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生态学杂志 ›› 2025, Vol. 44 ›› Issue (12): 4100-4109.doi: 10.13292/j.1000-4890.202512.015

• 研究报告 • 上一篇    下一篇

黄土高原地区蒸散发时空变异特征及土地利用变化对耗水量的影响

郭原宏1,刘文娟1*,李佳婷1,马琨2   

  1. 1宁夏大学农学院, 银川 750021; 2宁夏大学生态环境学院, 银川 750021)

  • 出版日期:2025-12-10 发布日期:2025-12-10

Spatiotemporal variations of evapotranspiration and the impact of land use change on water consumption in the Loess Plateau.

GUO Yuanhong1, LIU Wenjuan1*, LI Jiating1, MA Kun2   

  1. (1College of Agriculture, Ningxia University, Yinchuan 750021, China; 2School of Ecology and Environment, Ningxia University, Yinchuan 750021, China).

  • Online:2025-12-10 Published:2025-12-10

摘要: 精确评估实际蒸散发(ET)的时空分布特性及土地利用类型变化对ET的影响,对于实现区域水资源的合理利用和优化分配至关重要。本研究选取黄土高原作为对象,以MOD16A2为数据源,采用Theil-Sen趋势分析和Mann-Kendall检验方法,对2000—2022年间黄土高原地区实际蒸散发的时空分布特征及变化趋势进行了分析。同时,结合土地利用数据对研究区主要土地利用类型蒸散发的变化特征进行了分析,并对区域耗水量进行了估算。结果表明:(1)在时间尺度上,黄土高原地区的实际日均蒸散发呈现出逐年波动且整体呈现上升趋势,波动范围介于0.52~0.97 mm,逐年日均蒸散发的增长速度为0.015 mm·a-1;在空间分布特征上,黄土高原地区的ET值呈现出自西北到东南逐渐增加的趋势。(2)在黄土高原地区的4种主要土地利用类型中,平均蒸散发表现为:林地>耕地>草地>未利用地,林地ET显著高于其他3类用地。(3)2000—2020年黄土高原地区耕地面积净减少13377.0 km2,减少率为6.2%,受退耕还林政策的影响,林地的面积大幅度增加,增加了3748.6 km2;建设用地净增加11657.8 km2。(4)2000—2020年间耗水量的变化趋势与土地利用类型面积的变化基本一致,整体上呈现出增加态势。研究结果可为退耕还林背景下黄土高原地区水资源的利用与分配提供科学依据。


关键词: 蒸散发, MODIS ET数据, 黄土高原, 土地利用, 耗水特征

Abstract: Accurate assessments of the spatiotemporal variations of actual evapotranspiration (ET) and the impact of land use changes on ET are crucial for the rational utilization and optimal allocation of regional water resources. With MOD16A2 data as the primary data source, we analyzed the spatiotemporal distribution and trends of actual ET of Loess Plateau from 2000 to 2022 by Theil-Sen trend analysis and Mann-Kendall test. Additionally, land use data were incorporated to examine the variations in ET across the primary land use types within the study area and to estimate the regional water consumption. The results showed that: (1) Actual average daily ET in the Loess Plateau exhibited annual fluctuations with an overall increasing trend, ranging from 0.52 to 0.97 mm, with an average daily increase rate of 0.015 mm·a-1. Spatially, ET values showed an increasing trend from the northwest to the southeast of the region. (2) Among the four dominant land use types, the annual average evapotranspiration followed an order: forest land > cultivated land > grassland > unused land. (3) From 2000 to 2020, the cultivated land area in the Loess Plateau decreased by 13377.0 km2, with a reduction rate of 6.2%. In contrast, forest land area increased significantly by 3748.6 km2, primarily due to the “Grain for Green” policy, while constructed land increased by 11657.8 km2. (4) The trend in water consumption was consistent with the changes in land use areas, showing an overall increasing trend from 2000 to 2020. These findings provide a robust scientific foundation for the sustainable utilization and allocation of water resources in the Loess Plateau, particularly under the context of the “Grain for Green” policy.


Key words: evapotranspiration, MODIS ET data, Loess Plateau, land use, water consumption characteristic