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Vişne Chem

Applications

Water & Wastewater Treatment

Dose calculation and commissioning for pH correction, softening, heavy-metal precipitation and sludge conditioning.


Overview

Lime does not perform a single duty in water and wastewater treatment. The same hydroxide entering the reactor first binds the free carbon dioxide, then lifts the pH, then converts carbonate hardness and heavy metals into a solid phase, and finally decides how that solid settles and dewaters. These four effects occur in sequence, each consuming part of what the next one needs; tuning one alone inevitably shifts the others. A hydrated lime dose is therefore built not around the question “what pH did we reach” but around “how many moles of the hydroxide went into which reaction”.

The mistake we meet most often on site is a dose tied only to the number on the pH meter. The pH holds and the discharge analysis even meets the metal limit — but sludge volume comes out at twice the design figure, the filter press cycle stretches and cake haulage overruns the budget. The reverse is just as common: pushing pH above 11 “to be safe” redissolves zinc and lead as zincate and plumbate, and the metal in the effluent rises instead of falling. In both cases the fault is not in the dosing pump but in what the dose was tied to.

That is why everything set out here is organised around the process: which water property creates which lime demand, what gets measured, and which decision that measurement feeds. Part of it — acidity neutralisation and the high-density sludge (HDS) loop in particular — applies unchanged to drainage treatment on mining and ore beneficiation sites. What changes there is not the chemistry but the magnitude, acidity and hour-to-hour volatility of the incoming load.

What sets the dose is not pH but the list of demands

How much lime is consumed is decided by the buffer capacity of the water, not by pH. Free CO₂, mineral acidity, bicarbonate and the metals to be precipitated are separate hydroxide-consuming items inside the same reactor: 1 mg/L of free CO₂ takes about 1.7 mg/L of Ca(OH)₂, and neutralising 1 kg of sulphuric acid requires 0.76 kg of Ca(OH)₂ stoichiometrically. A pH meter cannot tell these items apart; it simply shows a number that climbs steeply once all of them have been satisfied. A dose calculated without a titration curve has been calculated without ever seeing the largest part of the demand.

Influent composition is not constant. Rainfall and snowmelt dilute alkalinity in a surface source while raising turbidity and natural organic matter; spring algal growth can swing pH by a full unit over a day. In an industrial plant, shift changes, batch dumps and CIP cycles move the load within minutes — on pulp and paper lines a single wash-water discharge can double the incoming acidity. Without an equalisation basin, dose control chases that swing and is always late; 8–24 hours of equalisation usually returns more than the chemical it saves.

In heavy-metal precipitation there is no single “correct pH”. Each metal hydroxide reaches minimum solubility at a different pH: ferric iron in a band as low as 4.0–5.0, ferrous iron at 8.0–8.5, copper at 8.5–9.5, zinc at 9.0–9.5, nickel at 10.0–11.0, cadmium at 10.5–11.5. Zinc, lead, chromium and aluminium are also amphoteric and redissolve 1–1.5 units above their own optimum. In a mixed effluent, single-stage precipitation cannot bring every metal to its best point at once; either a deliberate compromise band is chosen or staged precipitation is adopted. Where complexing agents such as cyanide, EDTA, citrate or ammonia are present, hydroxide precipitation alone is insufficient at any pH.

The fourth difficulty is not chemical but a materials-handling problem. Milk of lime is not a true solution but a settling suspension: in a line that has been stopped, solids separate within minutes and the line blocks on restart. The same suspension forms a CaCO₃ crust wherever it meets air; a slurry tank left open loses active content within a day and leaves hardened scale on the wall. Slurry slaked from quicklime carries 2–10% grit depending on feed quality, and if that abrasive fraction is not separated it wears pump rotors and valve seats out in weeks rather than months. The same scaling occurs on the glass surface of the pH electrode, and the control loop quietly starts working to a pH that does not exist.

