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1

Jiarun, Yin. "Stable carbon and oxygen isotopes in Jurassic shells as palaeosalinity indicators." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1991, no. 3 (1991): 163–76. http://dx.doi.org/10.1127/njgpm/1991/1991/163.

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2

Bashkin, James K., and Patrick J. Kinlen. "Oxygen-stable ferrocene reference electrodes." Inorganic Chemistry 29, no. 22 (1990): 4507–9. http://dx.doi.org/10.1021/ic00347a034.

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3

Wang, Zhenbin, Ya-Rong Zheng, Ib Chorkendorff, and Jens K. Nørskov. "Acid-Stable Oxides for Oxygen Electrocatalysis." ACS Energy Letters 5, no. 9 (2020): 2905–8. http://dx.doi.org/10.1021/acsenergylett.0c01625.

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4

Lacey, Steven D., Qi Dong, Zhennan Huang, et al. "Stable Multimetallic Nanoparticles for Oxygen Electrocatalysis." Nano Letters 19, no. 8 (2019): 5149–58. http://dx.doi.org/10.1021/acs.nanolett.9b01523.

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5

Hayward, James A., Daniel M. Levine, Lawrence Neufeld, Sanford R. Simon, David S. Johnston, and Dennis Chapman. "Polymerized liposomes as stable oxygen-carriers." FEBS Letters 187, no. 2 (1985): 261–66. http://dx.doi.org/10.1016/0014-5793(85)81255-2.

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6

Jain, Ankit, Zhenbin Wang, and Jens K. Nørskov. "Stable Two-Dimensional Materials for Oxygen Reduction and Oxygen Evolution Reactions." ACS Energy Letters 4, no. 6 (2019): 1410–11. http://dx.doi.org/10.1021/acsenergylett.9b00876.

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7

Shimizu, K., T. Sawano, T. Tokuda, S. Yoshida, and I. Tanaka. "High‐power stable chemical oxygen iodine laser." Journal of Applied Physics 69, no. 1 (1991): 79–83. http://dx.doi.org/10.1063/1.347660.

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8

Jayaraman, Ambalavanan, and Ralph T. Yang. "Stable oxygen-selective sorbents for air separation." Chemical Engineering Science 60, no. 3 (2005): 625–34. http://dx.doi.org/10.1016/j.ces.2004.08.032.

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9

Darmanyan, Alexander P., and Alexander S. Tatikolov. "Singlet oxygen quenching by stable nitroxy radicals." Journal of Photochemistry 32, no. 2 (1986): 157–63. http://dx.doi.org/10.1016/0047-2670(86)87005-8.

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10

Liu, Fei, Yaqi Ren, and Xixi Ji. "Nanosheet-Structured Boron Carbon Nitride Spheres as Stable Electrocatalyst Support for Oxygen Reduction Reaction." International Journal of Materials Science and Engineering 5, no. 4 (2017): 123–32. http://dx.doi.org/10.17706/ijmse.2017.5.4.123-132.

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11

Pack, Andreas, Stephan Hoernes, Matthias Göbbels, Rainer Bross, and Andreas Buhr. "Stable oxygen isotopes - A new approach for tracing the origin of oxide inclusions in steels." European Journal of Mineralogy 17, no. 3 (2005): 483–93. http://dx.doi.org/10.1127/0935-1221/2005/0017-0483.

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12

Treydte, Kerstin, Jan Esper, and Holger Gärtner. "Stabile Isotope in der Dendroklimatologie | Stable isotopes and dendroclimatology." Schweizerische Zeitschrift fur Forstwesen 155, no. 6 (2004): 222–32. http://dx.doi.org/10.3188/szf.2004.0222.

