CHEM3120 Environmental and Analytical Chemistry
CHEM3120 Overview
- University of Sydney
- S1 2027
- 10 chapters
- Chemistry
CHEM3120 Environmental and Analytical Chemistry is the University of Sydney's third-year unit in the School of Chemistry (Faculty of Science), dual-coded with the Advanced unit CHEM3920, and it runs in Semester 1 only.
- Assessed by Laboratory 40% · Final Exam 38% · Written Assignment 12% · Weekly Quizzes 10%
- Key terms Accuracy vs precision, Detection limit (LOD), Beer-Lambert law, Henry's law
- How to prepare Treat CHEM3120 as a set of recurring calculation types layered on a conceptual spine, and rehearse both weekly rather than cramming through STUVAC.
- Most asked Does CHEM3120 have a hurdle?
How CHEM3120 is assessed
| Component | Weight | Format |
|---|---|---|
| Laboratory | 40% | Across the semester (separate Canvas site) |
| Final Exam | 38% | Closed-book, 2 h writing + 10 min reading; Part A short-answer (~80 marks) + Part B 20 MCQ |
| Written Assignment | 12% | Short-answer, due ~Week 9; Turnitin (late -5%/day, zero after 10 days) |
| Weekly Quizzes | 10% | Weekly online quizzes; the best 7 count |
What CHEM3120 covers
CHEM3120 Environmental and Analytical Chemistry runs across three lecture blocks — analytical foundations and techniques, atmospheric chemistry, then aqueous and metal-ion chemistry — and this ten-chapter map follows that teaching schedule in order.
The unit is assessed through weekly online quizzes (best 7 count, 10%), a written assignment (12%, around Week 9), a 40% laboratory component and a closed-book final exam (38%), with a theory-versus-laboratory double hurdle: you must pass both the theory and the laboratory to pass the unit.
Use the map to see how each block's calculations — Beer-Lambert, Henry's law, acid-base and carbonate speciation, pE-pH diagrams — build toward Part A short-answer and Part B multiple-choice on the final.
Analytical Chemistry Foundations
Accuracy & precision · sampling · resolution & interference · errors and significant figures (L2)Lecture 2 lays the foundations of analytical measurement for CHEM3120: accuracy versus precision, representative sampling, and the three ideas that govern any measurement — resolution, interference and sampling — plus how to report a result with a sensible detection limit and the right number of significant figures.
- The analytical process governed by resolution, interference and sampling
- Accuracy (closeness to the true value) vs precision (reproducibility) — systematic vs random error
- Representative sampling: taking a sample whose composition reflects the bulk
- Sensitivity = signal change per unit concentration (slope of the calibration line)
- Detection limit: signal equal to about twice the peak-to-peak baseline noise
- Interference: a species that changes the signal for the analyte of interest
Analytical Techniques: GC, AAS & Flame Photometry
Gas chromatography (TCD/FID/ECD) · atomic absorption · calibration & Beer-Lambert (L3, L6, L7)Lectures 3, 6 and 7 cover the workhorse instruments of CHEM3120: gas chromatography (separation on a stationary phase, with TCD, FID and electron-capture detectors), atomic absorption spectroscopy (hollow-cathode lamp, flame atomisation, Beer-Lambert quantitation) and flame photometry (emission from thermally excited atoms).
- Gas chromatography: stationary phase (non-volatile coating) vs mobile phase (inert carrier gas); selective retardation and separation
- GC detectors: TCD (thermal-conductivity, filament resistance), FID (CH· + O → CHO+ + e-), electron-capture; GC-MS and single-ion monitoring
- FID limitation: responds to C-H organics only, not heteroatoms (O, S, N, P, Cl) and not CO
- Atomic absorption spectroscopy: hollow-cathode lamp, flame atomisation, absorption by ground-state atoms, chopper background correction
- Flame photometry (emission): thermal excitation then emission of a characteristic line; filters not a monochromator; Na, K, Li, Ca
- Beer-Lambert law A = -log(I/I0) = εcl for quantitation
Soil Chemistry & Salinity
Clay/silt/sand · alumino-silicates · cation exchange capacity · salinity & sodicity (L1, L4)Lectures 1 and 4 cover the chemistry of soil in CHEM3120: how weathering of silicate rock produces clay, silt and sand; the hydrated alumino-silicate structure of clays and their cation-exchange behaviour; and how land management drives salinity.
