Feinan Hu

Dr. Feinan Hu

orcid

Research Focus & Metrics

Academic Career Length

9Years (2018-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 July 2020 in CATENA
Verified
Journal Article
Closed access
JLJingfang Liu
Jingfang Liu
ZWZilong Wang
Zilong Wang
FHFeinan Hu
Feinan Hu
CXChenyang Xu
Chenyang Xu
RMRentian Ma
Rentian Ma
SZShiwei Zhao
Shiwei Zhao

1 November 2019 in Journal of Hydrology
Verified
Journal Article
Closed access
GLGang Liu
Gang Liu
FZFenli Zheng
Fenli Zheng
LJLu Jia
Lu Jia
YJYafei Jia
Yafei Jia
XZXun-Chang (John) Zhang
Xun-Chang (John) Zhang
JZJiaqiong Zhang
Jiaqiong Zhang

31 December 2024 in Journal of Hazardous Materials
Verified
Journal Article
Closed access
BCBokun Chang
Bokun Chang
TYTianhuan Yang
Tianhuan Yang
SFShubo Fan
Shubo Fan
LZLeming Zhen
Leming Zhen
XZXianbao Zhong
Xianbao Zhong
WDWei Du
Wei Du

22 January 2020 in PeerJ
Verified
Journal Article
Open access
PDF file
RMRentian Ma
Rentian Ma
FHFeinan Hu
Feinan Hu
JLJingfang Liu
Jingfang Liu
CWChunli Wang
Chunli Wang
ZWZilong Wang
Zilong Wang
SZShiwei Zhao
Shiwei Zhao
Background: Ecological stoichiometry (C:N:P ratios) in soil is an important indicator of the elemental balance in ecological interactions and processes. Long-term natural vegetation plays an important role in the accumulation and distribution of soil stoichiometry. However, information about the effects of long-term secondary forest succession on soil stoichiometry along a deep soil profile is still limited. Methods: We selected Ziwuling secondary succession forest developed from farmland as the study area, investigated the concentrations and stoichiometry of soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) at a depth of 0–100 cm along a 90-year succession chronosequence, including farmland (control), grassland, shrub, early forest, and climax forest. Results: SOC and TN concentrations significantly increased with increasing restoration age, whereas soil P concentration remained relatively stable across various successional stages. SOC and TN concentrations decreased with an increase in soil depth, exhibiting distinct soil nutrient “surface-aggregation” (high nutrients concentration in the top soil layer). The soil C:P and N:P ratios increased with an increase in restoration age, whereas the variation of the C:N ratio was small and relatively stable across vegetation succession. The nutrient limitation changed along with vegetation succession, transitioning from limited N in the earlier successional stages to limited P in the later successional stages. Conclusion: Our results suggest that more nitrogen input should be applied to earlier succession stages, and more phosphorus input should be utilized in later succession stages in order to address limited availability of these elements. In general, natural vegetation restoration was an ecologically beneficial practice for the recovery of degraded soils in this area. The findings of this study strengthen our understanding of the changes of soil nutrient concentration and nutrient limitation after vegetation restoration, and provide a simple guideline for future vegetation restoration and reconstruction efforts on the Loess Plateau.

1 March 2019 in Science of The Total Environment
Verified
Journal Article
Closed access
GLGang Liu
Gang Liu
FHFeinan Hu
Feinan Hu
FZFen-li Zheng
Fen-li Zheng
QZQiong Zhang
Qiong Zhang

31 January 2021 in European Journal of Soil Science
Verified
Journal Article
Closed access
PDF file
JLJingfang Liu
Jingfang Liu
CXChenyang Xu
Chenyang Xu
FHFeinan Hu
Feinan Hu
ZWZilong Wang
Zilong Wang
RMRentian Ma
Rentian Ma
SZShiwei Zhao
Shiwei Zhao