Chin J Plant Ecol ›› 2026, Vol. 50 ›› Issue (4): 959-970.DOI: 10.17521/cjpe.2025.0072 cstr: 32100.14.cjpe.2025.0072
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LI Jia-Ze1,2, JIA De-Bin1,*(
), HAO Yu-Sheng1, HAO Shuai2, SHANG Zi-Qin1, JI Ming-Yu1
Received:2025-02-26
Accepted:2025-05-28
Online:2026-04-20
Published:2026-06-29
Contact:
JIA De-Bin
Supported by:LI Jia-Ze, JIA De-Bin, HAO Yu-Sheng, HAO Shuai, SHANG Zi-Qin, JI Ming-Yu. Diurnal variation of oxygen isotope ratio and quantitative partitioning of evapotranspiration in Larix gmelinii forest in Da Hinggan Ling of Nei Mongol, China[J]. Chin J Plant Ecol, 2026, 50(4): 959-970.
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URL: https://www.plant-ecology.com/EN/10.17521/cjpe.2025.0072
Fig. 2 Vapor concentration and oxygen stable isotope ratio (δ18O) distribution characteristics in the Larix gmelinii forest in the Da Hinggan Ling of Nei Mongol.
Fig. 3 Daily variation of water vapor concentration at different heights in the Larix gmelinii forest in the Da Hinggan Ling of Nei Mongol. A, July 15th. B, August 15th. C, September 15th. D, October 15th.
Fig. 4 Daily variation of vapor oxygen stable isotope ratio (δ18O) at different heights in the Larix gmelinii forest in the Da Hinggan Ling of Nei Mongol. A, July 15th. B, August 15th. C, September 15th. D, October 15th.
| 日期 Date | 时间 Time | δs (‰) | δv (‰) | δE (‰) | 日期 Date | 时间 Time | δs (‰) | δv (‰) | δE (‰) |
|---|---|---|---|---|---|---|---|---|---|
| 2022-07-15 | 6:00-8:00 | -9.90 | -18.64 | -20.76 | 2022-09-15 | 6:00-8:00 | -11.69 | -21.82 | -22.91 |
| 8:00-10:00 | -8.56 | -17.37 | -18.96 | 8:00-10:00 | -11.03 | -20.21 | -21.92 | ||
| 10:00-12:00 | -8.30 | -16.52 | -18.55 | 10:00-12:00 | -10.72 | -20.21 | -21.39 | ||
| 12:00-14:00 | -8.25 | -16.81 | -18.31 | 12:00-14:00 | -10.06 | -19.56 | -20.59 | ||
| 14:00-16:00 | -9.08 | -16.74 | -19.22 | 14:00-16:00 | -10.65 | -19.74 | -21.03 | ||
| 16:00-18:00 | -9.84 | -16.82 | -20.29 | 16:00-18:00 | -11.33 | -20.37 | -21.83 | ||
| 18:00-20:00 | -10.44 | -17.35 | -21.14 | 18:00-20:00 | -12.01 | -20.86 | -23.00 | ||
| 2022-08-15 | 6:00-8:00 | -9.27 | -17.89 | -21.01 | 2022-10-15 | 6:00-8:00 | -14.39 | -24.54 | -26.76 |
| 8:00-10:00 | -8.88 | -16.36 | -19.71 | 8:00-10:00 | -13.81 | -24.60 | -26.14 | ||
| 10:00-12:00 | -8.41 | -16.44 | -18.79 | 10:00-12:00 | -13.25 | -23.81 | -25.50 | ||
| 12:00-14:00 | -8.17 | -16.06 | -18.48 | 12:00-14:00 | -13.54 | -23.11 | -25.78 | ||
| 14:00-16:00 | -8.33 | -16.17 | -18.57 | 14:00-16:00 | -13.86 | -22.92 | -26.16 | ||
