Exam 3 Study Guide
This guide covers chapters 7 through 9. You will draw molecules, work out their shapes, and decide whether they are polar. Then you will look deeper, at orbitals that overlap and spread across a whole molecule. The last chapter is gases, the one state that one equation can predict. Read each "what to know" list first. Copy out the equations by hand. Work the examples with the answers covered, then run the ten self-test items. The cram sheet at the end holds every equation and constant.
What this guide covers
- Chapter 7 · ionic bonds and lattice energy, electronegativity, Lewis structures, resonance, formal charge, VSEPR shapes and molecular polarity.
- Chapter 8 · orbital overlap, hybrid orbitals, sigma and pi bonds, restricted rotation, molecular orbital diagrams, bond order and magnetism.
- Chapter 9 · pressure, the simple gas laws, PV = nRT, gas density and stoichiometry, partial pressures, kinetic molecular theory and effusion.
Chapter 7Chemical Bonding and Molecular Geometry
What to know
An ionic bond moves an electron across. A metal hands electrons to a nonmetal, and the two opposite charges attract. The solid is a lattice, a repeating grid of ions, so the formula is just a ratio. Lattice energy measures how hard that grid is to pull apart. It rises with bigger ion charges and falls as the ions get larger.
A covalent bond shares a pair instead. The electronegativity difference, ΔEN, scores how fairly. Below 0.4 the bond is nonpolar covalent. From 0.4 to 1.8 it is polar covalent. Above 1.8 treat it as ionic. The more electronegative atom takes the partial negative end.
Drawing a Lewis structure follows five steps. Count all valence electrons, adding one for each negative charge and removing one for each positive charge. Pick the least electronegative atom as the center. Join atoms with single bonds. Put the remaining electrons as lone pairs on the outer atoms first. Then move lone pairs into double or triple bonds until every atom has a full shell.
The octet rule bends three ways. An odd electron count cannot pair up fully, as in NO. Boron and beryllium settle for fewer than eight. Atoms in period 3 and beyond can hold more than eight, as in SF6.
Resonance appears when one drawing is not enough. Ozone is the classic case. Neither drawing is right on its own. The real molecule is a blend, so both of its bonds are identical and sit at bond order 1.5.
Formal charge ranks competing structures. Compute it for each atom, and prefer the structure with charges closest to zero. Any negative formal charge should sit on the most electronegative atom.
VSEPR says electron domains push each other as far apart as they can. A domain is a bond or a lone pair, and a double bond counts as one domain. Count domains to get the electron geometry. Then ignore the lone pairs to read the molecular shape. Two domains give linear. Three give trigonal planar. Four give tetrahedral. Five give trigonal bipyramidal. Six give octahedral.
A molecule is polar only if its bond dipoles fail to cancel. Ask two questions. Are any bonds polar? Do the arrows cancel by symmetry? Carbon tetrachloride has four polar bonds that cancel exactly, so the molecule is nonpolar. Water's two bonds do not cancel, because the shape is bent.
- Lattice energy grows with charge and shrinks with distance.
- ΔEN under 0.4 is nonpolar, 0.4 to 1.8 is polar, over 1.8 is ionic.
- Count electrons, not pairs, and adjust for the ion's charge.
- A double or triple bond is still one electron domain.
- Electron geometry counts lone pairs. Molecular shape does not.
- Polar bonds alone do not make a polar molecule. Symmetry can cancel them.
Equations, units and symbols
| Equation | What each symbol means | Units |
|---|---|---|
| ΔHlattice ∝ Q1Q2 ÷ r0 | Q1 and Q2 are the ion charges, r0 is the distance between their centers | ΔHlattice in kJ/mol; Q in elementary charges; r0 in pm |
| ΔEN = ENhigher − ENlower | EN is each atom's electronegativity from the table | no unit; the scale runs 0.79 to 3.98 |
| valence electrons = Σ group counts − charge | the total to place in a Lewis structure | a plain count; subtracting a negative charge adds electrons |
| FC = V − L − ½B | V is valence electrons, L is lone pair electrons, B is bonding electrons | a whole number of charges |
| Σ formal charges = species charge | the check on a finished structure | 0 for a neutral molecule |
| domains = bonds + lone pairs on the central atom | multiple bonds count once | a plain count from 2 to 6 |
| bond order = bonds shared ÷ resonance forms | gives the blended value, like ozone's 1.5 | no unit |
Worked examples
Worked example 1 · a Lewis structure for carbon dioxide
Draw CO2 and check every shell.
