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  • 1
    In: Annals of the New York Academy of Sciences, Wiley, Vol. 1522, No. 1 ( 2023-04), p. 74-97
    Abstract: Vegetation and atmosphere processes are coupled through a myriad of interactions linking plant transpiration, carbon dioxide assimilation, turbulent transport of moisture, heat and atmospheric constituents, aerosol formation, moist convection, and precipitation. Advances in our understanding are hampered by discipline barriers and challenges in understanding the role of small spatiotemporal scales. In this perspective, we propose to study the atmosphere–ecosystem interaction as a continuum by integrating leaf to regional scales (multiscale) and integrating biochemical and physical processes (multiprocesses). The challenges ahead are (1) How do clouds and canopies affect the transferring and in‐canopy penetration of radiation, thereby impacting photosynthesis and biogenic chemical transformations? (2) How is the radiative energy spatially distributed and converted into turbulent fluxes of heat, moisture, carbon, and reactive compounds? (3) How do local (leaf‐canopy‐clouds, 1 m to kilometers) biochemical and physical processes interact with regional meteorology and atmospheric composition (kilometers to 100 km)? (4) How can we integrate the feedbacks between cloud radiative effects and plant physiology to reduce uncertainties in our climate projections driven by regional warming and enhanced carbon dioxide levels? Our methodology integrates fine‐scale explicit simulations with new observational techniques to determine the role of unresolved small‐scale spatiotemporal processes in weather and climate models.
    Type of Medium: Online Resource
    ISSN: 0077-8923 , 1749-6632
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2023
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    detail.hit.zdb_id: 211003-9
    detail.hit.zdb_id: 2071584-5
    SSG: 11
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  • 2
    In: Biogeosciences, Copernicus GmbH, Vol. 17, No. 14 ( 2020-07-31), p. 3903-3922
    Abstract: Abstract. Understanding the processes that affect the triple oxygen isotope composition of atmospheric CO2 during gas exchange can help constrain the interaction and fluxes between the atmosphere and the biosphere. We conducted leaf cuvette experiments under controlled conditions using three plant species. The experiments were conducted at two different light intensities and using CO2 with different Δ17O. We directly quantify the effect of photosynthesis on Δ17O of atmospheric CO2 for the first time. Our results demonstrate the established theory for δ18O is applicable to Δ17O(CO2) at leaf level, and we confirm that the following two key factors determine the effect of photosynthetic gas exchange on the Δ17O of atmospheric CO2. The relative difference between Δ17O of the CO2 entering the leaf and the CO2 in equilibrium with leaf water and the back-diffusion flux of CO2 from the leaf to the atmosphere, which can be quantified by the cm∕ca ratio, where ca is the CO2 mole fraction in the surrounding air and cm is the one at the site of oxygen isotope exchange between CO2 and H2O. At low cm∕ca ratios the discrimination is governed mainly by diffusion into the leaf, and at high cm∕ca ratios it is governed by back-diffusion of CO2 that has equilibrated with the leaf water. Plants with a higher cm∕ca ratio modify the Δ17O of atmospheric CO2 more strongly than plants with a lower cm∕ca ratio. Based on the leaf cuvette experiments, the global value for discrimination against Δ17O of atmospheric CO2 during photosynthetic gas exchange is estimated to be -0.57±0.14 ‰ using cm∕ca values of 0.3 and 0.7 for C4 and C3 plants, respectively. The main uncertainties in this global estimate arise from variation in cm∕ca ratios among plants and growth conditions.
    Type of Medium: Online Resource
    ISSN: 1726-4189
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
    detail.hit.zdb_id: 2158181-2
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2022
    In:  Rapid Communications in Mass Spectrometry Vol. 36, No. 12 ( 2022-06-30)
    In: Rapid Communications in Mass Spectrometry, Wiley, Vol. 36, No. 12 ( 2022-06-30)
    Abstract: Oxygen isotope exchange between O 2 and CO 2 in the presence of heated platinum (Pt) is an established technique for determining the δ 17 O value of CO 2 . However, there is not yet a consensus on the associated fractionation factors at the steady state. Methods We determined experimentally the steady‐state α 17 and α 18 fractionation factors for Pt‐catalyzed CO 2 ‐O 2 oxygen isotope exchange at temperatures ranging from 500 to 1200°C. For comparison, the theoretical α 18 equilibrium exchange values reported by Richet et al. (1997) have been updated using the direct sum method for CO 2 and the corresponding α 17 values were determined. Finally, we examined whether the steady‐state fractionation factors depend on the isotopic composition of the reactants, by using CO 2 and O 2 differing in δ 18 O value from −66 ‰ to +4 ‰. Results The experimentally determined steady‐state fractionation factors α 17 and α 18 are lower than those obtained from the updated theoretical calculations (of CO 2 ‐O 2 isotope exchange under equilibrium conditions) by 0.0024 ± 0.0001 and 0.0048 ± 0.0002, respectively. The offset is not due to scale incompatibilities between isotope measurements of O 2 and CO 2 nor to the neglect of non‐Born‐Oppenheimer effects in the calculations. There is a crossover temperature at which enrichment in the minor isotopes switches from CO 2 to O 2 . The direct sum evaluation yields a θ value of ~0.54, i.e. higher than the canonical range maximum for a mass‐dependent fractionation process. Conclusions Updated theoretical values of α 18 for equilibrium isotope exchange are lower than those derived from previous work by Richet et al. (1997). The direct sum evaluation for CO 2 yields θ values higher than the canonical range maximum for mass‐dependent fractionation processes. This demonstrates the need to include anharmonic effects in the calculation and definition of mass‐dependent fractionation processes for poly‐atomic molecules. The discrepancy between the theory and the experimental α 17 and α 18 values may be due to thermal diffusion associated with the temperature gradient in the reactor.
