Class 11 Chemistry · NCERT chapter 7 · 8 topics · free to read
Chemical Equilibrium
A reversible reaction reaches dynamic equilibrium when the rate of forward reaction equals the rate of backward reaction. Concentrations become constant (not equal) and all macroscopic properties stop changing, even though both reactions continue at the molecular level.
r_f = r_b (at equilibrium)
Reversible Reactions
A reversible reaction proceeds in both forward and backward directions simultaneously. Under given conditions, it never goes to completion — instead it reaches a state of balance.
Most chemical reactions are reversible — products can react to re-form reactants. We write them with a double arrow ( leftharpoons ). Example: N_2(g) + 3H_2(g) leftharpoons 2NH_3(g) . The forward reaction forms ammonia; the backward reaction decomposes it.
Irreversible reactions go to completion (e.g., combustion of wood, neutralization of strong acid + strong base in dilute solution)
Reversible reactions never go to completion — both reactants and products are always present
The double arrow leftharpoons indicates reversibility; a single arrow arrow indicates irreversibility
Reversibility depends on conditions — a reaction irreversible in one condition may be reversible in another
Dynamic Equilibrium
At dynamic equilibrium, the forward and backward reactions occur at equal rates. Concentrations remain constant but molecules are continuously interconverting.
When a reversible reaction starts, the forward rate is high (lots of reactants) and the backward rate is zero (no products yet). As products accumulate, the backward rate increases. Eventually, forward rate = backward rate. This is dynamic equilibrium.
At equilibrium: r_ forward = r_ backward
Equilibrium is dynamic — reactions don't stop, both continue at equal rates
Equilibrium is not static — molecules are continuously being formed and consumed
Concentrations become constant (not equal!) at equilibrium
Equilibrium can be attained from either direction — starting with reactants or products
Equilibrium can only be achieved in a closed system
Characteristics of Equilibrium
Chemical equilibrium has definite characteristics: closed system, constant macroscopic properties, dynamic nature, approachable from either side, and dependence on conditions.
Closed system required — no exchange of matter with surroundings (energy exchange is OK)
Constant macroscopic properties — concentration, pressure, color, density all remain constant
Dynamic nature — forward and backward rates are equal and non-zero
Attainable from either direction — same equilibrium state whether you start with reactants or products
Catalyst does NOT change equilibrium position — it only helps reach equilibrium faster
Involves phase change
Involves chemical reaction
H₂O(l) ⇌ H₂O(g) at 100°C
N₂ + 3H₂ ⇌ 2NH₃
CO₂(g) ⇌ CO₂(aq) in soda
CH₃COOH ⇌ CH₃COO⁻ + H⁺
Sugar(s) ⇌ Sugar(aq)
CaCO₃(s) ⇌ CaO(s) + CO₂(g)
Same substance, different phases
Different substances formed
Equilibrium Constant
The equilibrium constant K quantifies the position of equilibrium. K_c uses molar concentrations, K_p uses partial pressures. They are related by K_p = K_c(RT)^(Delta n). The reaction quotient Q predicts the direction a reaction will shift to reach equilibrium.
K_p = K_c(RT)^ n
Law of Chemical Equilibrium
For a balanced reaction at equilibrium, the ratio of product concentrations to reactant concentrations (each raised to their stoichiometric coefficients) is constant at a given temperature.
For a general reaction aA + bB leftharpoons cC + dD , the equilibrium constant expression is:
K_c = [C]^c [D]^d [A]^a [B]^b
This is the Law of Chemical Equilibrium (also called the Law of Mass Action applied to equilibrium). K_c depends only on temperature — not on initial concentrations, pressure, or catalysts.
Products in the numerator, reactants in the denominator
Each concentration raised to the power of its stoichiometric coefficient
K_c uses molar concentrations (mol/L)
Pure solids and pure liquids are excluded from the expression (their activity = 1)
K depends ONLY on temperature — not on concentration, pressure, volume, or catalyst
K_p Expression
For gaseous equilibria, K_p uses partial pressures instead of concentrations. K_p and K_c are related through the ideal gas equation.
