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2.2 Water Softening & Advanced Membrane Processes

Key Takeaways

  • Lime-soda ash softening removes hardness by precipitating calcium as calcium carbonate and magnesium as magnesium hydroxide.

  • Carbonate hardness is removed with lime; non-carbonate hardness requires soda ash.

  • Ion exchange uses resin to swap calcium and magnesium ions for sodium ions, requiring regeneration with NaCl.

  • Membrane flux is directly proportional to the transmembrane pressure minus the osmotic pressure difference.

  • RO membranes can remove dissolved salts, whereas MF and UF generally only remove particulate matter and macromolecules.

Last updated: July 2026

Water Softening & Advanced Membrane Processes

Water softening is the process of removing hardness-causing cations, primarily calcium (Ca2+Ca^{2+}) and magnesium (Mg2+Mg^{2+}), from water. Hard water leads to severe scaling in municipal distribution networks, industrial heat exchangers, boilers, and domestic appliances, while significantly suppressing the lathering action of soaps. Understanding the chemistry of chemical precipitation (lime-soda ash softening), ion exchange dynamics, and advanced pressure-driven membrane filtration systems is essential for environmental engineering practice and NCEES PE exam calculations.

Hardness Classification & Bar Graph Equivalence

Total Hardness (TH) is defined quantitatively as the sum of all multivalent metallic cations in solution, expressed in terms of calcium carbonate (CaCO3CaCO_3) equivalence (mg/L as CaCO3mg/L \text{ as } CaCO_3):

TH=Ca2++Mg2++other multivalent cationsTH = Ca^{2+} + Mg^{2+} + \text{other multivalent cations}

Hardness is subdivided based on the anion species present in the water:

  • Carbonate Hardness (CH): Hardness chemically associated with bicarbonate (HCO3−HCO_3^-) and carbonate (CO32−CO_3^{2-}) alkalinity. CH=min⁡(TH,Alkalinity)CH = \min(TH, \text{Alkalinity}).
  • Non-Carbonate Hardness (NCH): Hardness associated with non-alkalinity anions such as sulfate (SO42−SO_4^{2-}), chloride (Cl−Cl^-), and nitrate (NO3−NO_3^-). NCH=TH−CHNCH = TH - CH. If TH≤AlkalinityTH \le \text{Alkalinity}, then NCH=0NCH = 0.
  • Calcium Hardness (CH) vs. Magnesium Hardness (MH): TH=Ca2++Mg2+TH = Ca^{2+} + Mg^{2+}. Calcium precipitates readily at lower pH ($

To construct a milliequivalent bar graph or calculate chemical doses, concentrations in mg/Lmg/L of specific ions are converted to mg/L as CaCO3mg/L \text{ as } CaCO_3 using their equivalent weights (EWEW):

Concentration as CaCO3(mg/L)=Concentration of Ion (mg/L)×EWCaCO3EWIon\text{Concentration as } CaCO_3 (mg/L) = \text{Concentration of Ion } (mg/L) \times \frac{EW_{CaCO_3}}{EW_{Ion}}

Where EWCaCO3=50.05 g/eqEW_{CaCO_3} = 50.05 \text{ g/eq}, EWCa2+=20.04 g/eqEW_{Ca^{2+}} = 20.04 \text{ g/eq}, EWMg2+=12.15 g/eqEW_{Mg^{2+}} = 12.15 \text{ g/eq}, EWHCO3−=61.02 g/eqEW_{HCO_3^-} = 61.02 \text{ g/eq}, and EWCO2=22.0 g/eqEW_{CO_2} = 22.0 \text{ g/eq} (CO2CO_2 equivalent weight is based on 2 eq/mol).

Lime-Soda Ash Softening Chemistry & Stoichiometry

Chemical precipitation softening uses hydrated lime (Ca(OH)2Ca(OH)_2) and soda ash (Na2CO3Na_2CO_3) to drive Ca2+Ca^{2+} and Mg2+Mg^{2+} ions past their solubility limits, precipitating them as solid calcium carbonate (CaCO3(s)CaCO_3(s), Ksp≈4.8×10−9K_{sp} \approx 4.8 \times 10^{-9}) and magnesium hydroxide (Mg(OH)2(s)Mg(OH)_2(s), Ksp≈5.6×10−12K_{sp} \approx 5.6 \times 10^{-12}).

Stoichiometric Precipitation Reactions

  1. Neutralization of Dissolved Carbon Dioxide (CO2CO_2): Dissolved CO2CO_2 does not contribute to hardness but consumes lime prior to hardness removal:

    CO2+Ca(OH)2→CaCO3(s)+H2OCO_2 + Ca(OH)_2 \rightarrow CaCO_3(s) + H_2O

    (Lime Demand = 1.0 eq of Lime per eq of CO21.0 \text{ eq of Lime per eq of } CO_2)

  2. Precipitation of Calcium Carbonate Hardness: Bicarbonate alkalinity reacts with lime at pH≈9.3−10.0\text{pH} \approx 9.3 - 10.0:

    Ca(HCO3)2+Ca(OH)2→2CaCO3(s)+2H2OCa(HCO_3)_2 + Ca(OH)_2 \rightarrow 2CaCO_3(s) + 2H_2O

