Display title | Mason equation |
Default sort key | Mason equation |
Page length (in bytes) | 2,225 |
Namespace ID | 0 |
Page ID | 235693 |
Page content language | en - English |
Page content model | wikitext |
Indexing by robots | Allowed |
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Counted as a content page | Yes |
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Edit | Allow all users (infinite) |
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Page creator | imported>Rjetedi |
Date of page creation | 00:12, 7 February 2024 |
Latest editor | imported>Rjetedi |
Date of latest edit | 00:12, 7 February 2024 |
Total number of edits | 1 |
Recent number of edits (within past 90 days) | 0 |
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Description | Content |
Article description: (description ) This attribute controls the content of the description and og:description elements. | The Mason equation is an approximate analytical expression for the growth (due to condensation) or evaporation of a water droplet—it is due to the meteorologist B. J. Mason. The expression is found by recognising that mass diffusion towards the water drop in a supersaturated environment transports energy... |