Where lime comes in, and in what form

Hydrated lime is the backbone of chemical treatment because it supplies two things at once: hydroxide and calcium. The hydroxide carries the pH; the calcium precipitates as CaCO₃ with carbonate, hydroxyapatite with phosphate, CaF₂ with fluoride and gypsum with sulphate, and these dense crystals grow inside the metal hydroxide floc and give it mass. Sludge precipitated with caustic stays light and gelatinous and stalls at 60–80% volume in a 30-minute settling test; lime sludge falls to 10–20% over the same period and yields roughly twice the cake solids on dewatering. The real advantage of lime over caustic is not its price per tonne but the physics of the solid it produces.

The choice between quicklime and hydrated lime is decided by scale of consumption. The equivalence is unambiguous: 1 kg of CaO corresponds to 1.32 kg of Ca(OH)₂, so a quarter less product by mass delivers the same alkalinity. Above roughly 2–3 tonnes a day, on-site slaking usually repays the slaker and grit classifier within two years. Below that, ready hydrate is the better answer rather than quicklime; a slaker depends on operating discipline, and run badly it produces slurry worse than the hydrate you would have bought. The numbers to read before deciding are available CaO, t₆₀ reactivity to EN 459-2 and grit content; drinking water duties add the impurity limits of EN 12518.

In softening, the lime–soda process runs two separate calculations. Carbonate hardness takes one mole of Ca(OH)₂ per mole of calcium bicarbonate and precipitates as CaCO₃ around pH 10.3. Magnesium consumes two moles and precipitates as Mg(OH)₂ only in the pH 10.8–11.3 band, which is why an excess of 35–70 mg/L as CaO is applied when magnesium is targeted. Non-carbonate hardness does not precipitate with lime at all and needs soda ash — adding more lime here only raises pH and sludge. Typical residual hardness is 35–50 mg/L as CaCO₃; because the water leaves supersaturated, it is recarbonated with CO₂ down to pH 8.3–8.7 and settled into a saturation index between zero and +0.3.

The same lime–CO₂ pair drives the carbonatation station in sugar plants, where the aim is not hardness but collecting colloids onto growing CaCO₃ crystals — the mechanism is identical. Where the need runs the other way, that is where a soft and aggressive source water has to be hardened, a contactor packed with natural calcium carbonate replaces lime: the water dissolves the carbonate with its own aggressive carbon dioxide, calcium and alkalinity rise together, and the risk of overdosing disappears physically. The lime–CO₂ route is faster and more compact; the contactor is closed to operator error. The choice follows the operating capability of the plant.

In metal precipitation, lime is designed together with the pretreatment. Hexavalent chromium must first be reduced to the trivalent state with bisulphite at pH 2–3 and only then precipitated with lime; raising pH directly leaves chromate in solution. Baths containing complexing agents — cyanide plating, EDTA cleaning — must be segregated and treated on their own line in surface treatment and rolling mill effluents. Fluoride precipitates as CaF₂ with lime but its solubility floor keeps the residual at 8–15 mg/L; a second stage with an aluminium salt is needed for tighter targets. Sulphate has the same kind of limit: gypsum equilibrium stalls around 1500–2000 mg/L, and going lower requires ettringite precipitation at pH 11.5–12.