| 16:00-18:00 | -8.86 | -18.00 | -19.51 | 16:00-18:00 | -14.09 | -23.66 | -26.48 | ||
| 18:00-20:00 | -9.51 | -17.90 | -20.54 | 18:00-20:00 | -14.60 | -24.19 | -27.15 |
Table 1 δs, δv and δE in the Larix gmelinii forest in the Da Hinggan Ling of Nei Mongol calculated by Craig-Gordon model
| 日期 Date | 时间 Time | δs (‰) | δv (‰) | δE (‰) | 日期 Date | 时间 Time | δs (‰) | δv (‰) | δE (‰) |
|---|---|---|---|---|---|---|---|---|---|
| 2022-07-15 | 6:00-8:00 | -9.90 | -18.64 | -20.76 | 2022-09-15 | 6:00-8:00 | -11.69 | -21.82 | -22.91 |
| 8:00-10:00 | -8.56 | -17.37 | -18.96 | 8:00-10:00 | -11.03 | -20.21 | -21.92 | ||
| 10:00-12:00 | -8.30 | -16.52 | -18.55 | 10:00-12:00 | -10.72 | -20.21 | -21.39 | ||
| 12:00-14:00 | -8.25 | -16.81 | -18.31 | 12:00-14:00 | -10.06 | -19.56 | -20.59 | ||
| 14:00-16:00 | -9.08 | -16.74 | -19.22 | 14:00-16:00 | -10.65 | -19.74 | -21.03 | ||
| 16:00-18:00 | -9.84 | -16.82 | -20.29 | 16:00-18:00 | -11.33 | -20.37 | -21.83 | ||
| 18:00-20:00 | -10.44 | -17.35 | -21.14 | 18:00-20:00 | -12.01 | -20.86 | -23.00 | ||
| 2022-08-15 | 6:00-8:00 | -9.27 | -17.89 | -21.01 | 2022-10-15 | 6:00-8:00 | -14.39 | -24.54 | -26.76 |
| 8:00-10:00 | -8.88 | -16.36 | -19.71 | 8:00-10:00 | -13.81 | -24.60 | -26.14 | ||
| 10:00-12:00 | -8.41 | -16.44 | -18.79 | 10:00-12:00 | -13.25 | -23.81 | -25.50 | ||
| 12:00-14:00 | -8.17 | -16.06 | -18.48 | 12:00-14:00 | -13.54 | -23.11 | -25.78 | ||
| 14:00-16:00 | -8.33 | -16.17 | -18.57 | 14:00-16:00 | -13.86 | -22.92 | -26.16 | ||
| 16:00-18:00 | -8.86 | -18.00 | -19.51 | 16:00-18:00 | -14.09 | -23.66 | -26.48 | ||
| 18:00-20:00 | -9.51 | -17.90 | -20.54 | 18:00-20:00 | -14.60 | -24.19 | -27.15 |
| 日期 Date | 时间 Time | δET (‰) | δT-NSS (‰) | δT-ISS (‰) | 日期 Date | 时间 Time | δET (‰) | δT-NSS (‰) | δT-ISS (‰) |
|---|---|---|---|---|---|---|---|---|---|
| 2022-07-15 | 6:00-8:00 | -9.88 | -8.24 | -5.69 | 2022-09-15 | 6:00-8:00 | -13.27 | -11.13 | -9.03 |
| 8:00-10:00 | -9.55 | -7.33 | -6.08 | 8:00-10:00 | -12.43 | -10.30 | -8.58 | ||
| 10:00-12:00 | -8.74 | -7.31 | -5.31 | 10:00-12:00 | -11.21 | -9.74 | -7.87 | ||
| 12:00-14:00 | -8.06 | -6.63 | -5.69 | 12:00-14:00 | -10.28 | -8.81 | -7.90 | ||
| 14:00-16:00 | -8.22 | -6.94 | -5.83 | 14:00-16:00 | -10.85 | -9.36 | -8.35 | ||
| 16:00-18:00 | -9.00 | -6.95 | -5.90 | 16:00-18:00 | -11.73 | -9.64 | -8.73 | ||
| 18:00-20:00 | -9.63 | -6.95 | -6.25 | 18:00-20:00 | -13.22 | -10.75 | -9.25 | ||
| 2022-08-15 | 6:00-8:00 | -10.99 | -8.98 | -7.81 | 2022-10-15 | 6:00-8:00 | -15.48 | -11.99 | -10.53 |
| 8:00-10:00 | -10.01 | -8.36 | -7.10 | 8:00-10:00 | -13.72 | -10.47 | -9.04 | ||
