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首页> 外文期刊>Military operations research >The net primary productivity of early Permian peatland and their control factors: evidenced by the no. 6 coal seam of Jungar coalfield in North China
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The net primary productivity of early Permian peatland and their control factors: evidenced by the no. 6 coal seam of Jungar coalfield in North China

机译:二叠纪早期泥炭地的净初级生产力及其控制因素:华北准gar尔煤田6煤层

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Purpose - The purpose of this paper is to take the early Permian no.6 coal seam in Jungar coalfield of North China as an example, this paper studied the net primary productivity (NPP) level of the early Permian peatland and its relationship with the atmospheric environment at that time, analyzed the influence of the atmospheric environment, and discussed its control factors. Design/methodology/approach - First, geophysical logging signals were used for a spectrum analysis to obtain the Milankovitch cycle parameters in the no. 6 coal seam, including the eccentricity (95 ka); obliquity (35.6 ka); and precession (21.2 ka). These were then used to calculate the accumulation rate of the residual carbon in the no. 6 coal seam, which was determined to be between 49.44 and 50.57 gC/(m~2 • a). The carbon loss could be calculated according to the density and residual carbon content of the no. 6 coal seam. Then, the total carbon accumulation rate of the peatland was further derived as being between 64.91 and 66.40 gC/(m~2·a). Also, the NPP of the peatland was determined to be between 129.82 and 132.8 gC/(m~2·a). Finding - The result showed that the NPP of the early Permian peatland area was lower than that of the Holocene at the same latitude, and also lower than that of the later Permian of South China. Originality/value - This study's comprehensive analysis indicated that the temperature and humidity conditions, along with the oxygen and carbon dioxide levels in the atmosphere, were the main control factors of the NPP of the early Permian peatland. Also, wildfires were found to play a role.
机译:目的-本文以华北准gar尔煤田早二叠世六号煤层为例,研究了早二叠世泥炭地的净初级生产力(NPP)水平及其与大气的关系。当时的环境,分析了大气环境的影响,并讨论了其控制因素。设计/方法/方法-首先,将地球物理测井信号用于频谱分析,以获取No.中的Milankovitch循环参数。 6个煤层,包括偏心距(95 ka);倾角(35.6 ka);和进动(21.2 ka)。然后将这些用于计算No.4中残留碳的累积速率。 6煤层,确定为49.44至50.57 gC /(m〜2•a)。碳损失可以根据NO.1的密度和残余碳含量来计算。 6煤层。然后,进一步推算出泥炭地的总碳积累速率在64.91和66.40 gC /(m〜2·a)之间。此外,泥炭地的NPP被确定为129.82和132.8 gC /(m〜2·a)之间。发现-结果表明,在相同纬度下,早二叠世泥炭地的NPP低于全新世,也低于华南晚二叠纪的NPP。原创性/价值-这项研究的综合分析表明,温度和湿度条件以及大气中的氧气和二氧化碳水平是二叠纪泥炭地NPP的主要控制因素。此外,还发现了野火。

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