Why there is a " > " sign in the entropy of an isolated system

In summary, the conversation discusses the concept of entropy change in an isolated system. It is stated that in such a system, dQ (heat transfer) and dQrev (reversible heat transfer) are both equal to 0. However, the concept of dS>=0 is still applicable in an isolated system. This is because even though dQrev is 0, dQ (not reversible) can still be greater than 0 due to external factors such as friction. The difference between dQrev and dQirrev is also explained, with the example of stirring a viscous fluid given. The definition of a system in this context is also clarified. Finally, the formula for entropy change is mentioned, with an explanation
  • #1
tze liu
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it seems it is not reasonable
Sorry

it said that delta S>=0
in an isolated system. i know why they put " = " sign, but i don't know why it is still possible that dS>0 in an isolated systembecause in an isolated system,it is said that dQ=0 (because no heat transfer between the system and the enviroment?)
by the same logic,dQrev is also 0 in this case
So there should not have " > " sign in an isolated system?
any entropy change in any isolated system is 0 because dQrev is 0
so delat S=0 in an isolated system but not deltaS>=0?
what is the difference between dQrev and dQirrev ?
 

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  • #2
The classical example is that of stirring a viscous fluid with a paddle. Even if the system is thermally isolated, the work done on the system (stirring of the paddle) will be converted into internal energy. Basically, the friction will heat up the system (also no heat is transferred to the system by the boundaries!) . So its entropy will increase. As friction is dependent on velocity, this mechanism is absent when you only allow for reversible changes of the system. So if you want to bring the system from the same initial to the same final state, you have to provide the system with external heat, i.e. this process cannot be done both reversibly and adiabatically.
 
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  • #3
DrDu said:
The classical example is that of stirring a viscous fluid with a paddle. Even if the system is thermally isolated, the work done on the system (stirring of the paddle) will be converted into internal energy. Basically, the friction will heat up the system (also no heat is transferred to the system by the boundaries!) . So its entropy will increase. As friction is dependent on velocity, this mechanism is absent when you only allow for reversible changes of the system. So if you want to bring the system from the same initial to the same final state, you have to provide the system with external heat, i.e. this process cannot be done both reversibly and adiabatically.
but why the dQ (not reversible one) is 0 in such case?
 
  • #4
If you do it, say, in a Dewar, where should the heat come from?
 
  • #5
DrDu said:
The classical example is that of stirring a viscous fluid with a paddle. Even if the system is thermally isolated, the work done on the system (stirring of the paddle) will be converted into internal energy. Basically, the friction will heat up the system (also no heat is transferred to the system by the boundaries!) . So its entropy will increase. As friction is dependent on velocity, this mechanism is absent when you only allow for reversible changes of the system. So if you want to bring the system from the same initial to the same final state, you have to provide the system with external heat, i.e. this process cannot be done both reversibly and adiabatically.
i don't understand why the system is thermally isolated in this case.

can u define what is the "system" here
system means "fluid+paddle+one person that stir the fluid" or "paddle" only if the friction heats up the system that means even dQ is not zero?
because dQ is defined as the heat transfer in an irreversible path .
 
  • #6
Think of the fluid only as forming the system. The paddle may be as light as you want, so that it's heat capacity can be neglected. Furthermore, it can be idealized to not to conduct heat. Hence the system remains perfectly thermally isolated in the process. No change of the temperature of the surrounding will change the outcome of the experiment. This is how we define adiabatically isolated. In an isolated system, by definition, there is no heat flow into or out of the system.
In fact, this is how we define internal energy, namely the change in internal energy ##\Delta U## is defined as the work done on the system in an adiabatic process: ##\Delta U:=W_\mathrm{adia}##. Now the first law states that U is a state function. As energy is conserved, and U certainly is a form of energy, we define heat as ##Q:=\Delta U -W## for a general (non-adiabatic) process.

Be carefull because "heating up" does not necessarily mean that heat is transferred to the system, rather, it only means that its temperature rises.
 
