Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1111/gcb.13938 |
Dynamics of soil biogeochemical gas emissions shaped by remolded aggregate sizes and carbon configurations under hydration cycles | |
Ebrahimi, Ali; Or, Dani | |
2018 | |
发表期刊 | GLOBAL CHANGE BIOLOGY
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ISSN | 1354-1013 |
EISSN | 1365-2486 |
出版年 | 2018 |
卷号 | 24期号:1页码:E378-E392 |
文章类型 | Article |
语种 | 英语 |
国家 | Switzerland |
英文摘要 | Changes in soil hydration status affect microbial community dynamics and shape key biogeochemical processes. Evidence suggests that local anoxic conditions may persist and support anaerobic microbial activity in soil aggregates (or in similar hot spots) long after the bulk soil becomes aerated. To facilitate systematic studies of interactions among environmental factors with biogeochemical emissions of CO2, N2O and CH4 from soil aggregates, we remolded silt soil aggregates to different sizes and incorporated carbon at different configurations (core, mixed, no addition). Assemblies of remolded soil aggregates of three sizes (18, 12, and 6 mm) and equal volumetric proportions were embedded in sand columns at four distinct layers. The water table level in each column varied periodically while obtaining measurements of soil GHG emissions for the different aggregate carbon configurations. Experimental results illustrate that methane production required prolonged inundation and highly anoxic conditions for inducing measurable fluxes. The onset of unsaturated conditions (lowering water table) resulted in a decrease in CH4 emissions while temporarily increasing N2O fluxes. Interestingly, N2O fluxes were about 80% higher form aggregates with carbon placement in center (anoxic) core compared to mixed carbon within aggregates. The fluxes of CO2 were comparable for both scenarios of carbon sources. These experimental results highlight the importance of hydration dynamics in activating different GHG production and affecting various transport mechanisms about 80% of total methane emissions during lowering water table level are attributed to physical storage (rather than production), whereas CO2 emissions (similar to 80%) are attributed to biological activity. A biophysical model for microbial activity within soil aggregates and profiles provides a means for results interpretation and prediction of trends within natural soils under a wide range of conditions. |
英文关键词 | biogeochemical gas fluxes mechanistic modeling microbial community N2O emissions soil aggregate soil structure |
领域 | 气候变化 ; 资源环境 |
收录类别 | SCI-E |
WOS记录号 | WOS:000426506100029 |
WOS关键词 | PARTICULATE ORGANIC-MATTER ; NITROUS-OXIDE PRODUCTION ; WATER-TABLE ; METHANE EMISSION ; NITRIFIER DENITRIFICATION ; ENVIRONMENTAL SCIENCE ; CO2 EMISSIONS ; PORE-SPACE ; N2O ; FLUXES |
WOS类目 | Biodiversity Conservation ; Ecology ; Environmental Sciences |
WOS研究方向 | Biodiversity & Conservation ; Environmental Sciences & Ecology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/17215 |
专题 | 气候变化 资源环境科学 |
作者单位 | ETH, Dept Environm Syst Sci, Zurich, Switzerland |
推荐引用方式 GB/T 7714 | Ebrahimi, Ali,Or, Dani. Dynamics of soil biogeochemical gas emissions shaped by remolded aggregate sizes and carbon configurations under hydration cycles[J]. GLOBAL CHANGE BIOLOGY,2018,24(1):E378-E392. |
APA | Ebrahimi, Ali,&Or, Dani.(2018).Dynamics of soil biogeochemical gas emissions shaped by remolded aggregate sizes and carbon configurations under hydration cycles.GLOBAL CHANGE BIOLOGY,24(1),E378-E392. |
MLA | Ebrahimi, Ali,et al."Dynamics of soil biogeochemical gas emissions shaped by remolded aggregate sizes and carbon configurations under hydration cycles".GLOBAL CHANGE BIOLOGY 24.1(2018):E378-E392. |
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