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Journal of Desert Research ›› 2026, Vol. 46 ›› Issue (3): 175-186.DOI: 10.7522/j.issn.1000-694X.2026.00032

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Eco-environment evolution and driving factors of the Loess Plateau based on the XGBoost-SHAP approach

Xiaopeng Li1(), Kang Li1, Jing Xu2, Fugui Jia1, Shuang Lei1   

  1. 1.College of Agricultural,Forestry and Economic Management /, Lanzhou University of Finance and Economics,Lanzhou 730020,China
    2.School of Accounting, Lanzhou University of Finance and Economics,Lanzhou 730020,China
  • Received:2026-01-09 Revised:2026-03-02 Online:2026-05-20 Published:2026-06-11

Abstract:

To characterize long-term changes in eco-environment quality on the Loess Plateau and to reveal the underlying drivers, we constructed a spatiotemporal series of eco-environment quality for 2000-2025 using the Remote Sensing Ecological Index (RSEI). Class structure and transitions were analyzed, and Sen's slope estimation and the Mann-Kendall test were applied to identify change direction and significance. For mechanism interpretation, three representative years (2000, 2010, and 2020) were selected. Climate, topography, land use, and human-activity factors were integrated to develop XGBoost models, and SHAP was employed to decompose contributions and identify nonlinear responses. The results show that: (1) The multi-year mean RSEI was 0.449, with a distinct southeast-northwest gradient (higher in the southeast and lower in the northwest); the class composition was dominated by the “moderate” and “poor” categories, while higher-quality classes exhibited banded or patchy clustering. (2) Eco-environment quality improved overall from 2000 to 2025, with the annual mean RSEI increasing from 0.395 to 0.474 and the areal proportion of low-quality classes decreasing from 53.86% to 35.40%, indicating a structural shift toward medium-to-high classes. (3) Five-year class transitions were dominated by persistence, with stable proportions of 65.99%-80.32%, and changes mainly occurred as gradual shifts between adjacent classes, although the relative strength of improvement and degradation varied among periods. (4) Water-related factors consistently played a dominant role, with annual precipitation and water deficit ranking highest in contribution, and key drivers exhibited threshold and segmented responses, including a transition of slope effects from weakly negative to positive at approximately 10°, a shift of precipitation effects from inhibiting to promoting at around 400 mm, and a shift of water-deficit effects from positive or near-zero to persistently negative at about 50 mm. These findings provide quantitative evidence and mechanistic insights to support long-term monitoring and assessment, zoned management, and optimization of ecological restoration projects on the Loess Plateau.

Key words: Loess Plateau, RSEI, spatiotemporal dynamics, class transition, XGBoost, SHAP, driving factors

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