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Chapter 11 Source Answers and Examples

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Reviewed solution to Problem 1

For overall order n, [k]=M1−ns⁻¹. Thus inverse-second units imply n=1. Units alone do not identify which species appears or its individual exponent. If the law is specifically −d[A]/dt=k[A], it is first order in A.

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Reviewed solution to Problem 2

  1. Reciprocals are approximately0.1000,0.1100,0.1200,…,0.1700 M⁻¹, linear with time.
  2. The supported model is −d[A]/dt=k[A]²; equality of A and B is maintained by the stated1:1 stoichiometry. k≈(0.1700−0.1000)/35=0.00200 L mol⁻¹ s⁻¹.
  3. t½=1/(k[A]₀)=1/(0.00200×10.0)=50.0 s. M means molarity; lowercase m would mean molality. These high concentrations are formal model data.

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Reviewed solution to Problem 3

From the start, t=(1/[A]−1/[A]₀)/k=(1/0.230−1/10.0)/0.00200=2123.913 s≈2.12×10³ s. This is an extrapolation far beyond the35 s data window; it needs the explicitly stated constant-law assumption.

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Reviewed solution to Problem 4

A total-order-two constant does not establish the individual powers. The solid’s amount is not a dissolved molarity; dissolution, accessible surface area, liquid volume changes and the rate-controlling process are unspecified. A defined empirical rate law and a model for the reactive solid are needed to obtain reaction extent after300 s. Stoichiometry gives an upper bound, not the time course:0.100 mol acid is less than10/84.01=0.1190 mol bicarbonate, so no more than0.100 mol CO₂ could form in the stated stoichiometric model. At1 atm/298.15 K this ideal dry-gas upper bound is nRT/P=2.45 L; it is not the gas volume at5 min. The concentrations are formal source quantities, not practical instructions.

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Reviewed solution to Problem 5

The ln([A]/1 M)-versus-time graph is linear with slope−0.0230 s⁻¹. It supports first-order disappearance with k=0.0230 s⁻¹. The concentration and reciprocal plots are curved. A straight line drawn through a curved plot does not make it linear; the replacement figures omit the original misleading fitted lines and correct the vertical units.

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Reviewed solution to Problem 6

  1. T=318.15 K and Eₐ=422000 J mol⁻¹. k=4.31exp[−422000/(8.314×318.15)]=2.22326×10⁻⁶⁹ s⁻¹.
  2. t½=ln2/k=3.11771×10⁶⁸ s. The first-order half-life is independent of[A]₀.
  3. This enormous value follows from the supplied formal model; extrapolating one Arrhenius law over such a timescale has no established physical validity. Do not silently change422 to42.2.

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Reviewed solution to Problem 7

  1. Threshold mass=5.00×10.0=50.0 mg=0.0500 g; nu,target=0.0500/58.44=0.000855578 mol.
  2. t=ln(4.00/0.000855578)/0.320=26.4063 s≈26.4 s.
  3. The result belongs only to this explicitly supplied remaining-population model. No universal first-order law for real NaCl dissolution is asserted.

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Reviewed solution to Problem 8

  1. k85=0.230 s⁻¹ and k35=0.0500 s⁻¹ from the negative slopes. T values are358.15 and308.15 K.
  2. Eₐ=Rln(k85/k35)/(1/T35−1/T85)=28005.1 J mol⁻¹≈28.0 kJ mol⁻¹.
  3. A=k85exp(Eₐ/RT85)=2794.50 s⁻¹≈2.79×10³ s⁻¹. Two points supply a formal fit, not proof that one mechanism holds over other temperatures.

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Reviewed solution to Problem 9

−d[AB]/dt=r₁+r₂−r₃=0.00325[AB][CD]+0.221[AB]−0.322[A⁺][B⁻]. A negative value means net AB formation. The terms are supplied kinetic models; the schematic formulas do not establish an elementary chemical mechanism.

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Reviewed solution to Problem 10

X₁ disappears with k₁, so t½(X₁)=ln2/0.411=1.68649 s. Step2 has the longest isolated half-life, ln2/0.121=5.72849 s, because its first-order constant is smallest among directly comparable first-order laws. Actual fluxes are k₁[X₁], k₂[X₂] and k₃[X₃]; populations determine them. Identifying the smallest k does not replace the required concentration/mechanism analysis for a general bottleneck.

