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Title: ENV 3001 Introduction to Environmental Engineering


1
ENV 3001 Introduction to Environmental Engineering
Lecture II (c) Chemical Foundations Instructor
Dr. Ni-Bin Chang Spring, 2006
2
HW3
  • It is due on next the coming Friday.
  • Email to nibinchang_at_gmail.com

3
Buffers
  • Many solutions exist in nature which are capable
    of withstanding the addition of strong acids and
    bases with little change in pH.
  • These solutions are called buffers.

4
Buffers
  • They are generally combinations of weak acids and
    their salts.
  • For example, a combination of sodium bicarbonate
    (NaHCO3) and sodium carbonate ((Na)2CO3) will
    form a buffered solution with a pH near the pKA
    of bicarbonate, 6.35.
  • The ability of a buffered solution is not
    infinite, however, and works best within 1 pH
    unit of the system pKA.

5
The Carbonate System
  • One of the most important buffering systems in
    nature is the carbonate system, composed of
  • carbon dioxide (CO2),
  • carbonic acid (H2CO3),
  • bicarbonate (HCO3-) and
  • carbonate (CO32-) ions.

6
The Carbonate System
  • The total water system surrounding the planet
    Earth is called the hydrosphere.
  • It includes freshwater systems, oceans,
    atmosphere vapor, and biological waters.
  • The Arctic, Atlantic, Indian, and Pacific oceans
    cover 71 of the Earth surface, and contain 97
    of all water.

7
CO2 Reactions in Water
  • The dissolution of carbon dioxide in water
  • CO 2(gas) CO2(aq)
  • lt1 is hydrated to form carbonic acid
  • CO2 H2O H2CO3

8
CO2 Reactions in Water
  • Some of the carbonic acid dissociates into
    bicarbonate and hydrogen ions which lowers the
    pH
  • H2CO3 HCO3- H
  • As the pH rises, bicarbonate increases to 100
    at a pH of 8.3. Above this, it declines by
    dissociating into carbonate HCO3-
    CO3-2 H

9
Precipitation
  • The reaction between calcium and carbonate to
    form sparingly soluble calcite (calcium
    carbonate).
  • CaCO3 (s) Ca2 CO32-

10
Soda pop chemistry
11
Inorganic - C Equilibria
Note 100 CO2 for pHlt 4.5 100 bicarbonate
for pH 8 and 100 carbonate for pH gt 12
http//waterontheweb.org/curricula/ws/
12
Buffer
  • The ability of a natural water to withstand pH
    changes is measured by its acidity or alkalinity.

13
Inorganic - C Major Sources and Sinks
  • Sources
  • Atmospheric CO2 (invasion)
  • Respiration and other aerobic and anaerobic
    decomposition pathways in the water and sediments
  • Groundwater from soil decomposition products
  • Groundwater from volcanic seeps
  • Sinks
  • pH dependent conversions to bicarbonate and
    carbonate
  • Precipitation of CaCO3 and MgCO3 at high pH
  • Photosynthesis

14
CO2 Chemistry Alkalinity
  • Alkalinity the ability of water to neutralize
    acid a measure of buffering capacity or acid
    neutralizing capacity (ANC)
  • Total Alkalinity (eq/L) HCO3- 2CO32-
    OH- - H
  • Total Acidity (eq/L) 2H2CO3 HCO3-
    H - OH-
  • Total Alkalinity typically measured by titration
    with a strong acid.
  • The units are in mg CaCO3/L for reasons relevant
    to drinking water treatment (details in Chapter
    6)

15
Alkalinity and Water Treatment
  • Advanced wastewater treatment (domestic sewage)
  • Phosphorus nutrient removal by adding lime
    (Ca(OH)2) or calcium carbonate (CaCO3)
  • As pH increases gt9, it precipitates adsorbed
    PO4-3
  • Settle and filter the effluent to obtain 90-95
    removal
  • Used for particle (TSS) removal also
  • Drinking water treatment
  • For TSS removal prior to disinfection

16
Acid Rain Impacts
  • Acid-rain mitigation to whole lakes
  • Lime or limestone added as powdered slurry to
    increase impacted lake pH value
  • Also broadcast aerially to alkalize entire
    watersheds

17
Acidity of Rainfall in the United States in the
Period 1731 March 1973 (ANON 1974).
National Academy of Science, 2005
18
Acidity (as pH) in the Rainfall in the US in 1996
19
Example Problem 2.9
  • A 1-m deep lake with a surface area of 4,000 m2,
    has an initial pH of 6.5 buffered by the
    carbonate system (alkalinity 20 mg/L as CaCO3).
  • Calculate the pH of the lake after receiving 5
    cm of acid rain with a nitric acid (a strong
    acid) concentration of 2x10-4 M.