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This paper expounds the basics of isotope fixation in tree rings and relevant field and laboratory procedures. Examples from high mountain regions show both the potential and limits of employing these methods in dendroclimatological studies. Carbon isotopes yield seasonally resolved information on temperature,precipitation and relative humidity, whilst oxygen isotopes provide information on the isotope values of the source water,and thus, on precipitation. Inter-annual and decadal variations, in particular, reflect a strong common climatic signal that extends across a wide range of site ecologies. However, low frequency trends are masked by a non-climatic, human induced long-term trend, especially where carbon isotopes are concerned. At present,detrending methods are of a provisional nature and set a limit to stable isotopes for paleoclimatic questions. Highly resolved plant physiological and biochemical investigations should provide more insight into these unsolved problems.
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13

Saito, Mineo, and Atsushi Oshiyama. "Stable atomic geometries of oxygen microclusters in silicon." Physical Review B 38, no. 15 (1988): 10711–17. http://dx.doi.org/10.1103/physrevb.38.10711.

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14

Li, Yiming, Lei Li, Longfeng Zhu, Li Gu, and Xuebo Cao. "Interlocked multi-armed carbon for stable oxygen reduction." Chemical Communications 52, no. 32 (2016): 5520–22. http://dx.doi.org/10.1039/c6cc01095d.

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15

Wu, Shichao, Yu Qiao, Kezhu Jiang, Yibo He, Shaohua Guo, and Haoshen Zhou. "Tailoring Sodium Anodes for Stable Sodium-Oxygen Batteries." Advanced Functional Materials 28, no. 13 (2018): 1706374. http://dx.doi.org/10.1002/adfm.201706374.

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16

Zolper, John C., Albert G. Baca, and Scott A. Chalmers. "Thermally stable oxygen implant isolation ofp‐type Al0.2Ga0.8As." Applied Physics Letters 62, no. 20 (1993): 2536–38. http://dx.doi.org/10.1063/1.109288.

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17

Giustini, Francesca, Mauro Brilli, and Antonio Patera. "Mapping oxygen stable isotopes of precipitation in Italy." Journal of Hydrology: Regional Studies 8 (December 2016): 162–81. http://dx.doi.org/10.1016/j.ejrh.2016.04.001.

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18

Swart, Peter K., and Jim J. Leder. "The utility of stable isotopic signatures in coral skeletons." Paleontological Society Papers 1 (October 1996): 249–91. http://dx.doi.org/10.1017/s1089332600000127.

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There is a fundamental ecologic differentiation between zooxanthellate and non-zooxanthellate corals. This paper reviews factors which govern the stable carbon and oxygen isotopic composition of these groups of corals. Although the stable carbon and oxygen isotope compositions of coral skeletons are strongly influenced by environmental and physiological factors, the precise mechanisms remain a matter of debate. In particular the oxygen isotopic composition is known to be governed by the temperature and the oxygen isotopic composition of the water and perhaps also by kinetic factors. In contrast the carbon isotopic composition is controlled by a combination of photosynthesis, respiration, autotrophy, heterotrophy, and the isotopic composition of dissolved inorganic carbon. Using a combination of carbon and oxygen isotopes it is possible to distinguish zooxanthellate from non-zooxanthellate corals.
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19

Matsuzaki, Kenji M., Hiroshi Nishi, Hiroki Hayashi, et al. "Radiolarian biostratigraphic scheme and stable oxygen isotope stratigraphy in southern Japan (IODP Expedition 315 Site C0001)." Newsletters on Stratigraphy 47, no. 1 (2014): 107–30. http://dx.doi.org/10.1127/0078-0421/2014/0044.

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20

DeSantis, L. R. G., and C. Hedberg. "Stable isotope ecology of the koala (Phascolarctos cinereus)." Australian Journal of Zoology 64, no. 5 (2016): 353. http://dx.doi.org/10.1071/zo16057.

