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Ammonia Volatilization from Urea: How large is the issue and losses. David E. Kissel University of Georgia

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  • Ammonia Volatilization from

    Urea: How large is the issue

    and losses.

    David E. Kissel

    University of Georgia

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Urea

    Ammonium nitrate

    Nitrogen solutions

    Ammonium phosphate

    Total compound N

    0

    1973 / 74

    2004 / 05

    10 20 30 40 50

    www.fertilizer.org

    51%

    World Evolution of N Fertilizer

    Consumption

    Millions of tonnes

  • Urea

    Ammonium nitrate

    Nitrogen solutions

    Total compound N

    0

    1973 / 74

    2004 / 05

    1 2 3 4 5

    www.fertilizer.org

    21%

    Millions of tonnes

    USA Evolution of N Fertilizer

    Consumption

    Anhydrous ammonia

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Definitions• Dissolution: urea absorbs water

    and converts from solid to liquid

    • Hydrolysis: urea converts to ammonium (NH4

    +)

    • Diffusion: movement due to motion of molecules

    – Urea has no charge, diffuses easily

    – NH4+ has charge, diffuses slowly

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Q. Does any ammonia volatilize

    from UAN solutions before they are

    applied or during the application?

    A. None or very little, depending on

    if a small amount of ammonia is

    added to protect against corrosion of

    mild steel.

  • Composition of UAN 28% N

    • 14 % N from Ammonium Nitrate

    – 7% ammonium N

    – 7% nitrate N

    • 14% N from Urea

    • 30% water

    • + small amounts of inhibitors to inhibit

    corrosion of mild steel

  • Inhibitors to protect against

    corrosion of mild steel

    • 0.5 % ammonia (raises pH to about 7.5)

    • Ammonium phosphates at 0.2 % P2O5

    • Others

  • NH4 NH4 = NH3 + H

    +NH4 = NH3 + H

    +NH4 = NH3 + H+NH4+ = NH3 + H

    +

    (ion) (gas)

  • Urea Hydrolysis in UAN?

    • DOES NOT OCCUR

    – Therefore no ammonia is formed from the urea

    portion of the UAN solution from this process.

    – Therefore no ammonia loss from the urea

    portion of UAN solution before soil

    application.

  • Summary of ammonia loss from

    UAN

    • Urea in UAN does not hydrolyze in the fertilizer tank.

    • The NH4+ from the ammonium nitrate

    portion of the UAN cannot be lost as NH3.• The amount of NH3 added to some UAN to

    inhibit corrosion is very small, around 10 lb per ton. A small portion of this NH3 may be lost during application.

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Urea Dissolution

    • Urea has to be dissolved before it can be hydrolyzed

  • Urea Dissolution

    • Urea has to be dissolved before it can be hydrolyzed

    • Urea can absorb water from the atmosphere and from the soil/crop residue

  • Urea Dissolution

    • Urea has to be dissolved before it can be hydrolyzed

    • Urea can absorb water from the atmosphere and from the soil/crop residue

    • Absorption of water from the atmosphere depends on relative humidity (RH)

  • Urea Dissolution

    • Urea has to be dissolved before it can be hydrolyzed

    • Urea can absorb water from the atmosphere and from the soil/crop residue

    • Absorption of water from the atmosphere depends on relative humidity (RH)

    • Critical relative humidity (CRH) is the RH at which urea dissolves

  • Effect of Temperature on CRH

    and Water Solubility of Urea

    Air Temperature (oF)

    20 40 60 80 100 120Critical R

    ela

    tive H

    um

    idity f

    or

    Ure

    a (

    %)

    60

    65

    70

    75

    80

    85

    90

    Ure

    a S

    olu

    bili

    ty (

    lb/g

    allo

    n o

    f w

    ate

    r)

    4

    6

    8

    10

    12

    14

    16

    CRH

    Solubility

  • Urea Urea UreaUrea Urea Urea

    RH > CRH (80%)

