Study on multidimensional changes of rainfall erosivity during 1970-2017 in the North-South Transition Zone, China
文献类型:期刊论文
作者 | Li, Li2; Zhu, Wenbo3; Liu, Junjie5; Zhang, Li6; Zhu, Lianqi3; Wang, Liyuan3; Chen, Chaonan3; Ahmed, Naveed4; Gurung, Sher Bahadur1 |
刊名 | FRONTIERS IN ENVIRONMENTAL SCIENCE
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出版日期 | 2022-11-08 |
卷号 | 10页码:14 |
关键词 | rainfall erosivity geographic detectors relief degree multidimensional change Qinling-Daba mountains |
DOI | 10.3389/fenvs.2022.969522 |
通讯作者 | Zhu, Lianqi(lqzhu@henu.edu.cn) |
英文摘要 | China is one of the world's most seriously affected regions by water and soil erosion. Soil erosion is a major cause and an important component of land degradation, which has a negative impact on ecological protection and sustainable socioeconomic development. Rainfall erosivity (RE) is one of the key parameters to assess the degree of soil erosion. Quantifying the content of RE and the formation mechanism is important to accurately measure the degree of soil erosion and provide a theoretical basis for soil erosion management. Here, this study analyzed the spatial and temporal characteristics of RE and their driving mechanisms in the Qinba Mountains from 1970 to 2017 using a daily rainfall model. Furthermore, geographical detector methods were used to quantitatively identify the dominant factors affecting RE and the dominant factors affecting RE on different topographic reliefs. The results showed that the RE between 1970 and 2017 averaged 4,197.85 MJ mm hm(-2) h(-1) a(-1), with a mutation coefficient of 0.16. The spatial distribution of RE is high in the southeast and low in the northwest, and the mean annual RE declines with the increase in latitude in longitude and increases with the reduction in longitude in latitude. In addition, precipitation and temperature are the main factors affecting the spatial distribution of RE. Among these, precipitation can explain about 97% of the RE and temperature can explain about 65% of the RE. These findings should be essential for managing soil and water loss in the North-South Transition Zone, China. |
WOS关键词 | SOIL-EROSION ; LOESS PLATEAU ; TEMPORAL VARIABILITY ; RIVER BASIN ; PRECIPITATION ; PATTERNS ; PROVINCE ; RUNOFF ; TRENDS |
资助项目 | National Key Research and Development Program of China ; National Science and Technology Basic Resource Investigation Program of China ; [2021YFE0106700] ; [2017FY1009002] |
WOS研究方向 | Environmental Sciences & Ecology |
语种 | 英语 |
WOS记录号 | WOS:000890247800001 |
出版者 | FRONTIERS MEDIA SA |
资助机构 | National Key Research and Development Program of China ; National Science and Technology Basic Resource Investigation Program of China |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/187477] ![]() |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Zhu, Lianqi |
作者单位 | 1.Tribhuvan Univ, Cent Dept Geog, Kirtipur, Nepal 2.Beijing Normal Univ, Sch Govt, Beijing, Peoples R China 3.Henan Univ, Coll Geog & Environm Sci, Kaifeng, Peoples R China 4.Natl Univ Comp & Emerging Sci, FAST, Dept Civil Engn, Islamabad, Pakistan 5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing, Peoples R China 6.Beijing Normal Univ, Coll Water Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Li,Zhu, Wenbo,Liu, Junjie,et al. Study on multidimensional changes of rainfall erosivity during 1970-2017 in the North-South Transition Zone, China[J]. FRONTIERS IN ENVIRONMENTAL SCIENCE,2022,10:14. |
APA | Li, Li.,Zhu, Wenbo.,Liu, Junjie.,Zhang, Li.,Zhu, Lianqi.,...&Gurung, Sher Bahadur.(2022).Study on multidimensional changes of rainfall erosivity during 1970-2017 in the North-South Transition Zone, China.FRONTIERS IN ENVIRONMENTAL SCIENCE,10,14. |
MLA | Li, Li,et al."Study on multidimensional changes of rainfall erosivity during 1970-2017 in the North-South Transition Zone, China".FRONTIERS IN ENVIRONMENTAL SCIENCE 10(2022):14. |
入库方式: OAI收割
来源:地理科学与资源研究所
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