An Improved Craig–Gordon Isotopic Model: Accounting for Transpiration Effects on the Isotopic Composition of Residual Water during Evapotranspiration

Evapotranspiration (ET) is a crucial process in the terrestrial water cycle, and understanding its stable isotopic evolution is essential for comprehending hydrological processes. The Craig–Gordon (C-G) model is widely used to describe isotopic fractionation during pure evaporation. However, in natu...

Täydet tiedot

Bibliografiset tiedot

Päätekijät:	Yanwei Lu, Mingyi Wen, Peiyue Li, Jiaping Liang, Haoyan Wei, Min Li
Aineistotyyppi:	Artigo
Kieli:	Inglês
Julkaistu:	MDPI AG 2023-05-01
Sarja:	Agronomy
Aiheet:	evaporation transpiration water isotopes Craig–Gordon model ecohydrology
Linkit:	https://www.mdpi.com/2073-4395/13/6/1531
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