Factors controlling soil microbial respiration during the growing season in a mature larch plantation in Northern Japan
文献类型：期刊论文
| 作者 | Qu, Laiye; Kitaoka, Satoshi; Koike, Takayoshi |
| 刊名 | JOURNAL OF SOILS AND SEDIMENTS
 |
| 出版日期 | 2018-03-01 |
| 卷号 | 18期号:3页码:661-668 |
| 关键词 | Aboveground litter Japanese larch forest Soil microbial biomass Soil microbial respiration Soil temperature |
| ISSN号 | 1439-0108 |
| 文献子类 | Article |
| 英文摘要 | Soil microbes contribute significantly to soil respiration (SR) in boreal forests; however, there is limited knowledge on microbial contributions from long field investigations. The objective of this study was to estimate soil microbial respiration, as well as its primary controlling factors, for a period of three consecutive years. A trenching method was used to distinguish soil microbial respiration (R (Mic)) in a 55-year-old mature Japanese larch (Larix kaempferi) plantation in Northern Japan; the soil in which developed originally from volcanic soils containing pumice. We used a portable CO2 detection system to measure the soil respiration rate during the growing season. Environmental factors, soil physiochemical characteristics, and soil microbial biomass carbon and nitrogen (MBC and MBN) were analyzed to explain the seasonal variations of SR and R (Mic). The results showed that the estimated contribution of soil microbes to SR was 78, 62, and 55% during the three successive years, respectively. Respiration attributable to decomposition of aboveground litter contributed approximately 19% to SR. The major environmental factor that affected R (Mic) was soil temperature at 5 cm depth, which accounted for more than 70% of the seasonal variation in R (Mic) observed. There were close relations among MBC, MBN, and soil water content, but the soil water content showed no significant relation with R (Mic). The R (Mic) to SR varied from 78 to 55% following 3 years of trenching treatments. Our results demonstrated the important role of soil microbes on soil respiration in this larch forest. Soil temperature was the major positive factor that influenced R (Mic), while soil water content had no significant effect. Global warming will increase the loss of C into the atmosphere by increasing the R (Mic,) and could accelerate climate change. |
| 源URL | [http://ir.rcees.ac.cn/handle/311016/40554]  |
| 专题 | 生态环境研究中心_城市与区域生态国家重点实验室 |
| 推荐引用方式 GB/T 7714 | Qu, Laiye,Kitaoka, Satoshi,Koike, Takayoshi. Factors controlling soil microbial respiration during the growing season in a mature larch plantation in Northern Japan[J]. JOURNAL OF SOILS AND SEDIMENTS,2018,18(3):661-668. |
| APA | Qu, Laiye,Kitaoka, Satoshi,&Koike, Takayoshi.(2018).Factors controlling soil microbial respiration during the growing season in a mature larch plantation in Northern Japan.JOURNAL OF SOILS AND SEDIMENTS,18(3),661-668. |
| MLA | Qu, Laiye,et al."Factors controlling soil microbial respiration during the growing season in a mature larch plantation in Northern Japan".JOURNAL OF SOILS AND SEDIMENTS 18.3(2018):661-668. |
入库方式： OAI收割
来源：生态环境研究中心
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