How to resolve the heating and cooling of an object?

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Discussion Overview

The discussion revolves around the heating and cooling of an object, particularly how to model the simultaneous processes of heating and cooling when an object is subjected to a constant heat input while also losing heat to the environment. Participants explore the implications of Newton's law of cooling in this context and seek to combine equations for a comprehensive understanding.

Discussion Character

  • Exploratory
  • Technical explanation
  • Mathematical reasoning

Main Points Raised

  • One participant proposes a scenario where an object's heat energy increases at a rate of 2 degrees or 2 Joules per second, questioning how to incorporate cooling into this model.
  • Another participant suggests that the sign of the temperature difference determines the slope of the heat transfer rate, implying that the mathematics can handle the heating and cooling without separate equations.
  • A participant expresses uncertainty about the application of Newton's law of cooling, noting that it typically assumes a starting temperature above the ambient temperature and questions if a different equation is needed when starting at ambient temperature while applying heat.
  • One participant introduces a general equation relating the rate of heat input and output to the rate of change in stored heat, emphasizing the importance of keeping track of signs in the equations.
  • Another participant points out that the initial equation presented may not adequately account for the complexities of a system with both a heat source and a heat sink, suggesting that additional variables may need to be considered.

Areas of Agreement / Disagreement

Participants express differing views on how to model the heating and cooling processes, with no consensus on a single approach or equation that adequately addresses the scenario presented. The discussion remains unresolved regarding the best way to combine the equations for heating and cooling.

Contextual Notes

Participants highlight the need to consider the changing temperature difference over time and the implications of starting at ambient temperature, which may introduce complexities not fully addressed in the initial equations. There is also a mention of the limitations of the equations in specific scenarios, such as those involving heat transfer in environments with varying conditions.

fishspawned
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I am not sure how to proceed. This is just something that i have been thinking about and would love a little help with.

Lets say I have a situation where i am increasing an object's heat energy at some specific rate - for arguments sake, it's 2 degrees every second. If you like we can also rewrite this as an increase of energy of 2 Joules every second. Either will be fine.

let's make it super simple and call it:

dQ/dt [warming] = 2

I am wondering how to incorporate cooling. While this object is being warmed, it is also being cooled.

Newtons 's law of cooling is a function of time with a fixed beginning and ending temperature.

dQ/dt [cooling] = h x A x (T(t) - Tenv)

here h is the transfer coefficient, A is the transfer area, T is the temperature at a certain time, and Tenv is the ambient room temperature.


But what if you are simply starting from room temperature and raising it over time? The rate of cooling is changing as the temperature difference is changing due to the warming.

Is there an appropriate approach to this problem that would determine how much more time it would take for an object to warm to a certain temperature if we also included cooling into the picture? How can i combine the two equations in a sensible way?]

Any help would be greatly appreciated. Thanks
 
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The sign of the Temperature Difference is what determines the slope of dQ/dt. As with most other formulae, we don't have different equations for heating /cooling, traveling forwards/ backwards, filling / emptying a bucket; the Maths takes care of it all.
 
Perhaps I'm not completely understanding what you are saying, and my apologies for that.
The law of cooling seems to first assume you are at some temperature above Tenv and then will cool down - in the absence of any other heat in or out of the system. (If i am wrong in this, please let me know)

So what I am asking is if there is a different form of the equation if you are starting initially at Tenv but slowly apply heat energy [in which at the same time the object is also experiencing cooling as the temperature is raising.]

Just to be clear - i am suggesting that an outside source is providing additional heat to the system at a constant rate.
 
rate of heat in minus rate of heat out equals rate of change in stored heat. Normally considered as

dQin/dt - dQout/dt = M Cp dT/dt

Where M is the mass of your object, Cp is its specific heat, and T is its temperature (which is a function of time). Keep track of the signs, as @sophiecentaur says, and everything will work out right.
 
fishspawned said:
in which at the same time the object is also experiencing cooling as the temperature is raising
I think I can see your problem. The above statement is implicitly including a source plus a sink for the heat (an extra variable) What your initial equation is telling you is how quickly it will cool down in cold water and it will tell you how quickly it will warm up in hot water (no other heat path involved). That equation of yours is not sufficient for a heater in a room with thin walls (for instance), which is your additional bit.
 

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