Showing posts with label HEAT. Show all posts
Showing posts with label HEAT. Show all posts

Heat Transfer by Radiation

Conduction and convection require some material as a transport medium. These modes of heat transfer cannot operate between bodies separated by a distance in vacuum. But the earth does receive heat from the sun across a huge distance and we quickly feel the warmth of the fire nearby even though air conducts poorly and before convection can set in.

The third mechanism for heat transfer needs no medium; it is called radiation and the energy so radiated by electromagnetic waves is called radiant energy. In an electromagnetic wave electric and magnetic fields oscillate in space and time. Like any wave, electromagnetic waves can have different wavelengths and can travel in vacuum with the same speed, namely the speed of light i.e., 3 × 108 m s–1 .

This is how heat is transferred to the earth from the sun through empty space. All bodies emit radiant energy, whether they are solid, liquid or gases. The electromagnetic radiation emitted by a body by virtue of its temperature like the radiation by a red hot iron or light from a filament lamp is called thermal radiation.

When this thermal radiation falls on other bodies, it is partly reflected and partly absorbed. The amount of heat that a body can absorb by radiation depends on the colour of the body.The lack bodies absorb and emit radiant energy better than bodies of lighter colours.

Applications in our daily life: We wear white or light coloured clothes in summer so that they absorb the least heat from the sun. However, during winter, we use dark coloured clothes which absorb heat from the sun and keep our body warm. The bottoms of the utensils for cooking food are blackened so that they absorb maximum heat from the fire and give it to the vegetables to be cooked .

thermos bottle is a device to minimize heat transfer between the contents of the bottle and outside. It consists of a double-walled glass vessel with the inner and outer walls coated with silver. Radiation from the inner wall is reflected back into the contents of the bottle. The outer wall similarly reflects back any incoming radiation. The space between the walls is evacuted to reduce conduction and convection losses and the flask is supported on an insulator like cork. The device is, therefore, useful for preventing hot contents (like milk) from getting cold, or alternatively to store cold contents (like ice).

Other useful topics in physics

Heat transfer and conduction
Heat and Temperature
Change of State
Surface energy and tension
Viscosity
Dynamic lift


Heat Transfer and Convection

Convection is a mode of heat transfer by actual motion of matter. It is possible only in fluids. Convection can be natural or forced. In natural convection, gravity plays an important part.

When a fluid is heated from below, the hot part expands and, therefore, becomes less dense. Because of buoyancy, it rises and the upper colder part replaces it. This again gets heated, rises up and is replaced by the colder part of the fluid. The process goes on. This mode of heat transfer is evidently different from conduction.

Convection involves bulk transport of different parts of the fluid. In forced convection, material is forced to move by a pump or by some other physical means. The examples of forced convection systems are forced-air heating systems in home, the human circulatory system, and the cooling system of an automobile engine. In the human body, the heart acts as the pump that circulates blood through different parts of the body, transferring heat by forced convection and maintaining it at a uniform temperature.

Natural convection is responsible for many familiar phenomena. During the day, the ground heats up more quickly than large bodies of water do. This occurs both because the water has a greater specific heat and because mixing currents disperse the absorbed heat throughout the great volume of water.

The air in contact with the warm ground is heated by conduction. It expands, becoming less dense than the surrounding cooler air. As a result, the warm air rises (air currents) and other air moves (winds) to fill the space-creating a sea breeze near a large body of water. Cooler air descends, and a thermal convection cycle is set up, which transfers heat away from the land. At night, the ground loses its heat more quickly, and the water surface is warmer than the land. As a result, the cycle is reversed.

The other example of natural convection is the steady surface wind on the earth blowing in from north-east towards the equator, the so called trade wind.

The equatorial and polar regions of the earth receive unequal solar heat. Air at the earth’s surface near the equator is hot while the air in the upper atmosphere of the poles is cool. In the absence of any other factor, a convection current would be set up, with the air at the equatorial surface rising and moving out towards the poles, descending and streaming in towards the equator. The rotation of the earth, however, modifies this convection current. Because of this, air close to the equator has an eastward speed of 1600 km/h, while it is zero close to the poles. As a result, the air descends not at the poles but at 30° N (North) latitude and returns to the equator. This is called trade wind.


Other useful topics in physics

Heat transfer and conduction
Heat and Temperature
Change of State
Surface energy and tension
Viscosity
Dynamic lift


Heat Transfer

Heat is a disordered form of energy and it transfers from one body to other over temperature difference. There are three basic ways of heat transfer namely conduction ,convection and readiation.

Conduction happens through solids where no particle of medium is permanently displaced and heat transfer takes place because of vibration of particles about mean position.During the vibration particles transfers heat energy to next particles and so on.

In the case of convection each particle of the medium gets a permanent displacement and transfers the heat energy. Convection happens through liquids and gases. This is a bit quicker than conduction.

Radiation does not requires materiel medium for propagation and it happens even through vacuum. It is the quickest way of transfer of heat energy and happens with velocity of light.
Conduction :

Gases are poor thermal conductors while liquids have conductivities intermediate between solids and gases.

Let us consider a metallic bar of length L and uniform cross section A with its two ends maintained at different temperatures. Let us assume the ideal condition that the sides of the bar are fully insulated so that no heat is exchanged between the sides and the surroundings.


