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Porous Frameworks: Pores, Guests and Stability

Build a solid out of nodes and linkers and the empty space becomes the useful part. Pore size and the chemistry of the internal surface decide which guest goes in, how strongly it is held and whether the framework survives its removal.

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What a learner can do afterwards

  • Relates node connectivity and linker geometry to possible networks without assuming they determine a unique topology
  • Reads an adsorption isotherm, compares affinity under stated conditions and estimates pore volume using a stated adsorbed-phase density
  • Explains why some frameworks collapse when the solvent is removed and how that is avoided
  • Matches a separation or storage problem to a framework property that would address it

1 · Read

A node is a connection point; a linker bridges nodes. Together they form a network. Topology describes its connections. Geometry does not select a unique topology: different or interpenetrating networks can form. Longer linkers may enlarge pores, but topology or interpenetration can prevent this. Larger pores can weaken guest confinement or mechanical stability. Check accessible pore size, uptake and stability rather than assuming longer is better.

Try it together

Guests are molecules or ions in pores. Attraction holds them at surfaces during adsorption. Polar molecules have permanent charge separation; dispersion comes from fluctuating charge. Confinement brings guests close to pore walls. If two similar-sized gases both enter and dipole forces dominate, polar walls may adsorb the polar gas more strongly. This can help separation, but polarity alone does not guarantee it. Test mixture adsorption and transport at the intended temperature and pressure.

blocked pores: no entryopen pores: guest entryinternal surface: uptake
Accessible openings let guests reach internal surfaces and adsorb. Sealed cavities do not provide that access.

Liquid-vapour interfaces during drying can create capillary stress and collapse fragile frameworks. Supercritical drying avoids that interface; solvent exchange or rigid frameworks can also reduce risk. Lost uptake alone does not prove collapse: blockage or decomposition are alternatives. Check structure and composition.

For low-pressure methane uptake, test accessible pores near methane's size with attractive walls. Methane is nonpolar; dispersion and confinement matter. Uptake does not equal usable storage capacity. Gas must also be released, so stronger binding alone need not improve usable capacity.

An adsorption isotherm plots uptake against pressure at fixed temperature. A saturation plateau in mmol/g measures adsorbed amount per sample mass, not pore volume or binding energy. Initial slope reflects affinity and site number; binding comparisons need the same gas, temperature and comparable sites.

Estimate pore volume by converting saturated uptake to adsorbed mass, then dividing by an assumed adsorbed-phase density. For 2 mmol/g, molar mass 44 g/mol and density 0.88 g/cm3: 0.002 x 44 = 0.088 g/g; 0.088 / 0.88 = 0.10 cm3/g. The estimate depends on that density assumption.

Check pore access, guest interactions and stability. Isotherms measure uptake; pore-volume and binding estimates need stated assumptions.

Porous-framework explanations, access diagrams and questions were written for this project.

2 · Watch

En anglais

Take it off screen

Print a worksheetA4 with an answer key page for grown-ups. No screen, no internet.

Where it sits

Then practise

8 questions wait behind this lesson, each with its answer explained. Every answer feeds the sky: stars light as they are learned, and dim when it is time to come back.

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Porous Frameworks: Pores, Guests and Stability · Science, ages 22 to 23 · LightMySky