Evaluation and prediction of water conservation of the Yellow river basin in Sichuan Province, China, based on Google Earth Engine and CA-Markov

被引:3
作者
Yang, Zhichong [1 ]
Dai, Xiaoai [1 ]
Lu, Heng [2 ,3 ]
Liu, Chao [2 ,3 ]
Nie, Ruihua [2 ,3 ]
Zhang, Min [4 ]
Ma, Lei [5 ]
Li, Naiwen [2 ,3 ]
Liu, Tiegang [2 ,3 ]
He, Yuxin [2 ,3 ]
Yang, Zhengli [2 ,3 ]
Qu, Ge [1 ]
Li, Weile [6 ]
Wang, Youlin [7 ]
机构
[1] Chengdu Univ Technol, Coll Earth Sci, Chengdu 610059, Peoples R China
[2] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
[3] Sichuan Univ, Coll Hydraul & Hydroelect Engn, Chengdu 610065, Peoples R China
[4] Shanghai Normal Univ, Sch Environm & Geog Sci, Shanghai 200234, Peoples R China
[5] Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210093, Peoples R China
[6] Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Prot, Chengdu 610059, Peoples R China
[7] Northwest Engn Corp Ltd, Xian 710065, Peoples R China
关键词
Water conservation; Yellow river; Google Earth Engine; CA-Markov; Spatio-temporal analysis; COVER DATA SET; ECOSYSTEM SERVICES; LOESS PLATEAU; LAND-USE; CLIMATE SURFACES; SOIL; PRECIPITATION; EVAPORATION; EVOLUTION; DISCOVER;
D O I
10.1016/j.heliyon.2023.e17903
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Yellow River Basin in China has the world's most serious soil erosion problem. The Yellow River Basin in Sichuan Province (YRS), as the upper reaches of the Yellow River, and its water conservation (WC) capacity greatly affects the ecological environment of the downstream basin. In recent years, YRS has received more and more attention, and numerous policies have been developed to improve local WC. However, there is a vacancy in the long-term research of WC in the YRS due to the lack of in-situ data. This study quantitatively evaluated the WC of YRS from 2001 to 2020 through Google Earth Engine (GEE) and analyzed the spatio-temporal variations of WC and land cover (LC). CA-Markov predicted the LC and WC in 2025 under three scenarios to assess the contribution of different scenarios to WC. The WC in YRS fluctuated from 1.93 to 6.77 billion m3. The climate is the dominant factor of WC change, but the effect of LC on WC is also evident. The WC capacity increases with vegetation coverage and height. The WC capacity of forests per km2 exceeds 600 mm, while that of grasslands is about 250 mm, and barren can cause around 300 mm of WC loss. In 2025, the WC in YRS may exceed 7.5 billion m3, but the past ecological management mode should be transformed. Improving the quality of land use and converting grasslands to forests is better than reducing cropland to improve WC.
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页数:17
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