    Type of Medium: Online Resource
    ISSN: 0951-4198 , 1097-0231
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2022
    detail.hit.zdb_id: 2002158-6
    detail.hit.zdb_id: 58731-X
    SSG: 11
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  • 4
    Online Resource
    Online Resource
    Oxford University Press (OUP) ; 2023
    In:  Plant Physiology Vol. 192, No. 2 ( 2023-05-31), p. 1234-1253
    In: Plant Physiology, Oxford University Press (OUP), Vol. 192, No. 2 ( 2023-05-31), p. 1234-1253
    Abstract: Mesophyll conductance to CO2 from the intercellular air space to the CO2–H2O exchange site has been estimated using δ18O measurements (gm18). However, the gm18 estimates are affected by the uncertainties in the δ18O of leaf water where the CO2–H2O exchange takes place and the degree of equilibration between CO2 and H2O. We show that measurements of Δ17O (i.e.Δ17O=δ17O−0.528×δ18O) can provide independent constraints on gm (gmΔ17) and that these gm estimates are less affected by fractionation processes during gas exchange. The gm calculations are applied to combined measurements of δ18O and Δ17O, and gas exchange in two C3 species, sunflower (Helianthus annuus L. cv. ‘sunny’) and ivy (Hedera hibernica L.), and the C4 species maize (Zea mays). The gm18 and gmΔ17 estimates agree within the combined errors (P-value, 0.876). Both approaches are associated with large errors when the isotopic composition in the intercellular air space becomes close to the CO2–H2O exchange site. Although variations in Δ17O are low, it can be measured with much higher precision compared with δ18O. Measuring gmΔ17 has a few advantages compared with gm18: (i) it is less sensitive to uncertainty in the isotopic composition of leaf water at the isotope exchange site and (ii) the relative change in the gm due to an assumed error in the equilibration fraction θeq is lower for gmΔ17 compared with gm18. Thus, using Δ17O can complement and improve the gm estimates in settings where the δ18O of leaf water varies strongly, affecting the δ18O (CO2) difference between the intercellular air space and the CO2–H2O exchange site.
    Type of Medium: Online Resource
    ISSN: 0032-0889 , 1532-2548
    RVK:
    Language: English
    Publisher: Oxford University Press (OUP)
    Publication Date: 2023
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    detail.hit.zdb_id: 208914-2
    SSG: 12
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  • 5
    In: Scientific Reports, Springer Science and Business Media LLC, Vol. 11, No. 1 ( 2021-07-07)
    Abstract: The clumped isotope composition (Δ 47 , the anomaly of the mass 47 isotopologue relative to the abundance expected from a random isotope distribution) of CO 2 has been suggested as an additional tracer for gross CO 2 fluxes. However, the effect of photosynthetic gas exchange on Δ 47 has not been directly determined and two indirect/conceptual studies reported contradicting results. In this study, we quantify the effect of photosynthetic gas exchange on Δ 47 of CO 2 using leaf cuvette experiments with one C 4 and two C 3 plants. The experimental results are supported by calculations with a leaf cuvette model. Our results demonstrate the important roles of the Δ 47 value of CO 2 entering the leaf, kinetic fractionation as CO 2 diffuses into, and out of the leaf and CO 2 –H 2 O isotope exchange with leaf water. We experimentally confirm the previously suggested dependence of Δ 47 of CO 2 in the air surrounding a leaf on the stomatal conductance and back-diffusion flux. Gas exchange can enrich or deplete the Δ 47 of CO 2 depending on the Δ 47 of CO 2 entering the leaf and the fraction of CO 2 exchanged with leaf water and diffused back to the atmosphere, but under typical ambient conditions, it will lead to a decrease in Δ 47 .
    Type of Medium: Online Resource
    ISSN: 2045-2322
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2021
    detail.hit.zdb_id: 2615211-3
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