介绍了大约前20个月的测量值(使用涡度协方差)。这个草原以温暖的C4牧草为主,是堪萨斯州中部/俄克拉荷马州北部的典型地区。在测量期间的前三周(1996年7月中旬至8月中旬),普遍出现了水分胁迫条件。然而,在此期间的剩余时间内(至1998年3月),土壤水分是非限制性的。在高峰期(7月中旬),在充足的水条件下,午间净生态系统CO2交换(NEE)达到1.4 mg CO2 m(-2)s(-1)的最大值(向表面的通量为正)。 1997),绿叶面积指数为2.8。相反,在1996年相同生长阶段的水分胁迫条件下,午间NEE降低到接近零。夜间平均NEE范围从冬季休眠期间的接近零到峰值增长期间的-0.50 mg CO2 m(-2)s(-1)。平均夜晚NEE的大部分变化是由土壤温度(0.1 m深度)和绿叶面积的变化解释的。白天的NEE测量是根据与入射光合有效辐射的矩形双曲线关系进行检查的。分析表明,峰值增长过程中的量子产率与其他大草原上测得的量子产率相似,因此,当没有涡度协方差数据时,如此获得的y截距可潜在地用作夜间CO2排放的估算值。当绿色LAI最大(约2.8)时,每日综合NEE在7月中旬达到30.8 g CO2 m(-2)d(-1)(8.4 g C m(-2)d(-1))的峰值。 )。通常,每日NEE I(在相对晴朗的日子)的季节趋势遵循绿色LAI的季节趋势。在1997年和1998年之间的规定燃烧之间的年度综合碳交换量为268 g C m(-2)y(-1)。考虑到规定的燃烧过程中的碳损失,该草原的年净碳交换量在1998年几乎为零。

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