Specific heat capacity, Q = mcθ

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Homework Help Overview

The discussion revolves around a problem related to specific heat capacity, specifically using the equation Q = mcθ to analyze heat transfer between two bodies of water at different temperatures. The original poster presents an attempt to solve for the final temperature, assuming no heat loss to the surroundings.

Discussion Character

  • Exploratory, Assumption checking

Approaches and Questions Raised

  • The original poster attempts to equate the heat absorbed and released to find the final temperature. Some participants question the correctness of the final answer, leading to a debate about the assumptions made regarding heat loss.

Discussion Status

The discussion includes differing opinions on the correct answer to the problem, with some participants asserting that the answer is C, while others seem to agree with this correction. There is also mention of the impact of temperature on the heat capacity of water, suggesting a deeper exploration of the assumptions involved.

Contextual Notes

Participants note that the problem assumes no heat loss to the surroundings, which is a critical aspect of the discussion. Additionally, there is mention of the temperature dependence of water's heat capacity, which may influence the final temperature calculation.

a129

Homework Statement


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Here is the original question (just read the English version).

Homework Equations


Q = mcθ
Specific heat capacity of water, c = 4200 J/kg °C

The Attempt at a Solution


I did Q_(absorbed) = Q_(released)
mcθ = mcθ
mθ = mθ

And I solved for the final temperature, which is 23.33°C. However the correct answer here is A. I'm pretty sure this question is assuming that there is no heat lost to the surroundings.
Thanks!
 

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a129 said:
However the correct answer here is A.
No it isn't. It is C. (You are correct.)
 
Orodruin said:
No it isn't. It is C. (You are correct.)

Thank you!
 
Note that this is true even if you take into account that the heat capacity of water changes slightly decreases with temperature. (It does not change enough for the final temperature to deviate significantly from 23.33 °C.)

Here is a plot of the heat added to the initially 10 °C water and the heat lost by the initially 30 °C water:
upload_2017-11-4_8-46-49.png

The coloured lines are numerical integrations of the tabulated temperature dependent heat capacity of water. The dotted black lines represent the approximation of the heat capacity being 4.2 kJ/kg K. (I used 500 g and 1 kg masses, but only the proportion is relevant for the intersection point in T)
 

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