Step 1 · count valence electronsCarbon is group 14, so 4. Each oxygen is group 16, so 6. Total = 4 + 2(6) = 16 electrons, which is 8 pairs.
Step 2 · pick the centerCarbon is less electronegative than oxygen, so carbon sits in the middle.
Step 3 · single bonds firstO–C–O uses 4 electrons. That leaves 12 to place.
Step 4 · fill the outer atomsGive each oxygen three lone pairs, using all 12. Now both oxygens have 8 electrons, but carbon has only 4.
Step 5 · make double bondsMove one lone pair from each oxygen into a bond. The result is O=C=O. Carbon now has 8, and each oxygen has 2 lone pairs plus 4 bonding electrons, so 8 as well.
Check it a second wayCount the total again. Four bonds hold 8 electrons, and four lone pairs hold 8. That is 16, exactly what you started with.
Worked example 2 · formal charges in ozone
One resonance form of O3 has a double bond on the left and a single bond on the right. Find each atom's formal charge.
Step 1 · the central atomIt has 1 lone pair, so L = 2. It has three bonds, so B = 6. Then FC = 6 − 2 − 3 = +1.
Step 2 · the double-bonded oxygenIt has 2 lone pairs, so L = 4. It has two bonds, so B = 4. Then FC = 6 − 4 − 2 = 0.
Step 3 · the single-bonded oxygenIt has 3 lone pairs, so L = 6. It has one bond, so B = 2. Then FC = 6 − 6 − 1 = −1.
Step 4 · check the sum(+1) + 0 + (−1) = 0, and ozone is a neutral molecule. The work holds.
What it meansThe other resonance form is the mirror image. Blending the two spreads the charge evenly, so both bonds come out at bond order 1.5. That is why both O–O distances are measured to be the same.
Worked example 3 · shape and polarity of two molecules
Find the shape and polarity of SF4 and of CCl4.
Step 1 · count for SF4Valence electrons: 6 + 4(7) = 34. Four S–F bonds use 8. Each fluorine takes 3 lone pairs, using 24. That leaves 2 for sulfur, so one lone pair.
Step 2 · read the domainsSulfur has 4 bonds plus 1 lone pair, so 5 domains. The electron geometry is trigonal bipyramidal.
Step 3 · drop the lone pairIgnoring it, the shape is see-saw. The lone pair takes an equatorial spot, where it has the most room.
Step 4 · judge the polarityThe shape is lopsided, so the bond dipoles cannot cancel. SF4 is polar.
Step 5 · now CCl4Carbon has 4 bonds and no lone pairs, so 4 domains and a tetrahedral shape. Each C–Cl bond is polar, with ΔEN = 3.16 − 2.55 = 0.61.
Step 6 · check the symmetryThe four identical arrows point to the corners of a tetrahedron, so they cancel exactly. CCl4 is nonpolar, even though every bond in it is polar.
- Counting pairs when the step says electrons. CO2 has 16 valence electrons, which is 8 pairs.
- Ignoring an ion's charge. For NO3− you add one electron. For NH4+ you remove one.
- Treating a double bond as two domains. VSEPR counts regions, not bonds.
- Reporting the electron geometry as the shape. Water is tetrahedral in domains but bent in shape.
- Thinking resonance forms flip back and forth. The real molecule is one blended structure at all times.
- Assuming polar bonds make a polar molecule. Check whether the shape cancels the arrows.
- Expecting an octet everywhere. Boron takes six, and sulfur in SF6 takes twelve.
Chapter 7 self-test · ten items
Chapter 8Advanced Theories of Covalent Bonding
What to know
Valence bond theory builds a bond from two overlapping orbitals holding one paired-up pair of electrons. Push two atoms together and the energy drops, because each electron now feels two nuclei. Push too far and the nuclei repel. The lowest point on that curve gives the bond length, and the depth of the dip gives the bond energy.