After sometime, a steady state is reached; the temperature of the bar decreases uniformly with distance from TC to TD; (TC>TD). The reservoir at C supplies heat at a constant rate, which transfers through the bar and is given out at the same rate to the reservoir at D. The rate of flow of heat (or heat current) H is proportional to the temperature difference (TC – TD) and the area of cross section A and is inversely proportional to the length L :

H = KA [Tc –TD] / L

The constant of proportionality K is called the thermal conductivity of the material. The greater the value of K for a material, the more rapidly will it conduct heat.

Other useful topics in physics

Heat and Temperature
Change of State
Surface energy and tension
Viscosity
Dynamic lift


Change of State

A substance can change its state when sufficient energy is given.Matter normally exists in three states: solid, liquid, and gas. A transition from one of these states to another is called a change of state. Two common changes of states are solid to liquid and liquid to gas (and vice versa). These changes can occur when the exchange of heat takes place between the substance and its surroundings.

The change of state from solid to liquid is called melting and from liquid to solid is called fusion. The temperature remains constant until the entire amount of the solid substance melts. That is, both the solid and liquid states of the substance coexist in thermal equilibrium during the change of states from solid to liquid.

The temperature at which the solid and the liquid states of the substance in thermal equilibrium with each other is called its melting point. It is characteristic of the substance. It also depends on pressure. The melting point of a substance at standard atmospheric pressure is called its normal melting point.

The change of state from liquid to vapour (or gas) is called vaporisation. It is observed that the temperature remains constant until the entire amount of the liquid is converted into vapour. That is, both the liquid and vapour states of the substance coexist in thermal equilibrium, during the change of state from liquid to vapour. The temperature at which the liquid and the vapour states of the substance coexist is called its boiling point.

Other useful topics in physics

Heat and Temperature
Surface energy and tension
Viscosity
Dynamic lift
Venturi meter
Torricelli's theorem
Blood flow and heart attack
Stream line flow
What is pressure ?
Pressure variation with depth
Pascal's Law


Heat and Thermal Expansion

When is given to a body the particles of body or atoms starts oscillations.For a particle who comes back to its original position when this applied force because of heat is removed ,potential energy curve is symmetric.

But the general tendency of this potential energy curve is asymmetric and atoms are unable to come back to their original positions. This inter atomic distance increases and this is called thermal expansion.

The magnitude of expansion depends inversely on the force of attraction between the atoms of body. Thus the solids expands least, liquids ten to hundred times more (approximately) and gases expansion is much more.

A solid expands along three dimensions and they are called linear,areal and volume expansions.They are correspondingly measured with coefficients. These coefficients depends on the nature of materiel and independent of physical dimensions and temperature given to the body.

Most substances expand on heating and contract on cooling. A change in the temperature of a body causes change in its dimensions. The increase in the dimensions of a body due to the increase in its temperature is called thermal expansion.

The expansion in length is called linear expansion. The expansion in area is called area expansion. The expansion in volume is called volume expansion .

If the substance is in the form of a long rod, then for small change in temperature, ΔT, the fractional change in length, Δl/l, is directly proportional to ΔT. The proportionality constant is called linear expansion coefficient.

Similarly we can define areal and volume expansion coefficients.

Other useful topics in physics


Heat and Temperature
Surface energy and tension
Viscosity
Dynamic lift
Venturi meter
Torricelli's theorem
Blood flow and heart attack
Stream line flow
What is pressure ?
Pressure variation with depth
Pascal's Law


Heat and Tempearature

Heat is a form of energy which flow from a body a higher temperature to a body of lower temperature. Here we can say heat is the cause and temperature is its effect. We have to measure the flow of heat and it can be done only with the help of temparature.

Temperature is a relative measure, or indication of hotness or coldness. A hot utensil is said to have a high temperature, and ice cube to have a low temperature. An object that has a higher temperature than another object is said to be hotter. Hot and cold are relative terms, like tall and short. We can perceive temperature by touch.

Heat transfer takes place between the system and the surrounding medium, until the body and the surrounding medium are at the same temperature.

Heat is the form of energy transferred between two systems or a system and its surroundings by virtue of temperature difference. The SI unit of heat energy transferred is expressed in joule (J) while SI unit of temperature is kelvin (K), and °C is a commonly used unit of temperature. When an object is heated, many changes may take place. Its temperature may rise, it may expand or change state.

Measurement of Temperature :

A measure of temperature is obtained using a thermometer. Many physical properties of materials change sufficiently with temperature to be used as the basis for constructing thermometers. The commonly used property is variation of the volume of a liquid with temperature.

For example, a common thermometer (the liquid-in-glass type) and Mercury and alcohol are the liquids used in most liquid-in-glass thermometers.

Thermometers are calibrated so that a numerical value may be assigned to a given temperature. For the definition of any standard scale, two fixed reference points are needed. As all substances change dimensions with temperature, an absolute reference for expansion is not available. Any way the necessary fixed points may be correlated to physical phenomena that always occur at the same temperature. The ice point and the steam point of water are two convenient fixed points and are known as the freezing and boiling points.

The two points under consideration are the temperatures at which pure water freezes and boils under standard pressure. The two important temperature scales are the Fahrenheit temperature scale and the Celsius temperature scale. The ice and steam point have values 32 °F and 212 °F respectively, on the Fahrenheit scale and 0 °C and 100 °C on the Celsius scale. On the Fahrenheit scale, there are 180 equal intervals between two reference points, and on the celsius scale, there are 100.

Properties of Fluids :



Surface energy and tension
Viscosity
Dynamic lift
Venturi meter
Torricelli's theorem
Blood flow and heart attack
Stream line flow
What is pressure ?
Pressure variation with depth
Pascal's Law