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应用生态学报 ›› 2025, Vol. 36 ›› Issue (5): 1461-1468.doi: 10.13287/j.1001-9332.202505.023

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基于遥感蒸散量数据的辽宁省彰武县水量平衡特征

周全来1, 刘志民1*, 于航1, 马群1, 梁炜1, 姜艳2, 张家琪2, 马瑛培3   

  1. 1中国科学院沈阳应用生态研究所, 沈阳 110016;
    2中国科学院大学, 北京 100049;
    3沈阳大学环境学院, 沈阳 110044
  • 收稿日期:2024-09-30 修回日期:2025-03-09 出版日期:2025-05-18 发布日期:2025-11-18
  • 通讯作者: *E-mail: zmliu@iae.ac.cn
  • 作者简介:周全来, 男, 1974年生, 博士, 副研究员。主要从事恢复生态学研究。E-mail: zhouquanlai@iae.ac.cn
  • 基金资助:
    辽宁省科技厅科技重大专项课题“山水林田湖草沙一体化修复原理与设计”

Analyzing water balance characteristics with remote sensing evapotranspiration data in Zhangwu County, Liaoning Province, China

ZHOU Quanlai1, LIU Zhimin1*, YU Hang1, MA Qun1, LIANG Wei1, JIANG Yan2, ZHANG Jiaqi2, MA Yingpei3   

  1. 1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;
    2University of Chinese Academy of Sciences, Beijing 100049, China;
    3College of Environment, Shenyang University, Shenyang 110044, China
  • Received:2024-09-30 Revised:2025-03-09 Online:2025-05-18 Published:2025-11-18

摘要: 明确辽宁省彰武县水量平衡特征对生态环境保护和水资源可持续管理具有关键意义。本研究基于2017、2020和2023年土地利用遥感卫片、MOD16A2遥感蒸散量产品和气象数据,利用土地利用动态度模型、遥感数据反演等方法,研究该县不同土地利用类型的时空动态、水分蒸散动态及降水动态特征,量化区域水分平衡年际和季节动态。结果表明: 彰武县具有农业为主、农牧交错特征,研究期间,彰武县耕地和草地面积占86.5%,是主要蒸散发源,而建设用地仅占9.0%,综合土地利用动态度降低,生态要素格局趋于稳定可持续态势。年均蒸散量388.2 mm,是主要水分损失途径,蒸散量显著增加的阈值温度是15.9 ℃,蒸散量呈现生长季高于非生长季、高降水量年份高于低降水量年份的特征。年水量收支平均盈余86.7 mm,土壤水分盈亏表现为稳定期(11月至次年2月)、消耗期(3—6月)和补充期(7—10月)循环交替。应在土壤水分消耗期和补充期制定耕地土壤水分的水量平衡管理策略,以满足彰武县的水量平衡,保障该地区水资源可持续性。

关键词: 土地利用, 蒸散, 降水, 季节动态, 水分盈亏

Abstract: Clarifying the characteristics of water balance is the key to ecological environment protection and sustainable management of water resources. Based on 2017, 2020 and 2023 land use remote sensing images, MOD16A2 remote sensing evapotranspiration images and meteorological data, using land use dynamic degree model and remote sensing data inversion, we examined the temporal and spatial dynamics, evapotranspiration dynamics, and precipitation dynamics of different land-use types in Zhangwu County of Liaoning Province, and quantified the interannual and seasonal dynamics of regional water balance. The results showed that Zhangwu County featured an agricultural-dominated with mixed farming-grazing system. During the study period, farmland and grassland accounted for 86.5% of the total area, serving as primary evapotranspiration sources, while construction land only accounted for 9.0%. The comprehensive land-use dynamic degree decreased, suggesting stabilization of ecological elements toward a sustainable pattern. The evapotranspiration (388.2 mm) was the main water loss pathway, with a threshold temperature of 15.9 ℃ triggering significant evapotranspiration increase. Evapotranspiration exhibited higher values in growing season than non-growing season, and in years with abundant precipitation versus dry years. The annual water budget showed an average surplus of 86.7 mm, with soil moisture dynamics cycling through stable (November-February), depletion (March-June), and replenishment (July-October) periods. A water balance management strategy for soil moisture in farmland should be formulated during the soil moisture depletion and replenishment periods, to meet the water balance and ensure the sustainability of water resources of Zhangwu County.

Key words: land use, evapotranspiration, precipitation, seasonal dynamics, water budget