Professor Li Yu'e

Dr. Professor Li Yu'e

orcid

Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

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

Representative Publications

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1 November 2016 in Science of The Total Environment
Verified
Journal Article
Closed access
XIAOBO QINXIAOBO QIN
XIAOBO QIN
PYProfessor Li Yu'e
Professor Li Yu'e
HWHong Wang
Hong Wang
CLChong Liu
Chong Liu
JLJianling Li
Jianling Li
YLYulin Liao
Yulin Liao

1 June 2020 in Agricultural and Forest Meteorology
Verified
Journal Article
Closed access
HGHasbagan Ganjurjav
Hasbagan Ganjurjav
EGElise S. Gornish
Elise S. Gornish
GHGuozheng Hu
Guozheng Hu
MSMark W. Schwartz
Mark W. Schwartz
YWYunfan Wan
Yunfan Wan
QGQingzhu Gao
Qingzhu Gao

31 December 2024 in Proceedings of the National Academy of Sciences
Verified
Journal Article
Open access
ZZZhenghu Zhou
Zhenghu Zhou
CWChuankuan Wang
Chuankuan Wang
PYProfessor Li Yu'e
Professor Li Yu'e
XWXuhui Wang
Xuhui Wang
Xinhua HeXinhua He
Xinhua He
Andong CaiAndong Cai
Andong Cai
Increasing soil organic carbon (SOC) in agricultural systems is a primary nature-based option for mitigating climate change, improving soil fertility, and ensuring food security. However, the consequences of global warming and increases in carbon inputs on cropland SOC stocks over the last few decades remain largely unknown, particularly in deeper soil layers. Here, by using repeated measurements, we reassess variations in SOC stocks across a 0 to 100 cm soil profile at the same locations in China’s upland croplands in 1980 and 2023. We observe an overall net accumulation of 0.74 Pg SOC (7%) with a mean sequestration rate of 13.7 g SOC m −2 y −1 . This accumulation results from 0.86 Pg SOC gains at upper soil depths (0 to 60 cm) induced by carbon inputs, alongside 0.12 Pg SOC losses at deeper soil layers (60 to 100 cm) prompted by warming-enhanced decomposition. While our findings indicate a successful, though lower than expected, increase in overall net SOC stocks, the loss of more recalcitrant deeper SOC warrants further consideration of its effects on enhancing cropland SOC accumulation to achieve carbon neutrality over the long term.

1 December 2019 in Journal of Environmental Management
Verified
Journal Article
Closed access
HGHasbagan Ganjurjav
Hasbagan Ganjurjav
YZYong Zhang
Yong Zhang
EGElise S. Gornish
Elise S. Gornish
GHGuozheng Hu
Guozheng Hu
PYProfessor Li Yu'e
Professor Li Yu'e
QGQingzhu Gao
Qingzhu Gao

1 January 2021 in Science of The Total Environment
Verified
Journal Article
Closed access
BWBin Wang
Bin Wang
RLRan Li
Ran Li
YWYunfan Wan
Yunfan Wan
PYProfessor Li Yu'e
Professor Li Yu'e
WCWeiwei Cai
Weiwei Cai
AWAndreas Wilkes
Andreas Wilkes

XGXinyun Gu
Xinyun Gu
SWShimei Weng
Shimei Weng
PYProfessor Li Yu'e
Professor Li Yu'e
XZXiaoqi Zhou
Xiaoqi Zhou
Water and fertilizer management practices are considered to have great influence on soil methane (CH4) emissions from paddy fields. However, few studies have conducted a quantitative analysis of the effects of these management practices. Here, we selected 156 observations of water management from 34 articles and 288 observations of fertilizer management from 37 articles and conducted a global meta-analysis of the effects of water and fertilizer management practices on soil CH4 emissions in paddy fields. In general, compared with traditional irrigation (long-term flooding irrigation), water-saving irrigation significantly decreased soil CH4 emissions but increased rice yield. Among the different practices, intermittent irrigation had the fewest reductions in CH4 emissions but the greatest increase in rice yield. In addition, fertilization management practices such as manure, mixed fertilizer (mixture), and straw significantly enhanced CH4 emissions. Rice yields were increased under fertilization with a mixture, traditional fertilizer, and controlled release fertilizer. Our results highlight that suitable agricultural water and fertilizer management practices are needed to effectively reduce CH4 emissions while maintaining rice yields. We also put forward some prospects for mitigating soil CH4 emissions from paddy fields in the context of global warming in the future.