Soil Carbon Dynamics in Successional and Plantation Forests in Subtropical China

electronic supplementary material

2015international symposium on forest soils

Soil carbon dynamics in successional and plantation forests in subtropical China

Xinzhang Song1• Mark O. Kimberley2• Guomo Zhou1• Hailong Wang1,3

Received: 27 January 2016 / Accepted: 29 March 2016

© Springer-Verlag Berlin Heidelberg 2016

Responsible editor: Zhihong Xu

1Zhejiang Provincial Key Laboratory of Carbon Cycling in Forest Ecosystems and Carbon Sequestration, Zhejiang A＆F University, Lin’an, Hangzhou, Zhejiang Province, 311300, China

2Scion, Private Bag 3020, Rotorua 3046, New Zealand

3 Key Laboratory of Soil Contamination Bioremediation of Zhejiang Province,, Zhejiang A＆F University, Lin’an, Hangzhou, Zhejiang Province, 311300, China

Hailong Wang

;

Table S1 Detailsof the SOC and Rs database obtained from studiesof forest ecosystems across subtropical China.

SOC: soil organic carbon content (g C kg-1); Rs: soil respiration rate (t CO2 ha-1 yr-1); MAT: mean annual temperature (ºC); MAP: mean annual precipitation (mm); Age: years from forest conversion or plantation establishment.

EBF: evergreen broadleaf forest; BNMF: broadleaf and needleleaf mixed forest; MPF: Masson pine forest; CFF: Chinese fir forest; MBF: Moso bamboo forest.

DCC: dynamic closed chamber method; SCC: static closed chamber method; AA: alkali absorption method.

Y-R: yellow-red soil; R: red soil; Y: yellow soil; Y-B: yellow-brown soil.

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