首页> 外文期刊>農業気象 >CO2 efflux from decomposing leaf litter stacks is influenced by the vertical distribution of leaf litter water content and its temporal variation
【24h】

CO2 efflux from decomposing leaf litter stacks is influenced by the vertical distribution of leaf litter water content and its temporal variation

机译:分解叶片凋落物的二氧化碳排放量受叶片凋落物水分的垂直分布及其时间变化的影响

获取原文
获取原文并翻译 | 示例
           

摘要

We evaluated the temporal changes in the vertical distribution of leaf litter respiration (R-LL) due to changes of leaf litter water content (W-LL) within the leaf litter layer (L layer) using in situ direct measurements. To investigate the vertical distribution of R-LL and W-LL within the leaf litter layer over a time-series, we measured the R-LL and W-LL of 10 separate layers in vertical leaf litter stacks fixed to the forest floor using wire pins. Measurements were conducted for 30 stacks in a temperate broad-leaved secondary forest between May 2008 and January 2009. In the warm season, high R-LL was observed at high W-LL, while low R-LL was observed at low W-LL. R-LL was comparatively lower during the cool season than during the warm season regardless of the magnitude of W-LL. The temperature sensitivity of R-LL differed depending on W-LL; temperature increases under low-moisture conditions had small effects on R-LL, while under higher-moisture conditions, R-LL was more responsive to temperature increases. Small differences in position within the leaf litter stack affected the vertical variation of W-LL and, consequently, there was large distribution in R-LL during the wet period and small distribution in R-LL (totally small values) during the dry period. Thus, CO2 efflux from the net L layer was strongly affected by R-LL distribution induced by the local wetting within the L layer. In estimating CO2 efflux from the L layer using water content of the L layer, monitoring of the water content of the L layer, which takes into account the vertical distribution in W-LL within the L layer, is necessary.
机译:我们使用原位直接测量法评估了由于凋落物层(L层)内凋落物含水量(W-LL)的变化而导致的凋落物呼吸(R-LL)的垂直分布的时间变化。为了研究某个时间序列内叶子凋落物层中R-LL和W-LL的垂直分布,我们使用导线测量了固定在森林地面上的垂直叶子凋落物堆栈中10个单独层的R-LL和W-LL针脚。在2008年5月至2009年1月之间,在温带阔叶次生林中对30个烟囱进行了测量。在暖季,高W-LL时观测到高R-LL,而低W-LL时观测到低R-LL。 。无论W-LL的大小如何,在凉爽的季节,R-LL均比温暖的季节低。 R-LL的温度灵敏度随W-LL的不同而不同。在低水分条件下温度升高对R-LL的影响较小,而在高水分条件下,R-LL对温度升高更敏感。枯枝落叶堆中位置的微小差异会影响W-LL的垂直变化,因此,在湿润时期R-LL分布较大,而在干燥时期R-LL分布较小(总值很小)。因此,净L层的CO2流出强烈地受L层内局部润湿引起的R-LL分布的影响。在使用L层的水含量来估计来自L层的CO 2流出量时,需要对L层的水含量进行监测,该监测考虑了L层内W-LL中的垂直分布。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号