  • #7
DrDu said:
Think of the fluid only as forming the system. The paddle may be as light as you want, so that it's heat capacity can be neglected. Furthermore, it can be idealized to not to conduct heat. Hence the system remains perfectly thermally isolated in the process. No change of the temperature of the surrounding will change the outcome of the experiment. This is how we define adiabatically isolated. In an isolated system, by definition, there is no heat flow into or out of the system.
In fact, this is how we define internal energy, namely the change in internal energy ##\Delta U## is defined as the work done on the system in an adiabatic process: ##\Delta U:=W_\mathrm{adia}##. Now the first law states that U is a state function. As energy is conserved, and U certainly is a form of energy, we define heat as ##Q:=\Delta U -W## for a general (non-adiabatic) process.

Be carefull because "heating up" does not necessarily mean that heat is transferred to the system, rather, it only means that its temperature rises.
thank.
however the defination of entropy change is int dQ(rev)/T

that mean dQrev is not zero in this case?
 
  • #8
No, it isn't. Say the viscous fluid is water. Then you can use the paddle to increase its temperature by, say 10 deg. You could do this reversibly, e.g. doing no work at al, simply slowly heating the water. Assuming that the heat capacity C is approximately constant, ##\Delta S= \Delta U \int_{T_1}^{T_2} 1/T dT=\Delta U \ln (T_2/T_1)=W_\mathrm{adia}\ln (T_2/T_1)##, where ##W_\mathrm{adia}## is the amount of work done in the adiabatic process to achieve the same change of temperature form ##T_1## to ##T_2##.
 
  • #9
DrDu said:
No, it isn't. Say the viscous fluid is water. Then you can use the paddle to increase its temperature by, say 10 deg. You could do this reversibly, e.g. doing no work at al, simply slowly heating the water. Assuming that the heat capacity C is approximately constant, ##\Delta S= \Delta U \int_{T_1}^{T_2} 1/T dT=\Delta U \ln (T_2/T_1)=W_\mathrm{adia}\ln (T_2/T_1)##, where ##W_\mathrm{adia}## is the amount of work done in the adiabatic process to achieve the same change of temperature form ##T_1## to ##T_2##.
do u mean dQrev is the heat transfer between the systems but dQ is the heat transfer from outside to system.
the defination of entropy change is S2-S1= int dQrev/T>= dQ/T
if it is an isolated system, that means there is no change in dQ between the environment and the system.
however there is heat transfer between the system dQrev
do u mean any type of heat transfer between the system is reversible(which represents by d Qrev),so dQrev is not zero
so S2-S1=int (dQrev)/T is not 0 (which greater than 0)?
if Qrev is zero here ,then S2-S1 is definitely equal to zero.

So the formula should be S2-S1=0 no matter what S2 and S1 is
it is hard to understand what is the difference between dQrev and dQ
that means dQrev works in the heat transfer inside the system only but dQ is only responable for the heat transfer between the environment and the system?
 
  • #10
In an isolated system, dQrev is 0. The only way to calculate the entropy change using dQrev is to consider a reversible process instead, which can't be isolated.
I choose one where W=0, i.e. all the change of U is due to Qrev, which must equal Wadia in the irreversible,adiabatic case.
 
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  • #11
DrDu said:
In an isolated system, dQrev is 0. The only way to calculate the entropy change using dQrev is to consider a reversible process instead, which can't be isolated.
I choose one where W=0, i.e. all the change of U is due to Qrev, which must equal Wadia in the irreversible,adiabatic case.
do u agree that the definition of entropy change in general is Sb-Sa=intregrel(a to b) dQv(rev)/T (where it is >= intregrel (a to b) dQ(irrev)/T)

b and a represents any two points at any path of states.
 

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  • #12
DrDu said:
In an isolated system, dQrev is 0. The only way to calculate the entropy change using dQrev is to consider a reversible process instead, which can't be isolated.
I choose one where W=0, i.e. all the change of U is due to Qrev, which must equal Wadia in the irreversible,adiabatic case.
do u mean the definition "Sb-Sa=intregrel(a to b) dQv(rev)/T"" is only for non-isolated system?
this definition cannot apply in the isolated system?
but there is another definition of change of entropy such that it doesn't involve dQrev here?

so even in such isolated system, even dQrev is zero but the change of entropy still greater than zero?
 
