Temperature-Dependent Heat Capacity At low temperatures, the specific heats of solids are typically proportional to T3. The first understanding of this behavior was due to the Dutch physicist Peter Debye, who in 1912, treated atomic oscillations with the quantum theory that Max Planck had recently used for radiation. For instance, a good approximation for the specific heat 3 of salt, NaCl, is c = 3.33 × 104, J T kg · k(321 K. The constant 321 K is called the Debye temperature of NaCl, Op, and the formula works well when T < 0.040p. Using this formula, how much heat is required to raise the temperature of 24.0 g of NaCl from 5 K to 15 K?

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Temperature-Dependent Heat Capacity At low temperatures, the specific heats of solids are typically proportional to T3. The first understanding of this behavior was due to the Dutch physicist Peter Debye, who in 1912, treated atomic oscillations with the quantum theory that Max Planck had recently used for radiation. For instance, a good approximation for the specific heat of salt, NaCl, is c =3.33× 104 J ⎛ ⎞ kg·k ⎝ T 321 K ΘD, and the formula works well when ⎠ T
Temperature-Dependent Heat Capacity
At low temperatures, the specific heats of solids are typically proportional to T. The first understanding of this
behavior was due to the Dutch physicist Peter Debye, who in 1912, treated atomic oscillations with the quantum
the ory that Max Planck had recently used for radiation. For instance, a good approximation for the specific heat
3
of salt, NaCl, is c = 3.33 x 104,J T
kg · k(321 K)
The constant 321 K is called the Debye temperature of NaCl,
Op, and the formula works well when T < 0.040p. Using this formula, how much heat is required to raise
the temperature of 24.0 g of NaCl from 5 K to 15 K?
Transcribed Image Text:Temperature-Dependent Heat Capacity At low temperatures, the specific heats of solids are typically proportional to T. The first understanding of this behavior was due to the Dutch physicist Peter Debye, who in 1912, treated atomic oscillations with the quantum the ory that Max Planck had recently used for radiation. For instance, a good approximation for the specific heat 3 of salt, NaCl, is c = 3.33 x 104,J T kg · k(321 K) The constant 321 K is called the Debye temperature of NaCl, Op, and the formula works well when T < 0.040p. Using this formula, how much heat is required to raise the temperature of 24.0 g of NaCl from 5 K to 15 K?
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