- Soil = inorganic mineral fraction (from rock weathering) + organic (humic) matter
- Particle size classes: clay (fine, hydrated alumino-silicates), silt (intermediate), sand (0.7-1.4 mm; silica inland or CaCO3 on beaches)
- Clay from acid hydrolysis of silicate rocks; layered alumino-silicate structure
- Cation exchange: clay surfaces hold and swap exchangeable cations
- Dryland salinity: vegetation clearing raises the watertable, evaporation concentrates dissolved salts near the surface
- Heavy-metal soil contamination (Hg, Pb, Cd, Cr, Cu) from industry
Persistent Organic Pollutants
PCBs · DDT (mode of action + remediation) · dioxins · bioaccumulation (L5)Lecture 5 covers persistent organic pollutants (POPs) in CHEM3120: PCBs, DDT and dioxins such as 2,3,7,8-TCDD — why they persist, how they bioaccumulate up food chains, DDT's mode of action on nerves, and how contaminated sites are remediated.
- POPs: PCBs, DDT, dioxins — lipophilic, chemically stable, long environmental half-lives
- Bioaccumulation and biomagnification: fat-soluble pollutants concentrate up the food chain
- DDT as an insecticide: persistent, low vapour pressure, fat-soluble, slow-reacting
- DDT mode of action: holds open Na+ nerve channels, causing continuous nerve impulses
- Dioxin formation: heating a 2,4,5-trichlorophenylate salt on silica (280 °C) gives 2,3,7,8-TCDD
- Analysis of POPs by gas chromatography (links to the techniques block)
Atmospheric Chemistry & the Carbon/Nitrogen Cycles
Greenhouse effect · blackbody / Wien · energy balance · C and N cycles (L9-16)Block 2 (Lectures 9-16) of CHEM3120 covers the atmosphere: the carbon and nitrogen cycles, the greenhouse effect and Earth's radiative energy balance (blackbody emission, Wien's law), photochemical smog and NOx, and CFCs and the ozone hole.
- Blackbody radiation: any body at T > 0 emits; the peak wavelength shortens as T rises
- Wien's law λ_max · T = 2.898×10^6 K·nm; Earth's emission peaks in the infrared
- Greenhouse effect: Earth's IR emission overlaps the CO2 bending-mode absorption
- Why CO2 outweighs water vapour as a greenhouse gas near Earth's emission peak
- Radiative energy balance and the IPCC picture; Stefan-Boltzmann q = 4πr²σT⁴
- Photochemical smog: N2 + O2 → 2NO in engines (morning peak), O3 downstream at midday
Aqueous Chemistry: Water Properties & Hardness
Water hardness (Ca/Mg, CaCO3 equivalents) · Henry's law · dissolved O2 · COD/BOD (L17)Lecture 17 opens Block 3 of CHEM3120 with the chemistry of natural waters: hardness from Ca2+ and Mg2+ expressed as a CaCO3 equivalent, Henry's-law gas solubility (dissolved O2, N2, CO2), and the oxygen-demand measures COD and BOD.
- Global water distribution: ~97% oceans, only ~0.5% accessible freshwater
- Hardness from divalent Ca2+ and Mg2+, expressed as mg/L CaCO3 equivalent
- Soap scum: precipitation (e.g. calcium stearate) once the ion product exceeds Ksp
- Henry's law [X(aq)] = kH · P(X) for dissolved O2, N2, CO2 and volatile pollutants
- Dissolved oxygen and its temperature dependence
- Chemical oxygen demand (COD) by dichromate titration; electron bookkeeping to O2 equivalent
Acid-Base Speciation & Distribution Diagrams
Weak-acid pH · Ka/Kb · Henderson-Hasselbalch · alpha (distribution) diagrams (L18)Lecture 18 covers acid-base equilibria in environmental systems for CHEM3120: weak-acid and weak-base pH from Ka and Kb, the Henderson-Hasselbalch equation, and reading species-distribution (alpha) diagrams where the fraction of HA and A- crosses over at pH = pKa.