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Australia has undergone significant climate change, both today and in the past. Koalas, due to their restricted diet of predominantly eucalyptus leaves and limited drinking behaviour may serve as model organisms for assessing past climate change via stable isotopes of tooth enamel. Here, we assess whether stable carbon and oxygen isotopes from tooth enamel record known climate variables, including proxies of relative aridity (e.g. mean annual precipitation, mean annual maximum temperature, and relative humidity). The results demonstrate significant negative relationships between oxygen isotope values and both relative humidity and mean annual precipitation, proxies for relative aridity. The best model for predicting enamel oxygen isotope values incorporates mean annual precipitation and modelled oxygen isotope values of local precipitation. These data and the absence of any relationship between modelled oxygen isotope precipitation values, independently, suggest that koalas do not track local precipitation values but instead record relative aridity. The lack of significant relationships between carbon isotopes and climate variables suggests that koalas may instead be tracking the density of forests and/or their location in the canopy. Collectively, these data suggest that koalas are model organisms for assessing relative aridity over time – much like kangaroos.
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21

Helman, Yael, Eugeni Barkan, Doron Eisenstadt, Boaz Luz, and Aaron Kaplan. "Fractionation of the Three Stable Oxygen Isotopes by Oxygen-Producing and Oxygen-Consuming Reactions in Photosynthetic Organisms." Plant Physiology 138, no. 4 (2005): 2292–98. http://dx.doi.org/10.1104/pp.105.063768.

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22

Barbour, Margaret M. "Stable oxygen isotope composition of plant tissue: a review." Functional Plant Biology 34, no. 2 (2007): 83. http://dx.doi.org/10.1071/fp06228.

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With the development of rapid measurement techniques, stable oxygen isotope analysis of plant tissue is poised to become an important tool in plant physiological, ecological, paleoclimatic and forensic studies. Recent advances in mechanistic understanding have led to the improvement of process-based models that accurately predict variability in the oxygen isotope composition of plant organic material (δ18Op). δ18Op has been shown to reflect the isotope composition of soil water, evaporative enrichment in transpiring leaves, and isotopic exchange between oxygen atoms in organic molecules and local water in the cells in which organic molecules are formed. This review presents current theoretical models describing the influences on δ18Op, using recently published experimental work to outline strengths and weaknesses in the models. The potential and realised applications of the technique are described.
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23

Zakem, Emily J., Amala Mahadevan, Jonathan M. Lauderdale, and Michael J. Follows. "Stable aerobic and anaerobic coexistence in anoxic marine zones." ISME Journal 14, no. 1 (2019): 288–301. http://dx.doi.org/10.1038/s41396-019-0523-8.

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Abstract Mechanistic description of the transition from aerobic to anaerobic metabolism is necessary for diagnostic and predictive modeling of fixed nitrogen loss in anoxic marine zones (AMZs). In a metabolic model where diverse oxygen- and nitrogen-cycling microbial metabolisms are described by underlying redox chemical reactions, we predict a transition from strictly aerobic to predominantly anaerobic regimes as the outcome of ecological interactions along an oxygen gradient, obviating the need for prescribed critical oxygen concentrations. Competing aerobic and anaerobic metabolisms can coexist in anoxic conditions whether these metabolisms represent obligate or facultative populations. In the coexistence regime, relative rates of aerobic and anaerobic activity are determined by the ratio of oxygen to electron donor supply. The model simulates key characteristics of AMZs, such as the accumulation of nitrite and the sustainability of anammox at higher oxygen concentrations than denitrification, and articulates how microbial biomass concentrations relate to associated water column transformation rates as a function of redox stoichiometry and energetics. Incorporating the metabolic model into an idealized two-dimensional ocean circulation results in a simulated AMZ, in which a secondary chlorophyll maximum emerges from oxygen-limited grazing, and where vertical mixing and dispersal in the oxycline also contribute to metabolic co-occurrence. The modeling approach is mechanistic yet computationally economical and suitable for global change applications.
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24

Morales, Dulce M., Mariya A. Kazakova, Maximilian Purcel, Justus Masa, and Wolfgang Schuhmann. "The sum is more than its parts: stability of MnFe oxide nanoparticles supported on oxygen-functionalized multi-walled carbon nanotubes at alternating oxygen reduction reaction and oxygen evolution reaction conditions." Journal of Solid State Electrochemistry 24, no. 11-12 (2020): 2901–6. http://dx.doi.org/10.1007/s10008-020-04667-2.

