3.11 CELLS, EMF, INTERNAL RESISTANCE
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 (\( P \)) and the negative (\( N \)), as shown in Fig. 3.18. They are immersed in an electrolytic solution. Dipped in the solution, the electrodes exchange charges with the electrolyte. The positive electrode has a potential difference \( V_+ (V_+ > 0) \) between itself and the electrolyte solution immediately adjacent to it marked \( A \) in the figure. Similarly, the negative electrode develops a negative potential \( – (V_– ) (V_– \geq 0) \) relative to the electrolyte adjacent to it, marked as \( B \) in the figure. When there is no current, the electrolyte has the same potential throughout, so that the potential difference between \( P \) and \( N \) is \( V_+ – (–V_–) = V_+ + V_– \) . This difference is called the electromotive force (emf) of the cell and is denoted by \( \varepsilon \) . Thus
\[ \varepsilon=V_{+}+V_{-}>0 \](3.55)
Note that \( \varepsilon \) is, actually, a potential difference and not a force. The name emf, however, is used because of historical reasons, and was given at a time when the phenomenon was not understood properly.
To understand the significance of \( \varepsilon \) , consider a resistor \( R \) connected across the cell (Fig. 3.18). A current \( I \) flows across \( R \) from \( C \) to \( D \). As explained before, a steady current is maintained because current flows from \( N \) to \( P \) through the electrolyte. Clearly, across the electrolyte the same current flows through the electrolyte but from \( N \) to \( P \), whereas through \( R \), it flows from \( P \) to \( N \).
The electrolyte through which a current flows has a finite resistance \( r \), called the internal resistance. Consider first the situation when \( R \) is infinite so that \( I = V/R = 0 \), where \( V \) is the potential difference between \( P \) and \( N \). Now,
\[ \begin{eqnarray} V &=& \text{Potentlal difference between P and A} \\ &+& \text{Potential difference between A and B} \\ &+& \text{Potential difference between B and N} \\ &=& \varepsilon \end{eqnarray}\](3.56)
Thus, emf \( \varepsilon \) is the potential difference between the positive and negative electrodes in an open circuit, i.e., when no current is flowing through the cell.
If however \( R \) is finite, \( I \) is not zero. In that case the potential difference between \( P \) and \( N \) is
\[ \begin{aligned} V &=V_{+}+V_{-}-I r \\ &=\varepsilon-I r \end{aligned} \](3.57)
Note the negative sign in the expression (\( I r \)) for the potential difference between \( A \) and \( B \). This is because the current \( I \) flows from \( B \) to \( A \) in the electrolyte.
In practical calculations, internal resistances of cells in the circuit may be neglected when the current \( I \) is such that \( \varepsilon >> I r \). The actual values of the internal resistances of cells vary from cell to cell. The internal resistance of dry cells, however, is much higher than the common electrolytic cells.
We also observe that since \( V \) is the potential difference across \( R \), we have from Ohm’s law
\[ V=IR \](3.58)
Combining Eqs. (3.57) and (3.58), we get
\[ \begin{aligned} &I R=\varepsilon-I r\\ \text{Or, } &I=\frac{\varepsilon}{R+r} \end{aligned} \](3.59)
The maximum current that can be drawn from a cell is for \( R=0 \) and it is \( I_{max}= \varepsilon/r \). However, in most cells the maximum allowed current is much lower than this to prevent permanent damage to the cell.
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 \( 10^5 V/m \). A lightning flash is composed of a series of strokes with an average of about four and the duration of each flash is about \( 30 seconds \). The average peak power per stroke is about \( 10^{12} watts \).
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 \( 120 V/m \), which corresponds to a surface charge density of \( –1.2 × 10^{-9} C/m^2 \). Over the entire earth’s surface, the total negative charge amount to about \( 600 kC \). An equal positive charge exists in the atmosphere. This electric field is not noticeable in daily life. The reason why it is not noticed is that virtually everything, including our bodies, is conductor compared to air.
