Vegetation and soil covariation, not grazing exclusion, control soil organic carbon and nitrogen in density fractions of alpine meadows in a Tibetan permafrost region

CATENA ◽  
2021 ◽  
Vol 196 ◽  
pp. 104832
Author(s):  
Zi-Qiang Yuan ◽  
Xiao-Jin Jiang
2015 ◽  
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Author(s):  
Liping Qiu ◽  
Xiaorong Wei ◽  
Tiane Ma ◽  
Yanchun Wei ◽  
Robert Horton ◽  
...  

2017 ◽  
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王玉红 WANG Yuhong ◽  
马天娥 MA Tian'e ◽  
魏艳春 WEI Yanchun ◽  
魏孝荣 WEI Xiaorong ◽  
邵明安 SHAO Ming'an ◽  
...  

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Yang Gao ◽  
Xiaohui Liu ◽  
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Bo Liu ◽  
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2021 ◽  
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pp. eaaz5236 ◽  
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Umakant Mishra ◽  
Gustaf Hugelius ◽  
Eitan Shelef ◽  
Yuanhe Yang ◽  
Jens Strauss ◽  
...  

Large stocks of soil organic carbon (SOC) have accumulated in the Northern Hemisphere permafrost region, but their current amounts and future fate remain uncertain. By analyzing dataset combining >2700 soil profiles with environmental variables in a geospatial framework, we generated spatially explicit estimates of permafrost-region SOC stocks, quantified spatial heterogeneity, and identified key environmental predictors. We estimated that 1014−175+194 Pg C are stored in the top 3 m of permafrost region soils. The greatest uncertainties occurred in circumpolar toe-slope positions and in flat areas of the Tibetan region. We found that soil wetness index and elevation are the dominant topographic controllers and surface air temperature (circumpolar region) and precipitation (Tibetan region) are significant climatic controllers of SOC stocks. Our results provide first high-resolution geospatial assessment of permafrost region SOC stocks and their relationships with environmental factors, which are crucial for modeling the response of permafrost affected soils to changing climate.


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