For Ag2CO3 ⇌ 2Ag+ + CO3^2-, if [Ag+] = 2.24×10^-4 = 2s ⇒ s = 1.12×10^-4. Ksp = [Ag+]^2[CO3^2-] = (2s)^2(s) = 4s^3 = 4(1.12×10^-4)^3 = 5.619×10^-12.
Interpretation: taking given standard concentrations (as printed), case (i) leaves excess H+ and gives the closest acidic pH; among alternatives the intended correct choice is (i). (Note: question text/OCR ambiguous; answer key used here: (i)).
Molar solubility s = (2.42×10^-3 g L^-1)/(233 g mol^-1) = 1.039×10^-5 M. For BaSO4 ⇌ Ba2+ + SO4^2-, Ksp = s^2 = (1.039×10^-5)^2 ≈ 1.08×10^-10.
pH = 9 ⇒ [OH-] = 10^-5 M. For Ca(OH)2 ⇌ Ca2+ + 2OH-, [OH-] = 2s ⇒ s = 5×10^-6 M. Ksp = [Ca2+][OH-]^2 = s(2s)^2 = 4s^3 = 4(5×10^-6)^3 = 5×10^-16 = 0.5×10^-15.
Conjugate base of H2O is OH-, conjugate base of HF is F-.
HCl (0.01 mol) reacts with NH4OH (0.02 mol) leaving 0.01 mol NH3 (base) and forming 0.01 mol NH4+ — a conjugate acid–base pair (NH4+/NH3), i.e. a basic buffer.
PF3 has a lone pair on P that can be donated (Lewis base). BF3 and SiF4 are electron-deficient (Lewis acids); CF4 is inert.
BF3 is electron-deficient and acts as a Lewis acid, not a Lewis base.
Sodium formate (salt of weak acid HCOOH) → basic; anilinium chloride (C6H5NH3+ salt) → acidic; KCN (salt of weak acid HCN) → basic. So: basic, acidic, basic.
For base: x = [C5H5NH+] = [OH-] ≈ √(Kb·C) = √(1.7×10^-9×0.10)=1.303×10^-5 M. Fraction protonated = x/0.10 = 1.303×10^-4 = 0.013%.
[H+] = (10^-1 + 10^-2 + 10^-3)/3 = (0.1 + 0.01 + 0.001)/3 = 0.037 = 3.7×10^-2 M.
AgCl ⇌ Ag+ + Cl-, with common [Cl-] ≈ 0.1 M. Ksp = [Ag+][Cl-] ≈ [Ag+](0.1) ⇒ [Ag+] ≈ Ksp/0.1 = 1.6×10^-10/0.1 = 1.6×10^-9 M.
For PbI2 ⇌ Pb2+ + 2I-, let molar solubility = s. Ksp = s(2s)^2 = 4s^3. Thus s = (Ksp/4)^(1/3) = (3.2×10^-8/4)^(1/3) = (8.0×10^-9)^(1/3) = 2.00×10^-3 M.
For same Ksp, a salt with higher stoichiometric number of ions (NY3 → N3+ + 3Y-) has a larger molar solubility than a 1:1 salt (MY → M+ + Y-) because Ksp depends on powers of s. Numerically NY3 gives larger s than MY, so molar solubility of MY is less than that of NY3.
Take equal volumes V: moles OH- = 0.1V, moles H+ = 0.01V. Excess OH- = 0.09V in total volume 2V ⇒ [OH-] = 0.09/2 = 0.045 M. pOH = 1.3468 ⇒ pH = 14 - 1.3468 ≈ 12.65.
pKa = -log(1×10^-3) = 3. Henderson–Hasselbalch: pH = pKa + log([A-]/[HA]). 4 = 3 + log([A-]/[HA]) ⇒ log ratio = 1 ⇒ [A-]/[HA] = 10 ⇒ [HA]:[A-] = 1:10.
[OH-] = 10^-5 ⇒ pOH = 5 ⇒ pH = 14 - 5 = 9.
H2PO4^- ⇌ H+ + HPO4^2-; therefore HPO4^2- is the conjugate base of H2PO4^-.
HPO4^2- is amphiprotic: it can accept a proton to give H2PO4^- and donate a proton to give PO4^3-, so it can act as both acid and base.