20
Example Problem 2.9
  • Solution
  • First calculate the increase in the concentration
    of H in the lake due to the addition of the acid
    rain
  • 0.05 m rain x 4000 m2 surface area 200 m3
    200,000 L of acid rain
  • 200,000 L x 0.0002 moles/L HNO3
  • 40 moles H added
  • The final lake volume 4,000 m2 x 1 m 200,000
    L 4,200 m3 4,200,000 L

21
Example Problem 2.9
  • Thus the concentration of H added is
  • H 40 moles/4,200,000 L9.5 x 10-6 M
  • Because the pH is at 6.5, the concentration of
    carbonate is negligible and the buffering is
    provided by bicarbonate and carbonic acid (see
    next slide).
  • Now, calculate the concentration of bicarbonate
    and carbonic acid before the addition of the acid
    rain.

22
Inorganic - C Equilibria
Note 100 CO2 for pHlt 4.5 100 bicarbonate
for pH 8 and 100 carbonate for pH gt 12
http//waterontheweb.org/curricula/ws/
23
Example Problem 2.9
  • Using equation (2.23) and substituting for H
    10-6.5 M
  • H2CO3 0.71HCO3-
  • Alkalinity 20 mg/L as CaCO3 (Given condition)
  • Converting to eq/L (using equation 2.30)
  • 0.020 g/L/50 g/eq 4 x 10-4 eq/L

24
Example Problem 2.9
0
0
  • 4 x 10-4 eq/L HCO3- 2CO32- OH- -
    H
  • Neglecting both carbonate and hydroxide
    concentrations at the low pH of 6.5,
  • HCO3- - H 4 x 10-4 M
  • But H 10-6.5 M 3.16x 10-7 M
  • HCO3- 4 x 10-4 M
  • We already have had H2CO3 0.71HCO3-
  • H2CO3 0.71 x 4 x 10-4 2.8 x 10-4 M

25
Example Problem 2.9
  • With the addition of 9.5 x 10-6 M H in the acid
    rain, 9.5 x 10-6 M of bicarbonate is converted to
    carbonic acid with the following resulting
    concentrations
  • HCO3- 4 x 10-4 - 9.5 x 10-63.9 x 10-4M
  • H2CO3 2.8 x 10-4 9.5 x 10-6 2.9 x 10-4 M

26
Example Problem 2.9
  • H 3.32 x 10-7M
  • pH 6.48
  • Note that because of the effective buffer system
    present, the pH depression was limited to 0.02
    units.

27
Inorganic - C Equilibria
Note 100 CO2 for pHlt 4.5 100 bicarbonate
for pH 8 and 100 carbonate for pH gt 12
http//waterontheweb.org/curricula/ws/
28
Solubility Product
  • Another example of the application of the
    equilibrium concept is the solubility of solids.
  • The solubility product constant is an equilibrium
    constant which describes the dissolution of a
    solid into ions in aqueous solutions.

29
Solubility Product
  • It is widely used in designing methods to remove
    toxic metal ions dissolved in water.
  • Arsenic removal systems are needed for removal of
    arsenic to less than 10 ppb when groundwater
    system is part of the drinking water system.
  • The treatment process may also remove other heavy
    metals including lead, iron and manganese.

30
Solubility Product
  • AaBb(s) lt--------gt aAb bBa- (2.31)
  • The equilibrium constant is
  • Since the concentration of AaBb(s) is 1 M, by
    definition, the solubility product constant can
    be written as follows (for a system at
    equilibrium)
  • KSP AbaBa-b

31
Solubility Product
  • Write the expression for the solubility constant
    of mercury (I) sulfate, Hg2SO4
  • Hg2SO4 (s) ? Hg2 2(aq) SO42-(aq)
  • Ksp (Hg2 2) (SO42-)
  • So the product of the concentration of the ions,
    raised to the power of its coefficient in the
    solubility equation, is a constant.

32
Solubility Product
  • KSP is a function in terms of temperature and
    pressure.
  • The solubility constant, Ksp, has a fixed value
    at a given temperature (normally at 25 Degrees
    Celsius)
  • A solution can be described as being
  • saturated,
  • unsaturated, or
  • Supersaturated

33
Solubility Product
  • An unsaturated solution is not at equilibrium and
    can dissolve more solid.
  • A saturated solution is at equilibrium.
  • A saturated solution implies that the system
    cannot dissolve more solid unless the temperature
    or pressure is changed.

