2021
DOI: 10.1007/s10008-020-04896-5
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Applicability of gas-phase isotope exchange method for investigation of porous materials

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Cited by 3 publications
(2 citation statements)
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“…13,14 Thus, the GPE method was proposed by Ananyev et al to characterize the k tr of porous MIECs using La 0.6 Sr 0.4 MnO 3Àd as an example. 48 The GPE measurement is summarized as follows: (1) changing the oxygen atmosphere by introducing isotopic oxygen ( 18 O 2 ) to the atmosphere with natural oxygen ( 16 O 2 ) after the sample is in equilibrium with natural oxygen at the test temperature. (2) Recording the changes in gas phase 16 O 2 , 16 O 18 O, and 18 O 2 concentrations versus time.…”
Section: Oxygen Isotopic Exchangementioning
confidence: 99%
“…13,14 Thus, the GPE method was proposed by Ananyev et al to characterize the k tr of porous MIECs using La 0.6 Sr 0.4 MnO 3Àd as an example. 48 The GPE measurement is summarized as follows: (1) changing the oxygen atmosphere by introducing isotopic oxygen ( 18 O 2 ) to the atmosphere with natural oxygen ( 16 O 2 ) after the sample is in equilibrium with natural oxygen at the test temperature. (2) Recording the changes in gas phase 16 O 2 , 16 O 18 O, and 18 O 2 concentrations versus time.…”
Section: Oxygen Isotopic Exchangementioning
confidence: 99%
“…Because the composite effect has already been detected, we want to investigate the effect of the triple-phase boundary (TPB) in porous materials on the exchange kinetics. A unique in situ isotope exchange gas-phase equilibration (IE-GPE) method based on isotope 16 O/ 18 O equilibration in the gas phase allows to obtain the intrinsic values of heterogeneous exchange rates and oxygen diffusion. , It is also possible to obtain important information about the oxygen diffusion coefficient, namely, if the diffusion coefficient in the volume does not limit the process, and the diffusion along the grain boundaries is insignificant, then the values are comparable, obtained by the SIMS and IE GPE methods. It has been shown on lanthanum–strontium cobaltites, but for lanthanum–strontium manganites there are discrepancies in values, connected with the essential difference of diffusion coefficients in volume and on grain boundaries of materials .…”
Section: Introductionmentioning
confidence: 99%