$\text{1. Define Variables and Secular Equilibrium Condition}$
In secular equilibrium, the decay rate of the parent equals the decay rate of the daughter:
$$A_P = A_D$$
$$N_P \lambda_P = N_D \lambda_D$$
Where:
$P$ = Parent ($\text{Uranium-238, } {}^{238}\text{U}$)
$D$ = Daughter ($\text{Polonium-218, } {}^{218}\text{Po}$)
$N$ = Number of nuclei
$\lambda$ = Decay constant
The decay constant ($\lambda$) is related to the half-life ($t_{1/2}$) by:
$$\lambda = \frac{\ln(2)}{t_{1/2}}$$
Substituting the decay constants into the equilibrium equation:
$$N_P \left( \frac{\ln(2)}{t_{1/2, P}} \right) = N_D \left( \frac{\ln(2)}{t_{1/2, D}} \right)$$
This simplifies to the equilibrium ratio of the number of nuclei:
$$\frac{N_D}{N_P} = \frac{t_{1/2, D}}{t_{1/2, P}}$$
$\text{Given Values}$
$t_{1/2, D} ({}^{218}\text{Po}) = 138 \text{ days}$
$t_{1/2, P} ({}^{238}\text{U}) = 4.5 \times 10^9 \text{ years}$
$\text{2. Calculate the Mass Ratio}$
We need to find the ratio of masses ($\text{mass}_D / \text{mass}_P$). The number of nuclei ($N$) is related to mass ($m$) by:
$$N = \frac{m}{M} N_A$$
Where $M$ is the molar mass (approximately equal to the mass number in grams) and $N_A$ is Avogadro's constant.
The mass ratio is:
$$\frac{m_D}{m_P} = \frac{N_D M_D}{N_P M_P}$$
Substitute the equilibrium ratio $\left(\frac{N_D}{N_P} = \frac{t_{1/2, D}}{t_{1/2, P}}\right)$ into the mass ratio equation:
$$\frac{m_D}{m_P} = \left(\frac{t_{1/2, D}}{t_{1/2, P}}\right) \left(\frac{M_D}{M_P}\right)$$
$\text{Substitute Values}$
$\text{Mass Numbers (Molar Mass in grams):}$ $M_D = 218 \text{ g/mol}$, $M_P = 238 \text{ g/mol}$.
$\text{Half-lives (convert to the same unit, days):}$
$$t_{1/2, P} = 4.5 \times 10^9 \text{ y} \times 365.25 \frac{\text{days}}{\text{y}} = 1.643625 \times 10^{12} \text{ days}$$
$$\frac{m_D}{m_P} = \left(\frac{138 \text{ days}}{1.643625 \times 10^{12} \text{ days}}\right) \left(\frac{218 \text{ g/mol}}{238 \text{ g/mol}}\right)$$
$$\frac{m_D}{m_P} \approx (8.3963 \times 10^{-11}) \times (0.91596)$$
$$\frac{m_D}{m_P} \approx 7.6859 \times 10^{-11}$$
This value is the mass of ${}^{218}\text{Po}$ per gram of ${}^{238}\text{U}$ (since $m_P = 1 \text{ g}$).
$\text{3. Express the Answer in Logarithm}$
The question asks for the answer in $\log_{10}$ of this mass ratio:
$$\log_{10} \left(\frac{m_D}{m_P}\right) = \log_{10} (7.6859 \times 10^{-11})$$
Using the property $\log(A \times B) = \log(A) + \log(B)$:
$$\log_{10} \left(\frac{m_D}{m_P}\right) = \log_{10} (7.6859) + \log_{10} (10^{-11})$$
$$\log_{10} \left(\frac{m_D}{m_P}\right) \approx 0.8857 - 11$$
$$\log_{10} \left(\frac{m_D}{m_P}\right) \approx -10.1143$$
Two boreholes A and B, both inclined towards 270°, penetrate a dipping coal bed at the same point and pass through it entirely in the sub-surface as shown in the figure below. The bed dips towards 270°. The thickness of the coal bed, measured along the borehole A is 10 m and along borehole B is 8 m. The angle between the two boreholes is 20°. The orthogonal thickness \( x \) of the coal bed is ........ m. (Round off to one decimal place) 
The data tabulated below are for flooding events in the last 400 years.
The probability of a large flood accompanied by a glacial lake outburst flood (GLOF) in 2025 is ........... \(\times 10^{-3}\). (Round off to one decimal place)
| Year | Flood Size | Magnitude rank |
|---|---|---|
| 1625 | Large | 2 |
| 1658 | Large + GLOF | 1 |
| 1692 | Small | 4 |
| 1704 | Large | 2 |
| 1767 | Large | 2 |
| 1806 | Small | 4 |
| 1872 | Large + GLOF | 1 |
| 1909 | Large | 2 |
| 1932 | Large | 2 |
| 1966 | Medium | 3 |
| 2023 | Large + GLOF | 1 |
A satellite launching vehicle is carrying a lander for Moon mapping.
As shown in the figure below, P is the position where the gravitational forces exerted by Earth and Moon on the vehicle balance out.
The distance \( P \) from the center of the Earth is ........... \(\times 10^5\) km. (Round off to two decimal places)
The isobaric temperature-composition (T–X) phase diagram given below shows the phase relation between components M and N. The equilibrium melting undergone by the rock R to generate the liquid of composition L is .............. % (In integer )
Which of the following stereographic projections represent(s) an upright plunging fold? 
A magma having density of 2900 kg m\(^-3\) just reaches the surface through a two-layered crust as shown in the figure below. Assuming isostatic equilibrium, its depth of melting is .......... km. (Round off to one decimal place) 
A well-developed succession of laminated shale is bound by two volcanic ash beds that were precisely dated as shown in the schematic diagram given below. Assuming a constant sedimentation rate, the age of the fossiliferous limestone bed 65 m above the basal volcanic ash bed is ............ Ma. (Round off to nearest integer) 
The shaded region (P) in the given ACF diagram represents the compositional range of mafic rocks that have undergone granulite facies metamorphism. Which of the following equilibrium mineral assemblages is/are identified in these mafic rocks? 
Match the stratigraphic units in Group I with their corresponding basins in Group II.
| Group I | Group II |
|---|---|
| P. Kajrahat Limestone | 1. Cuddapah |
| Q. Shahabad Limestone | 2. Pranhita-Godavari |
| R. Chanda Limestone | 3. Vindhyan |
| S. Narji Limestone | 4. Bhima |
The schematic diagram given below shows textual relationship among garnet, muscovite, biotite and kyanite in a metapelite. Biotite defines S1 foliation and muscovite defines S2 and S3 foliations. S1, S2, and S3 fabrics were developed during distinct deformation events D1, D2, and D3, respectively. Which one of the following represents the pre-D3 mineral assemblage? 