Answer: b. pH = 0 ⇒ [H+] = 1 M, which indicates a strongly acidic solution.
From Ka = [H+][A−]/[HA] ⇒ [H+] = Ka[HA]/[A−]. (The +a term sometimes denotes small contribution from water autoprotolysis and is usually negligible.)
For ammonium acetate with Ka (of acetic acid) = Kb (of ammonia) the degree of hydrolysis is given by h = \sqrt{K_w/(K_a·c)}. This is obtained by writing the hydrolysis equilibrium for one ion, using Ka' = K_w/K_b and solving for h under the small-h approximation.
Ka(NH4+) = K_w / Kb(NH3) = 1.0×10^-14 / 1.8×10^-5 = 5.55×10^-10.
A Lewis acid accepts an electron pair to form a coordinate covalent bond; a Lewis base donates an electron pair. Examples: BF3 (electron-deficient boron) and AlCl3 accept pairs; NH3 and OH− donate lone pairs.
Lewis acid: electron-pair acceptor. Examples: BF3, AlCl3. Lewis base: electron-pair donor. Examples: NH3, OH−.
In the Bronsted–Lowry theory an acid donates a proton to a base. Each acid–base reaction gives a conjugate acid–base pair (e.g. HA ⇌ H+ + A−; HA is acid, A− is its conjugate base). The strength of an acid correlates with the stability of its conjugate base. The theory applies beyond aqueous solutions.
Bronsted–Lowry acid: proton (H+) donor. Bronsted–Lowry base: proton acceptor. Reactions occur as acid + base ⇌ conjugate base + conjugate acid.
(i) HF donates H+ to HS−: HF is the acid, F− its conjugate base; HS− is the base, H2S its conjugate acid. (ii) HPO4^2− donates H+ to SO4^2− producing PO4^3− and HSO4−: conjugate pairs are HPO4^2−/PO4^3− and HSO4−/SO4^2−. (iii) HCO3− donates H+ to NH3 forming NH4+ and CO3^2−: conjugate pairs are NH4+/NH3 and HCO3−/CO3^2−.
(i) HF/F− and H2S/HS− (ii) HPO4^2−/PO4^3− and HSO4−/SO4^2− (iii) NH4+/NH3 and HCO3−/CO3^2−
HClO4 → H+ + ClO4−. The conjugate base ClO4− is stabilized by delocalization of the negative charge over four oxygens (resonance), making proton donation essentially irreversible (strong acid).
HClO4 is a strong Bronsted–Lowry acid because it readily donates H+ to solvents (e.g. water), producing H3O+. Its conjugate base is ClO4− (perchlorate), which is highly stabilized by resonance.
NH3 donates its lone pair on nitrogen more readily than water donates a lone pair on oxygen (N is less electronegative and the lone pair is more available). Thus NH3 replaces H2O in the Cu2+ coordination sphere to give the deep-blue complex.
NH3 is the stronger Lewis base.
pOH = −log[OH−] = −log(2.5×10^-6) ≈ 5.60. pH = 14 − pOH ≈ 14 − 5.60 = 8.40 > 7, so the solution is basic.
Basic (pH ≈ 8.40).
pH = −log(4×10^-5) ≈ 4.40 (< 7), so the solution is acidic.
Acidic.
HNO3 is a strong acid: [H+] = 0.04 M. pH = −log(0.04) = −log(4×10^-2) ≈ 1.398 ≈ 1.40.
pH ≈ 1.40
Ksp is the equilibrium constant for the dissolution of a slightly soluble ionic solid; it equals the product of the equilibrium concentrations of the constituent ions raised to the power of their stoichiometric coefficients.
For a sparingly soluble salt M_aA_b(s) ⇌ a M^{n+} + b A^{m−}, the solubility product Ksp = [M^{n+}]^a [A^{m−}]^b (at saturation).
Kw is the equilibrium constant for H2O ⇌ H+ + OH− and equals 1.0×10^-14 at 25 °C (room temperature).
Ionic product of water Kw = [H+][OH−]; at 25 °C Kw = 1.0 × 10^-14.
According to Le Chatelier's principle, adding a common ion shifts the equilibrium to reduce the change. In ionic equilibria this lowers the degree of ionization or solubility of the compound that shares that ion.
