Changes to soil organic matter decomposition rate and its temperature sensitivity along water table gradients in cold-temperate forest swamps | |
Bian, Hongfeng1; Zheng, Shuai1; Liu, Yuan2; Xu, Li2; Chen, Zhi2; He, Nianpeng2,3,4,5 | |
刊名 | CATENA |
2020-11-01 | |
卷号 | 194页码:9 |
关键词 | Forest Swamp Water table Soil organic matter Decomposition Temperature sensitivity |
ISSN号 | 0341-8162 |
DOI | 10.1016/j.catena.2020.104684 |
通讯作者 | Xu, Li(xuli@igsnrr.ac.cn) |
英文摘要 | High-latitude forest swamp soil stores a large amount of carbon (C), because of its anaerobic condition and lower temperature. The combination of decreasing water table by artificial drainage and climate warming exert a considerable influence on soil C storage. In this study, we explored how the soil organic matter decomposition rate (R-s) and its temperature sensitivity (Q(10)) are altered with water-table gradients in high-latitude swamp soil. We sampled soil from cold-temperate forest swamps at three water-table gradients (permanently flooded, seasonally flooded, and non-flooded) in the high-latitude areas of Genhe and Mohe in China. We then conducted an incubation experiment using a new mode of varying incubation temperature, with rapid and continuous measurements of R-s. Our results showed that R-s at 20 degrees C (R-20) was significantly higher in seasonally flooded (SF) swamp soil, compared to permanently flooded (PF) or non-flooded (NF) soil. Soil redox condition mainly controlled R-20 during the early drying stage of forest swamps, while substrate quantity and quality dominated the latter stage. The highest Q(10) was observed in SF soils in Genhe, but this was not significant compared to the Q(10) in soils from Mohe. There were clear regional differences in Q(10) driven by changes to soil substrate (dissolved organic C and nitrogen) and physicochemical properties. Our findings indicate that high-latitude forest swamp soils may emit more CO2 and act as a C source under the scenarios of artificial draining and climate warming. |
资助项目 | Natural Science Foundation of China[31770655] ; Natural Science Foundation of China[41671045] ; Chinese Academy of Sciences Strategic Priority Research Program[XDA19020302] ; National Key R&D program of China[2017YFC0503904] ; program of Youth Innovation Research Team Project[LENOM2016Q0005] |
WOS关键词 | MICROBIAL RESPIRATION ; PHENOL OXIDASE ; CARBON ; COMMUNITY ; WETLAND ; PEATLANDS ; PATTERNS ; MOISTURE ; QUALITY ; LEVEL |
WOS研究方向 | Geology ; Agriculture ; Water Resources |
语种 | 英语 |
出版者 | ELSEVIER |
WOS记录号 | WOS:000566699000021 |
资助机构 | Natural Science Foundation of China ; Chinese Academy of Sciences Strategic Priority Research Program ; National Key R&D program of China ; program of Youth Innovation Research Team Project |
内容类型 | 期刊论文 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/156833] |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Xu, Li |
作者单位 | 1.Northeast Normal Univ, Sch Environm, State Environm Protect Key Lab Wetland Ecol & Veg, Changchun 130117, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China 3.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China 4.Northeast Normal Univ, Inst Grassland Sci, Changchun 130024, Peoples R China 5.Minist Educ, Key Lab Vegetat Ecol, Changchun 130024, Peoples R China |
推荐引用方式 GB/T 7714 | Bian, Hongfeng,Zheng, Shuai,Liu, Yuan,et al. Changes to soil organic matter decomposition rate and its temperature sensitivity along water table gradients in cold-temperate forest swamps[J]. CATENA,2020,194:9. |
APA | Bian, Hongfeng,Zheng, Shuai,Liu, Yuan,Xu, Li,Chen, Zhi,&He, Nianpeng.(2020).Changes to soil organic matter decomposition rate and its temperature sensitivity along water table gradients in cold-temperate forest swamps.CATENA,194,9. |
MLA | Bian, Hongfeng,et al."Changes to soil organic matter decomposition rate and its temperature sensitivity along water table gradients in cold-temperate forest swamps".CATENA 194(2020):9. |
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