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Abstract Successful design of reversible oxygen electrocatalysts does not only require to consider their activity towards the oxygen reduction (ORR) and the oxygen evolution reactions (OER), but also their electrochemical stability at alternating ORR and OER operating conditions, which is important for potential applications in reversible electrolyzers/fuel cells or metal/air batteries. We show that the combination of catalyst materials containing stable ORR active sites with those containing stable OER active sites may result in a stable ORR/OER catalyst if each of the active components can satisfy the current demand of their respective reaction. We compare the ORR/OER performances of oxides of Mn (stable ORR active sites), Fe (stable OER active sites), and bimetallic Mn0.5Fe0.5 (reversible ORR/OER catalyst) supported on oxidized multi-walled carbon nanotubes. Despite the instability of Mn and Fe oxide for the OER and the ORR, respectively, Mn0.5Fe0.5 exhibits high stability for both reactions.
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25

Song, Shidong, Wu Xu, Ruiguo Cao, et al. "B4C as a stable non-carbon-based oxygen electrode material for lithium-oxygen batteries." Nano Energy 33 (March 2017): 195–204. http://dx.doi.org/10.1016/j.nanoen.2017.01.042.

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26

Xiong, Jie, Hong Zhong, Jing Li, et al. "Engineering highly active oxygen sites in perovskite oxides for stable and efficient oxygen evolution." Applied Catalysis B: Environmental 256 (November 2019): 117817. http://dx.doi.org/10.1016/j.apcatb.2019.117817.

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27

Childress, J. J., and B. A. Seibel. "Life at stable low oxygen levels: adaptations of animals to oceanic oxygen minimum layers." Journal of Experimental Biology 201, no. 8 (1998): 1223–32. http://dx.doi.org/10.1242/jeb.201.8.1223.

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Zones of minimum oxygen level are found at intermediate depths in most of the world's oceans and, although the oxygen partial pressure in some of these 'oxygen minimum layers' is only a fraction of a kilopascal, populations of pelagic metazoans exist there. These oxygen minimum layers are areas of the water column and the associated benthos with stable conditions of continuously low oxygen level and low temperature at intermediate depths (400-1000 m depth) over vast areas. Off California, where PO2 at the oxygen minimum is 0.8 kPa, there are abundant populations of animals both in the water column and on the bottom. Farther to the south in the eastern tropical Pacific, oxygen partial pressures of less than approximately 0.4 kPa result in very low biomasses and diversity of animals at minimum layer depths. At the minimum oxygen levels found off California, most animals which inhabit the minimum zones appear to support their routine metabolic demands via aerobic metabolism. They do this by being very effective at removing oxygen from water. Among the adaptations of pelagic crustaceans to these conditions are: (1) enhanced ventilatory abilities, (2) enhanced percentage removal of O2 from the ventilatory stream, (3) large gill surface areas, (4) short diffusion distances from the water to the blood, and (5) hemocyanin respiratory proteins with a very high affinity for O2, high cooperativity and large Bohr effects. The lower O2 consumption rates of many deeper-living species are also functionally adaptive in that they facilitate aerobic survival at low PO2. However, they are not adaptations to the minimum layer, since similarly low rates are found in the same and comparable species living at the same depths in regions without well-developed minima, and these animals are unable to survive at the low PO2 values of the minima. While anaerobic metabolism may be important for metabolic rates above the routine level for most animals in the minimum layer, there is little evidence for the use of sustained anaerobiosis in the species studied. In summary, given the stable presence of very low O2 levels in the minima, the primary adaptations of animals living within them are those that support aerobic metabolism by giving the animals remarkable abilities to extract O2 from water. These abilities are notably better than those of animals adapted to unstable hypoxic environments, such as intertidal mudflats, while the latter animals rely to a much greater extent on anaerobiosis and perhaps on metabolic suppression to survive periods of anoxia.
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28

Ray, Jyotiranjan S., and R. Ramesh. "Stable Carbon and Oxygen Isotopic Compositions of Indian Carbonatites." International Geology Review 48, no. 1 (2006): 17–45. http://dx.doi.org/10.2747/0020-6814.48.1.17.

