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安吉毛竹林生长季CO2浓度的时空特征

陈晓峰1,江洪1,2*,孙文文1,舒海燕3,方成圆1,孙恒1#br#   

  1. 1浙江农林大学国际生态研究中心, 杭州 311300; 2南京大学国际地球系统科学研究所, 南京 210093; 3西南大学生命科学学院三峡库区生态环境教育部重点实验室, 重庆 400715)
  • 出版日期:2016-05-10 发布日期:2016-05-10

Spatiotemporal characteristics of CO2 concentration in Phyllostachys edulis forest in Anji during growing season.

CHEN Xiao-feng1, JIANG Hong1,2*, SUN Wen-wen1, SHU Hai-yan3, FANG Cheng-yuan1, SUN Heng1#br#   

  1. (1 International Ecological Research Center of Zhejiang Agriculture and Forestry University, Hangzhou 311300, China; 2 International Earth System Scientific Institute, Nanjing University, Nanjing 210093, China; 3 Ministry of Education Key Laboratory of Ecoenvironments of Three Gorges Reservoir Region, School of Life Science, Southwest University, Chongqing 400715, China).
  • Online:2016-05-10 Published:2016-05-10

摘要: 试验采用7层CO2廓线系统对安吉毛竹林生长季(5—10月)CO2浓度进行连续监测,同时结合同步CO2通量和气象资料,分析安吉毛竹林CO2浓度的时空动态和CO2储存通量的变化特征。结果表明:安吉毛竹林生长季CO2浓度表现出明显的日变化、季节变化和垂直梯度。日尺度上,CO2浓度在日出前后达到最大,随后出现一段快速释放过程,午后达到全天最低值;整个生长季尺度上,7月份林间CO2浓度最低(368.1 μmol·mol-1),10月份最高(402.6 μmol·mol-1);垂直梯度方面,林冠上层CO2垂直梯度明显小于林冠层和林冠下层;林冠层和林冠上层垂直梯度变化趋势较为一致,白天均为正值,呈现为碳汇,夜间为负值,呈现为碳源,林冠下层CO2梯度全天均为负值。利用廓线系统计算毛竹林CO2储存通量,半小时和日尺度上,CO2储存通量分别占净生态系统CO2交换量(NEE)的25.5%和8.9%,而在月尺度上仅占NEE的0.22%。因此,在半小时及日尺度上计算NEE时不可忽略CO2储存通量,而在计算月尺度及更长时间尺度NEE时可以忽略CO2储存通量。

关键词: 克隆文库, 空气细菌, 空气真菌, 群落结构, 微生物多样性

Abstract: The CO2 concentration of Phyllostachys edulis forest ecosystem during the growing season (from May to October) was continuously measured using a 7layer profile system in Anji, Zhejiang Province in 2011. The synchronized CO2 flux and meteorological data were applied to explore the temporal and spatial variations in the CO2 concentration and CO2 storage flux. The results showed that the CO2 concentration of P. edulis forest during the growing season exhibited obvious diurnal and seasonal variations, as well as vertical variations. In a single day, the CO2 concentration reached the maximum value at  the daybreak, and decreased to the minimum value in the afternoon after a rapid emission process. In the entire growing season, the minimum CO2 concentration of the forest appeared in July (368.1 μmol·mol-1), and the maximum one emerged in October (402.6 μmol·mol-1). What’s more, the CO2 vertical gradients above the canopy were lower than those in and below the canopy. The vertical gradients in and above the canopy showed a consistent variation trend: positive in the daytime (carbon sink) and negative at night (carbon source). However, the CO2 vertical gradients below the canopy were negative throughout the day. We found the proportion of the CO2 storage flux obtained from the profile system to net-ecosystem CO2 exchange (NEE) was 25.5% and 8.9% at a halfhour and daily scale, respectively, but was only 0.22% at a monthly scale. The results suggested that CO2 storage flux could not be neglected when NEE was estimated at a halfhour or daily scale, but could be ignored at a monthly or longer time scale.

Key words: clone library, airborne bacteria, airborne fungi, community structure, microbial diversity.