The Nucleation of Ice Formation by Silver Iodide¶
Vonnegut, B. (1947). The Nucleation of Ice Formation by Silver Iodide. Journal of Applied Physics, 18(7), 593-595.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Primes¶
- Nucleation
- The homogeneous-versus-heterogeneous distinction is decisive and practical: a dust speck or a deliberately added seed crystal supplies a pre-existing surface that slashes the surface-energy penalty, lowering the barrier and raising the rate by orders of magnitude — which is exactly why a jeweler drops a seed crystal into rock-candy syrup rather than waiting for spontaneous nucleation.
This sourceEstablishes silver-iodide particles as heterogeneous ice-nucleation sites whose lattice match to ice lowers the barrier and triggers droplet/ice formation — the canonical cloud-seeding / heterogeneous-nucleation case.
Supported in partVerified against the publisher's abstract
Vonnegut's abstract supports heterogeneous ice nucleation by silver-iodide particles via lattice match to ice, but supplies no surface-energy, barrier or rate-magnitude figures and no seed-crystal example.
“It is believed that silver iodide serves as a very effective nucleus because it very closely resembles ice in crystal structure.”
- The homogeneous-versus-heterogeneous distinction is decisive and practical: a dust speck or a deliberately added seed crystal supplies a pre-existing surface that slashes the surface-energy penalty, lowering the barrier and raising the rate by orders of magnitude — which is exactly why a jeweler drops a seed crystal into rock-candy syrup rather than waiting for spontaneous nucleation.
Verification¶
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Registry ID ref:4787e42f2dc7 · see in the full table