For gaseous reactions, it's often more convenient to use partial pressures instead of concentrations. For aA(g) + bB(g) leftharpoons cC(g) + dD(g) :
K_p = (p_C)^c (p_D)^d (p_A)^a (p_B)^b
Since p = cRT (from ideal gas law, where c = molar concentration), we can relate K_p and K_c :
K_p = K_c(RT)^ n_g
where n_g = (c + d) - (a + b) = moles of gaseous products - moles of gaseous reactants
R = 0.0821 L atm mol ^ -1 K ^ -1 (when pressure is in atm) or R = 8.314 J mol ^ -1 K ^ -1 (SI)
If n_g = 0 → K_p = K_c (e.g., H _2 + I _2 leftharpoons 2HI, n_g = 2-2 = 0 )
If n_g > 0 → K_p > K_c
If n_g < 0 → K_p < K_c
T must be in Kelvin — a common source of errors
Reaction Quotient Q
Q has the same expression as K but uses current (non-equilibrium) concentrations. Comparing Q with K tells you which direction the reaction will shift.
The reaction quotient Q has the exact same mathematical expression as K , but uses instantaneous concentrations (not equilibrium ones). It answers the question: 'Where is the reaction right now compared to equilibrium?'
Q_c = [C]^c [D]^d [A]^a [B]^b (at any instant)
Q < K → Too many reactants, too few products → reaction shifts forward (toward products)
Q > K → Too many products, too few reactants → reaction shifts backward (toward reactants)
Q = K → System is at equilibrium → no net shift
Manipulating K
When you reverse, multiply, or add reactions, the equilibrium constant changes in predictable ways. These rules are essential for multi-step equilibrium problems.
The value of K depends on exactly how the equation is written. Three key rules govern how K transforms:
Reverse the reaction → K' = 1 K
Multiply coefficients by n → K' = K^n
Divide coefficients by n → K' = K^ 1/n
Add two reactions → K_ net = K_1 K_2
Subtract a reaction → K_ net = K_1 K_2
Products dominate at equilibrium
Reactants dominate at equilibrium
Reaction is 'product-favored'
Reaction is 'reactant-favored'
Forward reaction nearly complete
Forward reaction barely proceeds
Example: 2H₂ + O₂ ⇌ 2H₂O, K ≈ 10⁸⁰
Example: N₂ + O₂ ⇌ 2NO, K ≈ 10⁻³⁰ at 298K
Units of K
The units of K depend on Delta n. When Delta n = 0, K is dimensionless. NCERT treats K as having units, but thermodynamic K (using activities) is always dimensionless.
The units of K_c and K_p depend on n :
Units of K_c = (mol/L)^ n Units of K_p = (atm)^ n_g
If n = 0 : K is unitless (e.g., H _2 + I _2 leftharpoons 2HI)
If n > 0 : K_c has units of (mol/L) ^ n
If n < 0 : K_c has units of (mol/L) ^ n = (L/mol) ^ | n|
Thermodynamic K (using activities) is always dimensionless — but NCERT problems use K_c and K_p with units
Le Chatelier's Principle
If a system at equilibrium is disturbed (by changing concentration, pressure, or temperature), it shifts in the direction that partially counteracts the disturbance. Catalyst and inert gas (at constant volume) do NOT shift equilibrium. The Haber process is the classic industrial application.
If stress applied equilibrium shifts to reduce the stress
Le Chatelier's Principle
A system at equilibrium responds to an external stress by shifting in the direction that partially undoes the stress. It never completely eliminates the stress — only partially counteracts it.
Le Chatelier's Principle (1884): If a change in concentration, pressure, or temperature is imposed on a system at equilibrium, the equilibrium shifts in the direction that tends to undo the effect of the change.
The shift is always partial — the system doesn't fully reverse the change
The principle predicts the direction of shift, not the magnitude
It applies to both chemical equilibria and physical equilibria
Three main stresses: change in concentration, pressure/volume, or temperature
A catalyst is NOT a stress — it does not shift equilibrium
Le Chatelier's Principle is the single most tested equilibrium topic in NEET. Expect 1-2 questions every year.
Effect of Concentration
Adding a reactant or removing a product shifts equilibrium forward. Adding a product or removing a reactant shifts it backward. The value of K remains unchanged.
For A + B leftharpoons C + D :
Add reactant (A or B) → Q < K → shifts forward → more products formed
Remove product (C or D) → Q < K → shifts forward → more products formed
Add product (C or D) → Q > K → shifts backward → more reactants formed
Remove reactant (A or B) → Q > K → shifts backward → more products consumed
K does NOT change — only the position of equilibrium changes
Effect of Pressure & Volume
Increasing pressure (decreasing volume) shifts equilibrium toward the side with fewer moles of gas. If Delta n_g = 0, pressure change has no effect.
