IIT-JAM Inorganic Qualitative Analysis — Salt Analysis and Its Chemistry
Salt analysis is taught in the laboratory as a sequence of steps to follow, and that is exactly how not to prepare it for IIT-JAM. A written paper cannot ask you to smell a gas; it asks why ammonium chloride is added before ammonia, why hydrogen sulphide separates copper from zinc, and which reagent will fail if an interfering radical is present. Every one of those answers is solubility-product and common-ion equilibrium in disguise. This guide walks through the group scheme with the equilibrium arithmetic actually computed, then lists the confirmatory tests and the equations worth writing out in full.
The one principle behind the whole scheme
For MxAy(s) ⇌ xMy+ + yAx−, Q = [My+]x[Ax−]y
Q > Ksp → precipitation · Q = Ksp → saturated · Q < Ksp → stays in solution
The whole group scheme is one idea used five times over: the analyst controls the concentration of the precipitating anion — Cl−, S2−, OH− or CO32− — so that Q crosses Ksp for one set of cations and not for the next. The control is exerted through pH and the common-ion effect. Nothing else is going on.
The group scheme in one table
| Group | Reagent | Cations | Precipitate and colour |
|---|---|---|---|
| 0 | NaOH, warm | NH4+ | NH3 gas, no precipitate |
| I | dilute HCl | Pb2+, Ag+, Hg22+ | PbCl2, AgCl, Hg2Cl2 — all white |
| II A | H2S in dilute HCl | Cu2+, Cd2+, Bi3+, Pb2+, Hg2+ | CuS black, CdS yellow, Bi2S3 brown, PbS black, HgS black |
| II B | same, then yellow (NH4)2Sx | As3+, Sb3+, Sn2+/4+ | As2S3 yellow, Sb2S3 orange, SnS2 yellow — these redissolve as thio-anions |
| III | NH4Cl then NH4OH | Fe3+, Al3+, Cr3+ | Fe(OH)3 reddish-brown, Al(OH)3 white gelatinous, Cr(OH)3 green |
| IV | H2S in ammoniacal solution | Zn2+, Mn2+, Ni2+, Co2+ | ZnS white, MnS buff, NiS black, CoS black |
| V | (NH4)2CO3 in ammoniacal solution | Ba2+, Sr2+, Ca2+ | BaCO3, SrCO3, CaCO3 — all white |
| VI | none (soluble group) | Mg2+, Na+, K+ | identified by flame test and specific reagents |
Group II B is separated from II A by the amphoteric, thiophilic character of arsenic, antimony and tin: their sulphides dissolve in yellow ammonium sulphide as thio-anions such as AsS43−, while the II A sulphides do not.
Worked example 1 — why ammonium chloride goes in before ammonia
Show numerically that adding NH4Cl before NH4OH stops magnesium from precipitating in group III, while still precipitating aluminium. Take Kb(NH3) = 1.8 × 10−5, both NH3 and NH4+ at 0.10 M, and each metal ion at 0.010 M.
Step 1 — hydroxide concentration from 0.10 M ammonia alone.
[OH−] = √(Kb × C) = √(1.8 × 10−5 × 0.10) = √(1.8 × 10−6)
= 1.34 × 10−3 M
(check: (1.34 × 10−3)2 = 1.80 × 10−6)
Step 2 — hydroxide concentration in the NH3/NH4+ buffer.
[OH−] = Kb × [NH3]/[NH4+] =
1.8 × 10−5 × (0.10 / 0.10) = 1.8 × 10−5 M
That is a fall by a factor of 1.34 × 10−3 ÷ 1.8 × 10−5 ≈ 75.
Step 3 — test magnesium. Using Ksp[Mg(OH)2] ≈ 1.8 × 10−11:
Without the buffer: Q = 0.010 × (1.34 × 10−3)2 = 0.010 × 1.80 × 10−6
= 1.8 × 10−8, which is about a thousand times larger than
Ksp → Mg(OH)2 would precipitate, wrongly putting magnesium
in group III.