Plain s and p orbitals point the wrong way for most molecules. So the atom mixes them into hybrid orbitals that point where the bonds need to go. Count the regions of electron density on the atom and read off the answer. Two regions give sp. Three give sp2. Four give sp3. Five give sp3d. Six give sp3d2.
Orbitals meet in two ways. Head-on overlap along the bond axis makes a sigma bond. Side-on overlap of two parallel p orbitals makes a pi bond. Every bond between two atoms starts with one sigma bond. A double bond is one sigma plus one pi. A triple bond is one sigma plus two pi.
A pi bond needs its p orbitals to stay parallel. Twisting the bond would pull them out of line and break the overlap. So a double bond cannot rotate. That lock is what makes cis and trans isomers real, separate compounds.
Molecular orbital theory spreads electrons over the whole molecule instead. Two atomic orbitals combine into two molecular orbitals. The bonding one sits lower in energy and piles electron density between the nuclei. The antibonding one sits higher and puts a node there instead. Fill them from the bottom, two electrons per level, following Hund's rule.
For period 2 diatomics, use only the valence electrons. In B2, C2 and N2 the pi 2p level sits below sigma 2p. In O2, F2 and Ne2 the two swap places.
Bond order ties it all together. Subtract antibonding electrons from bonding electrons, then halve it. A higher bond order means a shorter, stronger bond. A bond order of zero means no molecule forms.
Magnetism falls out of the same diagram. Any unpaired electron makes the molecule paramagnetic, so a magnet attracts it. All-paired electrons make it diamagnetic. Oxygen is the famous case. A Lewis structure predicts no unpaired electrons, but O2 really is paramagnetic, and the molecular orbital diagram shows exactly why.
- Count regions of electron density, not atoms, to get the hybridization.
- Every bond has exactly one sigma bond. The extras are pi bonds.
- A double bond will not rotate, because the pi overlap would break.
- Bond order = (bonding − antibonding) ÷ 2.
- Higher bond order means shorter and stronger.
- One unpaired electron is enough to make a molecule paramagnetic.
Equations, units and symbols
| Equation | What each symbol means | Units |
|---|---|---|
| bond order = (nb − na) ÷ 2 | nb is bonding electrons, na is antibonding electrons | no unit; it comes out in halves |
| regions = bonds + lone pairs on that atom | multiple bonds count once, as in VSEPR | a plain count from 2 to 6 |
| sigma bonds = number of bonded atom pairs | one per connected pair, single or multiple | a plain count |
| pi bonds = total bonds − sigma bonds | a double adds 1 pi, a triple adds 2 pi | a plain count |
| Ebond = (D × 1000) ÷ NA | D is the bond energy per mole, NA is Avogadro's number | J per bond, from D in kJ/mol |
| valence electrons in a period 2 diatomic | add both atoms' group electrons, then adjust for any charge | a plain count to fill the diagram |
Worked examples
Worked example 1 · hybridization and bond counting in ethene
For C2H4, give the hybridization on each carbon. Then count sigma and pi bonds.
Step 1 · draw itEach carbon bonds to two hydrogens and shares a double bond with the other carbon.
Step 2 · count regions on one carbonTwo C–H bonds plus one C=C bond gives 3 regions. The double bond counts once.
Step 3 · read the hybridThree regions means sp2. That leaves one unhybridized p orbital on each carbon.
Step 4 · count sigma bondsBonded pairs are four C–H and one C–C. That is 5 sigma bonds.
Step 5 · count pi bondsThe only multiple bond is the double bond, which adds 1 pi bond. It comes from the two leftover p orbitals overlapping side-on.
Check it a second wayThree sp2 lobes lie flat at 120°, so ethene is a flat molecule. That is exactly what measurement shows, and the pi bond above and below the plane is what holds it flat.
Worked example 2 · the oxygen molecule and its magnetism
Fill the molecular orbital diagram for O2. Find the bond order and the magnetism.
Step 1 · count valence electronsEach oxygen brings 6, so there are 12 to place.
