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1942
ContentsPageTable 161. Heat capacity of minerals2282. Heat capacity of rocks2353. Heats of transformation and of fusion2374. Heat capacity of gases241 Heat capacities of minerals.—In the tables (in this section), the minerals are classified according to the first elements of their chemical formulae; for example, albite (NaAlSi 8O 8) will
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ContentsPageTable 161. Heat capacity of minerals2282. Heat capacity of rocks2353. Heats of transformation and of fusion2374. Heat capacity of gases241 Heat capacities of minerals.—In the tables (in this section), the minerals are classified according to the first elements of their chemical formulae; for example, albite (NaAlSi 8O 8) will
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1966
One of the earliest empirical generalizations concerning the specific heat of solids was enunciated by Dulong and Petit in 1819. Its theoretical justification was advanced by Boltzmann in 1871, and in 1907 Einstein showed why it failed at low temperatures. These dates are among the principal landmarks in the study of specific heats.
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One of the earliest empirical generalizations concerning the specific heat of solids was enunciated by Dulong and Petit in 1819. Its theoretical justification was advanced by Boltzmann in 1871, and in 1907 Einstein showed why it failed at low temperatures. These dates are among the principal landmarks in the study of specific heats.
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