With the buffer: Q = 0.010 × (1.8 × 10−5)2 = 0.010 × 3.24 × 10−10
= 3.2 × 10−12, which is below Ksp → magnesium
stays in solution and reaches group VI where it belongs.
Step 4 — check aluminium still comes down. Ksp[Al(OH)3] is of the order of 10−33. In the buffer, Q = 0.010 × (1.8 × 10−5)3 = 0.010 × 5.83 × 10−15 = 5.8 × 10−17, which is roughly sixteen orders of magnitude above Ksp. Aluminium precipitates comfortably.
That is the whole answer to "why NH4Cl first". The common ion NH4+ pushes the ammonia equilibrium back and drops [OH−] into the narrow window that is high enough for the group III trivalent hydroxides and too low for the group VI divalent ones. Note that this margin is comfortable, so the conclusion survives the real spread in published Ksp values.
Worked example 2 — why H2S separates group II from group IV
Compute the sulphide-ion concentration in 0.30 M HCl and at pH 9, for a solution saturated with H2S at about 0.10 M.
Combining the two dissociation steps of H2S gives
[S2−] = Ka1Ka2 × [H2S] ÷ [H+]2
Take the commonly quoted representative values Ka1 ≈ 1.0 × 10−7 and Ka2 ≈ 1.0 × 10−14, so Ka1Ka2 ≈ 1.0 × 10−21. (Books differ noticeably on Ka2; use the value your own textbook gives and state it — the ratio below is what matters and it is unaffected.)
In 0.30 M HCl: [H+] = 0.30, so [H+]2 = 0.090.
[S2−] = (1.0 × 10−21 × 0.10) ÷ 0.090 = 1.0 × 10−22 ÷ 0.090 =
1.1 × 10−21 M
At pH 9 (ammoniacal): [H+] = 1.0 × 10−9, so
[H+]2 = 1.0 × 10−18.
[S2−] = 1.0 × 10−22 ÷ 1.0 × 10−18 = 1.0 × 10−4 M
Ratio: 1.0 × 10−4 ÷ 1.1 × 10−21 ≈ 9 × 1016 — the sulphide concentration rises by roughly seventeen orders of magnitude simply by changing the acidity.
What that buys: with 0.010 M metal ion, Q = 0.010 × 1.1 × 10−21 = 1.1 × 10−23 in acid. CuS, whose Ksp is quoted around 10−36, is far below that and comes down at once. ZnS, whose quoted Ksp scatters between about 10−21 and 10−24 depending on the source and on which crystalline form is meant, sits close to the line and does not precipitate reliably in acid. Move to pH 9 and Q = 0.010 × 1.0 × 10−4 = 1.0 × 10−6, which is enormously above any quoted ZnS value, so zinc precipitates without question. That is group II and group IV, separated by nothing but pH.
Anion (acid radical) tests worth knowing by equation
These four turn up as "write the reaction" questions rather than as lab procedure.
[Fe(H2O)6]2+ + NO → [Fe(H2O)5(NO)]2+ + H2O
Chromyl chloride (Cl−), red vapours:
4NaCl + K2Cr2O7 + 6H2SO4 → 2CrO2Cl2 + 2KHSO4 + 4NaHSO4 + 3H2O
Nessler's reagent (NH4+): K2[HgI4] in KOH gives a brown precipitate
Carbonate: CO32− + 2H+ → H2O + CO2, and CO2 + Ca(OH)2 → CaCO3↓ + H2O (limewater turns milky)
The chromyl chloride equation is the one most often written unbalanced. Count sodium, potassium, chlorine, chromium, sulphur, hydrogen and oxygen separately: 4 Na, 2 K, 4 Cl, 2 Cr, 6 S, 12 H and 31 O on each side.
