Chin J Plant Ecol ›› 2026, Vol. 50 ›› Issue (4): 959-970.DOI: 10.17521/cjpe.2025.0072  cstr: 32100.14.cjpe.2025.0072

• Research Articles • Previous Articles     Next Articles

Diurnal variation of oxygen isotope ratio and quantitative partitioning of evapotranspiration in Larix gmelinii forest in Da Hinggan Ling of Nei Mongol, China

LI Jia-Ze1,2, JIA De-Bin1,*(), HAO Yu-Sheng1, HAO Shuai2, SHANG Zi-Qin1, JI Ming-Yu1   

  1. 1 College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, National Key Laboratory of Water Engineering and Ecological Environment in Arid Regions, Hohhot 010018, China
    2 Forest Ecosystem National Observation and Research Station of Da Hinggan Ling in Nei Mongol, Genhe, Nei Mongol 022350, China
  • Received:2025-02-26 Accepted:2025-05-28 Online:2026-04-20 Published:2026-06-29
  • Contact: JIA De-Bin
  • Supported by:
    National Natural Science Foundation of China(52169003);Nei Mongol Natural Science Foundation Joint Project(2023LHMS05024)

Abstract:

Aims To comprehensively investigate the dynamics of atmospheric water vapor concentration, water vapor isotopes, and evapotranspiration components in the forest ecosystem of the Da Hinggan Ling across different plant growing seasons and at a diurnal scale.

Methods This study conducted high-frequency monitoring of water vapor concentrations and isotopes at different heights using a stable water vapor isotope analyzer, while also determining the oxygen stable isotope ratio (δ18O) of plants and soil using vacuum extraction and a liquid water isotope analyzer. Additionally, evapotranspiration components in the Larix gmelinii forest were partitioned and compared across different periods by applying Isotope Steady-State (ISS) and Non-Steady-State (NSS) theories.

Important findings During the vigorous growing period of Larix gmelinii (July-August), atmospheric water vapor concentration and isotopic enrichment were elevated, whereas depletion occurred during the leaf-fall period. Diurnal variations exhibited a complex “V” shaped cycle with high-low-high fluctuations. On the diurnal scale, the δ18O of soil evaporation vapor ranged from -27.15‰ to -18.31‰, while that of ecosystem evapotranspiration vapor varied between -15.48‰ and -8.05‰, both demonstrating unimodal trends. Under ISS conditions, the δ18O of plant transpiration vapor spanned -10.83‰ to -5.31‰, contrasting with -12.21‰ to -6.63‰ under NSS conditions. Minimal divergence between ISS and NSS estimates occurred during 13:00-17:00, where transpiration contributions showed closest alignment. Overall, the transpiration contribution to evapotranspiration was 69.48%-85.08% (ISS) and 76.38%-91.05% (NSS), indicating substantially lower soil evaporation compared to vegetation transpiration, with plant transpiration dominating the forest ecosystem’s evapotranspiration.

Key words: stable isotope, vapor, Larix gmelini, evapotranspiration, non-steady-state assumption