Consider a uniform rod of material whose temperature varies only along its length, in the xdirection. By considering the heat flowing from both directions into a small segment of length Δx

derive the heat equation,

Tt=K2Tx2

where K=kt/cρi, cis the specific heat of the material, and ρis its density. (Assume that the only motion of energy is heat conduction within the rod; no energy enters or leaves along the sides.) Assuming that Kis independent of temperature, show that a solution of the heat equation is

T(x,t)=T0+Atex2/4Kt,

where T0is a constant background temperature and Ais any constant. Sketch (or use a computer to plot) this solution as a function of x, for several values of t. Interpret this solution physically, and discuss in some detail how energy spreads through the rod as time passes.

Short Answer

Expert verified

The energy spreads through the rod as time passesdTdt=Kd2Tdx2

Step by step solution

01

Heat Conduction 

The trying to follow has been the warmth conduction law:

ΔQΔt=ktAdTdx

The warmth capacity is stated with ktExamine the diagram follows, then evaluate the derivation of all this problem to relation to xand let Δtdt,ΔQdQ, giving us:

d2Qdxdt=ktAd2Tdx2

The temperature is calculated using the the subsequent equation:

Q=mcΔT

The heft is determined by multiplying the length of the slice by both the packing density, as follows:

Q=cρΔVΔT

ΔV=AΔxis that the volumetric, and Ais that the larger surface section, thus:

dQdx=cρAdT

d2Qdxdt=cρAdTdt

cρAdTdt=ktAd2Tdx2

dTdt=Kd2Tdx2

K=ktcρA

02

Equation

Perhaps we must always show that such regression relation is simply the differential equation's response.

T(x,t)=T0+Atex2/4Kt

Calculation (3)'s LHS was even as continues to follow:

LHS=tT0+Atex2/4Kt

localid="1650352081120" LHS=12At3/2ex2/4Kt+At5/2x24Kex2/4Kt

Calculation (3) has had the relevant RHS:

RHS=KxxT0+Atex2/4Kt

RHS=At12txxex2/4Kt

RHS=At12txex2/4Ktx22Ktex2/4Kt

RHS=12At3/2ex2/4Kt+At5/2x24Kex2/4Kt

03

Plot the answer

They still must plan that approach.

T(x,t)T0A=1tex2/4Kt

Ihave used following syntax to print the road as an element of localid="1650354167789" xfor varying values of t, the variables of localid="1650354177813" twill still be in terms of both the fixed localid="1650354173027" K, the constants are:

localid="1650354128505" t1=0.01Kt2=0.1Kt3=1.0K

04

Graph

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Most popular questions from this chapter

The Fahrenheit temperature scale is defined so that ice melts at 320 F and water boils at 2120 F.

(a) Derive the formula for converting from Fahrenheit to Celsius and back

(b) What is absolute zero on the Fahrenheit scale?

Does it ever make sense to say that one object is "twice as hot" as another? Does it matter whether one is referring to Celsius or Kelvin temperatures? Explain.

Measured heat capacities of solids and liquids are almost always at constant pressure, not constant volume. To see why, estimate the pressure needed to keep Vfixed as Tincreases, as follows.

(a) First imagine slightly increasing the temperature of a material at constant pressure. Write the change in volume,dV1, in terms of dTand the thermal expansion coefficient βintroduced in Problem 1.7.

(b) Now imagine slightly compressing the material, holding its temperature fixed. Write the change in volume for this process, dV2, in terms of dPand the isothermal compressibility κT, defined as

κT1VVPT

(c) Finally, imagine that you compress the material just enough in part (b) to offset the expansion in part (a). Then the ratio of dPtodTis equal to (P/T)V, since there is no net change in volume. Express this partial derivative in terms of βandκT. Then express it more abstractly in terms of the partial derivatives used to define βandκT. For the second expression you should obtain

PTV=(V/T)P(V/P)T

This result is actually a purely mathematical relation, true for any three quantities that are related in such a way that any two determine the third.

(d) Compute β,κT,and(P/T)Vfor an ideal gas, and check that the three expressions satisfy the identity you found in part (c).

(e) For water at 25C,β=2.57×104K1andκT=4.52×1010Pa1. Suppose you increase the temperature of some water from 20Cto30C. How much pressure must you apply to prevent it from expanding? Repeat the calculation for mercury, for which (at25C)β=1.81×104K1andκT=4.04×1011Pa1

Given the choice, would you rather measure the heat capacities of these substances at constant vor at constant p?

Problem 1.36. In the course of pumping up a bicycle tire, a liter of air at atmospheric pressure is compressed adiabatically to a pressure of 7 atm. (Air is mostly diatomic nitrogen and oxygen.)

(a) What is the final volume of this air after compression?

(b) How much work is done in compressing the air?

(c) If the temperature of the air is initially300K , what is the temperature after compression?

When spring finally arrives in the mountains, the snow pack may be two meters deep, composed 50%of ice and 50%of air. Direct sunlight provides about 1000watts/m2to earth's surface, but the snow might reflect 90%of this energy. Estimate how many weeks the snow pack should last, if direct solar radiation is the only source of energy.

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