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生态学杂志 ›› 2025, Vol. 44 ›› Issue (12): 4008-4018.doi: 10.13292/j.1000-4890.202512.005

• 研究报告 • 上一篇    下一篇

塔里木河中游胡杨树干CH4、CO2和N2O通量及其影响因素

塔依尔江·艾山1,2,姚诗雨1,2,王慧娟1,3,玉米提·哈力克1,2*   

  1. 1新疆大学生态与环境学院, 乌鲁木齐 830017; 2绿洲生态教育部重点实验室, 乌鲁木齐 830017; 3新疆和田学院教育科学学院, 新疆和田 848000)

  • 出版日期:2025-12-10 发布日期:2025-12-08

CH4, CO2, and N2O fluxes of Populus euphratica trunk in the middle reaches of the Tarim River and influencing factors.

AISHAN Tayierjiang1,2, YAO Shiyu1,2, WANG Huijuan1,3, HALIK müt1,2*   

  1. (1College of Ecology and Environment, Xinjiang University, Urumqi 830017, China; 2Ministry of Education Key Laboratory of Oasis Ecology, Urumqi 830017, China; 3School of Education Science, Xinjiang Hetian College, Hetian  848000, Xinjiang, China).

  • Online:2025-12-10 Published:2025-12-08

摘要: 胡杨(Populus euphratica)作为塔里木河流域唯一的成林树种,在区域碳循环中起着关键作用。本研究以塔里木河中游天然胡杨为对象,通过原位观测法,对胡杨树干胸径(离树木基部130 cm)处CH4、CO2和N2O温室气体传输速率进行测量,探究其离河道不同距离位置的排放特征及影响因子。结果表明:胡杨树干CH4和CO2的排放通量显著受样地和温期的独立影响(P<0.05);CH4和CO2的排放通量在不同温度条件下存在显著差异(P<0.05),均为低温期(05:00—08:00)排放量大于高温期(16:00—19:00),而N2O通量在不同条件下差异不显著;低温期树干CH4、CO2和N2O气体通量分别为0.0583~0.6042、35.944~127.521和0.020~0.058 μg·m-2·h-1,高温期分别为0.0542~0.6085、33.968~101.344和0.019~0.102 μg·m-2·h-1。胡杨树干CO2通量在高温期与气温存在显著正相关;CO2和CH4气体排放通量主要受树芯含水量和密度的正向调控,且在高温期更显著(AM:P<0.01;PM:P<0.001),风速则对CO2排放具有显著负向影响(P<0.001),N2O排放不受生长和气象因子的显著影响。胡杨树干3种气体排放通量与土壤含水量呈指数函数关系,CH4和CO2排放通量随着含水量增加先降后升,N2O则相反。胡杨树干温室气体排放在样木间差异明显,CH4和CO2通量波动较大,且与土壤含水量和植物生长指标密切相关,N2O通量变化较小,受环境因子影响不显著。


关键词: 胡杨, 排放通量, 树干, 塔里木河中游, 温室气体

Abstract: As the single dominant tree species in the Tarim River Basin, Populus euphratica plays a significant role in the regional carbon cycle. We employed in situ observation methods to measure the emission rates of greenhouse gases (CH4, CO2, and N2O) in the trunk (at breast height, 130 cm from the base of the tree) in a natural Populus euphratica forest in the middle reaches of the Tarim River. The aim is to investigate the characteristics of CH4, CO2, and N2O emission fluxes from the tree trunk at different distances from the riverbank and to identify the potential influencing factors. The results showed that CH4 and CO2 emission fluxes from the trunks were significantly influenced by sampling site and temperature period (P<0.05). CH4 and CO2 emissions during the low-temperature period (05:00-08:00) were greater than those during the high-temperature period (16:00-19:00). In contrast, N2O flux was relatively stable. The fluxes of CH4, CO2, and N2O during the low-temperature period were within the ranges of 0.0583-0.6042, 35.944-127.521, and 0.020-0.058 μg·m-2·h-1, respectively. During the high-temperature period, the emission fluxes for CH4, CO2, and N2O were 0.0542-0.6085, 33.968-101.344, and 0.019-0.102 μg·m-2·h-1, respectively. CO2 fluxes showed a statistically significant positive correlation with air temperature during the high-temperature period. CO2 and CH4 emission fluxes were mainly positively regulated by core moisture content and core density, particularly more significant during high-temperature periods (AM: P<0.01; PM: P<0.001). Wind speed exerted a significant and negative impact on CO2 emissions (P<0.001), while N2O emissions were not affected by growth and meteorological factors. The emissions of CH4, CO2, and N2O from trunk showed nonlinear relationships with soil moisture. CH4 and CO2 fluxes initially decreased and then increased with increasing soil moisture, whereas the N2O emission fluxes displayed an opposite trend. In general, greenhouse gas emissions from Populus euphratica trunks varied significantly among individual trees. CH4 and CO2 fluxes showed large fluctuations that were closely associated with soil moisture and plant growth indicators. In contrast, N2O fluxes exhibited minimal variation and were insensitive to environmental factors.


Key words: Populus euphratica, emission flux, tree trunk, Tarim River, greenhouse gas