- Weak-acid pH via Ka = x²/(C - x) ≈ x²/C when dissociation is small
- Weak-base / salt hydrolysis via Kb = Kw/Ka
- The Henderson-Hasselbalch equation pH = pKa + log([A-]/[HA])
- Species-distribution (alpha) diagrams: fraction of HA vs A- against pH
- Crossover at pH = pKa (each species 50%); one species dominates about 2 pH units either side
- When to add water autoionisation at very low acid concentration ([H+] = √(Ka[HA] + Kw))
Carbonate & Sulfide Equilibria; Ocean Acidification
The H2CO3 / HCO3- / CO3^2- system · pKa1/pKa2 · ocean acidification (L19-20)Lectures 19-20 apply speciation to the carbonate and sulfide systems in CHEM3120: the H2CO3 / HCO3- / CO3^2- equilibria (pKa1 ~6.3, pKa2 ~10.3), why dissolved [H2CO3] is fixed by atmospheric CO2, and how rising CO2 drives ocean acidification and dissolves CaCO3.
- The carbonate system H2CO3 / HCO3- / CO3^2- with pKa1 ~6.3 and pKa2 ~10.3
- [H2CO3] fixed by atmospheric P(CO2) via Henry's law — pH-independent (horizontal on a log-speciation diagram)
- Which species dominates in each pH window; the two crossovers at the pKa values
- Ocean acidification: rising CO2 lowers pH and shifts speciation
- H2CO3 + CO3^2- → 2HCO3-: added CO2 consumes carbonate, lowering [CO3^2-]
- CaCO3 (aragonite/calcite) dissolves when [Ca2+][CO3^2-] falls below Ksp
Metal Ions: Hydrolysis, Redox & pE-pH Diagrams
Metal hydrolysis · redox in natural waters · pE-pH (Pourbaix) · transport & toxicity (L21-24)Lectures 21-24 cover the environmental chemistry of metal ions in CHEM3120: stepwise hydrolysis and speciation, redox in natural waters described by pE, the construction and reading of pE-pH (Pourbaix) diagrams, and metal transport and toxicity (mercury, lead).
- Stepwise metal-ion hydrolysis M^n+ → M(OH) → ... with successive pKa values
- Dominant hydroxide species between successive pKa; amphoteric hydroxides redissolve at high pH
- pE = -log[e-] as an electron-availability scale; pE° = E°/0.0592 at 25 °C
- Nernst-style pE lines pE = pE° - (m/n)pH from combining half-reactions with H+/e-
- pE-pH (Pourbaix) diagrams: lines separating oxidised/reduced and soluble/solid regions
- The iron example: Fe2+, Fe3+, Fe(OH)3 and Fe(s) regions
Water Purification & Desalination
Coagulation/flocculation · distillation · reverse osmosis · treatment trains (L25)Lecture 25 closes CHEM3120 with the chemistry of making water safe and fresh: coagulation and flocculation to remove suspended clay and colloids, sedimentation and filtration, disinfection, and distillation and reverse-osmosis desalination, assembled into a treatment train.
- Suspended solids, colloids and turbidity in raw water
- Coagulation and flocculation: destabilising and aggregating fine particles so they settle
- Sedimentation (Stokes' law) and filtration to remove aggregated solids
- Stokes settling velocity v = (2/9)·g·(ρ_s - ρ_d)·r²/η
- Disinfection of treated water
- Distillation and reverse osmosis (RO) for desalination
The unit joins two threads — the analytical chemistry of measuring species in the environment (sampling, resolution and interference, gas chromatography, atomic absorption and flame photometry, mass spectrometry and X-ray methods) and the environmental chemistry of the atmosphere, water and soil (the greenhouse effect and the carbon/nitrogen cycles, water hardness and dissolved oxygen, acid-base and carbonate speciation, ocean acidification, metal-ion redox and pE-pH diagrams, and water purification).
