Divergent patterns and drivers of water use efficiency across leaf and ecosystem scales in the Horqin Sandy Land
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Updated: Mar 31, 2026

Integrated Field Lysimetry and Porewater Sampling for Evaluation of Chemical Mobility in Soils and Established Vegetation
Published on: July 4, 2014
Xueer Kang1,2, Tingxi Liu3,4,5, Lina Hao3,4,5
1Institute of Grassland Research, Chinese Academy of Agricultural Sciences, Hohhot, China.
Introduction:
Water use efficiency (WUE) is crucial in the fragile Horqin Sandy Land, yet how global change and ecosystem traits influence its patterns remains unclear.
Methods:
This study focused on two ecosystems in the Horqin Sandy Land-semi-mobile dunes with Artemisia halodendron (SMAH) and a meadow wetland dominated by Phragmites australis (MPA). Using plant carbon isotope ratios and eddy covariance data from the 2022-2023 growing seasons, we revealed the distribution patterns of leaf-scale (WUEleaf ) and ecosystem-scale (WUEeco ) WUE and identified their environmental regulatory mechanisms.
Results:
The results showed that the variation trend of WUEleaf in SMAH closely tracked soil moisture dynamics, whereas WUEeco lagged behind WUEleaf , demonstrating that a low T/ET (transpiration to evapotranspiration ratio) plays a key "attenuator" role. In MPA, WUEeco variation aligned with groundwater level and temperature. Overall, WUEleaf and WUEeco responded oppositely to key drivers, but were both abiotic-dominated. WUEleaf was influenced mainly by soil temperature (with an optimum of 22.8°C) and soil organic carbon, while WUEeco was driven primarily by net radiation and vegetation cover.
Discussion:
WUEeco variation arose from vegetation-environment interactions rather than vegetation type alone. Thus, WUEeco cannot be directly extrapolated from WUEleaf . These results underscore aligning WUE metric selection with research objectives in water-carbon coupling studies, highlighting the role of ecosystem structure and functional traits in regulating water-carbon dynamics.
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