Vegetation degradation along water gradient leads to soil active organic carbon loss in Gahai wetland

2020 ◽  
Vol 145 ◽  
pp. 105666 ◽  
Author(s):  
Jiangqi Wu ◽  
Weiwei Ma ◽  
Guang Li ◽  
Abdul-Rauf M. Alhassan ◽  
Haiyan Wang ◽  
...  
2020 ◽  
Vol 36 (4) ◽  
pp. 581-593 ◽  
Author(s):  
Maciej Chowaniak ◽  
Tomasz Głąb ◽  
Kazimierz Klima ◽  
Marcin Niemiec ◽  
Tomasz Zaleski ◽  
...  

2019 ◽  
Vol XII ◽  
pp. 1-1
Author(s):  
Monika Jakubus

The paper presents the problems of various type of forest soil degradations. Soil degradation is characterized by a decline in quality and decrease in ecosystems goods and it is unfavorable phenomenon. Soil is a non-renewable resource and its vulnerability to degradation depends on complex interactions between processes, factors and causes occurring at spatial and temporal scales. Both natural and antropogenic factors and processes are listed as possible causes of soil degradation. Erosion, depletion of the soil organic carbon, loss of soil fertility and biodiversity as well as acidification are particularly fast and noticeable among the major soil degradation processes.


2017 ◽  
Vol 37 (1) ◽  
Author(s):  
朱丽琴 ZHU Liqin ◽  
黄荣珍 HUANG Rongzhen ◽  
段洪浪 DUAN Honglang ◽  
贾龙 JIA Long ◽  
王赫 WANG He ◽  
...  

PLoS ONE ◽  
2016 ◽  
Vol 11 (4) ◽  
pp. e0154591 ◽  
Author(s):  
Zhongwu Li ◽  
Xiaodong Nie ◽  
Xiaofeng Chang ◽  
Lin Liu ◽  
Liying Sun

2020 ◽  
Vol 49 (3) ◽  
pp. 541-547
Author(s):  
Manyuan Yang ◽  
Ning Yang

To explore the effect of vegetation restoration on soil carbon cycle and fractions of soil organic carbon pool on purple-soil hill slope in Hengyang City of Hunan Province, China was selected. The soil samples of 0 - 10 and 10 - 20 cm soil layers under three types of vegetation, i.e., grassland zone (GZ), grassland-forest zone (GFZ) and forest zone (FZ). The dynamics of soil active organic carbon (SAOC) fractions to provide theory basis for the influence of soil carbon cycle and different vegetation zones on the fractions of organic carbon pool and its stability. Results show: Microbial biomass carbon and easily oxidizable organic carbon exhibited a decreasing pattern: FZ, GZ, GFZ (p < 0.05); Dissolved organic carbon exhibited a decreasing pattern: FZ, GFZ, GZ (p < 0.05); Light fraction organic carbon was the highest in FZ (p < 0.05), and the second in GZ and GFZ; The availability of active organic carbon in 0 - 10 cm soil layer was higher than that of 10 - 20 cm soil layer (p < 0.05); In comparison with GFZ, the herb in GZ could increase the contents of active organic carbon.


2018 ◽  
Vol 8 (23) ◽  
pp. 11999-12010 ◽  
Author(s):  
Abdul-Rauf Malimanga Alhassan ◽  
Weiwei Ma ◽  
Guang Li ◽  
Zhirong Jiang ◽  
Jiangqi Wu ◽  
...  

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