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

Q3 Environmental Science
Quan-Lai Zhou, Zhi-Min Liu, Hang Yu, Qun Ma, Wei Liang, Yan Jiang, Jia-Qi Zhang, Ying-Pei Ma
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引用次数: 0

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.

基于遥感蒸散发数据的辽宁省张武县水分平衡特征分析
明确水平衡特征是生态环境保护和水资源可持续管理的关键。基于2017年、2020年和2023年土地利用遥感影像、MOD16A2遥感蒸散发影像和气象资料,利用土地利用动态度模型和遥感数据反演,分析了辽宁省张武县不同土地利用类型的时空动态、蒸散发动态和降水动态,量化了区域水平衡的年际和季节动态。结果表明:张武县是一个以农业为主、农牧混合的生态系统。研究期间,耕地和草地占总面积的86.5%,是主要蒸散源,而建设用地仅占9.0%。土地利用综合动态性下降,生态要素趋于稳定,并向可持续发展方向发展。蒸散发(388.2 mm)是主要的水分流失途径,阈值温度为15.9℃时,蒸散发显著增加。蒸散量在生长季高于非生长季,在丰水年高于干旱年。年水分收支平均盈余86.7 mm,土壤水分动态循环经历稳定期(11 - 2月)、耗竭期(3 - 6月)和补给期(7 - 10月)。在土壤水分枯竭和补给期,应制定农田土壤水分平衡管理策略,以满足水分平衡,保证彰武县水资源的可持续性。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
自引率
0.00%
发文量
11393
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