Pressure changes affect gaseous equilibria only. The key factor is n_g (difference in moles of gaseous products and reactants).
Increase pressure (or decrease volume) → shifts toward fewer moles of gas
Decrease pressure (or increase volume) → shifts toward more moles of gas
If n_g = 0 (same moles on both sides) → no effect of pressure change
This applies only to changes in total pressure by compression/expansion — NOT by adding inert gas at constant volume
Effect of Temperature
Temperature is the only factor that changes the value of K. Increasing temperature favors the endothermic direction; decreasing temperature favors the exothermic direction.
Temperature is special — it's the only stress that actually changes the value of K . Treat heat as a reactant (endothermic) or product (exothermic) and apply Le Chatelier's.
Exothermic reaction ( H < 0 ): heat is a 'product'. Increasing T → shifts backward → K decreases
Endothermic reaction ( H > 0 ): heat is a 'reactant'. Increasing T → shifts forward → K increases
Decreasing temperature always favors the exothermic direction
This is the ONLY factor that changes the numerical value of K
Effect of Catalyst
A catalyst increases the rates of both forward and backward reactions equally. It helps reach equilibrium faster but does not change the equilibrium position or K.
A catalyst provides an alternative reaction pathway with lower activation energy. It speeds up BOTH the forward and backward reactions by the same factor.
Catalyst does NOT change K
Catalyst does NOT shift the equilibrium position
Catalyst does NOT change G or H
Catalyst only reduces the time to reach equilibrium
Catalyst lowers activation energy for both forward AND backward reactions equally
Haber Process
The industrial synthesis of ammonia is the textbook application of Le Chatelier's Principle. Every condition is optimized to maximize NH₃ yield while maintaining practical reaction rates.
N_2(g) + 3H_2(g) leftharpoons 2NH_3(g) H = -92 kJ/mol
High pressure (200 atm): n_g = 2-4 = -2 , so high P favors product side (fewer gas moles). Yield increases
Moderate temperature (~700 K): Reaction is exothermic, so low T increases K . But too low = too slow. 700 K is a compromise
Iron catalyst (Fe + Mo promoter): Speeds up the reaction at 700 K. Doesn't change K but makes the compromise temperature workable
Remove NH₃ continuously: Removing product shifts equilibrium forward — more NH _3 produced
The Haber process is NCERT's favorite example. If NEET asks 'what conditions favor NH₃ production?' — answer: high pressure, moderate temperature, catalyst, continuous removal of NH₃.
Ionic Equilibrium & Acids-Bases
Ionic equilibrium deals with equilibria involving ions in aqueous solutions. Three definitions of acids and bases — Arrhenius, Bronsted-Lowry, Lewis — progressively broaden the concept. Strong electrolytes dissociate completely; weak electrolytes establish equilibrium characterized by K_a or K_b.
K_a = [H^+][A^-] [HA]
Arrhenius Theory
The simplest acid-base definition: acids produce H⁺ ions and bases produce OH⁻ ions in aqueous solution. Limited because it only works in water.
Arrhenius (1887): An acid is a substance that produces H^+ (or H_3O^+ ) in aqueous solution. A base is a substance that produces OH^- in aqueous solution.
HCl → H ^+ + Cl ^- (Arrhenius acid)
NaOH → Na ^+ + OH ^- (Arrhenius base)
Limitation: Only works in aqueous solutions. Cannot explain why NH _3 is basic (no OH ^- in its formula), or why HCl + NH _3 react in the gas phase
Cannot explain basicity of Na _2 CO _3 , NaHCO _3 (no OH ^- in formula)
H ^+ doesn't exist freely in water — it's hydrated as H_3O^+ (hydronium ion)
Bronsted-Lowry Theory
A broader definition: acids donate protons (H⁺) and bases accept protons. This introduces conjugate acid-base pairs and works in any solvent, not just water.
