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Computer Algebra Recipes

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210 CHAPTER 5. LINEAR PDE MODELS. PART 1<br />

35<br />

30<br />

25<br />

20<br />

0 0.1 0.2 0.3 0.4 0.5<br />

x<br />

Figure 5.1: Initial temperature pro¯le inside the adobe wall.<br />

On running the animation, the temperature curve will oscillate up and down<br />

as the externally imposed temperature on the surface varies during the day.<br />

However, the temperature variation drops to zero within a penetration depth<br />

of less than 0:4 m or 40 cm (16 in). Well within the surface, the temperature<br />

is in thermal equilibrium with the mean exterior temperature. Since the adobe<br />

walls of many of the historic buildings of Arizona and New Mexico are substantially<br />

thicker than 16 inches, the interior temperature of these buildings is quite<br />

insensitive to external temperature variations.<br />

PROBLEMS:<br />

Problem 5-1: A house of wood<br />

In the text recipe, make the following modi¯cations:<br />

(a) The region x>0 is composed of solid wood for which K =0:15 W/(m¢K),<br />

½ = 700 kg/m3 ,andC = 1800 J/(kg¢K).<br />

(b) The mean daily temperature is 30 ± Candtheamplitudeofthetemperature<br />

variation is 20 ± .<br />

Run the animation and determine the approximate depth in centimeters at<br />

which the temperature variation is essentially zero.<br />

Problem 5-2: Pulsating sphere<br />

The surface of a sphere of radius r = a, surrounded by an ideal compressible<br />

°uid, pulsates radially with frequency !. The radial velocity of the surface is<br />

given by V = U cos(!t). It is stated in an advanced calculus text that the<br />

steady-state °uid velocity at an arbitrary point r>ais of the form<br />

V =<br />

Ua2 (c2 + a2 ! 2 ) r2 £ ¤ 2 2<br />

(c +ar! )cos(μ)+c!(r ¡ a)sin(μ) ;

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