Operating ranges

  • Target pH — heavy metal precipitation

    8.5–11.0

    Per metal; 9.5–10.0 ceiling for amphoteric metals

  • Target pH — lime–soda softening

    10.3 / 10.8–11.3

    CaCO₃ / Mg(OH)₂ precipitation

  • Excess lime — magnesium removal

    35–70 mg/L

    As CaO, above stoichiometry

  • Typical dose — drinking water conditioning

    5–60 mg/L

    As Ca(OH)₂, with recarbonation

  • Typical dose — municipal wastewater

    50–300 mg/L

    As Ca(OH)₂

  • Typical dose — industrial / acid drainage

    200–3000 mg/L

    Set by acidity and metal load

  • Neutralisation equivalent

    0.76 kg Ca(OH)₂ / kg H₂SO₄

    0.84 kg of product at 90% available

  • CaO → Ca(OH)₂ conversion factor

    1.32

    1 kg CaO = 1.32 kg Ca(OH)₂ equivalent

  • Milk of lime concentration

    5–20% w/w

    Density 1.03–1.12 g/cm³; 4–6 : 1 water/lime in the slaker

  • Slurry temperature at end of slaking

    82–93 °C

    Soft-burnt CaO; t₆₀ ≤ 3 min, EN 459-2

  • Mixing — rapid / slow

    G 300–1000 s⁻¹, 1–3 min / G 20–80 s⁻¹, 15–30 min

    Gt 30,000–100,000

  • Milk of lime line velocity

    1.2–2.5 m/s

    Lower limit settling, upper limit erosion

Application steps

  1. 01

    Characterising the influent and the load

    The measurement list is fixed: alkalinity (EN ISO 9963), total and calcium hardness (ISO 6059), free CO₂, mineral acidity, suspended solids (EN 872), metal profile (EN ISO 11885) and temperature. A single grab sample represents none of them. A flow-proportional composite is taken over at least one full shift; on a surface source, wet and dry seasons are sampled separately. What sizes the plant is not the average but the peak-to-average ratio.

    Streams are separated at source. If an acid pickling bath, a cyanide plating bath, a wet scrubber blowdown and general process water all merge in one pit, none of them can be treated at its own optimum pH. Blowdown from a flue gas treatment line, for instance, carries high chloride and sulphate; kept separate, its gypsum precipitation can be run under control, while blended it produces unexpected scaling right along the plant.

    The output of characterisation is not a single table but a load profile: hourly flow, hourly acidity, hourly metal load. Equalisation volume is calculated from that profile. In practice 8–24 hours of equalisation halves the swing that dose control has to follow and gives a measurable drop in reagent consumption.

  2. 02

    Deciding which limit governs the dose

    A treatment line usually carries several targets: discharge limits, receiving-water conditions, the pH tolerance of the biological stage, residual hardness and, for drinking water, the saturation index. Only one of them is binding, and that one governs the dose. If the binding target is a metal, the working pH follows the metal profile; if it is hardness, it follows the 10.3 or 10.8–11.3 band; if it is neutralisation alone, it follows 6.5–9.0.

    Where that distinction is not made, the usual outcome is running at needlessly high pH. In a stream feeding a biological stage, going above pH 9 suppresses the nitrifiers and raises ammonium at the outlet, which then forces you to bring the lime-raised pH back down with acid. Choosing the right band from the start, instead of spending two chemicals in series, is the fastest saving available on most plants.

  3. 03

    Titration curve and jar test

    The titration curve comes first: lime slurry of known concentration is added in steps while pH is recorded. Flat plateaus on the curve identify the buffering items; the steep section shows the band where control will be difficult. In an effluent containing strong acid, the transition between pH 4 and 10 is almost vertical, and this curve shows on the design desk why a single-stage neutralisation basin will oscillate.

    The jar test is run within the frame of ASTM D2035: six 1 L beakers, 1 minute of rapid mixing at 120 rpm, 15 minutes of slow mixing at 30 rpm, 30 minutes of settling. Each beaker is measured for pH, turbidity, 30-minute settled sludge volume and metal concentration. One detail is critical: metals must be measured both on a 0.45 µm filtered sample and on an unfiltered one. Discharge limits are written on total metal; when the filtered result looks perfect but the unfiltered one exceeds the limit, the problem is not chemistry but fine floc carryover, and the answer is a coagulant aid or filtration.

    Sample age corrupts the result. A stored sample absorbs CO₂ from the air, ferrous iron oxidises and the true lime demand is measured wrongly; the test must be run within 24 hours. Moving from bench to plant, a scale-up factor of 1.1–1.3 is applied, because mixing uniformity and contact time in the real reactor sit below jar conditions.