  • #13
DrDu said:
In an isolated system, dQrev is 0. The only way to calculate the entropy change using dQrev is to consider a reversible process instead, which can't be isolated.
I choose one where W=0, i.e. all the change of U is due to Qrev, which must equal Wadia in the irreversible,adiabatic case.
still very confusing~~sorry >__<
 
  • #14
consider a cycle in a system W including of one reversible path and a non-reversible path where the reversible path call p1 and a non-reversible path call p2.
where they are connected together with point a and point b .
Now, we know the entropy change is ONLY DEFINED in a reversible path p1 but not in p2.
we assume the W is an isolated system and no heat can transfer between the system and the environment,
(1) the definition of the change of entropy is S2-S1= integral(a-> b) dQrev/T where we know it is >= integral(a->b) dQ/T
(2) the entropy change of an isolated system between point a and b has some probability greater than zero.
where dQ is the heat transfer in the irreversible path.
however, we know it is an isolated system, from the definition of an isolated system, there is no any heat transfer or work done, so dQ=0

so int (a->b)dQrev/T>=0 but dQrev is also zero because there is no heat transfer in an isolated system.
so according to the =(1) the change of entropy S is definitely zero because if S2-S1= integral(a-> b) dQrev/T=S2-S1= integral(a-> b) (0)/T=0,there is 0 possibility that it is greater than zero.

however from the result of the (2), the entropy change of an isolated system is S>=0 and have no probability greater than 0, so the definition of entropy is contradicted t o each other?
 
  • #15
Entropy is a state variable. That means that its value only depends on the actual equilibrium values of p, V, T ... but not on how you get there. However, you can only calculate the entropy change when going from state A to B, using your formula for a reversible path, not for an irreversible one.
 
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  • #16
DrDu said:
Entropy is a state variable. That means that its value only depends on the actual equilibrium values of p, V, T ... but not on how you get there. However, you can only calculate the entropy change when going from state A to B, using your formula for a reversible path, not for an irreversible one.
consider a cycle in a system W including of one reversible path and a non-reversible path where the reversible path call p1 and a non-reversible path call p2.
where they are connected together with point a and point b .
Now, we know the entropy change is ONLY DEFINED in a reversible path p1 but not in p2.
we assume the W is an isolated system and no heat can transfer between the system and the environment,
(1) the definition of the change of entropy is S2-S1= integral(a-> b) dQrev/T where we know it is >= integral(a->b) dQ/T
(2) the entropy change of an isolated system between point a and b has some probability greater than zero.
where dQ is the heat transfer in the irreversible path.
however, we know it is an isolated system, from the definition of an isolated system, there is no any heat transfer or work done, so dQ=0

so int (a->b)dQrev/T>=0 but dQrev is also zero because there is no heat transfer in an isolated system.
so according to the =(1) the change of entropy S is definitely zero because if S2-S1= integral(a-> b) dQrev/T=S2-S1= integral(a-> b) (0)/T=0,there is 0 possibility that it is greater than zero.

however from the result of the (2), the entropy change of an isolated system is S>=0 and have no probability greater than 0, so the definition of entropy is contradicted t o each other? so S=0 or S>= 0 is the actual formula of an isolated system?
 
  • #17
If you consider only adiabatic paths, in general there is no reversible path joining A and B, so you can't determine Qrev.
 
  • #18
DrDu said:
If you consider only adiabatic paths, in general there is no reversible path joining A and B, so you can't determine Qrev.
if not?
 
  • #19
You need a non-adiabatic processes to determine S. You simply can't determine the change of S as long as you only consider adiabatic processes.
 
  • #20
tze liu said:
it seems it is not reasonable
Sorry

it said that delta S>=0
in an isolated system. i know why they put " = " sign, but i don't know why it is still possible that dS>0 in an isolated system
because in an isolated system,it is said that dQ=0 (because no heat transfer between the system and the enviroment?)
by the same logic,dQrev is also 0 in this case
So there should not have " > " sign in an isolated system?
any entropy change in any isolated system is 0 because dQrev is 0
so delat S=0 in an isolated system but not deltaS>=0?
what is the difference between dQrev and dQirrev ?

Depending on the initial state immediately after isolation, even in isolated systems "internal things" can happen between the various parts of the system, e. g., reactions between components, redistribution of components by means of diffusion, phase transition etc., until the overall system has attained its absolute thermodynamic equilibrium state. That’s the general meaning of ΔSsystem >= 0 for isolated systems.
 