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Reviewed solution to Problem 11

  1. Equality persists under the specified1:1 reaction, so t=(1/3.00−1/10.0)/k.
  2. k35=0.0324exp[−24000/(8.314×308.15)]=2.76788×10⁻⁶ L mol⁻¹ s⁻¹; k20=1.71386×10⁻⁶ L mol⁻¹ s⁻¹.
  3. t35=84300.3 s≈23.4 h; t20=136145.2 s≈37.8 h. The warmer model reaches the target in1/1.615≈0.619 of the time, about14.4 h sooner. Its rate constant is1.615 times larger.

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Reviewed solution to Problem 12

k′=k[B]=0.734 s⁻¹. A is pseudo-first-order, so t½=ln2/0.734=0.944342 s≈0.944 s. The individual powers and maintained B concentration are explicitly supplied.

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Reviewed solution to Problem 13

  1. The known combined constant is0.0009562 s⁻¹, which predicts[A](210)=20exp(−0.0009562×210)=16.3615 M, far above0.596 M. Additional depletion or a model/data problem is present.
  2. First and last30 s average total disappearance rates are(20−14.6)/30=0.1800 and(1.72−0.596)/30=0.0374667 M s⁻¹. Subtracting the known sinks at interval mean concentrations gives approximate extra rates0.16345774 and0.03635939 M s⁻¹, which are not constant.
  3. Dividing these residual rates by their corresponding mean concentrations17.3 and1.158 M gives0.00945 and0.0314 s⁻¹; they are not one common first-order constant either. The interval approximation and rounding limit precision, but the discrepancy is large.
  4. No unique pure zero-, first- or second-order extra law is established by these data. Obtain initial-rate measurements with controlled concentrations, test competing models and report uncertainty. A finite table does not uniquely identify an arbitrary mechanism.

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Reviewed solution to Problem 14

Boiling occurs when the solution vapor pressure equals the external pressure. Pressure, composition effects and an applicable boiling condition are needed; reaction k does not provide them. If100.0 °C is only a stipulated target with a constant observed temperature rise, t=(100.0−35.0)/5.00=13.0 min. This conditional threshold time is not an established boiling time for the concentrated reacting solution. If a heating power rather than a temperature-rise rate were given, heat capacity and reaction enthalpy would also enter.

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Reviewed solution to Problem 15

The effective constant would be k′=k[O₂]fixed in yr⁻¹. Conversion24% leaves fraction0.76, so t=−ln0.76/(3.2421[O₂]fixed) yr with oxygen concentration in M. A numerical time needs that concentration or an independently supplied effective k′. Real corrosion also involves surfaces and changing conditions; no universal homogeneous iron law follows from these data.

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Reviewed solution to Problem 16

−d[A]/dt=r₁+2r₂=0.23511[A]²+0.662[A]. Product formation rates are d[AB]/dt=r₁ and d[A₂]/dt=r₂. The factor2 belongs to A consumption in the second reaction, even though its supplied empirical exponent is1. A numerical time and partition require[A]₀, initial product amounts and assurance that the laws remain valid while B is available. No unique numeric answer follows from the original data. If those were supplied, one would integrate this mixed-order law rather than use a single standard half-life formula.

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Reviewed solution to Problem 17

A constant second-step rate needs a stated zero-order regime, units and sufficient intermediate AB and other reactants. At initial AB=0, a step consuming AB cannot maintain a positive rate indefinitely. The source does not specify its initial AB/DE populations or zero-order range, so no unique physical bottleneck time follows. Conditionally, comparing the first-step rate with a stated capacity0.441 M s⁻¹ gives0.753[A]²=0.441 and[A]=0.765283 M. Calling this a true step-rate crossover still requires the missing conditions.

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Reviewed solution to Problem 18

  1. The first stage consumes3.00 M A and R in3.00/0.320=9.375 s, leaving[A]=2.00 M.
  2. The second stage takes ln(2.00/1.00)/0.02421=28.6306 s.
  3. Total=38.0056 s≈38.0 s. A catalyst participates and is regenerated by the catalytic cycle; a species consumed stoichiometrically is not a catalyst. These two empirical regimes are explicitly stipulated.

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Reviewed solution to Problem 19

k′=kp=1.05 h⁻¹. t=ln(1.00/0.200)/1.05=1.53280 h≈1.53 h. The original question omitted the partial pressure and a defined remaining-material rate law. C₆H₁₀O₅ is a cellulose repeat-unit formula, not the complete chemical composition of wood.