  4. 04

    Product selection and incoming quality control

    There is an order in which a certificate is read: available CaO or Ca(OH)₂ content, loss on ignition (the carbonation indicator), grit content, fineness and, for quicklime, reactivity. Total CaO on its own is misleading; hard-burnt lime looks clean in analysis but slakes slowly, leaves grit and contributes nothing to the reaction despite appearing in the dose calculation. Drinking water duties add the heavy metal and impurity limits of EN 12518, with the test methods defined in EN 12485.

    Incoming control is done on every consignment, not once a year. A two-point drop in available content translates directly into a pH shift on a fixed-volume dosing system and into a dose increase the operator cannot explain. Silo conditions matter as well: hydrated lime slowly carbonates with airborne moisture and CO₂, and a monthly loss of 1–3% in activity is normal in a silo whose vent air is not dried.

  5. 05

    Milk of lime preparation and grit separation

    Slaking is the step that sets the quality of everything downstream. A paste slaker is run at a water-to-lime ratio of 2.5–3.5 : 1, a slurry slaker at 4–6 : 1. The slurry is aimed at 82–93 °C at the end of the reaction: with water too cold or too plentiful the lime is “drowned” and forms coarse, low-surface particles; taken to boiling, the particles agglomerate. Either way the reactivity of the Ca(OH)₂ obtained falls and a higher dose is needed for the same pH.

    A grit classifier belongs at the slaker outlet. Varying between 2 and 10% with feed quality, this coarse abrasive fraction quickly eats pump rotors, valve seats and elbows if it is left in the line. Separated grit is also a quality signal: a sudden rise in the ratio is the first warning that the incoming lime is more hard-burnt than before.

    The prepared slurry is held in a covered, continuously agitated tank. Solids begin to separate within 10–20 minutes of the agitator stopping, and a CaCO₃ crust forms on any surface in contact with air. Storage should not exceed 24–48 hours. Concentration is most practically tracked through density: a 5% slurry runs at about 1.03 g/cm³ and a 20% slurry at about 1.12 g/cm³, so a density meter on the ring main continuously verifies the number the dose calculation rests on.

  6. 06

    The dosing line: managing blockage and scaling

    The milk of lime line is built as a ring main that leaves the tank, passes the dosing points and returns to the tank, so that it is never stagnant. Velocity is held between 1.2 and 2.5 m/s: below that solids settle, above it erosion accelerates. Dead legs, long vertical drops and sharp elbows are where blockage starts; dosing valves are taken off the ring on short branches and flushed with clean water at the end of every shift.

    Equipment selection follows the same logic. Hose (peristaltic) or progressive cavity pumps handle slurry well; diaphragm pumps with check valves block within weeks. On the valve side, pinch or knife gate valves are preferred. The injection point goes into a turbulent zone — right at the discharge of the mixer impeller — not onto a quiescent surface; otherwise a local zone above pH 12 forms, the metal hydroxides precipitated there never redissolve and a permanent crust builds at the pipe mouth.

    In this environment the pH electrode is a consumable. CaCO₃ deposited on the glass slows the measurement and drifts it low over time, and the consequence is a system that overdoses lime. A retractable electrode holder, automatic jet cleaning and weekly two-point calibration (pH 7 and pH 10 buffers) remove that drift.

  7. 07

    Reaction, flocculation and the pH control architecture

    The reaction starts in the rapid mix zone: G value 300–1000 s⁻¹ for 1–3 minutes. Flocculation follows at G 20–80 s⁻¹ for 15–30 minutes, that is a Gt product in the 30,000–100,000 band. If those two stages are not separated, either nucleation stays insufficient or the floc formed is broken up by high shear and shows as fine turbidity in the clarifier.

