期刊文献+

春季人工草地土壤CO_2和CH_4通量日变化研究 被引量:1

Diurnal Variations of Soil CO_2 and CH_4 Fluxes in Artificial Grassland in Spring
下载PDF
导出
摘要 采用最新的土壤温室气体通量监测系统,对人工草地春季土壤CO_2和CH_4通量进行测定,研究植物复苏期人工草地土壤CO_2和CH_4通量的日变化及其与环境因素的关系。结果表明:春季人工草地土壤CO_2通量有明显日变化特征,通量变化范围为-6.47~3.75μmol/(m^2·s),最大值出现在10∶00~12∶00之间,最小值出现在16∶00~17∶00之间,土壤5 cm温度是草地土壤CO_2通量日变化的主要影响因子;人工草地CH_4通量也有明显的昼夜变化规律,白天的波动性要大于夜晚,全天的波动范围为-16.31~13.13nmol/(m^2·s),在16∶00~18∶00之间出现最大值,在10∶00~11∶00之间降到最小值,土壤10 cm温度是草地土壤CH_4通量的主要影响因子。 The soil CO_2 and CH_4fluxes were measured monthly in artificial grassland in spring in 2015 using an Ultraportable Greenhouse Gas Analyzer( 951- 0011,LGR Inc.,USA) and SF- 3000 soil flux system equipped with the four soil flux chamber. The relationships of soil CO_2 and CH_4fluxes with environmental factors were also studied. The results showed that the soil CO_2 flux exhibited an apparent diurnal variation. Its value was between- 6. 47 and 3. 75 μmol/( m^2·s),and the peak value and valley value appeared at 10∶ 00 ~12∶ 00 and 16∶ 00 ~ 17∶ 00. It was mainly influenced by 5- cm soil temperature. The soil CH_4 flux also had obvious day and night law. The volatility in daytime was bigger than that in nighttime. The CH_4 flux values ranged from- 16. 31 to 13. 13 nmol/( m^2·s),and the peak value and valley value appeared at 16∶ 00 ~18∶ 00 and 10∶ 00 ~ 11∶ 00. The 10- cm soil temperature was its main influence factor.
出处 《山东农业科学》 2016年第7期91-94,共4页 Shandong Agricultural Sciences
基金 国家自然科学基金资助项目(41271510) 中央高校基本科研业务费项目(GK201601009)
关键词 人工草地 CO2通量 CH4通量 日变化 Artificial grassland CO2 flux CH4 flux Diurnal variation
  • 相关文献

参考文献16

  • 1IPCC.Climate change 2007:contribution of working groupⅠto the fourth assessment report of the intergovernmental panel on climate change[R].UK:Cambridge University Press,2007.
  • 2Raieh J W,Potter C S.Global patterns of carbon dioxide emissionsfrom soils[J].Global Biogeochemical Cycles,1995,9(1):23-26.
  • 3张炜,莫江明,方运霆,鲁显楷,王晖.氮沉降对森林土壤主要温室气体通量的影响[J].生态学报,2008,28(5):2309-2319. 被引量:42
  • 4Peng S S,Piao S L,Wang T,et al.Temperature sensitivity of soil respiration in different ecosystems in China[J].Soil Biology&Biochemistry,2009,41(5):1008-1014.
  • 5Janssens I A,Lankreijer H,Matteucci G,et al.Productivity overshadows temperature in determining soil and ecosystem respiration across European forests[J].Global Change Biology,2001,7:269-278.
  • 6罗光强,耿元波.羊草草原和贝加尔针茅草原生态系统呼吸的差异分析[J].环境科学,2010,31(11):2732-2739. 被引量:8
  • 7Song X Z,Yuan H Y,Kimberley M O,et al.Soil CO2flux dynamics in the two main plantation forest types in subtropical China[J].Science of The Total Environment,2013,444:363-368.
  • 8Savage K E,Parton W J,Davidson E A,et al.Long-term changes in forest carbon under temperature and nitrogen amendments in a temperate northern hardwood forest[J].Global Change Biology,2013,19(8):2389-2400.
  • 9Han G X,Zhou G S,Xu Z Z,et al.Soil temperature and biotic factors drive the seasonal variation of soil respiration in a maize(Zea mays L.)agricultural ecosystem[J].Plant Soil,2007,291:15-26.
  • 10Hendriks D D M,Dolman A J,Van de Molen M K,et al.A compact and stable eddy covariance set-up for methane measurements using off-axis integrated cavity output spectroscopy[J].Atmospheric Chemistry and Physics Discussions,2008,8:431-443.

二级参考文献116

共引文献214

同被引文献24

引证文献1

二级引证文献1

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部