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Reviewed solution to Problem 20

  1. C=1/(0.082057×298.15)=0.0408742 M. Each reactant concentration is0.0400C.
  2. r=0.321(0.0400C)² and d[AB]/dt=2r because each event produces2 AB.
  3. Target[AB]=0.0100C. t=0.0100C/[2×0.321(0.0400C)²]=238.1746 s≈238 s. The fixed-density reservoirs and no-product-removal assumptions are model inputs, not inferred from a real room.

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Worked examples and reviewed revisions

Example Problem 3.1.1

Worked example

Reviewed replacement, Example3.1.1: In a hypothetical fixed-volume model, −d[A]/dt=k=212 mol L⁻¹ s⁻¹ over the stated range. [A]₀=30.0 M. Find the mathematical exhaustion time. These formal concentration data illustrate zero-order integration; they are not a measured automobile catalytic-converter model.
  1. The prompt explicitly states A disappearance, so[A]=30.0−212t.
  2. At exhaustion0=30.0−212t; t=0.141509 s≈0.142 s.
  3. The formal zero-order regime cannot give negative concentrations. This is not a measured catalytic-converter model.

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Example Problem 3.1.2

Worked example

Reviewed Example3.1.2: The supplied concentration-versus-time fit is[A]=3.21−0.022t, with[A] in M and t in minutes. Assume the zero-order disappearance model is valid through the first halving interval. Find[A]₀, k and t½ using the reviewed graph.
  1. Read the supplied fit[A]=3.21−0.022t with concentration in M and t in minutes.
  2. [A]₀=3.21 M and k=0.022 M min⁻¹ on the A-disappearance basis.
  3. t½=[A]₀/(2k)=3.21/(2×0.022)=72.9545 min≈73 min. This model extends through the target concentration.

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Example Problem 3.2.1

Worked example

Reviewed Example3.2.1: Sulfuryl chloride, SO₂Cl₂, decomposes to sulfur dioxide, SO₂, and chlorine, Cl₂: SO₂Cl₂→SO₂+Cl₂. In the stated fixed-volume first-order disappearance model, k=4.2×10⁻⁴ s⁻¹ and [SO₂Cl₂]₀=4.0 M. Find its remaining concentration after60 s. The supplied concentration model is an exercise; SO₂ is sulfur dioxide, not sulfate gas.
  1. The balanced transformation is SO₂Cl₂→SO₂+Cl₂. SO₂ is sulfur dioxide.
  2. Convert1 min to60 s to match k=4.2×10⁻⁴ s⁻¹.
  3. [SO₂Cl₂]=(4.0 M)exp(−4.2×10⁻⁴×60)=3.900459 M≈3.9 M.

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Example 3.3.1

Worked example

Reviewed replacement, Example3.3.1: A hypothetical fixed-volume NO₂ disappearance model specifies −d[NO₂]/dt=(12 L mol⁻¹ s⁻¹)[NO₂]² and [NO₂]₀=0.0030 M. Find the half-life. This explicitly defines k on the disappearance basis and does not claim a measured nitrogen/oxygen catalytic-converter mechanism.
  1. The specified disappearance law is −d[NO₂]/dt=k[NO₂]².
  2. t½=1/(k[NO₂]₀)=1/(12×0.0030)=27.7778 s≈28 s.
  3. A normalized reaction-rate constant would need the stoichiometric factor. The new prompt explicitly defines its convention.

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Example 3.3.2

Worked example

Reviewed replacement, Example3.3.2: In a hypothetical fixed-volume model for A+B→P, [A]₀=[B]₀=6.00 M and −d[A]/dt=k[A][B]. Successive intervals to halve the remaining concentration are35.0,70.0 and140.0 s. The cumulative times to [A]₀/2, [A]₀/4 and [A]₀/8 are35.0,105.0 and245.0 s. Determine k. These formal data replace the source’s inconsistent35,70,105 successive intervals and are not a precipitation procedure. The actual sodium carbonate formula is Na₂CO₃; calcium carbonate is CaCO₃.
  1. The reviewed formal1:1 model has[A]₀=[B]₀=6.00 M and successive halving intervals35.0,70.0,140.0 s.
  2. Equal concentrations persist, so −d[A]/dt=k[A]². First t½=1/(k[A]₀); k=1/(35.0×6.00)=0.00476190 L mol⁻¹ s⁻¹.
  3. The next intervals are1/(k×3.00)=70.0 and1/(k×1.50)=140.0 s; cumulative times are35.0,105.0,245.0 s. The original105 s third interval does not fit this model.
  4. Increasing intervals alone do not prove second order; these declared data and model do. This is not a concentrated precipitation recipe.