34
Solubility Product
  • Supersaturated solutions are those solutions that
    contains more solute than it would if the
    dissolved solute were in equilibrium with the
    undissolved solute.
  • Supersaturated solutions are those solutions that
    are above the solubility limits.
  • Supersaturated solutions are meta stable.

35
Solubility Product
  • A supersaturated solution can be created by
    dissolving a solid at an elevated temperature and
    then allowing it to cool.
  • Once cooled, precipitation may not occur,
    although the solution is not at equilibrium.
  • Precipitation will occur if the reaction vessel
    is shaken or otherwise disturbed.

36
Supersaturated Solution
  • Crystallization from Supersaturated Solutions of
    Sodium Acetate
  • http//genchem.chem.wisc.edu/demonstrations/Gen_Ch
    em_Pages/11solutionspage/crystallization_from_supe
    r.htm
  • http//www.sdnhm.org/kids/minerals/grow-crystal2.h
    tml

http//www.sdnhm.org/fieldguide/minerals/index.htm
l
37
Theoretical Solubility of Copper Hydroxides
mg/L
Precipitation region
38
Theoretical Solubility of Nickel Hydroxides
39
(No Transcript)
40
Example Problem 2.10
  • Calculate the solubility of barium sulfate,
    BaSO4, in pure water at 25o C in mg/l.
  • What is the equilibrium concentration of barium
    (Ba2) in water that contains 10-3 M sulfate,
    SO42-?
  • At 25oC, the KSP for BaSO4 is 1.0 x 10-10.

41
Example Problem 2.10
  • Solution
  • Let x equal the number of moles/l of BaSO4 which
    will dissolve in pure water as follows
  • BaSO4(s) lt-------gt Ba2 SO42-
  • If x moles of BaSO4 dissolve, then x mole of Ba2
    and x moles of SO42- will enter the solution.
  • KSP 1.0 x 10-10 Ba2 SO42- x2
  • x 1.0 x 10-5 moles/L

42
Example Problem 2.10
  • If the water initially contains 10-3 M SO42-,
    after y moles/l of BaSO4 dissolve, the solution
    will contain (y 10-3) M SO42- and y moles/l of
    Ba2. Then
  • KSP 1.0 x 10-10 Ba2SO42-
  • y (y 10-3)
  • and using the quadratic formula

y 1.0 x 10-7 M
43
Example Problem 2.11
  • (a) Calculate the concentration of cadmium as the
    pH of a solution decreases from 11 to 10 to 9.
  • Assume that the solubility of cadmium is
    controlled only by hydroxide. The Ksp for
    cadmium hydroxide (Cd(OH)2) at 250C is 2.0 x
    10-14.
  • (b) The national groundwater drinking water
    standard for cadmium is 0.005 mg/l. Calculate
    the minimum hydroxide concentration required to
    meet the groundwater standard.

44
Example Problem 2.11
  • Solution
  • From the Ksp and the concentration of OH-, the
    concentration of Cd2 can be calculated.
  • Cd(OH)2 (s) lt--------gt Cd2 2OH-
  • Ksp Cd2OH-2
  • At pH 11, the concentration of OH- is 10-3 M,
    so the concentration of Cd2 is
  • Cd2 2.0 x 10-14/ (10-3)22.0 x 10-8 M (pH
    11)
  • At pH 10, the concentration of OH- is 10-4 M,
    so the concentration of Cd2 is
  • Cd2 2.0 x 10-14/ (10-4)22.0 x 10-6 M (pH
    10)

45
Example Problem 2.11
  • At pH 9, the concentration of OH- is 10-5 M, so
    the concentration of Cd 2 is
  • Cd 2 2.0 x 10-14/ (10-5)2 2.0 x 10-4 M (pH
    9)
  • As you can see, as the pH decreases (as the
    hydroxide concentration gets lower) the cadmium
    concentration (a toxic heavy metal) gets much
    higher.

46
Example Problem 2.11
  • In order to calculate the concentration of
    hydroxide when cadmium is 0.005 mg/L, first the
    concentration must be expressed in units of
    moles/L.
  • Cd 2 5x 10-6 g/L / 112.4 g/mole 4.45 x 10-8
    moles/L
  • From the Ksp, the minimum hydroxide concentration
    can be calculated
  • OH- (2.0 x 10-14/4.45 x 10-8)0.5 2.1 x 10-2 M
  • Note This corresponds to a pH of 10.8. So, to
    control Cd in water, we would need to add a base,
    like NaOH, to raise the pH to at least 10.8.