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29

Krauz, Ph, E. V. K. Rao, H. Thibierge, and J. C. Harmand. "Highly thermally stable electrical compensation in oxygen implantedp‐InAlAs." Applied Physics Letters 62, no. 8 (1993): 867–69. http://dx.doi.org/10.1063/1.108549.

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30

Wellington, G. M., R. B. Dunbar, and G. Merlen. "Calibration of stable oxygen isotope signatures in Galápagos corals." Paleoceanography 11, no. 4 (1996): 467–80. http://dx.doi.org/10.1029/96pa01023.

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31

van der Giessen, Lianne, Marije Bakker, Koen Joosten, Wim Hop, and Harm Tiddens. "Nocturnal oxygen saturation in children with stable cystic fibrosis." Pediatric Pulmonology 47, no. 11 (2012): 1123–30. http://dx.doi.org/10.1002/ppul.22537.

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32

Murin, L. I., V. A. Gurinovich, I. F. Medvedeva, and V. P. Markevich. "Thermally stable carbon–oxygen complexes in irradiated silicon crystals." Inorganic Materials: Applied Research 7, no. 2 (2016): 192–95. http://dx.doi.org/10.1134/s2075113316020143.

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33

Coplen, T. B. "Reporting of stable hydrogen, carbon, and oxygen isotopic abundances." Geothermics 24, no. 5-6 (1995): 707–12. http://dx.doi.org/10.1016/0375-6505(95)00024-0.

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34

Fleischer, Maximilian, and Hans Meixner. "Oxygen sensing with long-term stable Ga2O3 thin films." Sensors and Actuators B: Chemical 5, no. 1-4 (1991): 115–19. http://dx.doi.org/10.1016/0925-4005(91)80230-h.

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35

Hussein, Khaled, Atef Farouk Alkarn, Raafat El-Sokkary, Samiaa Hamdy, and Hamdy Shams. "Factors predicting exercise-induced oxygen desaturation in stable COPD." Egyptian Journal of Chest Diseases and Tuberculosis 62, no. 1 (2013): 59–63. http://dx.doi.org/10.1016/j.ejcdt.2013.02.009.

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36

Aljabour, Abdalaziz. "Highly Stable Co3O4 Nanofibers in Alkaline Oxygen Evolution Reaction." ECS Meeting Abstracts MA2021-01, no. 50 (2021): 2068. http://dx.doi.org/10.1149/ma2021-01502068mtgabs.

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37

Zhang, Shan-Lin, Dalton Cox, Hao Yang та ін. "High stability SrTi1−xFexO3−δ electrodes for oxygen reduction and oxygen evolution reactions". Journal of Materials Chemistry A 7, № 37 (2019): 21447–58. http://dx.doi.org/10.1039/c9ta07548h.

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38

Kwak, Won-Jin, Jiwon Park, Trung Thien Nguyen, et al. "A dendrite- and oxygen-proof protective layer for lithium metal in lithium–oxygen batteries." Journal of Materials Chemistry A 7, no. 8 (2019): 3857–62. http://dx.doi.org/10.1039/c8ta11941d.

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39

Sudayama, Takaaki, Kazuki Uehara, Takahiro Mukai, et al. "Multiorbital bond formation for stable oxygen-redox reaction in battery electrodes." Energy & Environmental Science 13, no. 5 (2020): 1492–500. http://dx.doi.org/10.1039/c9ee04197d.

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40

Rice, K. L., M. F. Schmidt, J. S. Buan, F. Lebahn, and T. K. Schwarzock. "AccuO2 Oximetry-Driven Oxygen-Conserving Device Versus Fixed-Dose Oxygen Devices in Stable COPD Patients." Respiratory Care 56, no. 12 (2011): 1901–5. http://dx.doi.org/10.4187/respcare.01059.

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41

Quiñones-Rivera, ZJ, B. Wissel, D. Justić, and B. Fry. "Partitioning oxygen sources and sinks in a stratified, eutrophic coastal ecosystem using stable oxygen isotopes." Marine Ecology Progress Series 342 (July 24, 2007): 69–83. http://dx.doi.org/10.3354/meps342069.