Bronsted-Lowry (1923): An acid is a proton ( H^+ ) donor. A base is a proton acceptor. Every acid-base reaction is a proton transfer.
acid_1 HA + base_2 B leftharpoons acid_2 BH^+ + base_1 A^-
Every acid has a conjugate base (acid minus one proton): HA → A ^-
Every base has a conjugate acid (base plus one proton): B → BH ^+
Conjugate pair = species that differ by one proton. E.g., HCl/Cl ^- , NH _3 /NH _4^+ , H _2 O/OH ^-
Water is amphoteric — acts as acid (donates H ^+ to NH _3 ) or base (accepts H ^+ from HCl)
The broadest definition: a Lewis acid accepts an electron pair, a Lewis base donates an electron pair. This extends acid-base chemistry beyond proton transfer to include BF₃, AlCl₃, metal ions, etc.
Lewis (1923): A Lewis acid is an electron pair acceptor. A Lewis base is an electron pair donor. The acid-base reaction forms a coordinate (dative) bond.
Lewis acids: Species with empty orbitals or electron-deficient centers — BF _3 , AlCl _3 , FeCl _3 , H ^+ , metal cations (Cu ^ 2+ , Fe ^ 3+ )
Lewis bases: Species with lone pairs — NH _3 , H _2 O, OH ^- , Cl ^- , ROH, amines
Every Bronsted acid is a Lewis acid, but NOT vice versa (BF _3 is Lewis acid but doesn't donate H ^+ )
Every Bronsted base is a Lewis base (they all have lone pairs to accept H ^+ )
Lewis theory is the most general — it encompasses both Arrhenius and Bronsted-Lowry
Arrhenius
H⁺ producer / OH⁻ producer
Bronsted-Lowry
Proton donor / Proton acceptor
Lewis
Electron pair acceptor / Electron pair donor
Scope
Narrowest → Broadest (Arrhenius ⊂ B-L ⊂ Lewis)
Strong vs Weak Acids/Bases
Strong acids/bases dissociate completely in water (α ≈ 1). Weak acids/bases reach an ionization equilibrium (α << 1) characterized by K_a or K_b. Ostwald's dilution law connects K, α, and concentration.
Strong acids (HCl, HBr, HI, HNO _3 , H _2 SO _4 , HClO _4 ) and strong bases (NaOH, KOH, Ca(OH) _2 , Ba(OH) _2 ) dissociate completely in dilute aqueous solution. Weak acids and bases establish an ionization equilibrium.
For a conjugate pair: K_a K_b = K_w = 10^ -14 at 25°C
pH Scale
The pH scale is a logarithmic measure of H⁺ concentration: pH = -log[H⁺]. Water auto-ionizes with K_w = [H⁺][OH⁻] = 10⁻¹⁴ at 25°C. pH + pOH = 14. For weak acids/bases, pH calculations require K_a/K_b and Ostwald's dilution law.
pH = - [H^+]
Auto-ionization of Water
Water molecules spontaneously transfer protons to each other, establishing an equilibrium that defines K_w, the ionic product of water. At 25°C, K_w = 10⁻¹⁴.
In pure water: [H^+] = [OH^-] = K_w = 10^ -7 M. This means even 'pure' water has a tiny but measurable ion concentration.
K_w is called the ionic product of water (or auto-protolysis constant)
K_w depends on temperature: at 25°C, K_w = 10^ -14 ; at higher T , K_w increases (auto-ionization is endothermic)
In pure water at 25°C: [H^+] = [OH^-] = 10^ -7 M → pH = 7 (neutral)
At temperatures above 25°C, neutral pH < 7 (because K_w > 10^ -14 , so [H^+] > 10^ -7 )
K_w = K_a K_b for any conjugate acid-base pair
pH & pOH
pH and pOH convert unwieldy H⁺ and OH⁻ concentrations into simple numbers. The relationship pH + pOH = 14 (at 25°C) is a direct consequence of K_w = 10⁻¹⁴.
pH scale typically ranges from 0 to 14, but can go beyond (e.g., 10 M HCl has pH -1 )
Each unit change in pH = 10-fold change in [H^+] (logarithmic scale)
pH of Strong Acids & Bases
For strong acids and bases, dissociation is complete. pH is calculated directly from the concentration without needing K_a or K_b.
Strong acids and bases dissociate completely. So [H^+] equals the acid concentration (for monobasic acids), and [OH^-] equals the base concentration (for monoacidic bases).
Strong monobasic acid (HCl, HNO _3 ): [H^+] = C → pH = - C
For weak acids/bases, only a fraction ionizes. Use K_a (or K_b) and concentration to find [H⁺] (or [OH⁻]), then compute pH.