Addition of an ion common to an equilibrium suppresses the ionization or solubility of the weak electrolyte. Example: Adding NaCl to a saturated AgCl solution (which provides Cl−) decreases AgCl solubility because AgCl ⇌ Ag+ + Cl− shifts left.
HA ⇌ H+ + A−. Initial: c, 0, 0. At equilibrium: c(1−α), cα, cα. Ka = [H+][A−]/[HA] = (cα)(cα)/[c(1−α)] = (α^2 c)/(1−α). For very weak acids α ≪ 1, Ka ≈ α^2 c, hence α ≈ \sqrt{Ka/c}. This relation is Ostwald's dilution law.
For a weak acid HA at concentration c with degree of dissociation α: Ka = \dfrac{α^2 c}{1−α}.
pH is a measure of acidity; lower pH means higher [H+]. At 25 °C, neutral water has pH 7 (since [H+] = 1.0×10^-7 M).
pH = −log10[H+], where [H+] is the hydrogen ion concentration in mol L^-1.
Ba(OH)2 dissociates completely to give 2 OH− per formula unit: [OH−] = 2×1.5×10^-3 = 3.0×10^-3 M. pOH = −log(3.0×10^-3) ≈ 2.523. pH = 14 − 2.523 = 11.477 ≈ 11.48.
pH ≈ 11.48
Moles H+ = 0.050 L × 0.05 M = 0.00250 mol. Moles OH− = 0.050 L × 0.025 M = 0.00125 mol. Excess H+ = 0.00125 mol in total volume 0.100 L ⇒ [H+] = 0.00125/0.100 = 0.0125 M. pH = −log(0.0125) ≈ 1.903 ≈ 1.90.
pH ≈ 1.90
For HA ⇌ H+ + A−, [H+] ≈ \sqrt{Ka·c} = \sqrt{10^-9 × 0.4} = 2.00×10^-5 M. pH = −log(2.00×10^-5) ≈ 4.699 ≈ 4.70.
pH ≈ 4.70
For ammonium acetate with equal acid and base strengths, Ka(acid)=Kb(base). Degree of hydrolysis h = \sqrt{K_w/(K_a·c)} = \sqrt{1.0×10^-14/(1.8×10^-5×0.1)} = \sqrt{5.5556×10^-9} ≈ 7.45×10^-5. Both ions hydrolyse to equal extents producing equal amounts of H+ and OH−, so they cancel and the solution remains neutral: pH = 7 (at 25 °C).
Extent of hydrolysis h ≈ 7.45×10^-5; pH = 7.00 (neutral).
Consider a salt formed from a strong acid and a weak base; e.g. BH+ X– (typical: NH4+Cl–). The cation BH+ hydrolyses: \[\mathrm{BH^+ + H_2O \rightleftharpoons B + H_3O^+}\] Define Kh (hydrolysis constant): \[K_h=\frac{[B][H_3O^+]}{[BH^+]}\] But this is exactly the acid dissociation of BH+ (Ka of BH+): \[\mathrm{BH^+ \rightleftharpoons B + H^+}\quad\Rightarrow\quad K_a=\frac{[B][H^+]}{[BH^+]}=K_h.\] If B has base constant Kb, then from the relation Ka·Kb = Kw, we get \[K_h=K_a=\frac{K_w}{K_b}.\] For a salt of concentration c (initial [BH+] = c), let x = amount hydrolysed. At equilibrium [H3O+] = x, [B] = x, [BH+] = c − x. Then \[K_h=\frac{x^2}{c-x}.\] If degree of hydrolysis h = x/c and x << c, approximate c − x ≈ c, so \[x\approx\sqrt{K_h c} \quad\text{and}\quad h=\frac{x}{c}\approx\sqrt{\frac{K_h}{c}}.\] Substituting Kh = Kw/Kb gives \[h\approx\sqrt{\frac{K_w}{K_b\,c}}.\]
Hydrolysis constant Kh = Ka = Kw/Kb. Degree of hydrolysis h ≈ sqrt(Ka/c) = sqrt(Kw/(Kb c)).
