In accordance with the bohr's model the quantum number that characterises the earth revolution around the sun in an orbit of radius 1.5 x 1011 m with orbital speed 3 x 104 m/s is [given mass of the earth = 6 x 1024 kg]
8.57x 1064
5.98 x 1064
2.57 x 1074
2.57x 1038
According to Bohr’s model, angular momentum is quantized and given by:
\( mvr = \dfrac{nh}{2\pi} \)
Rearranging to find \( n \):
\( n = \dfrac{2\pi mvr}{h} \)
Substitute the known values:
\[ n = \frac{2\pi \times 6.0 \times 10^{24} \times 3 \times 10^4 \times 1.5 \times 10^{11}}{6.62 \times 10^{-34}} \]
Simplifying the numerator:
\[ 2\pi \times 6.0 \times 3 \times 1.5 = 2\pi \times 27 = 169.65 \quad \text{(approx)} \]
So the numerator becomes:
\[ 169.65 \times 10^{24 + 4 + 11} = 169.65 \times 10^{39} \]
Finally:
\[ n = \frac{169.65 \times 10^{39}}{6.62 \times 10^{-34}} \approx 25.61 \times 10^{73} \approx 2.6 \times 10^{74} \]
Hence, the quantum number that characterizes Earth's revolution around the Sun is:
\( \boxed{2.6 \times 10^{74}} \)
According to Bohr's model quantization condition, the angular momentum (L) of an object revolving in a stable orbit is an integer multiple of \( \frac{h}{2\pi} \), where \( h \) is Planck's constant and \( n \) is the principal quantum number. \[ L = n \frac{h}{2\pi} \] The angular momentum \( L \) for an object of mass \( m \) moving with speed \( v \) in an orbit of radius \( r \) is given by: \[ L = mvr \] Combining these two equations, we get: \[ mvr = n \frac{h}{2\pi} \]
We are asked to find the quantum number \( n \) that characterizes the Earth's revolution around the Sun. We are given the following values:
Rearranging the quantization condition to solve for \( n \): \[ n = \frac{mvr}{\left(\frac{h}{2\pi}\right)} = \frac{2\pi mvr}{h} \]
First, let's calculate the angular momentum \( L = mvr \): \[ L = (6 \times 10^{24} \text{ kg}) \times (3 \times 10^{4} \text{ m/s}) \times (1.5 \times 10^{11} \text{ m}) \] \[ L = (6 \times 3 \times 1.5) \times 10^{(24 + 4 + 11)} \text{ kg m}^2/\text{s} \] \[ L = 27 \times 10^{39} \text{ Js} \]
Now, substitute the value of \( L \) and \( h \) into the equation for \( n \): \[ n = \frac{2\pi \times (27 \times 10^{39} \text{ Js})}{6.626 \times 10^{-34} \text{ Js}} \] Using \( \pi \approx 3.14159 \): \[ n = \frac{2 \times 3.14159 \times 27}{6.626} \times 10^{39 - (-34)} \] \[ n = \frac{169.64586}{6.626} \times 10^{73} \] \[ n \approx 25.603 \times 10^{73} \] Writing this in standard scientific notation: \[ \mathbf{n \approx 2.5603 \times 10^{74}} \]
Comparing this result with the given options:
The calculated value \( 2.5603 \times 10^{74} \) is closest to \( 2.57 \times 10^{74} \).
The quantum number characterizing the Earth's revolution is approximately 2.57 x 1074.
Electron belongs to the family of
Thomson atomic model was proposed by William Thomson in the year 1900. This model explained the description of an inner structure of the atom theoretically. It was strongly supported by Sir Joseph Thomson, who had discovered the electron earlier.
Thomson assumed that an electron is two thousand times lighter than a proton and believed that an atom is made up of thousands of electrons. In this atomic structure model, he considered atoms surrounded by a cloud having positive as well as negative charges. The demonstration of the ionization of air by X-ray was also done by him together with Rutherford. They were the first to demonstrate it. Thomson’s model of an atom is similar to a plum pudding.
Rutherford’s conducted an experiment by bombarding a thin sheet of gold with α-particles and then studied the trajectory of these particles after their interaction with the gold foil.
Bohr model of the atom was proposed by Neil Bohr in 1915. It came into existence with the modification of Rutherford’s model of an atom. Rutherford’s model introduced the nuclear model of an atom, in which he explained that a nucleus (positively charged) is surrounded by negatively charged electrons.