Knowledge Management System Of Institute Of Botany,CAS
Controls of Initial Wood Decomposition on and in Forest Soils Using Standard Material | |
Risch, Anita C. C.; Page-Dumroese, Deborah S. S.; Schweiger, Anna K.; Beattie, James R. R.; Curran, Mike P. P.; Finer, Leena5; Hyslop, Mike D. D.; Liu, Yong7; Schuetz, Martin; Terry, Tom A. A.; Wang, Weiwei7,8; Jurgensen, Martin F. F. | |
2022 | |
发表期刊 | FRONTIERS IN FORESTS AND GLOBAL CHANGE |
卷号 | 5 |
摘要 | Forest ecosystems sequester approximately half of the world's organic carbon (C), most of it in the soil. The amount of soil C stored depends on the input and decomposition rate of soil organic matter (OM), which is controlled by the abundance and composition of the microbial and invertebrate communities, soil physico-chemical properties, and (micro)-climatic conditions. Although many studies have assessed how these site-specific climatic and soil properties affect the decomposition of fresh OM, differences in the type and quality of the OM substrate used, make it difficult to compare and extrapolate results across larger scales. Here, we used standard wood stakes made from aspen (Populus tremuloides Michx.) and loblolly pine (Pinus taeda L.) to explore how climate and abiotic soil properties affect wood decomposition across 44 unharvested forest stands located across the northern hemisphere. Stakes were placed in three locations: (i) on top of the surface organic horizons (surface), (ii) at the interface between the surface organic horizons and mineral soil (interface), and (iii) into the mineral soil (mineral). Decomposition rates of both wood species was greatest for mineral stakes and lowest for stakes placed on the surface organic horizons, but aspen stakes decomposed faster than pine stakes. Our models explained 44 and 36% of the total variation in decomposition for aspen surface and interface stakes, but only 0.1% (surface), 12% (interface), 7% (mineral) for pine, and 7% for mineral aspen stakes. Generally, air temperature was positively, precipitation negatively related to wood stake decomposition. Climatic variables were stronger predictors of decomposition than soil properties (surface C:nitrogen ratio, mineral C concentration, and pH), regardless of stake location or wood species. However, climate-only models failed in explaining wood decomposition, pointing toward the importance of including local-site properties when predicting wood decomposition. The difficulties we had in explaining the variability in wood decomposition, especially for pine and mineral soil stakes, highlight the need to continue assessing drivers of decomposition across large global scales to better understand and estimate surface and belowground C cycling, and understand the drivers and mechanisms that affect C pools, CO2 emissions, and nutrient cycles. |
关键词 | climate properties soil properties aspen pine incubation location in-situ incubation mass loss unharvested forest stands |
学科领域 | Ecology ; Forestry |
DOI | 10.3389/ffgc.2022.829810 |
收录类别 | SCI |
语种 | 英语 |
WOS关键词 | LITTER DECOMPOSITION ; CARBON POOLS ; NITROGEN ; DECAY ; RATES ; TEMPERATURE ; CLIMATE ; PINE ; MINERALIZATION ; ECOSYSTEMS |
WOS研究方向 | Science Citation Index Expanded (SCI-EXPANDED) |
WOS记录号 | WOS:000789025800001 |
出版者 | FRONTIERS MEDIA SA |
文献子类 | Article |
出版地 | LAUSANNE |
EISSN | 2624-893X |
资助机构 | Swiss Federal Institute for Forest, Snow and Landscape Research (WSL). |
作者邮箱 | anita.risch@wsl.ch |
作品OA属性 | Green Accepted, gold, Green Published |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ibcas.ac.cn/handle/2S10CLM1/29041 |
专题 | 植被与环境变化国家重点实验室 |
作者单位 | 1.Swiss Fed Inst Forest Community Ecol Snow & Land, Birmensdorf, Switzerland 2.Page-Dumroese, Deborah S. S.] USDA Forest Serv, Rocky Mountain Res Stn, Moscow, ID USA 3.Schweiger, Anna K.] Univ Zurich, Remote Sensing Labs, Dept Geog, Zurich, Switzerland 4.Beattie, James R. R.] Australian Natl Univ, Res Sch Astron & Astrophys, Canberra, ACT, Australia 5.Curran, Mike P. P.] British Columbia Minist Forests Lands & Nat Resour, Victoria, BC, Canada 6.Nat Resources Inst Finland, Joensuu, Finland 7.Hyslop, Mike D. D.; Jurgensen, Martin F. F.] Michigan Technol Univ Coll Forest Resources & Envi, Houghton, MI USA 8.Beijing Forestry Univ, Key Lab Silviculture Conservat, Minist Educ, Beijing, Peoples R China 9.Chinese Academyof Sci, State Key Lab Vegetat & Environm Change, Inst Bot, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Risch, Anita C. C.,Page-Dumroese, Deborah S. S.,Schweiger, Anna K.,et al. Controls of Initial Wood Decomposition on and in Forest Soils Using Standard Material[J]. FRONTIERS IN FORESTS AND GLOBAL CHANGE,2022,5. |
APA | Risch, Anita C. C..,Page-Dumroese, Deborah S. S..,Schweiger, Anna K..,Beattie, James R. R..,Curran, Mike P. P..,...&Jurgensen, Martin F. F..(2022).Controls of Initial Wood Decomposition on and in Forest Soils Using Standard Material.FRONTIERS IN FORESTS AND GLOBAL CHANGE,5. |
MLA | Risch, Anita C. C.,et al."Controls of Initial Wood Decomposition on and in Forest Soils Using Standard Material".FRONTIERS IN FORESTS AND GLOBAL CHANGE 5(2022). |
条目包含的文件 | ||||||
文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
1704954527_cb568c3ed(2169KB) | 期刊论文 | 出版稿 | 开放获取 | CC BY-NC-SA | 浏览 请求全文 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论