It is a calculation-dense unit: the marks live in choosing the right relationship (Beer-Lambert A = εcl, Henry's law, Ka/Kb and Henderson-Hasselbalch, Ksp precipitation tests, pE-pH lines), substituting with correct units, and interpreting the number.
The University of Sydney assesses CHEM3120 through weekly online quizzes (best 7 count, 10%), a written assignment (12%, around Week 9, submitted on Canvas via Turnitin), a 40% laboratory component and a closed-book final exam worth 38% (2 hours writing + 10 minutes reading; Part A short-answer ~80 marks + Part B 20 multiple-choice).
Critically, there is a theory-versus-laboratory double hurdle — you must pass BOTH the theory component and the laboratory to pass the unit — so steady work across the semester matters, and the CHEM3120 result feeds the Weighted Average Mark (WAM) that later chemistry units build on.
Worked example · free
Total water hardness as a CaCO3 equivalent
- +1Convert each divalent cation to moles. Ca2+: 40.0 mg ÷ 40.0 g/mol = 1.00 mmol. Mg2+: 12.15 mg ÷ 24.3 g/mol = 0.500 mmol. Hardness counts only the divalent ions Ca2+ and Mg2+.
- +1Add to get the total moles of hardness-causing ions: n = 1.00 + 0.500 = 1.50 mmol in 0.500 L.
- +1Each mole of divalent ion is expressed as one mole of CaCO3 equivalent, so moles of CaCO3 equivalent = 1.50 mmol. Convert to a concentration: 1.50 mmol ÷ 0.500 L = 3.00 mmol/L.
- +1Multiply by the molar mass of CaCO3: 3.00 mmol/L × 100.0 mg/mmol = 300 mg/L as CaCO3.
Key terms
- Accuracy vs precision
- Accuracy is closeness to the true value; precision is the reproducibility (spread) of repeated measurements. A method can be precise but inaccurate (a systematic bias) or accurate on average but imprecise.
- Detection limit (LOD)
- The lowest concentration giving a signal reliably distinguishable from baseline noise — commonly the concentration at which the peak height equals about twice the peak-to-peak baseline noise.
- Beer-Lambert law
- A = -log(I/I0) = εcl: absorbance is proportional to the molar absorption coefficient ε, concentration c and path length l. The quantitative backbone of AAS and molecular absorption.
- Henry's law
- At fixed temperature the dissolved concentration of a gas is proportional to its partial pressure: [X(aq)] = kH · P(X). Governs dissolved O2, N2 and CO2 in natural waters.
- Speciation (distribution) diagram
- A plot of the fraction of each acid-base species versus pH. Two species cross over (each 50%) at pH = pKa; one dominates roughly two pH units either side.
- pE
- A measure of a solution's electron availability, pE = -log[e-], analogous to pH for electrons; pE° = E°/0.0592 at 25 °C. High pE = oxidising, low pE = reducing conditions.
CHEM3120 FAQ
Is CHEM3120 hard?
It is demanding more for its breadth and its calculation load than for any single hard idea. CHEM3120 spans analytical techniques, atmospheric chemistry, aqueous equilibria and metal-ion redox, and most exam marks come from quantitative work — Beer-Lambert, Henry's law, Ka/Kb and Henderson-Hasselbalch, Ksp precipitation tests and pE-pH lines.
The exam is CLOSED-book but a formula sheet, a periodic table and standard reduction potentials are provided, so you memorise method, not constants. Students who rehearse the recurring calculation types weekly through the semester, rather than cramming through STUVAC, generally find it manageable, and a HD (>=85) is realistic with steady practice.
Does CHEM3120 have a hurdle?
Yes — a theory-versus-laboratory DOUBLE hurdle. CHEM3120 has two components, theory (the weekly quizzes, the written assignment and the final exam, together 60%) and laboratory (40%), and you must pass BOTH independently to pass the unit; a strong theory mark cannot rescue a failed lab, and vice versa.
