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首页> 外文期刊>Forest Ecology and Management >Partitioning soil respiration of subtropical forests with different successional stages in south China.
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Partitioning soil respiration of subtropical forests with different successional stages in south China.

机译:华南地区不同演替阶段的亚热带森林土壤呼吸分配

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The methods of root-excision and trenching were employed concurrently in the present study in order to partition total soil respiration (Rtotal) into root respiration (Rroot), rhizomicrobial respiration (Rrhizo) and root free soil microbial respiration (Rrfs). This study was conducted under the monsoon evergreen broadleaf forest (BF), the pine forest (PF) and the pine and broadleaf mixed forest (MF) in Dinghushan Biosphere Reserve, subtropical China from April 2001 to March 2002. The three forests represent different successional stages in this region. The results showed that mean Rtotal were 477.9+or-96.3, 429.5+or-61.0 and 435.4+or-95.1 mg CO2 m-2 h-1 in BF, PF and MF, respectively. Rtotal were significantly higher in rainy season than those in dry season. However, no significant variations were found among three forests. Soil respiration rates were highly dependent on the combined effects of soil temperature and soil water content. Rroot was significantly higher in rainy season than that in dry season, with the values of 113.8-166.0 mg CO2 m-2 h-1 in rain season and 48.6-97.1 mg CO2 m-2 h-1 in dry season. There were no significant differences for Rrfs and Rrhizo between rain and dry season. However, the contributions of each component to Rtotal in rainy season differed from those in dry season. In rainy season, Rroot-to-Rtotal, Rrfs-to-Rtotal and Rrhizo-to-Rtotal ratios were in the range of 26.1-35.4, 40.6-43.7, and 20.9-36.6%. In dry season, they were 18.1-22.1, 44.8-47.6 and 30.3-37.1%, respectively..
机译:为了将土壤总呼吸(Rtotal)划分为根呼吸(Rroot),根际微生物呼吸(Rrhizo)和无根土壤微生物呼吸(Rrfs),本研究同时采用了根切除和挖沟的方法。这项研究是在2001年4月至2002年3月在中国亚热带鼎湖山生物圈保护区的季风常绿阔叶林(BF),松林(PF)以及松阔混交林(MF)下进行的。这三种森林代表了不同的演替该区域的阶段。结果表明,BF,PF和MF中的平均Rtotal分别为477.9+或-96.3、429.5+或-61.0和435.4+或-95.1 mg CO2 m-2 h-1。雨季的Rtotal明显高于旱季的Rtotal。但是,三个森林之间没有发现显着差异。土壤呼吸速率高度依赖于土壤温度和土壤水分的综合影响。雨季的Rroot显着高于旱季,雨季的Rroot值为113.8-166.0 mg CO2 m-2 h-1,而旱季的值为48.6-97.1 mg CO2 m-2 h-1。在雨季和旱季之间,Rrfs和Rrhizo没有显着差异。但是,雨季中各个成分对Rtotal的贡献与旱季中的有所不同。在雨季,Rroot对Rtotal,Rrfs对Rtotal和Rrhizo对Rtotal的比例在26.1-35.4、40.6-43.7和20.9-36.6%之间。在干旱季节,它们分别为18.1-22.1%,44.8-47.6和30.3-37.1%。

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