Source
Hierarchically porous metal–organic frameworks with red topology for hydrogen and methane storage PRIMARY_TEXT
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FETCHED at 2026-09-29T03:57:04Z · https://www.nature.com/articles/s44160-026-01163-9?error=cookies_not_supported&code=b88fdddf-2994-4073-95c8-48c7edc7e29a · seq 24806
| Excerpt | Finding |
|---|---|
| CU-6-Fe and CU-6-Cr exhibit an interconnected hierarchical pore system with Brunauer–Emmett–Teller surface areas up to 7,145 m2 g−1. | normalized — the passage is on the page once typography is folded together |
| CU-6-Fe and CU-6-Cr exhibit gravimetric H2 uptakes of 17.5 and 15.9 wt%, respectively, at 100 bar and 77 K, while maintaining high volumetric uptakes of 45.4... | not found — this server looked at the page and did not find the passage |
| At 80 bar, CU-6-Fe and CU-6-Cr show total gravimetric CH4 uptakes of 0.67, 0.59 and 0.53 g g−1, and 0.63, 0.56 and 0.50 g g−1, at 273, 288 and 298 K, respect... | not found — this server looked at the page and did not find the passage |
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Locations
| Locator | Excerpt |
|---|---|
QUOTE {} | CU-6-Fe and CU-6-Cr exhibit an interconnected hierarchical pore system with Brunauer–Emmett–Teller surface areas up to 7,145 m2 g−1. |
QUOTE {} | CU-6-Fe and CU-6-Cr exhibit gravimetric H2 uptakes of 17.5 and 15.9 wt%, respectively, at 100 bar and 77 K, while maintaining high volumetric uptakes of 45.4 and 45.5 g l−1. |
QUOTE {} | At 80 bar, CU-6-Fe and CU-6-Cr show total gravimetric CH4 uptakes of 0.67, 0.59 and 0.53 g g−1, and 0.63, 0.56 and 0.50 g g−1, at 273, 288 and 298 K, respectively. |