47
Gas Law and Environmental Applications
  • Stripping of nuisance gases, such as ammonia,
    hydrogen sulfide, etc involves the transfer of
    these gases from water or wastewater to the
    atmosphere.
  • The transfer of oxygen into water to support
    aquatic life and the biological degradation of
    organic compounds.
  • .

48
Hydrogen Sulfide
  • Individuals living near a wastewater treatment
    plant, a gas and oil drilling operation, a farm
    with manure storage or livestock confinement
    facilities, or a landfill may be exposed to
    higher levels of hydrogen sulfide.
  • Just a few breaths of air containing high levels
    of hydrogen sulfide gas can cause death.
  • Lower, longer-term exposure can cause eye
    irritation, headache, and fatigue.

49
Ammonia Impacts
  • The US EPA (1984) reports LC50 (Lethal
    Concentration ) of ammonia in the aquatic
    environment starting at 0.53 mg/L NH3.
  • Ammonia stripping is a simpledesorption method
    that is employed to lower the ammonia content of
    a wastewater stream.

50
Ammonia Stripping
  • lime or caustic soda is added to the wastewater
    until the pH reaches 10.8 to 11.5.
  • NH4 (aq) OH-(aq) H2O NH3 (gas)
  • The reaction is highly dependent on the pH. At
    high pH (above pH 9), the ammonia (NH3) is
    liberated from the wastewater into the gas phase

51
Ammonia Stripping
  • Counterflow stripping columns (air stripper) are
    the most common design.
  • By a combination of pH adjustment and
    temperature, we calculate the tower size for any
    required efficiency.

52
Gas Law
  • Ideal Gas Law P, V, T
  • Daltons Law Partial Pressure in a mixed gas
  • Roults Law volatile liquid
  • Henrys Law volatile liquid

53
Ideal Gas Law
  • The Ideal Gas Law can be expressed more
    universally as shown below
  • PV nRT (2.34)
  • where
  • n number of moles of gas present, and
  • R the universal gas constant.
  • The units of the universal gas constant, R, are a
    function of the units of the pressure, volume,
    and temperature terms.

54
Ideal Gas Law
  • The Ideal Gas Law can be used to determine the
    volume of one mole of gas at Standard Temperature
    and Pressure (STP 25o C, 1 atm) as follows.
  • V/n RT/P
  • V/n (0.08205 L-atm/mol-K)(25 273 oK)/
  • (1 atm) 24.45 L/gmole

55
Ideal Gas Law
  • The Ideal Gas Law can also be used to convert
    between two popularly used expressions of gas
    concentrations, ppm (by volume) and µg/m3.
  • An example of this conversion using the above
    calculation is shown in the following equation

56
Dalton's Law of Partial Pressure
  • In a mixture of gases, each gas exerts pressure
    independently of other gases present.
  • The partial pressure exerted by each gas is
    proportional to the amount (by volume) of gas
    present.

57
Example Problem
  • The 1-hour National Ambient Air Quality Standard
    for CO is 35 ppm. Calculate the corresponding
    concentration in mg/m3, at 250 C and atmospheric
    pressure.
  • Solution
  • For gases in air, ppm refers to volume fraction.
  • So 35 ppm is equivalent to 35 ml of CO per
    million ml of polluted air, or 35 ml of CO per m3
    of air.
  • The mass density of pure CO in mg/ml can be
    derived from the ideal gas law

58
Example Problem
Thus, the concentration of CO in air (in mg / m3
) is
59
Dalton's Law of Partial Pressure
  • Dalton's Law can be expressed mathematically by
    the following equations.
  • PT P1 P2 P3 ..... Pi SPi or VT S
    Vi
  • Where
  • Pi the partial pressure exerted by gas i
    (if gas i were the only gas present in the total
    volume VT)
  • Vi the partial volume occupied by gas i
    (at the total pressure PT)

60
Dalton's Law of Partial Pressure
  • From the Ideal Gas Law
  • Pi niRT/vT or Vi ni RT/PT
  • PT nTRT/vT or VT nT RT/PT
  • Pi/PT ni/nT or Vi/VT ni/nT
  • Where
  • ninumber of moles of gas i
  • nT total number of moles of gas

61
Raoult's Law
  • A volatile liquid or mixture of liquids may be in
    equilibrium with the gas phase above it.
  • The partial pressure of the component in the gas
    phase will be directly proportional to the mole
    fraction of the component in the liquid mixture.
  • It also is proportional to the volatility of the
    component as measured by its vapor pressure.