    Sludge recycle is the least known and most effective adjustment in this process. Returning part of the clarifier underflow to the reaction tank makes the existing CaCO₃ and metal hydroxide crystals act as seed; new solid grows on those seeds instead of nucleating as fines in solution. The result is a coarser, faster-settling and far better dewatering sludge — this is exactly the high-density sludge (HDS) loop in acid drainage treatment, which lifts sludge solids from 1–5% to 20–30%.

    The control architecture cannot be single-stage. In a stream containing strong acid, the titration curve is nearly vertical between pH 4 and 10; trying to hold that band with one valve in one basin produces continuous oscillation. The right answer is two or three stages in series, each given a 2–4 pH unit duty, with a small-capacity trim valve on the last stage. Add feed-forward computed from inlet flow and acidity and the system responds to a load spike without waiting for the measurement lag.

  8. 08

    Sludge line, seasonal adjustment and commissioning

    On the sludge side lime does two jobs. For conditioning, lime at 10–25% of dry solids together with ferric chloride lowers specific filtration resistance and allows a filter press to deliver a cake at 25–35% dry solids, where a polymer-conditioned belt press stays at 18–22%. The effect is quantified by capillary suction time (EN 14701-1) or specific resistance in a Büchner funnel — judging by the look of the cake is misleading. For stabilisation, the target is to reach pH ≥ 12 and hold it for two hours, then stay above 11.5 for 22 hours. Two costs come with it: cake mass rises, and above pH 11 ammonium converts entirely to free ammonia, so the filtrate returns to the plant inlet with a high nitrogen load. Lime-stabilised biosolids can, within the applicable limits, be used as a liming material in agriculture and soil improvement.

    Seasonal adjustment is a natural part of this process and has two physical causes. First, calcium carbonate has retrograde solubility: it dissolves more readily in cold water. Holding the same residual hardness in winter therefore requires the pH to be lifted by 0.2–0.3 of a unit. Second, viscosity: water at 1.31 mPa·s at 10 °C falls to 0.89 mPa·s at 25 °C, so the same floc settles roughly a third more slowly in cold water. That is why winter calls for a lower surface loading, lamella modules brought into service, or a longer flocculation time. Add the dilution of alkalinity in the wet season, and a fixed dose either falls short or wastes reagent and produces sludge for nothing.

    During commissioning the dose is raised in steps, and at each step pH, turbidity, sludge volume, cake solids and effluent metal are recorded together. The aim is not to find a single operating point but to see where the curve plateaus and to set alarm bands accordingly. Water characterisation, jar test protocol, lime specification and dosing architecture can be worked out for your specific plant with our technical team.

Products used in this field

Frequently asked questions

Should I use hydrated lime or quicklime?

Consumption scale sets the threshold. Below roughly 2–3 tonnes a day, ready hydrated lime is the better answer: it is dosed directly and needs no slaker, grit classifier or heat control. Above that, on-site slaking becomes sensible; since 1 kg of CaO corresponds to 1.32 kg of Ca(OH)₂ as active substance, unit cost drops markedly. But a slaker lives on operating discipline: without control of water-to-lime ratio and slurry temperature, the slurry produced comes out worse than the hydrate you would have bought.

Why does lime dosing increase sludge volume so much?

Because lime does not only raise pH, it creates solids. Every 74 g of Ca(OH)₂ that reacts with bicarbonate yields 100 g of CaCO₃ — about 1.35 kg of dry solids per kilogram of lime — and metal hydroxides add to that. This is the desired outcome, since precipitated solid is removed pollutant, but the sludge line has to be sized for that production. Raising the dose while watching pH alone is the fastest way to push sludge past its design figure.

Is a single pH enough for heavy metal removal?

Not in mixed effluent. Every metal has its own pH of minimum solubility: ferrous iron 8.0–8.5, copper 8.5–9.5, zinc 9.0–9.5, nickel 10.0–11.0, cadmium 10.5–11.5. If you must run one stage, choose a deliberate compromise band and add a polishing step for whatever remains. Where nickel and cadmium coexist with zinc, staged precipitation — first at 9.0–9.5, then a second stage at 10.5–11 after solids removal — gives a far safer result.