Example 3.5
A network of resistors is connected to a \( 16 V \) battery with internal resistance of \( 1\Omega \), as shown in Fig. 3.19:
(a) Compute the equivalent resistance of the network.
(b) Obtain the current in each resistor.
(c) Obtain the voltage drops \( V_{AB} \), \( V_{BC} \) and \( V_{CD} \).
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The network is a simple series and parallel combination of resistors. First the two \( 4\Omega \) resistors in parallel are equivalent to a resistor \( =[(4 \times 4) /(4+4)] \Omega=2 \Omega \)
In the same way, the \( 12\Omega \) and \( 6\Omega \) resistors in parallel are equivalent to a resistor of \[ [(12 \times 6) /(12+6)] \Omega=4 \Omega \]
The equivalent resistance \( R \) of the network is obtained by combining these resistors (\( 2\Omega \) and \( 4\Omega \)) with \( 1\Omega \) in series, that is, \[ R=2 \Omega+4 \Omega+1 \Omega=7 \Omega \]
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The total current I in the circuit is \[ I=\frac{\varepsilon}{R+r}=\frac{16 V}{(7+1) \Omega}=2 A \]
Consider the resistors between \( A \) and \( B \). If \( I_1 \) is the current in one of the \( 4\Omega \) resistors and \( I_2 \) the current in the other, \[ I_1\times4=I_2\times4 \] that is, \( I_1=I_2 \), which is otherwise obvious from the symmetry of the two arms. But \( I_1 + I_2 = I = 2 A \). Thus, \[ I_1=I_2=1A \]
that is, current in each \( 4\Omega \) resistor is \( 1A \). Current in \( 1\Omega \) resistor between \( B \) and \( C \) would be \( 2 A \).
Now, consider the resistances between \( C \) and \( D \). If \( I_3 \) is the current in the \( 12\Omega \) resistor, and \( I_4 \) in the \( 6\Omega \) resistor, \[ I_{3} \times 12=I_{4} \times 6, \text { 1.e., } I_{4}=2 I_{3} \] But, \( I_3+I_4=I=2A \)
Thus, \( I_{3}=\left(\frac{2}{3}\right) \mathrm{A}\), \(I_{4}=\left(\frac{4}{3}\right) \mathrm{A} \)
that is, the current in the \( 12\Omega \) resistor is \( (2/3) A \), while the current in the \( 6\Omega \) resistor is \( (4/3) A \). -
The voltage drop across \( AB \) is \[ V_{A B}=I_{1} \times 4=1 \mathrm{~A} \times 4 \Omega=4 \mathrm{~V} \] This can also be obtained by multiplying the total current between \( A \) and \( B \) by the equivalent resistance between \( A \) and \( B \), that is, \[ V_{A B}=2 \mathrm{~A} \times 2 \Omega=4 \mathrm{~V} \] The voltage drop across \( BC \) is \[ V_{B C}=2 \mathrm{~A} \times 1 \Omega=2 \mathrm{~V} \] Finally, the voltage drop across \( CD \) is \[ V_{C D}=12 \Omega \times I_{3}=12 \Omega \times\left(\frac{2}{3}\right) \mathrm{A}=8 \mathrm{~V} \]
This can alternately be obtained by multiplying total current between \( C \) and \( D \) by the equivalent resistance between \( C \) and \( D \), that is, \[ V_{C D}=2 \mathrm{~A} \times 4 \Omega=8 \mathrm{~V} \] Note that the total voltage drop across \( AD \) is \( 4 V + 2 V + 8 V = 14 V \). Thus, the terminal voltage of the battery is \( 14 V \), while its emf is \( 16 V \). The loss of the voltage (\( = 2 V \)) is accounted for by the internal resistance \( 1\Omega \) of the battery [\( 2 A × 1 \Omega = 2 V \)].