62
Raoult's Law
  • Raoult's Law may be expressed by the following
    equation
  • Pi XiPV
  • Where
  • Pi partial pressure of component i in the
    gas phase,
  • Xi mole fraction of i in the liquid mixture,
  • PV vapor pressure of component i.

63
Applications of Raoult's Law
  • Raoult's Law can be used to predict the vapor
    phase concentration of components of gasoline
    spilled into the subsurface when the gasoline is
    present as a floating pool.
  • It is the case of nonaqueous phase liquid on the
    water table in site remediation.

64
Henry's Law
  • Often, environmental pollutants are present in
    very dilute solutions and Raoult's Law is not
    applicable.
  • For dilute solutions, a variation on Raoult's Law
    called Henry's Law can be applied.

65
Henry's Law
  • Henry's Law states that, under equilibrium
    conditions, the concentration of a gas dissolved
    in a liquid is proportional to its concentration
    in the gas that is in contact with the liquid.

66
Henry's Law
  • The proportionality constant is called Henry's
    Constant and takes on many different units,
    depending on the units of the gas and liquid
    concentration terms.
  • Caq KHPg
  • KH Henrys law constant, mole/L- atm
  • PaHaXa
  • Ha Henrys law constant, atm/mole fraction
  • Pa partial pressure of the solute a in the
    gas phase
  • Xa mole fraction of solute a in the liquid
    phase

67
Henrys Constant for Environmental Significant
Gases (25oC)
68
Example Problem 2.12
  • A drinking water must be treated to control
    taste and odor due to the presence of 6.4 mg/L of
    H2S.
  • It is proposed to remove the H2S from the water
    by transferring it to an air stream in a
    stripping tower.
  • Within the stripping tower, water flows downward
    at 40 million gallons/day (MGD) and air flows
    upward at 120,000 standard cubic feet per min
    (scf/min).
  • The temperature is 25oC and the pressure is 1
    atm.

69
Example Problem 2.12
  • First, calculate the air concentration of H2S in
    µg/m3 and ppm assuming that the H2S is completely
    removed from the water.
  • Next calculate the equilibrium concentration of
    H2S in the air assuming the water concentration
    remains at 6.4 mg/L.

70
Example Problem 2.12
  • Solution
  • First, calculate the H2S mass flow rate in g/sec.
  • Mass Flowrate C (g/L) x Q (L/sec)
  • Q(40 MGD)(106 gal/MG)(3.785 L/gal)/(86,400
    sec/d)
  • Q43.8 L/sec
  • Mass Flowrate(0.0064 g/L)(43.8 L/sec)
  • 11.17 g/sec

71
Example Problem 2.12
  • Now calculate the concentration of the H2S in the
    air, assuming that all H2S is transferred to gas.
  • Cgas, µg/m3(Mass Flowrate, µg/sec)/(QAir m3/sec)
  • QAir, m3/sec(120,000 scf/min)/(60
    sec/min)(35.31 ft3/m3) 56.6 m3/sec
  • C (11.17 x 10 6 µg/sec)/ 56.6 m3/sec
  • 197,200 µg/m3

72
Example Problem 2.12
  • Calculate the concentration of H2S in the air if
    it were in equilibrium with the incoming water
    using Henry's Law.
  • Henry's Constant for H2S is 0.1022 mol/L-atm.
  • Pg KH Caq
  • Pg (0.0064 g/L)/(34 g/mole)(0.1022
    mole/l-atm) 0.00184 atm

73
Example Problem 2.12
  • From the ideal gas law
  • Cg, mole/L n/VPg/RT(0.00184atm)/0.08206)(298)
  • 7.52 x 10-5 moles/L
  • Cg (7.52 x 10-5)(0.08206)(298)106/1
  • Cg 1840 ppm

74
Example Problem 2.12
  • The equilibrium gas concentration of H2S (1840
    ppm) is much higher than the actual exit gas
    concentration (142 ppm) achieved by completely
    stripping the H2S from the water.
  • Since the required exit gas concentration is much
    lower than the concentration achievable under
    equilibrium conditions, the air flow is probably
    sufficient to remove the gas.
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