  • #21
Another example is free expansion of a gas: you have two cylinders (thermally isolated), one filled with gas, the other vacuum. You suddenly puncture the membrane between the two cylinders. If the gas is ideal, p*V doesn't change and so doesn't T. Neither does internal energy. Nevertheless entropy increases.
To calculate the entropy change you can again consider a reversible process, this time without thermal insulation, where the gas is slowly brought from V1 to V2 at constant T. As U is a state variable and didn't change in the adiabatic process, Qrev must equal -W in the new process.
 
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  • #22
Lord Jestocost said:
Depending on the initial state immediately after isolation, even in isolated systems "internal things" can happen between the various parts of the system, e. g., reactions between components, redistribution of components by means of diffusion, phase transition etc., until the overall system has attained its absolute thermodynamic equilibrium state. That’s the general meaning of ΔSsystem >= 0 for isolated systems.
even in isolated systems "internal things" can happen between the various parts of the system, e. g., reactions between components, redistribution of components by means of diffusion, phase transition etc.,
------------
if this is true ,why dQ is zero here? there is dQ because there are "internal things" happen
 
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  • #23
tze liu said:
even in isolated systems "internal things" can happen between the various parts of the system, e. g., reactions between components, redistribution of components by means of diffusion, phase transition etc.,
------------
if this is true ,why dQ is zero here? there is dQ because there are "internal things" happen

In an isolated system dQ = 0 because no energy is transferred between the system and the enviroment. Whatever happens inside an isolated system results in an increase of the system's entropy.
 
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  • #24
tze liu said:
even in isolated systems "internal things" can happen between the various parts of the system, e. g., reactions between components, redistribution of components by means of diffusion, phase transition etc.,
------------
if this is true ,why dQ is zero here? there is dQ because there are "internal things" happen
Do you know how to determine the change in entropy of an isolated system that has experienced an irreversible change?

Are you aware that, in determining the change in entropy for an isolated system that has experienced an irreversible process, the reversible path you choose (to evaluate the integral of ##dS=dQ_{rev}/T##) does not have to bear any resemblance whatsoever to the actual path followed by the irreversible process (as long as it passes through the same two end states), and this includes paths for which the system is not isolated. In fact, for any reversible path between these same two end states, ##dQ_{rev}## is not zero. Here is a link that gives a recipe for determining the entropy change for an irreversible process, and includes examples applied to two isolated systems: https://www.physicsforums.com/insights/grandpa-chets-entropy-recipe/
 
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  • #25
Chestermiller said:
Do you know how to determine the change in entropy of an isolated system that has experienced an irreversible change?

Are you aware that, in determining the change in entropy for an isolated system that has experienced an irreversible process, the reversible path you choose (to evaluate the integral of ##dS=dQ_{rev}/T##) does not have to bear any resemblance whatsoever to the actual path followed by the irreversible process (as long as it passes through the same two end states), and this includes paths for which the system is not isolated. In fact, for any reversible path between these same two end states, ##dQ_{rev}## is not zero. Here is a link that gives a recipe for determining the entropy change for an irreversible process, and includes examples applied to two isolated systems: https://www.physicsforums.com/insights/grandpa-chets-entropy-recipe/
why!? if dQrev doesn't actually exist in the process, why we can still use this "dQrev" to calculate the entropy.
then where is this dQrev coming from

dQrev is defined as the heat transfer between the system and the environment in the reversible process
 
  • #26
Lord Jestocost said:
In an isolated system dQ = 0 because no energy is transferred between the system and the environment. Whatever happens inside an isolated system results in an increase of the system's entropy.
but dQrev is zero also because the definition of dQrev is the heat transfer between the system and the environment.
do u mean dQrev counts the internal heat change but dQ doesn't?
seems this violate the definition of dQrev.
dQrev just means the heat transfer between the isolated system and the environment in reversible path of a system.
the dQrev is only greater than zero if it is in an non-isolated system, right?
iit is an isolated system then there is NO HEAT TRANSFER BETWEEN THE SYSTEM AND THE ENVIRONMENT (NO MATTER IT IS REVERSIBLE OR NOT REVERSIBLE)

so dQrev should be zero all the time in a 100%isolated system?
because "what happens inside the isolated system" doesn't relate to dQrev which is defined as the heat transfer between the system and the environment.
 
