AUTHOR=Dong Zhiqiang , Hu Hongchang , Wei Zhongwang , Liu Yaping , Xu Hanlin , Yan Hong , Chen Lajiao , Li Haoqian , Khan Mohd Yawar Ali
TITLE=Estimating the Actual Evapotranspiration of Different Vegetation Types Based on Root Distribution Functions
JOURNAL=Frontiers in Earth Science
VOLUME=10
YEAR=2022
URL=https://www.frontiersin.org/journals/earth-science/articles/10.3389/feart.2022.893388
DOI=10.3389/feart.2022.893388
ISSN=2296-6463
ABSTRACT=Background and Aims: Evapotranspiration is an important part of the water cycle and energy cycle. However, even under the same climatic condition, there are spatial differences in actual evapotranspiration (ETa) due to different land use and land cover. To characterize the influence of different vegetation types on ETa in China, this study parameterized the vertical distribution of the root systems of different vegetation types.
Methods: A one-dimensional soil-plant-atmosphere continuum (SPAC) model was constructed, and these root distribution functions were used to improve the root water absorption modulus of the soil-plant-atmosphere continuum model. Based on the improved model, the actual evaporation actual transpiration and ETa under different vegetation types were calculated, and the reasons for different ETa of different vegetation types were analyzed.
Results: The results show that the root distribution of all vegetation types increases first and then decreases as the depth increases, and almost all the maximum values are in the range of 0–20 cm. The savanna has the shallowest root system, while the barren has the deepest root system. The average ETa calculated in China was about 342.2 mm/y in 2015. The average ETa of the broadleaf evergreen forests is the largest, about 773 mm/y and the barren is the smallest, about 151 mm/y. The average annual precipitation is the most important factor affecting the ETa differences of different vegetation types.
Conclusion: The results provide solutions for estimating the ETa of different vegetation types and are significant to water resources management and soil and water conservation.