Responses of soil organic carbon turnover to nitrogen deposition are associated with nitrogen input rates: Derived from soil 14C evidences

2018 ◽  
Vol 238 ◽  
pp. 500-507 ◽  
Author(s):  
Qiqi Tan ◽  
Guoan Wang ◽  
Xuejun Liu ◽  
Tianxiang Hao ◽  
Wenbing Tan
2021 ◽  
pp. 108322
Author(s):  
Junsheng Huang ◽  
Weixing Liu ◽  
Sen Yang ◽  
Lu Yang ◽  
Ziyang Peng ◽  
...  

2018 ◽  
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Minghua Song ◽  
Yu Guo ◽  
Feihai Yu ◽  
Xianzhou Zhang ◽  
Guangmin Cao ◽  
...  

CATENA ◽  
2020 ◽  
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Wendi Qu ◽  
Guangxuan Han ◽  
Franziska Eller ◽  
Baohua Xie ◽  
Jian Wang ◽  
...  

2004 ◽  
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Volker Hahn ◽  
Nina Buchmann

2006 ◽  
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pp. 443-450 ◽  
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C. G. Carlson ◽  
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Li-Hua TU ◽  
Ting-Xing HU ◽  
Jian ZHANG ◽  
Ren-Hong LI ◽  
Hong-Zhong DAI ◽  
...  

Author(s):  
Olha Stepanchenko ◽  
Liubov Shostak ◽  
Olena Kozhushko ◽  
Viktor Moshynskyi ◽  
Petro Martyniuk

The content of organic carbon is one of the essential factors that define soil quality. It is also notoriously challenging to model due to a multitude of biological and abiotic factors influencing the process. In this study, we investigate how decomposition of soil organic matter is affected by soil moisture and temperature. Soil organic carbon turnover is simulated by the CENTURY model. The accuracy of soil moisture data used is ensured by data assimilation approach, combing mathematical model and satellite retrievals. Numerical experiments demonstrate the influence of soil moisture regimes and climate on the quantity of soil humus stocks.


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