    (Lime Demand = 1.0 eq of Lime per eq of Ca2+ CH1.0 \text{ eq of Lime per eq of } Ca^{2+} \text{ CH})

  3. Precipitation of Magnesium Carbonate Hardness: Precipitating Mg2+Mg^{2+} requires elevating the pH above 10.6−11.010.6 - 11.0 to form Mg(OH)2Mg(OH)_2. This requires two equivalents of lime:

    Mg(HCO3)2+2Ca(OH)2→Mg(OH)2(s)+2CaCO3(s)+2H2OMg(HCO_3)_2 + 2Ca(OH)_2 \rightarrow Mg(OH)_2(s) + 2CaCO_3(s) + 2H_2O

    (Lime Demand = 2.0 eq of Lime per eq of Mg2+ CH2.0 \text{ eq of Lime per eq of } Mg^{2+} \text{ CH})

  4. Precipitation of Calcium Non-Carbonate Hardness: Calcium NCH (e.g., CaSO4CaSO_4) requires soda ash to supply the necessary carbonate ion:

    CaSO4+Na2CO3→CaCO3(s)+Na2SO4CaSO_4 + Na_2CO_3 \rightarrow CaCO_3(s) + Na_2SO_4

    (Soda Ash Demand = 1.0 eq of Soda Ash per eq of Ca2+ NCH1.0 \text{ eq of Soda Ash per eq of } Ca^{2+} \text{ NCH})

  5. Precipitation of Magnesium Non-Carbonate Hardness: Magnesium NCH requires both lime (to convert Mg2+Mg^{2+} to Mg(OH)2Mg(OH)_2) and soda ash (to precipitate the added calcium):

    MgSO4+Ca(OH)2+Na2CO3→Mg(OH)2(s)+CaCO3(s)+Na2SO4MgSO_4 + Ca(OH)_2 + Na_2CO_3 \rightarrow Mg(OH)_2(s) + CaCO_3(s) + Na_2SO_4

    (Lime Demand = 1.0 eq1.0 \text{ eq}, Soda Ash Demand = 1.0 eq per eq of Mg2+ NCH1.0 \text{ eq per eq of } Mg^{2+} \text{ NCH})

Excess Lime, Split Treatment & Recarbonation

To ensure complete removal of Mg(OH)2Mg(OH)_2, an excess lime dose of 35−50 mg/L as CaCO335 - 50 \ mg/L \text{ as } CaCO_3 is added to maintain a high pH (>11.0> 11.0). In split-treatment design, a portion of the raw water bypasses the primary excess-lime reactor and is mixed with the high-pH effluent in a second stage. The natural CO2CO_2 and HCO3−HCO_3^- in the bypassed raw water neutralize the excess lime, dramatically reducing chemical purchase costs and sludge volume.

Following precipitation, the water is supersaturated with CaCO3CaCO_3 and has a high pH. Recarbonation involves bubbling carbon dioxide gas (CO2CO_2) into the softened water in two stages:

  • First-Stage Recarbonation: Lowers pH from >11.0>11.0 to ∼9.5\sim 9.5, converting excess OH−OH^- to CO32−CO_3^{2-} and precipitating residual CaCO3CaCO_3.
  • Second-Stage Recarbonation: Lowers pH further to ∼8.3−8.6\sim 8.3 - 8.6, converting insoluble CO32−CO_3^{2-} to soluble HCO3−HCO_3^-, stabilizing the water against scaling prior to distribution.

Synthetic Ion Exchange Softening

Ion exchange replaces hardness ions with non-hardness cations (typically Na+Na^+) using a synthetic cation exchange resin bed (e.g., sulfonated polystyrene divinylbenzene copolymer).

Exchange Mechanics & Regeneration

Resin-2Na++Ca2+⇌Resin-Ca2++2Na+\text{Resin-2Na}^+ + Ca^{2+} \rightleftharpoons \text{Resin-Ca}^{2+} + 2Na^+

As hard water flows through the vessel, the resin selectivity favors Ca2+Ca^{2+} and Mg2+Mg^{2+} over Na+Na^+. Operating parameters include:

  • Exchange Capacity: Expressed in kilograins of CaCO3CaCO_3 per cubic foot of resin (kgr/ft3kgr/ft^3, where 1 kgr=1,000 grains1 \ kgr = 1,000 \text{ grains}, and 1 lb=7,000 grains1 \text{ lb} = 7,000 \text{ grains}). Typical capacities range from 20−30 kgr/ft320 - 30 \ kgr/ft^3.
  • Breakthrough Curve: Monitoring hardness in the effluent reveals an initial period of zero hardness followed by a rapid rise (breakthrough). When effluent hardness exceeds the operational limit, the bed is removed from service.
  • Regeneration Cycle: The exhausted resin is backwashed, regenerated with a concentrated saturated brine solution (10−15% NaCl10 - 15\% \ NaCl), and rinsed. Mass action drives Na+Na^+ back onto the resin, releasing Ca2+Ca^{2+} and Mg2+Mg^{2+} into a concentrated brine waste stream.

