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How do you measure your body temperature For example, if you suspect that you have a fever, you might place a thermometer in your mouth and wait for a few minutes before checking the thermometer for your temperature reading The microscopic process involved in measuring temperature involves collisions and energy transfers between the thermometer and your body Your body is hot compared to the thermometer, which means that the particles in your body have greater thermal energy and are moving faster than the particles in the thermometer When the cold glass tube of the thermometer touches your skin, which is warmer than the glass, the faster-moving particles in your skin collide with the slower-moving particles in the glass Energy is then transferred from your skin to the glass particles by the process of conduction, which is the transfer of kinetic energy when particles collide The thermal energy of the particles that make up the thermometer increases, while at the same time, the thermal energy of the particles in your skin decreases Thermal equilibrium As the particles in the glass gain more energy, they begin to give some of their energy back to the particles in your body At some point, the rate of transfer of energy between the glass and your body becomes equal, and your body and the thermometer are then at the same temperature At this point, your body and the thermometer are said to have reached thermal equilibrium, the state in which the rate of energy flow between two objects is equal and the objects are at the same temperature, as shown in Figure 12-3 The operation of a thermometer depends on some property, such as volume, which changes with temperature Many household thermometers contain colored alcohol that expands when heated and rises in a narrow tube The hotter the thermometer, the more the alcohol expands and the higher it rises in the tube In liquid-crystal thermometers, such as the one shown in Figure 12-4, a set of different kinds of liquid crystals is used Each crystal s molecules rearrange at a specific temperature, which causes the color of the crystal to change and indicates the temperature by color Medical thermometers and the thermometers that monitor automobile engines use very small, temperature-sensitive electronic circuits to take rapid measurements.



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Thread-1 Thread-1 Thread-2 Thread-3 Thread-1

Figure 12-3 Thermal energy is transferred from a hot object to a cold object When thermal equilibrium is reached, the transfer of energy between objects is equal

Figure 12-4 Thermometers use a change in physical properties to measure temperature A liquidcrystal thermometer changes color with a temperature change

Surface of earth Ground currents 2-16 Distortion of vertically polarized electric field by lossy ground resistance

Superconductivity Life below this exists temperature Temperature (K)

Thread-2 Thread-3 Thread-2 Thread-1 Thread-1

Figure 12-5 There is an extremely wide range of temperatures throughout the universe Note that the scale has been expanded in areas of particular interest

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Over the years, scientists developed temperature scales so that they could compare their measurements with those of other scientists A scale based on the properties of water was devised in 1741 by Swedish astronomer and physicist Anders Celsius On this scale, now called the Celsius scale, the freezing point of pure water is defined to be 0 C The boiling point of pure water at sea level is defined to be 100 C Temperature limits The wide range of temperatures present in the universe is shown in Figure 12-5 Temperatures do not appear to have an upper limit The interior of the Sun is at least 15 107 C Temperatures do, however, have a lower limit Generally, materials contract as they cool If an ideal gas, such as the helium in a balloon is cooled, it contracts in such a way that it occupies a volume that is only the size of the helium atoms at 27315 C At this temperature, all the thermal energy that can be removed has been removed from the gas It is impossible to reduce the temperature any further Therefore, there can be no temperature lower than 27315 C, which is called absolute zero The Celsius scale is useful for day-to-day measurements of temperature It is not conducive for working on science and engineering problems, however, because it has negative temperatures Negative temperatures suggest a molecule could have negative kinetic energy, which is not possible because kinetic energy is always positive The solution to this issue is to use a temperature scale based on absolute zero The zero point of the Kelvin scale is defined to be absolute zero On the Kelvin scale, the freezing point of water (0 C) is about 273 K and the boiling point of water is about 373 K Each interval on this scale, called a kelvin, is equal to 1 C Thus, TC 273 TK Figure 12-6 shows representative temperatures on the three most-common scales: Fahrenheit, Celsius, and Kelvin Very cold temperatures are reached by liquefying gases Helium liquefies at 42 K, or 269 C Even colder temperatures can be reached by making use of special properties of solids, helium isotopes, and atoms and lasers.

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4 Given:

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Type of soil Salt water Fresh water Pastoral hills Marshy, wooded Rocky hills Sandy Cities Dielectric constant 81 80 14 20 12 12 14 10 3 5 Conductivity (siemens/meter) 5 0001 003 001 00075 10 0002 0001 Relative quality Best Very poor Very good Average/poor Poor Poor Very poor

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2 class Feline { } 3 public class BarnCat2 extends Feline { 4 public static void main(String[] args) { 5 Feline ff = new Feline(); 6 BarnCat2 b = new BarnCat2(); 7 // insert code here 8 } 9 }

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The wavefront of a surface wave is tilted because of the losses in the ground that tend to retard the wavefront s bottom (also in Fig 2-16) The tilt angle is a function of the frequency, as shown in Table 2-2

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