3.11 CELLS, EMF, INTERNAL RESISTANCE
(a) Sketch of an electrolyte cell with positive terminal
(b) the symbol for a cell,
We have already mentioned that a simple device to maintain a steady current in an electric circuit is the electrolytic cell. Basically a cell has two electrodes, called the positive (
Note that
To understand the significance of
The electrolyte through which a current flows has a finite resistance
Thus, emf
If however
Note the negative sign in the expression (
In practical calculations, internal resistances of cells in the circuit may be neglected when the current
We also observe that since
Combining Eqs. (3.57) and (3.58), we get
The maximum current that can be drawn from a cell is for
CHARGES IN CLOUDS
In olden days lightning was considered as an atmospheric flash of supernatural origin. It was believed to be the great weapon of Gods. But today the phenomenon of lightning can be explained scientifically by elementary principles of physics.
Atmospheric electricity arises due to the separation of electric charges. In the ionosphere and magnetosphere strong electric current is generated from the solarterrestrial interaction. In the lower atmosphere, the current is weaker and is maintained by thunderstorm.
There are ice particles in the clouds, which grow, collide, fracture and break apart. The smaller particles acquire positive charge and the larger ones negative charge. These charged particles get separated by updrifts in the clouds and gravity. The upper portion of the cloud becomes positively charged and the middle negatively charged, leading to dipole structure. Sometimes a very weak positive charge is found near the base of the cloud. The ground is positively charged at the time of thunderstorm development. Also, cosmic and radioactive radiations ionise air into positive and negative ions and the air becomes (weakly) electrically conductive. The separation of charges produce tremendous amount of electrical potential within the cloud, as well, as between the cloud and ground. This can amount to millions of volts and eventually the electrical resistance in the air breaks down and lightning flash begins and thousands of amperes of current flows. The electric field is of the order of
During fair weather also there is charge in the atmosphere. The fair weather electric field arises due to the existence of a surface charge density at ground and an atmospheric conductivity, as well as, due to the flow of current from the ionosphere to the earth’s surface, which is of the order of picoampere / square metre. The surface charge density at ground is negative; the electric field is directed downward. Over land the average electric field is about
Example 3.5
A network of resistors is connected to a
(a) Compute the equivalent resistance of the network.
(b) Obtain the current in each resistor.
(c) Obtain the voltage drops
-
The network is a simple series and parallel combination of resistors. First the two
resistors in parallel are equivalent to a resistorIn the same way, the
and resistors in parallel are equivalent to a resistor ofThe equivalent resistance
of the network is obtained by combining these resistors ( and ) with in series, that is, -
The total current I in the circuit is
Consider the resistors between
and . If is the current in one of the resistors and the current in the other, that is, , which is otherwise obvious from the symmetry of the two arms. But . Thus,that is, current in each
resistor is . Current in resistor between and would be .Now, consider the resistances between
and . If is the current in the resistor, and in the resistor, But,
Thus, ,
that is, the current in the resistor is , while the current in the resistor is . -
The voltage drop across
is This can also be obtained by multiplying the total current between and by the equivalent resistance between and , that is, The voltage drop across is Finally, the voltage drop across isThis can alternately be obtained by multiplying total current between
and by the equivalent resistance between and , that is, Note that the total voltage drop across is . Thus, the terminal voltage of the battery is , while its emf is . The loss of the voltage ( ) is accounted for by the internal resistance of the battery [ ].