Step 2 · fill in orderOxygen is on the side where sigma 2p sits below pi 2p. So: σ2s2, σ*2s2, σ2p2, π2p4, π*2p2. That adds to 12.
Step 3 · sort bonding from antibondingBonding: 2 + 2 + 4 = 8. Antibonding: the starred levels, 2 + 2 = 4.
Step 4 · bond order(8 − 4) ÷ 2 = 2. That matches the double bond a Lewis structure draws.
Step 5 · look at the top levelThe π*2p level is two orbitals of equal energy holding two electrons. Hund's rule puts one in each, unpaired. So O2 is paramagnetic.
Why this mattersLiquid oxygen really does cling to a magnet. A Lewis structure pairs every electron and cannot explain that. This is the clearest win for molecular orbital theory.
Worked example 3 · bond order comparisons and one bond's energy
Find the bond order of N2 and of F2. Then find the energy of a single H–H bond, given D = 436 kJ/mol.
Step 1 · nitrogen's electronsEach nitrogen brings 5, so 10 valence electrons. Nitrogen is on the side where pi 2p sits below sigma 2p. Fill: σ2s2, σ*2s2, π2p4, σ2p2.
Step 2 · nitrogen's bond orderBonding = 2 + 4 + 2 = 8. Antibonding = 2. So (8 − 2) ÷ 2 = 3, a triple bond. Every electron is paired, so N2 is diamagnetic.
Step 3 · fluorine's electronsEach fluorine brings 7, so 14 electrons. Fill: σ2s2, σ*2s2, σ2p2, π2p4, π*2p4.
Step 4 · fluorine's bond orderBonding = 8. Antibonding = 2 + 4 = 6. So (8 − 6) ÷ 2 = 1, a single bond. All paired, so it is diamagnetic.
Step 5 · one bond's energyConvert 436 kJ/mol to joules: 436,000 J/mol. Divide by Avogadro's number: 436,000 ÷ (6.022 × 1023) = 7.24 × 10−19 J per bond.
Check the rankingN2 at bond order 3 should be the shortest and strongest of the two, and F2 at bond order 1 the longest and weakest. Measurement agrees: N≡N takes 945 kJ/mol to break, while F–F takes only 159.
- Counting bonds instead of regions. The carbon in CO2 has 2 regions, so it is sp, not sp3.
- Forgetting lone pairs in the region count. Nitrogen in NH3 has 4 regions, so it is sp3.
- Calling a double bond two pi bonds. It is one sigma plus one pi.
- Including core electrons in a period 2 diagram. Use valence electrons only.
- Using the wrong level order. B2, C2 and N2 put pi 2p lower. O2, F2 and Ne2 put sigma 2p lower.
- Forgetting to halve. Bond order divides the difference by two.
- Pairing the top electrons by habit. Two electrons in two equal orbitals stay unpaired, which is what makes O2 paramagnetic.
Chapter 8 self-test · ten items
Chapter 9Gases
What to know
Pressure is a push spread over an area, so P = F/A. In a gas it is particles drumming on a wall. More particles, faster particles or a smaller box all raise the pressure. Learn the conversions: 1 atm = 760 torr = 760 mmHg = 101.325 kPa.
A barometer measures the air itself. A manometer compares two pushes. With a closed end, the height difference is the gas pressure outright. With an open end, you add or subtract the room's pressure depending on which side is higher.
Every gas law needs kelvin. Add 273.15 to a Celsius value before anything else. Using Celsius is the single most common error in this chapter, and it can even give you a negative temperature.
The simple laws all fall out of one combined law. Boyle holds temperature and amount, so P1V1 = P2V2. Charles holds pressure, so V1/T1 = V2/T2. Gay-Lussac holds volume, so P1/T1 = P2/T2. Avogadro holds pressure and temperature, so V1/n1 = V2/n2. The combined form is P1V1/T1 = P2V2/T2.
One equation does most of the work: PV = nRT. Use R = 0.08206 L·atm/mol·K with pressure in atm and volume in liters. Switch to R = 8.314 J/mol·K for energy and speed problems. The two-state laws compare two conditions. PV = nRT handles one condition at a time.
