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不同影响因素下盐结皮蒸发阻力定量模拟研究

李佳琳 李新虎 王弘超 崔萌萌 郭语博 靳浩东 任萧萧

干旱区地理2026,Vol.49Issue(1):80-93,14.
干旱区地理2026,Vol.49Issue(1):80-93,14.DOI:10.12118/j.issn.1000-6060.2025.079

不同影响因素下盐结皮蒸发阻力定量模拟研究

Quantitative modeling of evaporation resistance in salt crusts under varying influencing factors

李佳琳 1李新虎 1王弘超 1崔萌萌 2郭语博 1靳浩东 3任萧萧3

作者信息

  • 1. 中国科学院新疆生态与地理研究所荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,新疆 乌鲁木齐 830011||新疆阿克苏绿洲农田生态系统国家野外科学观测研究站,新疆 阿克苏 843017||中国科学院大学,北京 100049
  • 2. 新疆阿克苏绿洲农田生态系统国家野外科学观测研究站,新疆 阿克苏 843017
  • 3. 中国科学院新疆生态与地理研究所荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,新疆 乌鲁木齐 830011||中国科学院大学,北京 100049
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摘要

Abstract

Salt crusts are a typical surface structure in arid regions and significantly affect soil-atmosphere water transfer processes.The evaporation resistance of salt crusts is a key controlling parameter in the soil water-vapor evaporation process.However,quantitative understanding of salt crust evaporation resistance under varying influ-encing factors remains limited.Therefore,this study employs simulation experiments and theoretical analyses to dynamically monitor and analyze salt crust formation and the evolution of evaporation resistance under the in-fluences of soil particle size(fine sand:0.10-0.25 mm;coarse sand:0.50-0.85 mm),radiation(200 W·m-2,500 W·m-2,and 800 W·m-2),salt concentration(5.0%and 17.5%NaCl),wind speed(3.5 m·s-1 and 8.0 m·s-1),hydraulic conditions(with and without fixed groundwater),and evolution time.Using the Shapley additive expla-nation method,we quantified the contributions of the various factors and ranked their relative importance.The re-sults were as follows:(1)Salt crust evaporation resistance increased continuously over time.At the end of the ex-periment,the maximum evaporation resistance(9.39×104 s·m-1)occurred under the DL3 treatment(5.0%NaCl,no fixed groundwater,800 W·m-2 radiation,fine sand),whereas the minimum resistance(293.08 s·m-1)was ob-served under the WH2 treatment(5.0%NaCl,fixed groundwater,8.0 m·s-1 wind speed,fine sand).(2)The contri-bution ranking of the influencing factors was:hydraulic condition>radiation>evolution time>soil particle size>salt concentration>wind speed.Among these factors,radiation exerted a significant positive effect,whereas soil particle size had a negative impact on salt crust evaporation resistance.These findings provide theoretical support for the quantitative characterization of salt crust evaporation resistance.

关键词

盐结皮/蒸发阻力/影响因素/SHAP方法

Key words

salt crust/evaporation resistance/influencing factors/SHAP method

引用本文复制引用

李佳琳,李新虎,王弘超,崔萌萌,郭语博,靳浩东,任萧萧..不同影响因素下盐结皮蒸发阻力定量模拟研究[J].干旱区地理,2026,49(1):80-93,14.

基金项目

国家自然科学基金项目(42277314) (42277314)

天山英才培养计划项目(2022TSYCCX0008)资助 (2022TSYCCX0008)

干旱区地理

1000-6060

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