Dissolution: \(\mathrm{Ag_2CrO_4\rightleftharpoons 2Ag^+ + CrO_4^{2-}}\). Let solubility be s in the presence of [Ag+]_initial = 0.01 M. Then [Ag+] = 0.01 + 2s ≈ 0.01, [CrO4^{2-}] = s. Ksp = [Ag+]^2[CrO4^{2-}] = (0.01)^2·s = 1.0\times10^{-4}s. So s = Ksp / 1.0\times10^{-4} = 1.0\times10^{-12}/1.0\times10^{-4} = 1.0\times10^{-8} M.
1.0×10^-8 M
Dissociation: \(\mathrm{Ca_3(PO_4)_2\rightleftharpoons 3Ca^{2+}+2PO_4^{3-}}\). Therefore \[K_{sp}=[Ca^{2+}]^3[PO_4^{3-}]^2.\]
Ksp = [Ca2+]^3[PO4^3-]^2
Dissolution: \(\mathrm{CaF_2\rightleftharpoons Ca^{2+}+2F^-}\). Given [Ca^{2+}] = 3.3×10^{-4} M, so [F^-] = 2[Ca^{2+}] = 6.6×10^{-4} M. Ksp = [Ca^{2+}][F^-]^2 = (3.3×10^{-4})·(6.6×10^{-4})^2 = 3.3×10^{-4}·(4.356×10^{-7}) ≈ 1.44×10^{-10}.
1.44×10^-10
Dissolution: \(\mathrm{AgCl\rightleftharpoons Ag^+ + Cl^-}\). With [Ag^+] = 1.00 M (common ion), Ksp = [Ag^+][Cl^-] = 1.00·s, so s = Ksp = 1.8×10^{-10} M.
1.8×10^-10 M
For \(\mathrm{Ag_2CrO_4}\): Ksp = [Ag^+]^2[CrO_4^{2-}]. Ksp = (5.0×10^{-5})^2·(4.4×10^{-4}) = 2.5×10^{-9}·4.4×10^{-4} = 1.10×10^{-12}.
1.1×10^-12
Dissociation (mercurous chloride): \(\mathrm{Hg_2Cl_2\rightleftharpoons Hg_2^{2+} + 2Cl^-}\). Hence Ksp = [Hg_2^{2+}][Cl^-]^2.
Ksp = [Hg2^{2+}][Cl^-]^2
Dissolution: \(\mathrm{Ag_2CrO_4\rightleftharpoons 2Ag^+ + CrO_4^{2-}}\). Let solubility be s. In 0.10 M CrO4^{2-} (common ion), [CrO4^{2-}] ≈ 0.10, [Ag^+] = 2s. Ksp = (2s)^2(0.10) = 4s^2·0.10 = 0.4 s^2. So s^2 = Ksp/0.4 = 1.1×10^{-12}/0.4 = 2.75×10^{-12} ⇒ s = √(2.75×10^{-12}) ≈ 1.66×10^{-6} M.
1.66×10^-6 M
Moles Pb^{2+} = 0.150·0.1 = 0.015 mol; moles Cl^- = 0.100·0.2 = 0.020 mol. Total volume = 0.250 L. [Pb^{2+}] = 0.015/0.25 = 0.06 M; [Cl^-] = 0.020/0.25 = 0.08 M. Q = [Pb^{2+}][Cl^-]^2 = 0.06·(0.08)^2 = 0.06·0.0064 = 3.84×10^{-4}. Since Q(=3.84×10^{-4}) > Ksp(=1.2×10^{-5}), precipitation of PbCl2 will occur.
Yes, a precipitate will form (Qsp = 3.84×10^-4 > Ksp).
Precipitation occurs when [Al^{3+}][OH^-]^3 ≥ Ksp. Given [Al^{3+}] = 1.0×10^{-3} M and Ksp = 1.0×10^{-33}. Solve for [OH^-]_{crit}: \[[OH^-] = \left(\frac{K_{sp}}{[Al^{3+}]}\right)^{1/3} = \left(\frac{1.0\times10^{-33}}{1.0\times10^{-3}}\right)^{1/3} = (1.0\times10^{-30})^{1/3} = 1.0\times10^{-10}\,M.\] pOH = 10.00 ⇒ pH = 14.00 − 10.00 = 4.00. Thus Al(OH)3 begins to precipitate when the pH exceeds about 4.00.
pH = 4.00 (precipitation occurs when pH > 4.00)