Pressure-Driven Membrane Filtration Systems

Membranes act as selective semi-permeable physical barriers for solid-liquid and solute-liquid separation.

Membrane Spectrum & Classifications

ProcessPore Size RangeOperating Pressure RangeTarget Contaminants Removed
Microfiltration (MF)0.1−3.0 μm0.1 - 3.0 \ \mu m3−30 psi3 - 30 \ psi (0.2−2 bar0.2 - 2 \ bar)Suspended solids, turbidity, algae, protozoan cysts (Giardia, Crypto), bacteria
Ultrafiltration (UF)0.01−0.1 μm0.01 - 0.1 \ \mu m10−100 psi10 - 100 \ psi (0.7−7 bar0.7 - 7 \ bar)Macromolecules, proteins, colloidal silica, all viruses
Nanofiltration (NF)0.001−0.01 μm0.001 - 0.01 \ \mu m50−200 psi50 - 200 \ psi (3.5−14 bar3.5 - 14 \ bar)Softening membrane; multivalent ions (Ca2+,Mg2+,SO42−Ca^{2+}, Mg^{2+}, SO_4^{2-}), natural organic matter (NOM)
Reverse Osmosis (RO)<0.001 μm< 0.001 \ \mu m (dense polymer)200−1200 psi200 - 1200 \ psi (14−83 bar14 - 83 \ bar)Monovalent ions (Na+,Cl−Na^+, Cl^-), dissolved salts, trace micropollutants, PFAS

Governing Flux and Osmotic Equations

Water flux (JwJ_w, in L/m2⋅hL/m^2\cdot h or gfdgfd) across a reverse osmosis or nanofiltration membrane is governed by the net driving pressure:

Jw=A(ΔP−Δπ)J_w = A (\Delta P - \Delta \pi)

Where:

  • AA = Water permeability coefficient of the membrane (L/m2⋅h⋅barL/m^2\cdot h \cdot bar)
  • ΔP\Delta P = Transmembrane pressure gradient (Pfeed−Ppermeate−ΔPfriction2P_{feed} - P_{permeate} - \frac{\Delta P_{friction}}{2})
  • Δπ\Delta \pi = Osmotic pressure differential across the active layer (πfeed/boundary−πpermeate\pi_{feed/boundary} - \pi_{permeate})

Osmotic pressure (π\pi) is estimated using the Van 't Hoff equation for dilute solutions:

π=iMRT\pi = i M R T

Where ii is the van 't Hoff factor (number of ions per molecule, e.g., i=2i=2 for NaClNaCl), MM is molar concentration (mol/Lmol/L), RR is the ideal gas constant (0.0821 L⋅atm/mol⋅K0.0821 \ L\cdot atm/mol\cdot K), and TT is absolute temperature (KK).

Solute flux (JsJ_s) across the membrane is driven by concentration gradient:

Js=B(Cm−Cp)J_s = B (C_m - C_p)

Where BB is the solute permeability coefficient and CmC_m is the solute concentration at the membrane surface.

Operational Metrics & Fouling Management

  1. Recovery Rate (RR): Percentage of raw feedwater converted into purified permeate product: R=QpQf×100%R = \frac{Q_p}{Q_f} \times 100\%
  2. Solute Rejection (RrejR_{rej}): Efficiency of solute retention: Rrej=(1−CpCf)×100%R_{rej} = \left(1 - \frac{C_p}{C_f}\right) \times 100\%
  3. Concentration Polarization (CP): Solutes rejected by the membrane accumulate at the boundary layer, elevating local concentration (Cm>CbC_m > C_b). The concentration polarization factor is modeled as CP=Cm−CpCb−Cp=exp⁡(Jwk)CP = \frac{C_m - C_p}{C_b - C_p} = \exp\left(\frac{J_w}{k}\right), where kk is the boundary layer mass transfer coefficient. Elevated CPCP increases osmotic pressure and accelerates membrane scaling.
  4. Fouling Control & CIP: Pretreatment (cartridge filters, antiscalant dosing, acid addition) minimizes mineral scaling (CaSO4,CaCO3CaSO_4, CaCO_3) and biofouling. Periodic Clean-In-Place (CIP) operations utilize low-pH citric acid flushes (to dissolve mineral scale) and high-pH caustic flushes with surfactants (to strip organic and biological foulants).
Test Your Knowledge

Which chemical must be added to remove calcium non-carbonate hardness (NCH) during precipitation softening?

A

Carbon dioxide

B

Sodium hydroxide

C

Calcium hydroxide (Lime)

D

Sodium carbonate (Soda ash)

Test Your Knowledge

What is the primary purpose of recarbonation in a lime-soda ash softening plant?

A

To lower the pH and stabilize the water to prevent scaling.

B

To increase the pH to precipitate magnesium hydroxide.

C

To add carbonate hardness back into the water for taste.

D

To neutralize excess chlorine from disinfection.

Test Your Knowledge

In the membrane flux equation J = A(ΔP - Δπ), what does Δπ represent?

A

Transmembrane applied pressure gradient

B

Osmotic pressure gradient across the membrane

C

Membrane permeability coefficient

D

Concentration polarization factor

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