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When the temperature of liquid mercury increases by one degree Celsius (or one kelvin), its volume increases by one part in 550,000 . The fractional increase in volume per unit change in temperature (when the pressure is held fixed) is called the thermal expansion coefficient, β :
β≡ΔV/VΔT
(where V is volume, T is temperature, and Δ signifies a change, which in this case should really be infinitesimal if β is to be well defined). So for mercury, β =1 / 550,000 K-1=1.81 x 10-4 K-1. (The exact value varies with temperature, but between 0oC and 200oC the variation is less than 1 %.)
(a) Get a mercury thermometer, estimate the size of the bulb at the bottom, and then estimate what the inside diameter of the tube has to be in order for the thermometer to work as required. Assume that the thermal expansion of the glass is negligible.
(b) The thermal expansion coefficient of water varies significantly with temperature: It is 7.5 x 10 -4 K-1 at 100oC, but decreases as the temperature is lowered until it becomes zero at 4oC. Below 4oC it is slightly negative, reaching a value of -0.68 x 10-4K-1 at 0oC. (This behavior is related to the fact that ice is less dense than water.) With this behavior in mind, imagine the process of a lake freezing over, and discuss in some detail how this process would be different if the thermal expansion coefficient of water were always positive.


Short Answer

Expert verified

a) Diameter of the bulb is = 2 .8 x 10-3m

b) Water has very different behavior of thermal expansion.

Step by step solution

01

Part(a) Step1: Given information

for mercury, β =1 / 550,000 K-1=1.81 x 10-4 K-1.

02

Part(a)Step2: Explanation

Lets assume that a typical mercury thermometer with cylindrical bulb having
height h= 1 cm = 1 x 10-2 m
radius r=0.2 cm = 0.2 x 10-2 m
and the scale on the thermometer is 1 mm (= 1 x 10-3 m) per degree.

Volume can be calculate by using

V = π r2h

Substitute the values we get

V=π0.2×10-2m2×1×10-2mV=1.25×10-7m3

Coefficient of thermal expansion is calculated as
β=ΔVVΔTSimplify,ΔV=βVΔT

Substitute the value in above equation to calculate change in volume

ΔV=(1.81×10-4K-1)×(1.256×10-7m3)×(274.15K)ΔV=6.19×10-9m3

The inner radius of the thermometer bulb ri can be obtained from the change in volume
ΔV=πri2ΔlSolveforradiusri=ΔVπΔlSubstitutevaluesri=6.19×10-9m3π×10-3mri=1.4×10-3m

So diameter is 2 x radius = 2 x 1.4 x 10-3m = 2 .8 x 10-3m

03

Part(B)Step1: Given information

The thermal expansion coefficient of water varies significantly with temperature: It is 7.5 x 10 -4 K-1 at 100oC, but decreases as the temperature is lowered until it becomes zero at 4oC. Below 4oC it is slightly negative, reaching a value of -0.68 x 10-4K-1 at 0oC.

04

Part(b) Step2: Explanation

Thermal expansion coefficient of water behaves very differently.

β varies much in the liquid region.

As the temperature drops it decreases. But value of β is negative in between 0oC and 4oC i.e., ice generally seems to contract as temperature goes up to 4oC.

If β were positive over the entire region of range , means always in one side of the curve.

This would lead to a water body (Lake, Pond) would start to freeze from bottom up Not from from the top down.


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Most popular questions from this chapter

Two identical bubbles of gas form at the bottom of a lake, then rise to the surface. Because the pressure is much lower at the surface than at the bottom, both bubbles expand as they rise. However, bubble A rises very quickly, so that no heat is exchanged between it and the water. Meanwhile, bubble B rises slowly (impeded by a tangle of seaweed), so that it always remains in thermal equilibrium with the water (which has the same temperature everywhere). Which of the two bubbles is larger by the time they reach the surface? Explain your reasoning fully.

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

κT≡−1V∂V∂PT

(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

∂P∂TV=−(∂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 25∘C,β=2.57×10−4K−1andκT=4.52×10−10Pa−1. Suppose you increase the temperature of some water from 20∘Cto30∘C. How much pressure must you apply to prevent it from expanding? Repeat the calculation for mercury, for which (at25∘C)β=1.81×10−4K−1andκT=4.04×10−11Pa−1

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