Review of "Stable isotopic constraints on global soil organic carbon turnover"

2017 ◽  
Author(s):  
Anonymous
2017 ◽  
Author(s):  
Chao Wang ◽  
Benjamin Z. Houlton ◽  
Dongwei Liu ◽  
Jianfeng Hou ◽  
Weixin Cheng ◽  
...  

2021 ◽  
pp. 108322
Author(s):  
Junsheng Huang ◽  
Weixing Liu ◽  
Sen Yang ◽  
Lu Yang ◽  
Ziyang Peng ◽  
...  

2004 ◽  
Vol 18 (1) ◽  
pp. n/a-n/a ◽  
Author(s):  
Volker Hahn ◽  
Nina Buchmann

2015 ◽  
Vol 6 ◽  
pp. 9-16 ◽  
Author(s):  
Uta Stockmann ◽  
José Padarian ◽  
Alex McBratney ◽  
Budiman Minasny ◽  
Delphine de Brogniez ◽  
...  

2019 ◽  
Author(s):  
Marco Pfeiffer ◽  
José Padarian ◽  
Rodrigo Osorio ◽  
Nelson Bustamante ◽  
Guillermo Federico Olmedo ◽  
...  

Abstract. One of the critical aspects in modelling soil organic carbon (SOC) predictions is the lack of access to soil information which is usually concentrated in regions of high agricultural interest. In Chile, most soil and SOC data to date is highly concentrated in 25 % of the territory that has intensive agricultural or forestry use. Vast areas beyond those forms of land use have few or no soil data available. Here, we present a new database of SOC for the country, which is the result of an unprecedented national effort under the frame of the Global Soil Partnership that help to build the largest database on SOC to date in Chile named “CHLSOC" comprising 13,612 data points. This dataset is the product of the compilation from numerous sources including unpublished and difficult to access data, allowing to fill numerous spatial gaps where no SOC estimates were publicly available before. The values of SOC compiled in CHLSOC range from 6×10−5 to 83.3 percent, reflecting the variety of ecosystems that exists in Chile. Profiting from the richness of geochemical, topographic and climatic variability in Chile, the dataset has the potential to inform and test models trying to predict SOC stocks and dynamics at larger spatial scales. Dataset available at https://www.doi.org/10.17605/OSF.IO/NMYS3 (Pfeiffer et al., 2019b).


2020 ◽  
Author(s):  
Zhongkui Luo ◽  
Raphael Viscarra-Rossel

Abstract. Soil organic carbon (SOC) accounts for two-thirds of terrestrial carbon. Yet, the role of soil physiochemical properties in regulating SOC stocks is unclear, inhibiting reliable SOC predictions under land use and climatic changes. Using legacy observations from 141,584 soil profiles worldwide, we disentangle the effects of biotic, climatic and edaphic factors (a total of 30 variables) on the global spatial distribution of SOC stocks in four sequential soil layers down to 2 m. The results indicate that the 30 variables can explain 70–80 % of the global variance of SOC in the four layers, to which edaphic properties contribute ~ 60 %. Soil lower limit is the most important individual soil properties, positively associated with SOC in all layers, while climatic variables are secondary. This dominant effect of soil properties challenges current climate-driven framework of SOC dynamics, and need to be considered to reliably project SOC changes for effective carbon management and climate change mitigation.


2006 ◽  
Vol 98 (3) ◽  
pp. 443-450 ◽  
Author(s):  
D. E. Clay ◽  
C. G. Carlson ◽  
S. A. Clay ◽  
C. Reese ◽  
Z. Liu ◽  
...  

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