I raised the pH but zinc in the effluent went up. Why?

Two explanations, both common. First, amphoterism: zinc, lead, chromium and aluminium redissolve as soluble complexes such as zincate and plumbate 1–1.5 units above their own optimum. Second, fine floc carryover — the chemistry is right but the floc is escaping the clarifier. Telling them apart is easy: filter the sample at 0.45 µm and measure. If the filtered result is low and the unfiltered one high, the problem is settling or filtration; if both are high, you need to bring the pH back down.

How do we prevent blockage and scaling in milk of lime lines?

Build the line as a ring main: out of the tank, past the dosing points and back to the tank, never stagnant. Hold velocity between 1.2 and 2.5 m/s, avoid dead legs, take dosing valves off on short branches and flush at the end of the shift. Choose hose or progressive cavity pumps, and pinch or knife gate valves. The second source of scale is air: a CaCO₃ crust forms on an open tank surface, so storage must be covered and continuously agitated, and should not exceed 24–48 hours.

Do we have to retune the dose seasonally?

Yes, and there are two physical reasons. Calcium carbonate has retrograde solubility — it dissolves more readily in cold water — so holding the same residual hardness in winter needs the pH lifted by 0.2–0.3 of a unit. The second is viscosity: water at 1.31 mPa·s at 10 °C falls to 0.89 mPa·s at 25 °C, so the same floc settles about a third more slowly in the cold. Add the dilution of alkalinity in the wet season, and a fixed dose either falls short or wastes reagent and produces sludge for nothing.

When is soda ash needed in lime–soda softening?

Whenever non-carbonate hardness is present. Lime can only precipitate calcium and magnesium associated with bicarbonate; hardness tied to sulphate or chloride needs a source of carbonate ion, and that is soda ash. If total hardness in the raw water exceeds alkalinity, the difference is non-carbonate hardness, and adding more lime will not close it — it only raises pH and sludge. The right approach is to calculate the two reagents separately and confirm with the titration curve.

How should I set up a jar test so it predicts plant performance?

Stay with the ASTM D2035 protocol: 1 L beakers, 1 minute rapid mix at 120 rpm, 15 minutes slow mix at 30 rpm, 30 minutes settling. Measure more than pH and turbidity — record settled sludge volume, capillary suction time and metals both filtered and unfiltered. Keep the sample under 24 hours old, otherwise CO₂ absorption and iron oxidation change the lime demand. Apply a scale-up factor of 1.1–1.3 when moving to the plant, because real-reactor mixing sits below jar conditions.

How do I calculate the dose and account for purity?

The base formula is simple: lime feed (kg/h) = flow (m³/h) × dose (g/m³) ÷ 1000. The dose there is expressed as active substance, that is as Ca(OH)₂; divide the result by the product's available content to get the actual feed rate. With a hydrate at 92% available, 100 kg of active substance requires 109 kg of product. If you work with quicklime, first convert to Ca(OH)₂ equivalent using the factor 1.32. A two-point fall in certified available content silently underdoses the plant, which is why incoming control is done on every consignment.

What are the advantages and the price of using lime instead of caustic?

The advantage lies in the physics of the solid it produces: calcium gives the floc mass and crystalline structure, lime sludge settles to 10–20% volume in 30 minutes and yields roughly twice the cake solids of caustic sludge on dewatering. It also removes phosphate, fluoride and sulphate along the way. The price is operational: a slaking or slurry preparation unit, handling a settling suspension, scale maintenance and a larger sludge volume. On small flows with no sludge line, caustic still makes more sense; the decision needs stream characterisation and sludge disposal cost weighed together.

Sample and dose recommendation for this process

Describe your current usage and target; our technical team will come back with a suitable specification and a starting dose.