The exact numeric pass mark for each component is not stated in the public materials, so confirm it on Canvas and the current unit outline. This is why steady work on both fronts across the semester matters for your WAM.
Is the CHEM3120 final open- or closed-book?
It is a CLOSED-book exam — no materials are permitted into the room. You may bring a non-programmable calculator, and the paper itself provides a formula sheet, a full periodic table with atomic weights and a table of standard reduction potentials. The exam is 2 hours of writing plus 10 minutes reading time, with Part A short-answer (~80 marks) and Part B (20 multiple-choice, answered on a Gradescope bubble sheet).
Always confirm the exact date, room and permitted materials on Canvas and the University of Sydney exam timetable before the day.
Can AI help me with CHEM3120?
Yes, as a study aid. Sia is an AI tutor trained on how CHEM3120 is actually taught and assessed: it can walk you through a Beer-Lambert or standard-addition calculation, explain why the space of dominant carbonate species shifts with pH, unpack how a pE-pH (Pourbaix) line is derived, or check the units in your own working — step by step, so you learn the method.
It explains and checks your reasoning; it does NOT do graded assessment for you, and University of Sydney academic-integrity rules still apply.
Where can I find past exam papers/practice for CHEM3120?
Start on Canvas, where the unit posts practice questions, quiz material and any released past papers, and check the University of Sydney Library's past-exam-paper collection. Your weekly quizzes and the lecture problem sets are the closest match to the exam's style, since the final favours short, precise conceptual answers and the recurring calculation types.
This guide also includes a re-authored practice exam that mirrors the paper's shape (Part A short-answer + Part B MCQ across analytical techniques, atmospheric, aqueous and metal-ion chemistry) with fresh numbers, and you can ask Sia to build extra questions in the same style and explain each step.
Questions students ask in each CHEM3120 chapter
- What is the difference between accuracy and precision?
- Accuracy is closeness to the true value; precision is the spread of repeated results. They are independent: you can be precise but consistently wrong (a systematic bias), or accurate on average but scattered (random error). A good method needs both, which is why calibration checks and replicates matter. Chapter 01 · Analytical Chemistry Foundations
- What is the difference between AAS and flame photometry?
- Both atomise the sample in a flame, but AAS measures ABSORPTION by ground-state atoms of light from a hollow-cathode lamp (it needs an external light source), while flame photometry measures the EMISSION from the small fraction of atoms that the flame thermally excites (no lamp). Emission suits easily excited elements like Na, K and Li; AAS is more general and uses Beer-Lambert, A = εcl, for quantitation. Chapter 02 · Analytical Techniques: GC, AAS & Flame Photometry
- What actually makes a clay different from sand?
- Chiefly particle size and structure. Clays are the finest fraction — hydrated, layered alumino-silicates from the acid hydrolysis of silicate rock — with very high surface area, so they hold water and exchange cations strongly. Sand is much coarser (roughly 0.7-1.4 mm grains, mostly silica inland or CaCO3 on beaches) with little surface chemistry. Silt sits in between. The clay fraction is where most of a soil's chemistry happens. Chapter 03 · Soil Chemistry & Salinity
- What makes a pollutant persistent?
- Chemical stability plus low reactivity and low volatility. A persistent organic pollutant resists photochemical and biological breakdown, so it has a long environmental half-life, and because it is fat-soluble it partitions into living tissue rather than being flushed away in water. Those same features let it travel and accumulate, which is why PCBs, DDT and dioxins remain in the environment long after use. Chapter 04 · Persistent Organic Pollutants
- Why is CO2 a more important greenhouse gas than water vapour, despite being less abundant?
- Because of WHERE it absorbs. Earth's thermal emission peaks in the infrared near 10 µm (Wien's law at ~288 K), and CO2's vibrational modes absorb strongly in that region, so CO2 intercepts a large share of the outgoing longwave radiation. Water vapour absorbs more at shorter IR wavelengths where Earth radiates comparatively little, so per molecule near the emission peak CO2 is disproportionately effective. Chapter 05 · Atmospheric Chemistry & the Carbon/Nitrogen Cycles
- How do I express water hardness as a CaCO3 equivalent?
