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
DOI10.1016/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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