Given:
Horizontal component of Earth's magnetic field, \(B_H = 3 \times 10^{-5}\,T\)
Angle of dip, \( \delta = 45^\circ \)
Step-by-Step Explanation:
Step 1: Recall the relation between the resultant magnetic field (\( B \)), horizontal component (\( B_H \)), and angle of dip (\( \delta \)):
\[ B_H = B\cos\delta \]
Step 2: Solve for resultant magnetic field \( B \):
\[ B = \frac{B_H}{\cos\delta} \]
Step 3: Substitute given values:
\[ B = \frac{3 \times 10^{-5}}{\cos 45^\circ} \]
We know \(\cos 45^\circ = \frac{1}{\sqrt{2}}\). Thus:
\[ B = \frac{3 \times 10^{-5}}{\frac{1}{\sqrt{2}}} = 3\sqrt{2} \times 10^{-5}\,T \]
Final Conclusion:
The resultant magnetic field at the given place is \(3\sqrt{2}\times10^{-5}\,T\).
Let the horizontal component of Earth's magnetic field be $B_H$ and the vertical component be $B_V$. From the given data, we know that $B_H = 3 \times 10^{-5}$ T. The dip $\delta = 45^\circ$, so we can use the formula for the resultant magnetic field $B$ as: \[ B = \sqrt{B_H^2 + B_V^2} \] Also, the vertical component $B_V$ is related to the horizontal component by the angle $\delta$: \[ B_V = B_H \tan \delta \] Substituting $\delta = 45^\circ$ and $\tan 45^\circ = 1$, we get: \[ B_V = B_H \] Now, we substitute into the formula for the resultant magnetic field: \[ B = \sqrt{B_H^2 + B_H^2} = \sqrt{2 B_H^2} = B_H \sqrt{2} \] Substitute the value of $B_H$: \[ B = 3 \times 10^{-5} \times \sqrt{2} = 3 \sqrt{2} \times 10^{-5} \, \text{T} \] Thus, the resultant magnetic field is $3 \sqrt{2} \times 10^{-5}$ T.
List- I (Layer of atmosphere) | List- II (Approximate height over earth's surface) | ||
A. | F1-Layer | I. | 10 km |
B. | D-Layer | II. | 170-190 km |
C. | Troposphere | III. | 100 km |
D. | E-layer | IV. | 65-75 km |
The graph between variation of resistance of a wire as a function of its diameter keeping other parameters like length and temperature constant is
While determining the coefficient of viscosity of the given liquid, a spherical steel ball sinks by a distance \( x = 0.8 \, \text{m} \). The radius of the ball is \( 2.5 \times 10^{-3} \, \text{m} \). The time taken by the ball to sink in three trials are tabulated as shown: