The temperature within the Earth’s crust increases about 1.0 C° for each 30 m of depth. The thermal conductivity of the crust is 0.80 J/s C°. Determine the heat transferred from the interior to the surface for the entire Earth in 1.0 h.
Ch. 19 - Heat and the First Law of Thermodynamics
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Giancoli Douglas 5th edition
Ch. 19 - Heat and the First Law of Thermodynamics
Problema 99d
Giancoli Douglas 5th edition
Ch. 19 - Heat and the First Law of Thermodynamics
Problema 99dCapitolo 19, Problema 99d
Calculate what will happen when 1000 J of heat is added to 100 grams of water at 100°C.
Guida verificata passo dopo passo1
Step 1: Identify the key concepts involved in the problem. Here, the problem involves heat transfer, phase change, and the specific heat of water. Since the water is already at 100°C, any additional heat will go into changing the phase of water from liquid to vapor (boiling), not increasing its temperature.
Step 2: Recall the formula for heat transfer during a phase change: , where is the heat added, is the mass of the substance, and is the latent heat of vaporization. For water, the latent heat of vaporization is approximately .
Step 3: Convert the mass of water from grams to kilograms if necessary. In this case, the mass is already given in grams (), so no conversion is needed.
Step 4: Use the formula to determine how much of the water will vaporize. Rearrange the formula to solve for the mass of water vaporized: . Substitute and into the equation.
Step 5: Calculate the result to determine how much of the 100 grams of water will vaporize. If the heat provided is insufficient to vaporize all the water, the remaining water will stay in liquid form. Ensure the units are consistent throughout the calculation.

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Specific Heat Capacity
Specific heat capacity is the amount of heat required to raise the temperature of a unit mass of a substance by one degree Celsius. For water, this value is approximately 4.18 J/g°C. Understanding this concept is crucial for calculating temperature changes when heat is added or removed from a substance.
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Specific Heat & Temperature Changes
Phase Changes
Phase changes occur when a substance transitions between solid, liquid, and gas states, often involving significant energy transfer without a temperature change. For water, adding heat at 100°C can lead to boiling, where the temperature remains constant while the water changes from liquid to vapor, requiring additional energy known as the latent heat of vaporization.
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Latent Heat & Phase Changes
Thermodynamics
Thermodynamics is the branch of physics that deals with heat, work, and energy transfer. It encompasses laws that describe how energy is conserved and transformed. In this context, understanding the first law of thermodynamics helps explain how the added heat affects the water's temperature and phase, ensuring energy conservation throughout the process.
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The First Law of Thermodynamics
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