At standard temperature and pressure, one mole of any gas fills 22.4 L. STP here means 273.15 K and 1 atm. So the density of a gas at STP is just its molar mass divided by 22.4.
Density and molar mass follow from PV = nRT. Replace n with m/M and you get d = PM/RT. Rearranged, M = dRT/P. That is how you identify an unknown gas from a measured density.
Each gas in a mixture acts as if it were alone. So Ptotal is the sum of the partial pressures. The share each one takes follows its mole fraction: PA = XAPtotal. A gas collected over water picks up water vapor, so subtract the water's vapor pressure to get the dry gas pressure.
Kinetic molecular theory explains why all this works. Temperature sets the average kinetic energy, and it is the same for every gas at a given temperature. Mass then sets the speed, so light molecules move faster. That is why light gases escape through a pinhole faster, which is Graham's law. Real gases stray from ideal when they are cold and squeezed, because then the particles' own volume and their attractions start to matter.
- Kelvin or nothing. Add 273.15 first, every time.
- 1 atm = 760 torr = 101.325 kPa.
- R = 0.08206 L·atm/mol·K, or 8.314 J/mol·K for energy work.
- One mole fills 22.4 L at STP, whatever the gas.
- Partial pressure follows the mole fraction, not the mass.
- At the same temperature, every gas has the same average kinetic energy.
Equations, units and symbols
| Equation | What each symbol means | Units |
|---|---|---|
| P = F ÷ A | P is pressure, F is force, A is area | Pa = N/m2 |
| P1V1 = P2V2 | Boyle's law, at fixed T and n | any matching P and V units |
| V1 ÷ T1 = V2 ÷ T2 | Charles's law, at fixed P and n | V in L; T in K only |
| P1 ÷ T1 = P2 ÷ T2 | Gay-Lussac's law, at fixed V and n | P in atm; T in K only |
| V1 ÷ n1 = V2 ÷ n2 | Avogadro's law, at fixed P and T | V in L; n in mol |
| P1V1 ÷ T1 = P2V2 ÷ T2 | the combined gas law, at fixed n | T in K; P and V units just have to match |
| PV = nRT | P pressure, V volume, n moles, R the gas constant, T temperature | atm, L, mol, L·atm/mol·K, K |
| d = PM ÷ RT | d is density, M is molar mass | g/L; M in g/mol |
| M = dRT ÷ P | same equation, solved for molar mass | g/mol |
| Ptotal = PA + PB + ... | Dalton's law of partial pressures | all in the same pressure unit |
| XA = nA ÷ ntotal, and PA = XAPtotal | XA is the mole fraction of gas A | X has no unit; P in any one unit |
| Pgas = Ptotal − Pwater | for a gas collected over water | torr or atm, matched |
| KEavg = (3/2)RT | average kinetic energy per mole | J/mol, using R = 8.314 |
| urms = √(3RT ÷ M) | urms is the root-mean-square speed | m/s; R = 8.314 and M in kg/mol |
| rateA ÷ rateB = √(MB ÷ MA) | Graham's law of effusion | no unit; note the masses swap sides |
| (P + an2/V2)(V − nb) = nRT | van der Waals; a corrects for attraction, b for particle volume | a in L2·atm/mol2; b in L/mol |
Worked examples
Worked example 1 · solving PV = nRT for volume
Find the volume of 2.50 mol of gas at 1.20 atm and 35 °C.
Step 1 · convert the temperature35 + 273.15 = 308.15 K. The 35 is known to the ones place, so use 308 K.
Step 2 · rearrangeV = nRT ÷ P.
Step 3 · put the numbers inV = (2.50 mol)(0.08206 L·atm/mol·K)(308 K) ÷ (1.20 atm).
Step 4 · multiply the top2.50 × 0.08206 = 0.20515. Then 0.20515 × 308 = 63.19 L·atm.
Step 5 · divide63.19 ÷ 1.20 = 52.66 L, so 52.7 L.
Check the unitsMoles cancel with moles, kelvin with kelvin, and atm with atm. Liters are left, which is what a volume needs to be.
Worked example 2 · the combined gas law
A 3.00 L balloon sits at 25 °C and 1.00 atm. It rises to where the pressure is 0.500 atm, and it warms to 100 °C. Find the new volume.
