Does tree species composition affect soil CO2 emission and soil organic carbon storage in plantations?

Trees ◽  
2016 ◽  
Vol 30 (6) ◽  
pp. 2071-2080 ◽  
Author(s):  
Shaojun Wang ◽  
Hong Wang ◽  
Jihang Li
2020 ◽  
Author(s):  
Zhenhui Jiang ◽  
Anna Gunina ◽  
Lucas Merz ◽  
Yihe Yang ◽  
Yakov Kuzyakov ◽  
...  

<p>Afforestation with pure and mixed-species is an important strategy to improve soil organic carbon (SOC) stocks and restore degraded lands. However, what remains unclear is the stability of SOC to microbial degradation after afforestation and the effect of tree species composition. Moreover, it is important to reveal how sensitive the SOC in afforestation lands is to environmental changes, such as warming. To study the combined effects of warming and the tree species composition on decomposition of SOC by microorganisms and enzyme activities, soils were collected from the monocultural and mixtures of Silver birch (Betula Pendula) and European beech (Fagus Silvatica) (BangorDiversity, UK, 12 years since afforestation) and were incubated for 169 days at 0, 10, 20, 30 °C at 60 % of WHC. The field experiment is arranged into a completely randomized design with n=4. The CO<sub>2</sub> efflux was measured constantly, whereas activities of β-glucosidase, chitinase and acid phosphatase, and content of microbial biomass C (MBC) were obtained at the end of the incubation. Results showed that soil cumulative CO<sub>2</sub> efflux increased by 34.7–107% with the temperature. Potential enzyme activities were dependent on tree species composition. Warming, but not tree species exhibited a significant impact on the temperature sensitivity (Q10) of soil cumulative CO<sub>2</sub> efflux and enzyme activities. The greatest temperature sensitivity (Q<sub>10</sub>) of total CO<sub>2</sub> efflux was found at 10–20 °C and was 2.0–2.1, but that of enzyme activities were found as 0.9–1.1 at 0–10 °C. These results suggest that warming has an asynchronous effect on the SOC decomposition and enzyme activity, and enzymes cannot account for the temperature sensitivity of soil respiration. Thus, thermal adaptations of SOC mineralization is independent of the adaptation of the enzyme pool.</p>


2007 ◽  
Vol 50 (7) ◽  
pp. 1103-1114 ◽  
Author(s):  
Zhen Tao ◽  
ChengDe Shen ◽  
QuanZhou Gao ◽  
YanMin Sun ◽  
WeiXi Yi ◽  
...  

2011 ◽  
Vol 262 (10) ◽  
pp. 1895-1904 ◽  
Author(s):  
Eugenio Díaz-Pinés ◽  
Agustín Rubio ◽  
Helga Van Miegroet ◽  
Fernando Montes ◽  
Marta Benito

Land ◽  
2021 ◽  
Vol 10 (5) ◽  
pp. 517
Author(s):  
Sunwei Wei ◽  
Zhengyong Zhao ◽  
Qi Yang ◽  
Xiaogang Ding

Soil organic carbon storage (SOCS) estimation is a crucial branch of the atmospheric–vegetation–soil carbon cycle study under the background of global climate change. SOCS research has increased worldwide. The objective of this study is to develop a two-stage approach with good extension capability to estimate SOCS. In the first stage, an artificial neural network (ANN) model is adopted to estimate SOCS based on 255 soil samples with five soil layers (20 cm increments to 100 cm) in Luoding, Guangdong Province, China. This method is compared with three common methods: The soil type method (STM), ordinary kriging (OK), and radial basis function (RBF) interpolation. In the second stage, a linear model is introduced to capture the regional differences and further improve the estimation accuracy of the Luoding-based ANN model when extending it to Xinxing, Guangdong Province. This is done after assessing the generalizability of the above four methods with 120 soil samples from Xinxing. The results for the first stage show that the ANN model has much better estimation accuracy than STM, OK, and RBF, with the average root mean square error (RMSE) of the five soil layers decreasing by 0.62–0.90 kg·m−2, R2 increasing from 0.54 to 0.65, and the mean absolute error decreasing from 0.32 to 0.42. Moreover, the spatial distribution maps produced by the ANN model are more accurate than those of other methods for describing the overall and local SOCS in detail. The results of the second stage indicate that STM, OK, and RBF have poor generalizability (R2 < 0.1), and the R2 value obtained with ANN method is also 43–56% lower for the five soil layers compared with the estimation accuracy achieved in Luoding. However, the R2 of the linear models built with the 20% soil samples from Xinxing are 0.23–0.29 higher for the five soil layers. Thus, the ANN model is an effective method for accurately estimating SOCS on a regional scale with a small number of field samples. The linear model could easily extend the ANN model to outside areas where the ANN model was originally developed with a better level of accuracy.


Geoderma ◽  
2006 ◽  
Vol 134 (1-2) ◽  
pp. 200-206 ◽  
Author(s):  
Huajun Tang ◽  
Jianjun Qiu ◽  
Eric Van Ranst ◽  
Changsheng Li

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