Mean residence time of global topsoil organic carbon depends on temperature, precipitation and soil nitrogen-Reference-Cited by-同舟云学术

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Mean residence time of global topsoil organic carbon depends on temperature, precipitation and soil nitrogen

Published:2013-01 Issue: Volume:100 Page:99-108
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Chen Shutao,Huang Yao,Zou Jianwen,Shi Yanshu

Funder

National Natural Science Foundation of China

Ministry of Science and Technology of Chin

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference62 articles.

1. Total carbon and nitrogen in the soils of the world;Batjes;European Journal of Soil Science,1996

2. ISRIC–WISE global data set of derived soil properties on a 0.5 by 0.5 degree grid (Version 3.0);Batjes,2005

3. Effect of N deposition on decomposition of plant litter and soil organic matter in forest systems;Berg;Environmental Reviews,1997

4. Tree root and soil heterotrophic respiration as revealed extending observations beyond the first year;Bhupinderpal-Singh;Plant, Cell & Environment,2003

5. A global relationship between the heterotrophic and autotrophic components of soil respiration?;Bond-Lamberty;Global Change Biology,2004

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