Confirmatory tests for the common cations
| Cation | Reagent | Observation |
|---|---|---|
| Pb2+ | KI, or K2CrO4 | Yellow PbI2 (golden spangles on cooling); yellow PbCrO4 |
| Ag+ | excess NH3 | AgCl dissolves as [Ag(NH3)2]+, reappears on acidifying |
| Cu2+ | excess NH3; or K4[Fe(CN)6] | Deep blue [Cu(NH3)4]2+; chocolate-brown Cu2[Fe(CN)6] |
| Fe3+ | K4[Fe(CN)6]; or KSCN | Prussian blue; blood-red [Fe(SCN)]2+ |
| Al3+ | NaOH then blue litmus solution | Hydroxide dissolves in excess NaOH (amphoteric); blue lake |
| Cr3+ | NaOH + H2O2 | Yellow chromate, then orange dichromate on acidifying |
| Zn2+ | NaOH | White hydroxide dissolving in excess as zincate (amphoteric) |
| Mn2+ | NaOH in air | White hydroxide darkening to brown on oxidation |
| Ni2+ | dimethylglyoxime in ammonia | Rose-red chelate precipitate |
| Co2+ | NH4SCN in amyl alcohol | Blue [Co(SCN)4]2− in the organic layer |
| Ba2+, Sr2+, Ca2+ | flame test | Apple-green, crimson and brick-red respectively |
| Mg2+ | Na2HPO4 in ammonia | White crystalline Mg(NH4)PO4 |
Flame colours are a genuine spectroscopic observation, not a trick: the heat excites a valence electron, and the light emitted as it falls back has a wavelength set by the energy gap, which is characteristic of the element.
Interfering radicals — the standard exam question
Certain anions bind cations so tightly that the group reagent never gets a chance, or they carry a cation forward into the wrong group. The textbook set is oxalate, borate, fluoride, phosphate and tartrate. Phosphate is the classic: it precipitates the group V and VI cations as phosphates along with the group III hydroxides, so a correct scheme removes phosphate first (as ferric phosphate in the presence of excess Fe3+, in acetic acid) before proceeding. If a question tells you the salt contains phosphate, the expected answer names the interference and the removal step — not a colour.
Common mistakes that cost marks
- Explaining group order by "solubility" rather than by Ksp and Q. The reagent concentration is what is being manipulated; say so explicitly.
- Adding NH4OH before NH4Cl. The order is the whole point, and worked example 1 is the reason.
- Saying H2S in acid "does not ionise". It does; its ionisation is simply suppressed, and the suppression is quantitative — a factor of about 1017 in [S2−].
- Confusing PbCl2 with AgCl. Both are white, but PbCl2 dissolves in hot water and AgCl dissolves in ammonia. Lead therefore appears in both group I and group II, which is expected, not an error.
- Writing chromyl chloride from memory without balancing. Check every element count.
- Quoting a Ksp as if it were exact. Published sulphide values scatter by orders of magnitude; state the source value you used and reason from the ratio.
- Forgetting that the brown ring must be done with cold, concentrated H2SO4 layered underneath. Mixing destroys the ring.
How to prepare this unit
| Theme | What you must be able to do without hesitation |
|---|---|
| Q versus Ksp | Decide precipitation for any cation at a stated ion concentration |
| Common-ion effect | Compute [OH−] with and without a buffer and compare the two |
| Sulphide equilibrium | Use [S2−] = Ka1Ka2[H2S]/[H+]2 at any pH |
| Group scheme | Name reagent, cations, precipitate and colour for all six groups |
| Amphoterism | Explain Al, Zn, Sn and Cr hydroxides dissolving in excess alkali |
| Confirmatory reactions | Write balanced equations, not just colours |
| Interfering radicals | Name them and state the removal step for phosphate |
Treat that as a revision checklist, not as a prediction of the paper. For the syllabus and the current pattern, read the official IIT-JAM notification for your year.
Practise the precipitation decision itself. Every step of the group scheme is a Ksp comparison, and the fastest way to build a feel for it is to run the numbers on real salts — solubility to Ksp and back, and the effect of a common ion. The solubility product calculator does exactly that, so you can check the working in examples 1 and 2 and then try your own.
Open the Solubility Product (Ksp) Calculator →Preparing for IIT-JAM, GATE, CSIR-NET or CUET-PG? ABC Chemistry runs dedicated competitive-exam batches — classroom at the Gurugram coaching centre and live online classes for students anywhere in India. Details at abcchemistry.in.