Mass Relationships in Chemical Reactions
Atomic Mass & Isotopes
- Atomic mass (amu): mass of a single atom on the 12C-scale
- By definition 112C atom "weighs" 12amu
- Typical values: 1H=1.008amu,16O=16.00amu
- Average (weighted) atomic mass = Σ(isotopic mass × fractional abundance)
- Copper example (Example 3.1):
- 2963Cu: 62.93 amu, 69.09 % (→0.6909)
- 2965Cu: 64.9278 amu, 30.91 % (→0.3091)
- MˉCu=0.6909(62.93)+0.3091(64.9278)=63.55amu
- Check: result lies between the two isotopic masses and is closer to the more abundant isotope.
- Mass spectrometer separates ions by m/q; Ne spectrum shows three peaks (amu ≈19, 20, 22) with relative intensities 0.26 %, 90.92 %, 8.82 %.
Atomic Mass on the Periodic Table
- Each element square lists atomic number (Z) and average atomic mass (weighted).
- Atomic masses (amu) numerically equal molar masses (g mol⁻¹).
The Mole & Avogadro’s Number
- Mole (mol): quantity containing NA=6.0221415×1023 elementary entities.
- By definition: 12.00g 12C contains NA atoms.
- Analogous to “dozen” = 12, “pair” = 2.
- Molar mass (M): mass of 1 mol of substance in grams.
- For elements: numerical value equals atomic mass (amu).
- Illustrations: 1 mol of Li atoms = 6.941 g; 1 mol 12C atoms = 12.00 g.
- Unit relations
- 1amu=1.66×10−24g
- 1g=6.022×1023amu
Mass↔Moles↔Particles Conversions (Key Formulae)
- moles=Mmass (g)
- particles=moles×NA
Worked Examples
- Example 3.2 (He): 6.46gHe⇒1.61mol (using MHe=4.003 g mol⁻¹).
- Example 3.3 (Zn): 0.356molZn⇒23.3g (using MZn=65.39 g mol⁻¹).
- Example 3.4 (S): 16.3gS⇒3.06×1023atoms (two-step: g→mol→atoms).
- Example 3.6 (CH₄): 6.07gCH4⇒0.378mol.
- Molecular mass (aka molecular weight): Σ atomic masses of all atoms in a molecule.
- SO2: 32.07+2(16.00)=64.07amu
- Caffeine C<em>8H</em>10N<em>4O</em>2: 8(12.01)+10(1.008)+4(14.01)+2(16.00)=194.20amu.
- Formula mass: analogous sum for ionic compounds.
- NaCl: 22.99+35.45=58.44amu.
- Identity rule: “amu-value” = “g per mole”.
Percent Composition by Mass
- General formula:
%element=M</em>compoundnM<em>element×100%
where n = number of that element’s atoms per formula unit. - Ethanol example C<em>2H</em>6O:
%C=52.14,%H=13.13,%O=34.73 (%s sum to 100). - Example 3.8 (H<em>3PO</em>4):
%H=3.09,%P=31.61,%O=65.31 (round-off ↔100.01 %).
- Workflow (Fig 3.7):
mass % → g → divide by molar mass → moles → divide by smallest → ratio → integer subscripts. - Vitamin C Example 3.9: 40.92 %C, 4.58 %H, 54.50 %O.
- From 100 g sample → moles → C<em>3.407H</em>4.54O3.406.
- Divide by 3.406 → CH1.33O.
- Multiply subscripts by 3 → empirical formula C<em>3H</em>4O3.
- NOₓ Example 3.11: 30.46 % N, 69.54 % O.
- Empirical formula NO2 (46.01 g mol⁻¹).
- Experimental molar mass 90–95 g → ratio ≈2 → molecular formula N<em>2O</em>4 with exact M=92.02g mol−1.
Chemical Equations & Balancing
- Chemical reaction: Reactants → Products.
- Reading equations: coefficients express numbers of atoms, moles, or masses in molar masses—not plain grams (e.g.
2Mg+O2→2MgO corresponds to 48.6 g Mg + 32.0 g O₂ → 80.6 g MgO). - Balancing procedure (ethane example):
- Write correct formulas.
- Adjust coefficients; do not alter subscripts.
- Balance elements appearing in single reactant/product first (C, H).
- Balance remaining (O); fractions allowed, then clear denominators.
- Verify atom counts.
- Aluminum oxidation Example 3.12: final balanced 4Al+3O<em>2→2Al</em>2O3.
Stoichiometric Calculations (Quantities of Reactants & Products)
- General roadmap:
- Balanced equation.
- Convert known masses → moles.
- Apply mole ratio to find unknown moles.
- Convert moles → requested units (mass, volume, particles).
- Glucose degradation Example 3.13: 856 g C<em>6H</em>12O<em>6 produces 1.25×103g CO</em>2.
- Lithium & water Example 3.14: 9.89 g H2 needs 68.1 g Li.
Limiting Reactants & Excess
- Limiting reagent: reactant consumed first → limits product.
- Illustration: CO+2H<em>2→CH</em>3OH (if H2 < stoichiometric, it limits).
- Urea synthesis Example 3.15:
- Reaction 2NH<em>3+CO</em>2→(NH<em>2)</em>2CO+H<em>2O with 637.2 g NH</em>3 & 1142 g CO2.
- NH3 limits (produces 18.71 mol product).
- Mass of urea formed: 1124g.
- Excess CO2 left: 319 g.
- Complex organic example 3.16: for 10 g CH<em>3OH need 29.6 g CH</em>3Br (stoich) and 50.0 g LiC<em>4H</em>9 (2.5 equiv).
Reaction Yield
- Theoretical yield: product amount calculated from limiting reagent.
- Actual yield: amount isolated.
- Percent yield: %yield=theoreticalactual×100%.
- Titanium extraction Example 3.17:
- Limiting TiCl4 gives theoretical 8.95×106g Ti.
- Actual 7.91×106g → 88.4% yield.
- Example path:
- Measure g CO2 → mol C → g C.
- Measure g H2O → mol H → g H.
- g O = sample mass − (g C + g H).
- Convert g → mol → divide → ratio → empirical formula (e.g.
C<em>2H</em>6O from C 0.5, H 1.5, O 0.25 → divide by 0.25).
Practical Chemistry Context: Fertilizers
- Essential plant macronutrients: N, P, K, Ca, S, Mg.
- Ammonia synthesis: 3H<em>2+N</em>2→2NH3.
- Nitric acid neutralization: NH<em>3+HNO</em>3→NH<em>4NO</em>3 (fertilizer).
- Phosphate rock (fluorapatite) with sulfuric acid:
2Ca<em>5(PO</em>4)<em>3F+7H</em>2SO<em>4→3Ca(H</em>2PO<em>4)</em>2+7CaSO4+2HF
yields soluble phosphate fertilizers.