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Example Problem 3.4.1

Worked example

Reviewed diagnostic, Example3.4.1: The source supplied four schematic steps with constants0.1353,0.00052 and0.022 L mol⁻¹ s⁻¹, and0.04 for a unimolecular BX→B+X step. If that last step is explicitly elementary first order, its k must have units s⁻¹. Explain why these constants alone cannot establish a rate-limiting step or overall empirical rate law. Species concentrations, a chemically consistent elementary mechanism and appropriate kinetic assumptions are missing.
  1. Different-order constants cannot be compared by their numerical values. For an explicitly elementary unimolecular BX step, k has s⁻¹ units.
  2. Step fluxes depend on the concentration factors. The source supplies no populations and no validated elementary mechanism.
  3. No unique rate-limiting step or overall empirical law can be determined. Conditionally, an elementary B+C step would have r₂=0.00052[B][C] M s⁻¹, but that does not establish it as the bottleneck.

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Example Problem 3.4.2

Worked example

Reviewed replacement, Example3.4.2: Use a hypothetical acid-family pre-equilibrium HA⇌H⁺+A⁻, with Kₐ=[H⁺][A⁻]/[HA]=10⁻⁴·⁷⁶ in the conventional ideal concentration calculation. It is explicitly fast enough to maintain pre-equilibrium while a declared slow elementary capture A⁻+S⁺→AS occurs, with r=kₛ[A⁻][S⁺] and kₛ=0.0003465 L mol⁻¹ s⁻¹. Eliminate A⁻ from the rate law. This formal model replaces the unsupported silver-carbonate dissolution mechanism. The real names/formulas are acetic acid CH₃COOH and silver carbonate Ag₂CO₃; acetic acid is not HCl. The prompt explicitly declares the fast pre-equilibrium and slow elementary capture; acid identity or a smaller numerical k does not establish them.
  1. The reviewed prompt explicitly declares a fast HA⇌H⁺+A⁻ pre-equilibrium and slow elementary A⁻+S⁺ capture, not a demonstrated silver-carbonate mechanism.
  2. Start with r=kₛ[A⁻][S⁺]. From the ideal concentration relation, [A⁻]=Kₐ[HA]/[H⁺].
  3. Substitute: r=kₛKₐ[S⁺][HA]/[H⁺]. The conventional concentration Kₐ=10⁻⁴·⁷⁶ M gives kₛKₐ=6.021479872×10⁻⁹ s⁻¹, so multiplying by[S⁺][HA]/[H⁺] gives M s⁻¹.
  4. The approximation requires pre-equilibrium to be maintained. Acetic acid is CH₃COOH; silver carbonate is Ag₂CO₃.

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Example Problem 3.4.3

Worked example

Reviewed diagnostic, Example3.4.3: The source supplies [CO₃²⁻]=4.00 M, [Ca²⁺]=2.10 M and [OH⁻]=1.20 M, and proposes two sink laws r₁=0.00324[Ca²⁺][CO₃²⁻] and r₂=0.00562[Ca²⁺][OH⁻], with coefficients in L mol⁻¹ s⁻¹, plus a calcium supply0.0332[CaCl₂] M s⁻¹. Treat these as formally supplied empirical laws, not laws inferred from reaction stoichiometry. Write the conditional net disappearance expression and determine what further information a numerical answer needs. The formal molecular CaCl₂ source model is not established for an already dissolved strong electrolyte.
  1. Use the supplied empirical sink laws, not exponents inferred from the net ionic equations.
  2. r₁=0.00324×2.10×4.00=0.027216 and r₂=0.00562×2.10×1.20=0.0141624 M s⁻¹. Carbonate has2− charge.
  3. Conditional net disappearance is −d[Ca²⁺]/dt=0.0413784−0.0332[CaCl₂] M s⁻¹, with concentration in M.
  4. Its numerical value is underdetermined because the source concentration is missing and a molecular CaCl₂ reservoir is not justified for already dissolved electrolyte. A source contribution reduces net disappearance.

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