Carbon storage and its allocation pattern of forest ecosystems with different restoration methods in subtropical China

2012 ◽  
Vol 57 (17) ◽  
pp. 1553-1561 ◽  
Author(s):  
FengTing YANG ◽  
YueBao DI ◽  
XiaoLi FU ◽  
YueLong LIANG ◽  
Hua ZHOU ◽  
...  
Author(s):  
Li Dai ◽  
Yufang Zhang ◽  
Lei Wang ◽  
Shuanli Zheng ◽  
Wenqiang Xu

The natural mountain forests in northwest China are recognized as a substantial carbon pool and play an important role in local fragile ecosystems. This study used inventory data and detailed field measurements covering different forest age groups (young, middle-aged, near-mature, mature, old-growth forest), structure of forest (tree, herb, litter and soil layer) and trees (leaves, branches, trunks and root) to estimate biomass, carbon content ratio, carbon density and carbon storage in Altai forest ecosystems. The results showed that the average biomass of the Altai Mountains forest ecosystems was 126.67 t·hm−2, and the descending order of the value was tree layer (120.84 t·hm−2) > herb layer (4.22 t·hm−2) > litter layer (1.61 t·hm−2). Among the tree parts, trunks, roots, leaves and branches accounted for 50%, 22%, 16% and 12% of the total tree biomass, respectively. The average carbon content ratio was 0.49 (range: 0.41–0.52). The average carbon density of forest ecosystems was 205.72 t·hm−2, and the carbon storage of the forest ecosystems was 131.35 Tg (standard deviation: 31.01) inside study area. Soil had the highest carbon storage (65.98%), followed by tree (32.81%), herb (0.78%) and litter (0.43%) layers. Forest age has significant effect on biomass, carbon content ratio, carbon density and carbon storage. The carbon density of forest ecosystems in study area was spatially distributed higher in the south and lower in north, which is influenced by climate, topography, soil types and dominant tree species.


2016 ◽  
Vol 36 (1) ◽  
Author(s):  
明安刚 MING Angang ◽  
刘世荣 LIU Shirong ◽  
莫慧华 MO Huihua ◽  
蔡道雄 CAI Daoxiong ◽  
农友 NONG You ◽  
...  

Forests ◽  
2015 ◽  
Vol 6 (12) ◽  
pp. 794-808 ◽  
Author(s):  
Yuanqi Chen ◽  
Zhanfeng Liu ◽  
Xingquan Rao ◽  
Xiaoling Wang ◽  
Chenfei Liang ◽  
...  

2008 ◽  
Vol 5 (3) ◽  
pp. 2679-2706 ◽  
Author(s):  
J. X. Liu ◽  
D. Q. Zhang ◽  
G. Y. Zhou ◽  
B. Faivre-Vuillin ◽  
Q. Deng ◽  
...  

Abstract. The effect of high atmospheric CO2 concentrations on the dynamics of mineral nutrient is not well documented, especially for subtropical China. We used model forest ecosystems in open-top chambers to study the effects of CO2 enrichment alone and together with N addition on the dynamics of soil cations and anions. Two years of exposure to a 700 ppm CO2 atmospheric concentration resulted in increased annual nutrient losses by leaching below 70 cm soil profile. Compared to the control, net Mg2+ losses increased by 385%, K+ by 223%, Ca2+ by 167% and N-NO3- by 108%, respectively. Increased losses following exposure to elevated CO2 were related to both faster soil weathering/organic matter decomposition and greater amounts of water leaching during high rainfall as a consequence of higher soil moisture. Net annual nutrient losses in the high CO2 concentration chambers reached 22.2 kg ha−1 year−1 for K+, 171.3 kg ha−1 year−1 for Ca2+, 8.2 kg ha−1 year−1 for Mg2+ and about 2 kg ha−1 year−1 for N-NO3-. The N addition alone had no significant effect on the mineral nutrient leaching losses. However, addition of N together with the high CO2 treatment significantly reduced mineral nutrient losses. We hypothesize that forests in subtropical China might suffer nutrient limitation and reduction in plant biomass under elevated CO2 concentration due to mineral leaching losses in the future.


2012 ◽  
Vol 363 (1-2) ◽  
pp. 123-138 ◽  
Author(s):  
Hai Ren ◽  
Hua Chen ◽  
Linjun Li ◽  
Pingheng Li ◽  
Changmou Hou ◽  
...  

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