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基于改进S-W模型的南小河沟流域蒸散发分配及控制机制

杨楠 丁林 李浩霖 宋孝玉 邓建伟 李蓝君 赵新凯 孟鹏飞 符冲 魏婉茵 张育斌

干旱区研究2024,Vol.41Issue(11):1819-1830,12.
干旱区研究2024,Vol.41Issue(11):1819-1830,12.DOI:10.13866/j.azr.2024.11.03

基于改进S-W模型的南小河沟流域蒸散发分配及控制机制

Research on the distribution and control mechanism of evapotranspiration in the Nanxiaohegou watershed based on an improved S-W model

杨楠 1丁林 1李浩霖 2宋孝玉 3邓建伟 1李蓝君 3赵新凯 3孟鹏飞 3符冲 3魏婉茵 3张育斌1

作者信息

  • 1. 甘肃省水利科学研究院,甘肃 兰州 73000
  • 2. 北京工业大学,北京 100124
  • 3. 西安理工大学省部共建西北旱区生态水利国家重点实验室,陕西 西安 710048
  • 折叠

摘要

Abstract

In this study,we aimed to accurately quantify evapotranspiration(ET)and its components while explor-ing the factors that control it,which will facilitate the practical evaluation,planning,and management of regional water resources.Utilizing continuous long-term observation data and field tests conducted from 2016 to 2020 in the Nanxiaohegou watershed—a typical small watershed for water and soil conservation on the Loess Plateau—this study simulated the dynamic changes of ET and its components in typical plantation land using the improved Shuttleworth-Wallace(S-W)model.Additionally,we analyzed the coupling relationships between plant transpira-tion(T),soil evaporation(E),and control factors using a structural equation model.The results revealed the fol-lowing:(1)The modified S-W model was effective for evaluating ET and its components in Nanxiaohe Valley.The threshold value of soil surface resistance(rss)was 50-2500 s·m-1,exhibiting an exponential relationship with the empirical function of soil surface water content(θ);moreover,higher sand content in the soil particles correlated with a steeper linear slope.(2)ET ranged from 276.76 mm to 402.86 mm in typical plantation land,with annual averages of Tand E accounting for 51.6%and 48.4%of ET,respectively.While monthly ET,T,and E patterns were not pronounced,daily fluctuations were significant.The fluctuation trends of T and E largely reflect-ed annual precipitation patterns but lagged behind rainfall.(3)Structural equation modeling analysis revealed that net radiation(Rn),temperature(Ta),and θ exerted the most significant effects on ET,with Rn having the largest im-pact on T(total impact of 0.614)and Ta having the most significant impact on E(total impact of 0.426).Twas pos-itively correlated with E,with a contribution coefficient of 0.503.Evaluating ET and its components using an im-proved S-W model establishes a foundation for a deeper understanding of ecological and hydrological processes in arid and semiarid regions.

关键词

蒸散发组分/改进S-W模型/SEM模型/蒸发抗阻力/南小河沟流域

Key words

evaporative components/improve the S-W model/SEM model/evaporation resistance/Nanxiaohe-gou watershed

引用本文复制引用

杨楠,丁林,李浩霖,宋孝玉,邓建伟,李蓝君,赵新凯,孟鹏飞,符冲,魏婉茵,张育斌..基于改进S-W模型的南小河沟流域蒸散发分配及控制机制[J].干旱区研究,2024,41(11):1819-1830,12.

基金项目

甘肃省重点研发计划项目(22YF7FA081) (22YF7FA081)

陕西省自然科学基础研究计划项目(2023-JC-ZD-30,2019JZ-45) (2023-JC-ZD-30,2019JZ-45)

甘肃省水利科研与技术推广计划项目(24GSLK007,23GSLK012,23GSLK013) (24GSLK007,23GSLK012,23GSLK013)

干旱区研究

OA北大核心CSTPCD

1001-4675

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