| 10:00-12:00 | -8.90 | -7.59 | -6.38 | 10:00-12:00 | -12.60 | -10.08 | -8.92 | ||
| 12:00-14:00 | -8.05 | -7.02 | -6.03 | 12:00-14:00 | -11.17 | -9.20 | -8.32 | ||
| 14:00-16:00 | -8.71 | -7.56 | -6.47 | 14:00-16:00 | -11.21 | -9.44 | -8.59 | ||
| 16:00-18:00 | -9.58 | -7.90 | -6.82 | 16:00-18:00 | -12.93 | -10.21 | -9.14 | ||
| 18:00-20:00 | -10.17 | -8.36 | -7.08 | 18:00-20:00 | -15.29 | -12.21 | -10.83 |
Table 2 δET of the Larix gmelinii forest in the Da Hinggan Ling of Nei Mongol calculated by Keeling Plot
| 日期 Date | 时间 Time | δET (‰) | δT-NSS (‰) | δT-ISS (‰) | 日期 Date | 时间 Time | δET (‰) | δT-NSS (‰) | δT-ISS (‰) |
|---|---|---|---|---|---|---|---|---|---|
| 2022-07-15 | 6:00-8:00 | -9.88 | -8.24 | -5.69 | 2022-09-15 | 6:00-8:00 | -13.27 | -11.13 | -9.03 |
| 8:00-10:00 | -9.55 | -7.33 | -6.08 | 8:00-10:00 | -12.43 | -10.30 | -8.58 | ||
| 10:00-12:00 | -8.74 | -7.31 | -5.31 | 10:00-12:00 | -11.21 | -9.74 | -7.87 | ||
| 12:00-14:00 | -8.06 | -6.63 | -5.69 | 12:00-14:00 | -10.28 | -8.81 | -7.90 | ||
| 14:00-16:00 | -8.22 | -6.94 | -5.83 | 14:00-16:00 | -10.85 | -9.36 | -8.35 | ||
| 16:00-18:00 | -9.00 | -6.95 | -5.90 | 16:00-18:00 | -11.73 | -9.64 | -8.73 | ||
| 18:00-20:00 | -9.63 | -6.95 | -6.25 | 18:00-20:00 | -13.22 | -10.75 | -9.25 | ||
| 2022-08-15 | 6:00-8:00 | -10.99 | -8.98 | -7.81 | 2022-10-15 | 6:00-8:00 | -15.48 | -11.99 | -10.53 |
| 8:00-10:00 | -10.01 | -8.36 | -7.10 | 8:00-10:00 | -13.72 | -10.47 | -9.04 | ||
| 10:00-12:00 | -8.90 | -7.59 | -6.38 | 10:00-12:00 | -12.60 | -10.08 | -8.92 | ||
| 12:00-14:00 | -8.05 | -7.02 | -6.03 | 12:00-14:00 | -11.17 | -9.20 | -8.32 | ||
| 14:00-16:00 | -8.71 | -7.56 | -6.47 | 14:00-16:00 | -11.21 | -9.44 | -8.59 | ||
| 16:00-18:00 | -9.58 | -7.90 | -6.82 | 16:00-18:00 | -12.93 | -10.21 | -9.14 | ||
| 18:00-20:00 | -10.17 | -8.36 | -7.08 | 18:00-20:00 | -15.29 | -12.21 | -10.83 |
Fig. 7 Relationships of atmospheric water vapor oxygen isotope value (δ18O) with environmental factors. Orange, growing season (July to August); blue, leaf senescence period (September to October). Solid lines, linear regression fits.
Fig. 8 Contribution rate of transpiration to evapotranspiration in Larix gmelinii forest (mean ± SD). A, July 15th. B, August 15th. C, September 15th. D, October 15th. δT-NSS, oxygen stable isotope ratio (δ18O) of plant transpiration vapor under Non-Steady-Stateconditions; δT-ISS, the δ18O of plant transpiration vapor under isotope steady-stateconditions; FT, the contribution of plant transpiration to evapotranspiration.
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