- Convert the mass of each divalent ion (Ca2+, Mg2+) to moles, add the moles together, then re-express that total as CaCO3 by multiplying by 100 g/mol and dividing by the sample volume. The key idea is that hardness is a mole count of divalent ions on a common CaCO3 scale — you never simply add the milligrams of Ca2+ and Mg2+ together, because they have different molar masses. Chapter 06 · Aqueous Chemistry: Water Properties & Hardness
- When can I use [H+] = √(Ka·C) for a weak acid?
- When dissociation is small — the rule of thumb is that x = [H+] should be under about 5% of the initial concentration C. Then Ka = x²/(C - x) simplifies to x²/C and gives [H+] = √(Ka·C). Always check x/C afterwards; if it exceeds 5%, or the acid is very dilute, solve the full quadratic (supplied on the exam formula sheet) or add the water term [H+] = √(Ka[HA] + Kw). Chapter 07 · Acid-Base Speciation & Distribution Diagrams
- Which carbonate species dominates in natural water?
- Bicarbonate, HCO3-, across most of the natural range. Because HCO3- is the middle species and it dominates between pKa1 (~6.3) and pKa2 (~10.3), and most natural waters sit in that window (seawater ~8.1), bicarbonate is the main form of dissolved inorganic carbon. Carbonic acid dominates only below ~6.3 and carbonate ion only above ~10.3, both unusual in ordinary waters. Chapter 08 · Carbonate & Sulfide Equilibria; Ocean Acidification
- What is pE and how does it relate to E°?
- pE = -log[e-] is to electrons what pH is to protons: a measure of how oxidising or reducing a solution is. It links directly to electrode potential through pE° = E°/0.0592 at 25 °C, so a couple with a high standard potential has a high pE° and describes oxidising conditions. High pE means electrons are scarce (oxidising); low pE means electrons are abundant (reducing). Chapter 09 · Metal Ions: Hydrolysis, Redox & pE-pH Diagrams
- What is the difference between coagulation and flocculation?
- They are two stages of the same goal — getting fine particles to settle. Coagulation chemically destabilises the particles, overcoming the surface charge that keeps them apart, usually by adding an electrolyte or coagulant. Flocculation then uses gentle mixing to let those destabilised particles collide and grow into larger aggregates (flocs). Coagulation makes sticking possible; flocculation grows the flocs big enough to remove by sedimentation or filtration. Chapter 10 · Water Purification & Desalination
How to study for the exam
Treat CHEM3120 as a set of recurring calculation types layered on a conceptual spine, and rehearse both weekly rather than cramming through STUVAC.
Each week, take that block's signature calculation end to end — Beer-Lambert or standard addition for the analytical techniques, Wien's law and the energy balance for the atmosphere, hardness and Henry's law for water, Ka/Kb and speciation fractions for acid-base, the carbonate and pE-pH systems for the aqueous-metals block — and write the relationship, substitute with units, compute once, then interpret and sanity-check the result.
Because the weekly quizzes count best-7-of and the assignment falls around Week 9, keep every block warm rather than filing it away. The final is closed-book but supplies a formula sheet, periodic table and reduction-potential table, so drill METHOD and units, not memorised constants; and because there is a theory-versus-laboratory double hurdle, protect your laboratory marks as carefully as your exam preparation.
When a step will not click, ask Sia to re-explain that one step a different way and set you a fresh practice question in the same style — it teaches the method and checks your reasoning, and it never substitutes for your own graded work. Confirm the exam date, room and permitted materials on Canvas and the exam timetable.
Your AI Chemistry tutor for CHEM3120
Stuck on a hard CHEM3120 question? Sia is AskSia’s AI Chemistry tutor — ask any CHEM3120 Environmental and Analytical Chemistry question and get a clear, step-by-step explanation grounded in how the course is actually taught and assessed. Read this whole study guide free, then take your hardest questions to Sia.