For a weak acid HA with concentration C and ionization constant K_a :
[H^+] = K_a C (when 1 , i.e., K_a C)
pH = 1 2 (pK_a - C) = 1 2 pK_a - 1 2 C
For a weak base B with concentration C and ionization constant K_b :
[OH^-] = K_b C pOH = 1 2 (pK_b - C)
pH = 14 - pOH = 14 - 1 2 (pK_b - C)
The approximation [H^+] = K_a C is valid when < 0.05 (less than 5% ionization)
If is not negligible, solve the full quadratic: K_a = x^2 C-x where x = [H^+]
pK_a = - K_a and pK_b = - K_b
Relationship: pK_a + pK_b = pK_w = 14 (at 25°C)
Lower pK_a → stronger acid. Lower pK_b → stronger base
Buffer Solutions
Buffer solutions resist changes in pH upon addition of small amounts of acid or base. Acidic buffers (weak acid + conjugate base salt) and basic buffers (weak base + conjugate acid salt) are described by the Henderson-Hasselbalch equation. Buffer capacity depends on total concentration and the ratio of components.
pH = pK_a + [Salt] [Acid]
Buffer Solutions
A buffer solution maintains nearly constant pH when small amounts of acid or base are added. It consists of a weak acid/base and its conjugate salt.
A buffer solution is a solution that resists significant pH change upon addition of small amounts of strong acid or strong base. It works by having a reservoir of both a weak acid (to neutralize added base) and its conjugate base (to neutralize added acid).
Acidic buffer: Weak acid + salt of its conjugate base (e.g., CH _3 COOH + CH _3 COONa). pH < 7
Basic buffer: Weak base + salt of its conjugate acid (e.g., NH _4 OH + NH _4 Cl). pH > 7
Buffer does NOT prevent pH change entirely — it minimizes the change
Buffer fails if the added acid/base exceeds the buffer's capacity (one component gets used up)
Henderson-Hasselbalch Equation
This equation directly gives the pH of a buffer solution from pK_a (or pK_b) and the ratio of salt to acid (or salt to base). It's the single most useful equation for buffer problems.
For an acidic buffer (weak acid HA + salt NaA):
pH = pK_a + [A^-] [HA] = pK_a + [Salt] [Acid]
For a basic buffer (weak base B + salt BHCl):
pOH = pK_b + [BH^+] [B] = pK_b + [Salt] [Base]
When [Salt] = [Acid]: (1) = 0 → pH = p K_a (buffer pH equals p K_a of the acid)
When [Salt] > [Acid]: > 0 → pH > p K_a
When [Salt] < [Acid]: < 0 → pH < p K_a
Buffer works best when [Salt]/[Acid] is between 0.1 and 10 (pH within 1 of p K_a )
To prepare buffer at a target pH, choose an acid with p K_a close to the target pH
Buffer Capacity
Buffer capacity is the amount of acid or base a buffer can neutralize before its pH changes significantly. It depends on total concentration and the ratio of components.
Buffer capacity ( ) measures the effectiveness of a buffer — how many moles of strong acid or base can be added per liter before pH changes by one unit.
Buffer capacity is maximum when [Acid] = [Salt] (i.e., pH = p K_a )
Higher total concentration = higher buffer capacity (1 M buffer resists more than 0.01 M buffer)
Buffer capacity decreases as the ratio [Salt]/[Acid] deviates from 1
Effective buffer range: p K_a 1 (pH range where buffer works well)
Buffer is overwhelmed when all of one component is consumed
Solubility Equilibrium
Sparingly soluble salts establish a solubility equilibrium characterized by K_sp (solubility product). Molar solubility can be calculated from K_sp and vice versa. The common ion effect reduces solubility. Precipitation occurs when Q (ionic product) exceeds K_sp.
K_ sp = [A^+]^m[B^-]^n for A_mB_n
K_ sp Expression
K_sp is the equilibrium constant for the dissolution of a sparingly soluble salt. It represents the maximum product of ion concentrations that can exist in solution.
For a sparingly soluble salt A_mB_n dissolving in water:
A_mB_n(s) leftharpoons mA^ n+ (aq) + nB^ m- (aq)
K_ sp = [A^ n+ ]^m [B^ m- ]^n
The solid doesn't appear in the expression (activity = 1). K_ sp depends only on temperature.