Step 1 · both temperatures to kelvinT1 = 25 + 273.15 = 298 K. T2 = 100 + 273.15 = 373 K.
Step 2 · rearrangeV2 = P1V1T2 ÷ (T1P2).
Step 3 · substituteV2 = (1.00)(3.00)(373) ÷ [(298)(0.500)] = 1,119 ÷ 149 = 7.51 L.
Step 4 · report itThe new volume is 7.51 L.
Check it a second wayHalving the pressure should double the volume, giving 6.00 L. Warming from 298 K to 373 K multiplies by 373/298 = 1.25. Then 6.00 × 1.25 = 7.50 L. That matches within rounding.
Worked example 3 · identify a gas from its density
A gas has a density of 1.96 g/L at STP. Find its molar mass and name a likely gas.
Step 1 · pick the equationYou have density and want molar mass, so use M = dRT ÷ P.
Step 2 · list the conditionsAt STP, T = 273.15 K and P = 1.00 atm.
Step 3 · substituteM = (1.96 g/L)(0.08206 L·atm/mol·K)(273.15 K) ÷ (1.00 atm).
Step 4 · multiply1.96 × 0.08206 = 0.16084. Then 0.16084 × 273.15 = 43.93, so 43.9 g/mol.
Step 5 · name itCarbon dioxide is 44.01 g/mol, so the gas is very likely CO2.
Check it a second wayAt STP you can skip R. Molar mass = d × 22.4 = 1.96 × 22.4 = 43.9 g/mol. Same answer, far less arithmetic.
Worked example 4 · partial pressures and effusion
A flask holds 0.200 mol of N2 and 0.300 mol of O2 at a total pressure of 2.50 atm. Find each partial pressure. Then compare how fast helium and oxygen effuse.
Step 1 · total moles0.200 + 0.300 = 0.500 mol.
Step 2 · mole fractionsX(N2) = 0.200 ÷ 0.500 = 0.400. X(O2) = 0.300 ÷ 0.500 = 0.600. They add to 1.000.
Step 3 · split the pressureP(N2) = 0.400 × 2.50 = 1.00 atm. P(O2) = 0.600 × 2.50 = 1.50 atm. The two add back to 2.50 atm.
Step 4 · set up Graham's lawrate(He) ÷ rate(O2) = √(M of O2 ÷ M of He) = √(32.00 ÷ 4.003).
Step 5 · take the root32.00 ÷ 4.003 = 7.994, and √7.994 = 2.83. So helium effuses 2.83 times faster.
Why the masses swapThe lighter gas is the faster one, so its mass belongs on the bottom inside the root. If you get an answer below 1 for the lighter gas, you flipped the fraction.
- Leaving temperature in Celsius. Convert to kelvin before touching any gas law.
- Using the wrong R. Pair 0.08206 with atm and liters. Pair 8.314 with joules, kg/mol and pascals.
- Using 22.4 L away from STP. That molar volume only holds at 273.15 K and 1 atm.
- Forgetting the water vapor. A gas collected over water needs Pwater subtracted first.
- Splitting pressure by mass. Partial pressure follows the count of particles, so use mole fractions.
- Flipping Graham's law. The masses trade places, so the lighter gas comes out faster.
- Using g/mol in urms. That equation needs kg/mol, so divide the molar mass by 1,000.
Chapter 9 self-test · ten items
One pageCram sheet
Everything from chapters 7 to 9 in one place. Cover the right column and rebuild each row from memory.