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42

Schimmelmann, Arndt, and Michael J. DeNiro. "Determination of oxygen stable isotope ratios in organic matter containing carbon, hydrogen, oxygen, and nitrogen." Analytical Chemistry 57, no. 13 (1985): 2644–46. http://dx.doi.org/10.1021/ac00290a048.

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43

BRENT, B. N., R. A. MATTHAY, D. A. MAHLER, H. J. BERGER, B. L. ZARET, and G. LISTER. "Relationship Between Oxygen Uptake and Oxygen Transport in Stable Patients with Chronic Obstructive Pulmonary Disease." Survey of Anesthesiology 29, no. 1 (1985): 2. http://dx.doi.org/10.1097/00132586-198502000-00002.

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44

Koo, Sojung, Jaewoon Lee, Jinwoo Lee, Sangho Yoon, and Duho Kim. "Importance of metal−oxygen bond for stable oxygen-redox reaction in Li-excess layered oxides." Energy Storage Materials 42 (November 2021): 764–72. http://dx.doi.org/10.1016/j.ensm.2021.08.024.

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45

Morris, D. E., K. K. Singh, and A. P. B. Sinha. "A novel stable solid formed by C60 + oxygen at high P(O2)." Journal of Materials Research 8, no. 9 (1993): 2273–76. http://dx.doi.org/10.1557/jmr.1993.2273.

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We report the formation of a novel solid form of carbon + oxygen. Exposure of C60 to high oxygen pressure [P(O2) ≍ 100 MPa] for several days at slightly above ambient temperature results in absorption of significant amounts of oxygen (up to ∼48% by weight after 3 days). X-ray diffraction measurements showed that the C60 pellets had become amorphous. Although part of the added weight is slowly lost in flowing oxygen at ambient pressure and temperature, most remains up to at least 100 °C. Heating in flowing He at 200 °C brought the weight back to near the original value. The reaction appears to be specific to C60 since the amorphous outgassed material had lost the capacity to absorb oxygen at high P(O2), and the oxygen absorption effect was absent in powdered graphite and in commercial amorphous carbon. The Raman spectrum differs from those of C60, soot, amorphous carbon, graphite, and diamond.
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46

Cao, Qun, Laura M. Dornan, Luke Rogan, N. Louise Hughes, and Mark J. Muldoon. "Aerobic oxidation catalysis with stable radicals." Chem. Commun. 50, no. 35 (2014): 4524–43. http://dx.doi.org/10.1039/c3cc47081d.

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Selective oxidation reactions are challenging when carried out on an industrial scale. Many traditional methods are undesirable from an environmental or safety point of view. There is a need to develop sustainable catalytic approaches that use molecular oxygen as the terminal oxidant. This review will discuss recent advances in the use of stable radicals in aerobic oxidation catalysis.
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47

Lou, Peili, Zhonghui Cui, and Xiangxin Guo. "Achieving highly stable Li–O2 battery operation by designing a carbon nitride-based cathode towards a stable reaction interface." Journal of Materials Chemistry A 5, no. 34 (2017): 18207–13. http://dx.doi.org/10.1039/c7ta05009g.

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48

Lu, Matthew Y., Justin G. Railsback, Hongqian Wang та ін. "Stable high current density operation of La0.6Sr0.4Co0.2Fe0.8O3−δ oxygen electrodes". Journal of Materials Chemistry A 7, № 22 (2019): 13531–39. http://dx.doi.org/10.1039/c9ta04020j.

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49

Kwak, Won-Jin, Atif Mahammed, Hun Kim, et al. "Controllable and stable organometallic redox mediators for lithium oxygen batteries." Materials Horizons 7, no. 1 (2020): 214–22. http://dx.doi.org/10.1039/c9mh01043b.

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50

Mills, Andrew, Susan Giddings, Ila Patel, and Carl Lawrence. "Thermally activated ruthenium dioxide hydrate. A reproducible, stable oxygen catalyst." Journal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases 83, no. 8 (1987): 2331. http://dx.doi.org/10.1039/f19878302331.

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