Ca _3 (PO _4 ) _2 (s) leftharpoons 3Ca ^ 2+ + 2PO _4^ 3- : K_ sp = [Ca^ 2+ ]^3[PO_4^ 3- ]^2
Larger K_ sp → more soluble (for salts with the same ion ratio)
K_ sp is valid ONLY for sparingly soluble salts (not for NaCl, KNO _3 etc.)
Molar Solubility
Molar solubility (s) is the number of moles of salt that dissolve per liter to form a saturated solution. It's calculated from K_sp using stoichiometry.
If the molar solubility of A_mB_n is s mol/L, then [A^ n+ ] = ms and [B^ m- ] = ns .
K_ sp = (ms)^m (ns)^n = m^m n^n s^ (m+n)
AB type (AgCl, BaSO _4 ): K_ sp = s^2 → s = K_ sp
AB _2 type (PbCl _2 , CaF _2 ): K_ sp = 4s^3 → s = ( K_ sp 4 )^ 1/3
A _2 B type (Ag _2 CrO _4 ): K_ sp = 4s^3 → s = ( K_ sp 4 )^ 1/3
A _2 B _3 type (Bi _2 S _3 ): K_ sp = 108s^5 → s = ( K_ sp 108 )^ 1/5
Solubility in g/L = s M (where M = molar mass)
Common Ion Effect
Adding a common ion to a solution of a sparingly soluble salt decreases its solubility. This is a direct application of Le Chatelier's Principle to solubility equilibrium.
The common ion effect: Adding an ion that is already present in the equilibrium shifts the dissolution equilibrium backward, decreasing the solubility of the salt.
Common ion effect decreases solubility of the sparingly soluble salt
K_ sp remains unchanged — only the solubility ( s ) changes
In the presence of a common ion at concentration C : set up the K_ sp expression with the extra ion concentration included
For AgCl in 0.1 M NaCl: K_ sp = [Ag^+](0.1 + s) [Ag^+] 0.1 (since s 0.1 )
Precipitation Condition
Compare the ionic product Q with K_sp: if Q > K_sp, precipitation occurs. If Q < K_sp, more salt can dissolve. If Q = K_sp, the solution is exactly saturated.
The ionic product (IP or Q ) has the same form as K_ sp but uses actual (non-equilibrium) ion concentrations. Comparing Q with K_ sp tells you whether precipitation will occur.
Q < K_ sp : Solution is unsaturated → no precipitate, more salt can dissolve
Q = K_ sp : Solution is saturated → at equilibrium, no net change
Q > K_ sp : Solution is supersaturated → precipitate forms until Q = K_ sp
Hydrolysis of Salts
When salts dissolve in water, the ions from the weak component undergo hydrolysis (react with water), making the solution acidic or basic. Salt of strong acid + weak base → acidic. Salt of weak acid + strong base → basic. Salt of weak acid + weak base → depends on K_a vs K_b.
pH = 7 + 1 2 pK_a - 1 2 pK_b (WA + WB salt)
Salt Hydrolysis
Hydrolysis is the reverse of neutralization. The ion from the weak component reacts with water, shifting the [H⁺]/[OH⁻] balance and making the solution acidic or basic.
Hydrolysis = the reaction of a salt's ions with water. Only the ion from the weak component undergoes hydrolysis. The ion from the strong component is a spectator.
Strong acid + Strong base salt (NaCl, KNO _3 ): No hydrolysis → pH = 7 (neutral)
Strong acid + Weak base salt (NH _4 Cl, FeCl _3 ): Cation hydrolyzes → pH < 7 (acidic)
Weak acid + Strong base salt (CH _3 COONa, Na _2 CO _3 ): Anion hydrolyzes → pH > 7 (basic)
Weak acid + Weak base salt (CH _3 COONH _4 ): Both ions hydrolyze → pH depends on relative K_a and K_b
Hydrolysis is really just Le Chatelier applied to the auto-ionization of water. Adding CH _3 COO ^- removes H ^+ (by forming CH _3 COOH) → water ionizes more → [OH ^- ] increases → solution becomes basic.
Strong Acid + Weak Base Salt
In salts like NH₄Cl, the cation (NH₄⁺) is the conjugate acid of a weak base. It donates H⁺ to water, making the solution acidic.