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  • #27
DrDu said:
Another example is free expansion of a gas: you have two cylinders (thermally isolated), one filled with gas, the other vacuum. You suddenly puncture the membrane between the two cylinders. If the gas is ideal, p*V doesn't change and so doesn't T. Neither does internal energy. Nevertheless entropy increases.
To calculate the entropy change you can again consider a reversible process, this time without thermal insulation, where the gas is slowly brought from V1 to V2 at constant T. As U is a state variable and didn't change in the adiabatic process, Qrev must equal -W in the new process.
the entropy should be zero?

because there is no dQrev transfer in such process?

the adiabatic process is not the free expansion and it is non isolated, and it is totally different system.
i agree the Qrev is increasing in the isothermal/adiabatic process.
but there is no heat transfer between outside and the system in free expansion.that means the dQrev is actually zero.
and dQrev doesn't related to the internal change of the heat(even the something can change inside the free expansion) but it just count the reverible path between (1)the system and the environment.
if the reversible path doesn't exist in free expansion, how comes there is dQrev change?
because there is no such reversible path for dQrev to transfer
 
  • #28
tze liu said:
why!? if dQrev doesn't actually exist in the process, why we can still use this "dQrev" to calculate the entropy.
then where is this dQrev coming from

dQrev is defined as the heat transfer between the system and the environment in the reversible process
For an isolated system that has experienced an irreversible process, it is impossible to get from the initial state to the final state using a reversible process path, without also exchanging heat with the greater surroundings. When we talk about dQrev, what we really mean that we are setting up an alternate process that follows a reversible path between the same pair of end states. So yes, dQrev doesn't exist for the actual process, only for its two end states. This is how we determine the entropy change between the two states.
 
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  • #29
Chestermiller said:
For an isolated system that has experienced an irreversible process, it is impossible to get from the initial state to the final state using a reversible process path, without also exchanging heat with the greater surroundings. When we talk about dQrev, what we really mean that we are setting up an alternate process that follows a reversible path between the same pair of end states. So yes, dQrev doesn't exist for the actual process, only for its two end states. This is how we determine the entropy change between the two states.
but in some process, dQ should be less than dS T

can we use dU=ds T -p dv this law in such irreversible path

when dQ=/ ds T, then something will change here
i know this formula can be used in such case
but i get confused here
why!? thank
 
  • #30
tze liu said:
but in some process, dQ should be less than dS T

can we use dU=ds T -p dv this law in such irreversible path

when dQ=/ ds T, then something will change here
i know this formula can be used in such case
but i get confused here
why!? thank
For a process taking place in an isolated system, ##\Delta S## cannot be less than zero. In a closed system where external work is done and/or heat is transferred out of the system, ##\Delta S## can be negative. But, for a closed system, irrespective of whether the process is reversible or irreversible and whether external work and/or heat are exchanged with the surroundings, the following inequality must always be satisfied: $$\Delta S\geq \int{\frac{dQ}{T_{int}}}$$ where ##T_{int}## is the temperature at the interface between the system and the surroundings where the heat transfer is occurring. For an isolated system or an adiabatic closed system, this reduces to ##\Delta S \geq 0##. The equal sign in these equations applies to a reversible path and the greater than sign applies to an irreversible path.
 
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1. Why is there a ">" sign in the entropy of an isolated system?

The ">" sign in the entropy of an isolated system represents the direction of change in entropy. It indicates that the entropy of the system is increasing over time.

2. What does the ">" sign mean in the context of entropy?

In the context of entropy, the ">" sign signifies that the system is moving towards a state of disorder or randomness. This is because entropy is a measure of the disorder or randomness in a system.

3. How does the ">" sign relate to the second law of thermodynamics?

The second law of thermodynamics states that the total entropy of an isolated system will always increase over time or remain constant in ideal cases. The ">" sign in the entropy equation reflects this by showing that the entropy of the system is always increasing or staying the same.

4. Can the ">" sign ever be a "<" sign in the entropy of an isolated system?

No, the ">" sign cannot be a "<" sign in the entropy of an isolated system. This is because the second law of thermodynamics states that entropy can only increase or remain constant, it cannot decrease.

5. Why is the ">" sign important in understanding entropy?

The ">" sign is important in understanding entropy because it helps us understand the direction of change in a system. It also helps us understand the second law of thermodynamics and how entropy is related to the spontaneous direction of processes in an isolated system.

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