On decreasing the πH from 7 to 2, the solubility of a sparingly soluble salt (MX) of a weak acid (HX) increased from 10β4 mol Lβ1 to 10β3 mol Lβ1. The πKa of HX is
3
4
5
2
Correct option is:(B) 4.
The increase in solubility with decreasing pH suggests that HX is undergoing a dissociation process as the pH decreases. This is characteristic of a weak acid (HX) undergoing dissociation:
HXβH++Xβ
The solubility of MX is directly related to the concentration of HX that dissociates into H+ and Xβ. Lowering the pH shifts the equilibrium to the right, leading to an increase in the concentration of H+, which in turn increases the solubility of MX.
From the given information, we can conclude that the pKa of HX is 44. This is because at pH=pKa, the concentrations of the dissociated +H+ and the undissociated HX are equal, resulting in a solubility of 10β410β4 mol Lβ1β1. As the pH drops below pKa, the concentration of +H+ exceeds the concentration of undissociated HX, leading to an increase in solubility.
The Correct Answer is option \(\mathbf{(B) \, 4}\) \[ \text{MX} \rightleftharpoons \text{M}^{\oplus} + \text{X}^{\ominus} \] \[ \text{X}^{\ominus} + \text{H}^{\oplus} \rightleftharpoons \text{HX} \] \[ S = \sqrt{\frac{K_{sp}}{1 + \frac{H^{\oplus}}{K_a}}} \] \[ 10^{-4} = \sqrt{\frac{K_{sp}}{1 + \frac{10^{-7}}{K_a}}} \quad \text{...(1)} \] \[ 10^{-3} = \sqrt{\frac{K_{sp}}{1 + \frac{10^{-2}}{K_a}}} \quad \text{...(2)} \] Dividing Equation (1) by Equation (2): \[ \frac{10^{-4}}{10^{-3}} = \sqrt{\frac{1 + \frac{10^{-7}}{K_a}}{1 + \frac{10^{-2}}{K_a}}} \] \[ 10^{-2} = \sqrt{\frac{1 + \frac{10^{-7}}{K_a}}{1 + \frac{10^{-2}}{K_a}}} \] Squaring both sides: \[ 10^{-4} + \frac{10^{-7}}{K_a} = 1 + \frac{10^{-7}}{K_a} \] Rearranging terms: \[ 10^{-4} - 10^{-7} = \frac{10^{-2}}{K_a} \] \[ 10^{-4} = 0.99 \frac{10^{-2}}{K_a} \] Solving for \(K_a\): \[ K_a = \frac{10^{-4}}{0.99} \times 10^{-2} \] \[ K_a \approx \frac{1}{99} \times 10^{-2} \] Calculating the logarithm for \(pK_a\): \[ pK_a = 2 + \log 99 \approx 4 \]
List-I | List-II | ||
(A) | 1 mol of H2O to O2 | (I) | 3F |
(B) | 1 mol of MnO-4 to Mn2+ | (II) | 2F |
(C) | 1.5 mol of Ca from molten CaCl2 | (III) | 1F |
(D) | 1 mol of FeO to Fe2O3 | (IV) | 5F |
List-I | List-II | ||
(A) | [Co(NH3)5(NO2)]Cl2 | (I) | Solvate isomerism |
(B) | [Co(NH3)5(SO4)]Br | (II) | Linkage isomerism |
(C) | [Co(NH3)6] [Cr(CN)6] | (III) | Ionization isomerism |
(D) | [Co(H2O)6]Cl3 | (IV) | Coordination isomerism |
Organic Chemistry is a subset of chemistry dealing with compounds of carbon. Therefore, we can say that Organic chemistry is the chemistry of carbon compounds and is 200-225 years old. Carbon forms bond with itself to form long chains of hydrocarbons, e.g.CH4, methane and CH3-CH3 ethane. Carbon has the ability to form carbon-carbon bonds quite elaborately. Polymers like polyethylene is a linear chain where hundreds of CH2 are linked together.
Read Also: Organic Compounds
Organic chemistry is applicable in a variety of areas including-