Effect of Vegetation Rehabilitation on Soil Carbon and Its Fractions in Mu Us Desert, Northwest China

2014 ◽  
Vol 17 (6) ◽  
pp. 529-537 ◽  
Author(s):  
Jia-Bin Liu ◽  
Yu-Qing Zhang ◽  
Bin Wu ◽  
Shu-Gao Qin ◽  
Xin Jia ◽  
...  
2015 ◽  
Vol 312 ◽  
pp. 1-10 ◽  
Author(s):  
Fan Zhang ◽  
Changsheng Li ◽  
Zheng Wang ◽  
Stanley Glidden ◽  
Danielle S. Grogan ◽  
...  

PeerJ ◽  
2018 ◽  
Vol 6 ◽  
pp. e4859 ◽  
Author(s):  
Jun-Wei Yue ◽  
Jin-Hong Guan ◽  
Lei Deng ◽  
Jian-Guo Zhang ◽  
Guoqing Li ◽  
...  

Background The spruce forests are dominant communities in northwest China, and play a key role in national carbon budgets. However, the patterns of carbon stock distribution and accumulation potential across stand ages are poorly documented. Methods We investigated the carbon stocks in biomass and soil in the natural spruce forests in the region by surveys on 39 plots. Biomass of tree components were estimated using allometric equations previously established based on tree height and diameter at breast height, while biomass in understory (shrub and herb) and forest floor were determined by total harvesting method. Fine root biomass was estimated by soil coring technique. Carbon stocks in various biomass components and soil (0–100 cm) were estimated by analyzing the carbon content of each component. Results The results showed that carbon stock in these forest ecosystems can be as high as 510.1 t ha−1, with an average of 449.4 t ha−1. Carbon stock ranged from 28.1 to 93.9 t ha−1 and from 0.6 to 8.7 t ha−1 with stand ages in trees and deadwoods, respectively. The proportion of shrubs, herbs, fine roots, litter and deadwoods ranged from 0.1% to 1% of the total ecosystem carbon, and was age-independent. Fine roots and deadwood which contribute to about 2% of the biomass carbon should be attached considerable weight in the investigation of natural forests. Soil carbon stock did not show a changing trend with stand age, ranging from 254.2 to 420.0 t ha−1 with an average of 358.7 t ha−1. The average value of carbon sequestration potential for these forests was estimated as 29.4 t ha−1, with the lower aged ones being the dominant contributor. The maximum carbon sequestration rate was 2.47 t ha−1 year−1 appearing in the growth stage of 37–56 years. Conclusion The carbon stock in biomass was the major contributor to the increment of carbon stock in ecosystems. Stand age is not a good predictor of soil carbon stocks and accurate evaluation of the soil carbon dynamics thus requires long-term monitoring in situ. The results not only revealed carbon stock status and dynamics in these natural forests but were helpful to understand the role of Natural Forest Protection project in forest carbon sequestration as well.


2010 ◽  
Vol 26 (1) ◽  
pp. 153-161 ◽  
Author(s):  
Jianbiao Zhang ◽  
Tieliang Shangguan ◽  
Ziqiang Meng

2016 ◽  
Vol 163 ◽  
pp. 274-281 ◽  
Author(s):  
Zhongming Ma ◽  
Juan Chen ◽  
Xiaodong Lyu ◽  
Li-li Liu ◽  
Kadambot H.M. Siddique

2019 ◽  
Vol 50 (5) ◽  
pp. 1410-1423
Author(s):  
Hongjie Guan ◽  
Rongjiang Cao

Abstract How the presence of biocrusts regulates runoff generation in the Mu Us Desert is not well known. Runoff experiments under natural and artificial rainfalls and numerical simulations were conducted in semiarid environments to evaluate the effects of biocrust type and rainfall characteristics on runoff. The experimental results showed that the water drop penetration time (WDPT) of the moss-dominated biocrusts was 68.7% higher than that of lichen-dominated biocrusts. Nevertheless, the saturated hydraulic conductivity (Ks) for moss-dominated biocrusts was 72.7% lower than that for the lichen-dominated biocrusts. Runoff yield for moss-dominated biocrusts was significantly higher than that for lichen-dominated biocrusts. Runoff yield was mainly explained by rainfall amount (or maximum 5-min rainfall intensity, I5max) (P < 0.001) and WDPT (P = 0.001). The influences of biocrust type, rainfall intensity, and their interaction on runoff coefficient were significant at the probability level of 0.01. The results of numerical simulations concluded that surface runoff was generated for lichen- and moss-dominated biocrusts when rainfall intensity reached 73.5 and 49 mm h–1, respectively. Runoff coefficient in the moss-covered soil increased obviously when rainfall intensity changed from 49 to 73.5 mm h–1. The results suggest that runoff could be changed substantially under increasing trends in rainfall intensity in the Mu Us Desert.


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