Porosity — Cooperative Proton and Li-ion Conduction in a 2D-Layered MOF via Mechanical Insertion of Lithium Halides

Measurement evidence

Porosity

Cooperative Proton and Li-ion Conduction in a 2D-Layered MOF via Mechanical Insertion of Lithium Halides · Sarango-Ramirez M.K., Donoshita M., Yoshida Y. et al. · Angewandte Chemie - International Edition · 2023 · e202301284

4 measurement groups · 8 results

Reported values remain attached to the sample, method, conditions, extraction quality and source location that produced them.

H2O vapour sorption isotherm

Ti-dobdc pristine · Pellet

Activated at 373 K under vacuum (10^-2 Pa) for 4 h; H2O vapour sorption measured at 298 K.

Temperature
298
Atmosphere
H2O vapour
Context
water uptake/hygroscopicity relevant to proton and Li-ion conduction
Measurement source
S2/S8 · Materials and Methods · Figure S6
PropertyReported valueNormalised valueUncertaintyOrigin and qualitySource
H2O uptake near P/P0 = 0.9about 13 mol mol^-1 at P/P0 ~0.9Visual Estimate
Approximate
S8 · Figure S6 · Figure S6c

H2O vapour sorption isotherm

Ti-dobdc-LiBr (MOF:LiBr = 1:1) · Pellet

Activated at 373 K under vacuum (10^-2 Pa) for 4 h; H2O vapour sorption measured at 298 K.

Temperature
298
Atmosphere
H2O vapour
Context
water uptake/hygroscopicity relevant to proton and Li-ion conduction
Measurement source
S2/S8 · Materials and Methods · Figure S6
PropertyReported valueNormalised valueUncertaintyOrigin and qualitySource
LiX sample uptake relative to pristine at P/P0 = 0.9three times higher than pristine Ti-dobdcText
Approximate
3 · Results · Figure S6c
H2O uptake at P/P0 = 0.02approximately six H2O molecules per formula unitText
Approximate
3 · Results · Figure S6a
H2O uptake near P/P0 = 0.9about 34 mol mol^-1 at P/P0 ~0.9Visual Estimate
Approximate
S8 · Figure S6 · Figure S6c

H2O vapour sorption isotherm

Ti-dobdc-LiCl (MOF:LiCl = 1:1) · Pellet

Activated at 373 K under vacuum (10^-2 Pa) for 4 h; H2O vapour sorption measured at 298 K.

Temperature
298
Atmosphere
H2O vapour
Context
water uptake/hygroscopicity relevant to proton and Li-ion conduction
Measurement source
S2/S8 · Materials and Methods · Figure S6
PropertyReported valueNormalised valueUncertaintyOrigin and qualitySource
H2O uptake at P/P0 = 0.02approximately six H2O molecules per formula unitText
Approximate
3 · Results · Figure S6a
H2O uptake near P/P0 = 0.9about 31 mol mol^-1 at P/P0 ~0.9Visual Estimate
Approximate
S8 · Figure S6 · Figure S6c

H2O vapour sorption isotherm

Ti-dobdc-LiI (MOF:LiI = 1:1) · Pellet

Activated at 373 K under vacuum (10^-2 Pa) for 4 h; H2O vapour sorption measured at 298 K.

Temperature
298
Atmosphere
H2O vapour
Context
water uptake/hygroscopicity relevant to proton and Li-ion conduction
Measurement source
S2/S8 · Materials and Methods · Figure S6
PropertyReported valueNormalised valueUncertaintyOrigin and qualitySource
H2O uptake at P/P0 = 0.02approximately six H2O molecules per formula unitText
Approximate
3 · Results · Figure S6a
H2O uptake near P/P0 = 0.9about 29 mol mol^-1 at P/P0 ~0.9Visual Estimate
Approximate
S8 · Figure S6 · Figure S6c