The ratio of transpiration to evapotranspiration and water use efficiency in an irrigated oasis agroecosystem: Different temporal-scale effects
Agroecosystems play an important role in carbon sequestration and water consumption of global terrestrial ecosystems. However, the magnitude, pattern, and regulation of the ratio of transpiration to evapotranspiration ( T /ET), and also water use efficiency at ecosystem (WUE e ) and canopy (WUE c ) scales, remain unclear in agroecosystems in arid areas. In this study, a six-year synchronous observation of water-carbon fluxes and sap flow by the eddy covariance and sap flow techniques was conducted in an irrigated vineyard in northwest China. We found that T /ET, WUE e , and WUE c changed dynamically at the daily (1.0–98.6%, 0.3–4.9 g C kg –1 H 2 O, 0.4–5.9 g C kg –1 H 2 O) and monthly (26.0–71.0%, 0.8–1.8 g C kg –1 H 2 O, 2.3–3.2 g C kg –1 H 2 O) scales. At the annual scale, the range was relatively narrow, with mean values of 61.7% ± 3.7%, 1.5 ± 0.1 g C kg –1 H 2 O, and 2.4 ± 0.3 g C kg –1 H 2 O, respectively (mean ± standard deviation). Biological and environmental factors regulated their dynamics on different temporal scales. Specifically, leaf area index (LAI) and canopy conductance ( g c ) mainly determined the seasonal variation of T /ET, WUE e , and WUE c at the daily and monthly scales. However, at the annual scale, vapor pressure deficit (VPD) and air temperature ( T a ) became the main influencing factors. These results highlight the complexity of water-carbon coupling in agroecosystems and the necessity of considering specific factors at different temporal scales when modeling and managing agricultural water resources. In addition, there is still great water-saving potential from the perspective of WUE in the cultivation of vines in Northwest China. • Sap flow and water-carbon fluxes are measured synchronously for 6 years in an oasis agroecosystem. • The ratio of transpiration to evapotranspiration ( T /ET) is 61.7% ± 3.7% during growing season. • Water use efficiency (WUE) at the ecosystem scale is 1.6 times than that of the canopy. • Gas exchange metric and WUE explain 73.7% of the multi-dimensional space variation of plant traits.
Authors
- Cong Xu (ORCID: https://orcid.org/0000-0002-7467-2083)
- Shangtao Wang (ORCID: https://orcid.org/0009-0004-1246-3552)
- Gaofeng Zhu (ORCID: https://orcid.org/0000-0002-3533-9106)
- Haochen Fan (ORCID: https://orcid.org/0000-0002-9615-3815)
- Tao Che (ORCID: https://orcid.org/0000-0001-6848-7271)
- Yang Zhang (ORCID: https://orcid.org/0000-0003-4102-2671)
- Huiling Chen (ORCID: https://orcid.org/0000-0002-7714-9693)
- Yuzhong Zhang (ORCID: https://orcid.org/0000-0001-7116-9135)
- Yonghong Su
Institutions
- Qinghai University (CN)
- Zhejiang Normal University (CN)
- Chinese Academy of Sciences (CN)
- Northwest Institute of Eco-Environment and Resources (CN)
- Lanzhou University (CN)
Publication Details
- Journal
- Agricultural Water Management
- Published
- 2024-08-05
- DOI
- https://doi.org/10.1016/j.agwat.2024.108980
- Citations
- 5
- Primary Topic
- Plant Water Relations and Carbon Dynamics
- Type
- article
- Field-Weighted Citation Impact
- 1.41
Funders
- National Natural Science Foundation of China
- Natural Science Foundation of Gansu Province