{"id":108,"date":"2022-12-30T18:15:40","date_gmt":"2022-12-30T18:15:40","guid":{"rendered":"https:\/\/books.gw-project.org\/variable-density-groundwater-flow\/chapter\/solution-exercise-7\/"},"modified":"2023-01-08T04:32:51","modified_gmt":"2023-01-08T04:32:51","slug":"solution-exercise-7","status":"publish","type":"chapter","link":"https:\/\/books.gw-project.org\/variable-density-groundwater-flow\/chapter\/solution-exercise-7\/","title":{"raw":"Solution Exercise 7","rendered":"Solution Exercise 7"},"content":{"raw":"
\r\n

The value for H<\/em> can be obtained from Figure\u00a09<\/a>, with which the Rayleigh number can be calculated as:<\/p>\r\n

[latex]\\displaystyle Ra=\\frac{\\Delta \\rho gkH}{\\mu D_{T}}=\\frac{3\\times 9.81\\times 10^{-10}\\times 100}{1.0\\times 10^{-3}\\times 1.0\\times 10^{-6}}=2.9\\times 10^{2}[\/latex]<\/p>\r\n

Return to <\/span>Exercise <\/span>7<\/span><\/a><\/p>\r\n

<\/p>\r\n\r\n<\/div>","rendered":"

\n

The value for H<\/em> can be obtained from Figure\u00a09<\/a>, with which the Rayleigh number can be calculated as:<\/p>\n

\"\displaystyle Ra=\frac{\Delta \rho gkH}{\mu D_{T}}=\frac{3\times 9.81\times 10^{-10}\times 100}{1.0\times 10^{-3}\times 1.0\times 10^{-6}}=2.9\times 10^{2}\"<\/p>\n

Return to <\/span>Exercise <\/span>7<\/span><\/a><\/p>\n

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