Equations
| Name | Equation | Units |
|---|---|---|
| Lattice energy trend | ΔHlattice ∝ Q1Q2 ÷ r0 | kJ/mol |
| Bond polarity | ΔEN = ENhigher − ENlower | no unit |
| Formal charge | FC = V − L − ½B | whole number |
| Bond order from resonance | bonds shared ÷ resonance forms | no unit |
| Bond order from orbitals | (bonding − antibonding) ÷ 2 | no unit |
| Energy of one bond | (D × 1000) ÷ NA | J per bond |
| Pressure | P = F ÷ A | Pa = N/m2 |
| Boyle | P1V1 = P2V2 | matching units |
| Charles | V1/T1 = V2/T2 | T in K |
| Gay-Lussac | P1/T1 = P2/T2 | T in K |
| Avogadro | V1/n1 = V2/n2 | L and mol |
| Combined | P1V1/T1 = P2V2/T2 | T in K |
| Ideal gas law | PV = nRT | atm, L, mol, K |
| Gas density | d = PM ÷ RT | g/L |
| Molar mass from density | M = dRT ÷ P | g/mol |
| Dalton's law | Ptotal = PA + PB + ... | matching units |
| Mole fraction | XA = nA/ntotal, PA = XAPtotal | X has no unit |
| Gas over water | Pgas = Ptotal − Pwater | torr or atm |
| Average kinetic energy | KEavg = (3/2)RT | J/mol |
| Molecular speed | urms = √(3RT ÷ M) | m/s; M in kg/mol |
| Graham's law | rateA/rateB = √(MB/MA) | no unit |
| Van der Waals | (P + an2/V2)(V − nb) = nRT | atm, L, mol, K |
Constants and values
| Quantity | Value | Note |
|---|---|---|
| Gas constant | R = 0.08206 L·atm/mol·K | use with atm and liters |
| Gas constant, energy form | R = 8.314 J/mol·K | use for KEavg and urms |
| Pressure conversions | 1 atm = 760 torr = 760 mmHg = 101.325 kPa | 1 bar = 100 kPa, slightly under 1 atm |
| STP | 273.15 K and 1 atm | molar volume there is 22.4 L/mol |
| Absolute zero | 0 K = −273.15 °C | so K = °C + 273.15 |
| Water vapor pressure | 23.8 torr at 25 °C | subtract it for a gas over water |
| Avogadro's number | NA = 6.022 × 1023 /mol | for per-bond energies |
| Electronegativity values | F 3.98, O 3.44, Cl 3.16, N 3.04, C 2.55, H 2.20, Na 0.93, K 0.82 | fluorine is the highest of all |
| Bond energies | H–H 436, Cl–Cl 242, F–F 159, O=O 498, N≡N 945, C–C 347, C≡C 839 | all in kJ/mol |
| Molar masses used here | He 4.003, CH4 16.04, N2 28.01, O2 32.00, CO2 44.01, SO2 64.06 | in g/mol |
Shape and orbital tables
| Domains | Electron geometry | Shapes as lone pairs are added | Hybrid |
|---|---|---|---|
| 2 | linear, 180° | linear | sp |
| 3 | trigonal planar, 120° | trigonal planar, then bent | sp2 |
| 4 | tetrahedral, 109.5° | tetrahedral, then trigonal pyramidal, then bent | sp3 |
| 5 | trigonal bipyramidal, 90° and 120° | trigonal bipyramidal, then see-saw, then T-shaped, then linear | sp3d |
| 6 | octahedral, 90° | octahedral, then square pyramidal, then square planar | sp3d2 |
Rules that are not equations
| Topic | The rule |
|---|---|
| Bond type by ΔEN | Under 0.4 nonpolar covalent. From 0.4 to 1.8 polar covalent. Over 1.8 treat as ionic. |
| Lewis structures | Count electrons, place the least electronegative atom in the center, bond, fill the outer atoms, then form multiple bonds to complete shells. |
| Octet exceptions | Odd electron counts, short shells on Be and B, and expanded shells from period 3 down. |
| Best resonance form | Formal charges nearest zero, with any negative charge on the most electronegative atom. |
| Molecular polarity | Polar bonds plus a shape that does not cancel them. Symmetry with identical outer atoms cancels. |
| Sigma and pi | One sigma per bonded pair. A double adds 1 pi, a triple adds 2 pi. |
| Rotation | Sigma bonds rotate freely. Pi bonds lock the geometry, which creates cis and trans isomers. |
| Level order in period 2 | B2, C2 and N2 put π2p below σ2p. O2, F2 and Ne2 swap them. |
| Magnetism | Any unpaired electron means paramagnetic. All paired means diamagnetic. |
| Real gases | They stray from ideal when cold and squeezed, because particle volume and attractions start to matter. |