    Crop residue

    Urea dissolution

    and diffusion

    Dry Soil

    www.agrium.com

  • Urea Urea Urea

    Urea dissolution

    and diffusion

    Urea Urea UreaCrop residue

    Urea Urea Urea

    www.agrium.com

    1/2 inch

    Wet Soil

  • Urea Diffusion into Soil (after 10 days)Urea Concentration in Soil (ppm)

    0 100 200 300 400 500 600 700

    Soil

    Depth

    (m

    m)

    0

    10

    20

    30

    40

    50

    Drier

    Wetter

  • Urea Urea UreaUrea Urea UreaCrop residue

    Urea Urea Urea2 inches

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Urea Hydrolysis

    Urea 2 Urease enzyme

    + H+2 NH4+

    • Urease is derived from crop residues

    and soil microorganisms

  • Urea Urea UreaUrea Urea Urea

    Crop residue

    Urease inhibitor

    Urea Urea Urea

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • (aq)

    Soil solution

    NH4+

    NH3 Volatilization Process

    Urea

    Atmosphere

    Clay

    OM

    NH4+

    NH4+

    NH4+

    Hydrolysis

    NH4+

    (aq)+

    Equilibrium

    NH3 H+

    (gas)

    Soil air

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    + 2 H+ 2

  • Soil pH

    5 6 7 8 9

    NH

    3 (

    as %

    of

    To

    tal A

    mm

    on

    iaca

    l N

    )

    0

    5

    10

    15

    20

    25

    30

    68oF

    Effect of soil pH on NH3 as % of Total N

  • (aq)

    Soil solution

    NH4+

    NH3 Volatilization Process

    Urea

    Atmosphere

    Clay

    OM

    NH4+

    NH4+

    NH4+

    Hydrolysis

    NH4+

    (aq)+

    Equilibrium

    NH3 H+

    (gas)

    Soil air

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    + H+

  • Ferguson et al. (1984)

    Days Since Urea Application

    0 2 4 6 8 10 12

    So

    il p

    H

    6

    7

    8

    9

    NH

    3 L

    oss (

    kg

    N h

    a-1

    )

    0

    4

    8

    12

    High Buffering Capacity

    Low Buffering Capacity

    Low Buffering Capacity

    High Buffering Capacity

    •Increase in soil pH

    depends on soil H+

    buffering capacity

    •Higher clay and OM

    contents lead to higher

    soil H+ buffering

    capacity

  • Atmosphere

    H+

    H+H+

    H+

    H+

    H+

    H+

    NH4+

    Urea

    Urea

    NH4+

    NH4+

    NH4+

    NH4+

    NH4+

    NH4+

    NH4+

    Urea

    ½ inch

    pH 6 7 8 9

    NH4+NH4

    +

    NH4+NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    CECH+

    Urea

    Urea hydrolyzes on the soil surface

  • H+

    H+

    H+H+

    H+

    H+

    H+

    H+

    NH4+

    Urea Urea

    Urea

    NH4+

    NH4+NH4

    +

    NH4+

    Urea

    2 inches

    pH 6 7

    NH4+NH4

    +

    NH4+

    NH4+NH4+

    NH4+NH4+NH4

    +NH4+

    NH3

    Urea Urea

    Urea

    Urea

    CEC

    Urea hydrolyzes below the soil surface

  • Soil

    +

    Effect of Temperature on NH3 Volatilization

    NH4+Urea NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    ½ inch

    Temperature

  • Effect of Temperature on Urea Hydrolysis

    Temperature (oF)

    30 40 50 60 70 80 90 100 110

    Rela

    tive U

    rease A

    ctivity

    0

    1

    2

    3

    4

    5

    6

    Gould et al. (1973)

  • Soil

    +

    Effect of Temperature on NH3 Volatilization

    NH4+Urea NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    ½ inch

    Temperature

  • Temperature (oF)

    30 40 50 60 70 80 90 100 110

    NH

    3 (

    as %

    of

    Tota

    l A

    mm

    onia

    cal N

    )

    0

    5

    10

    15

    20

    25

    30

    35

    Effect of Temperature on % of NH3

    pH = 8.5

  • Soil

    +

    Effect of Temperature on NH3 Volatilization

    NH4+Urea NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    ½ inch

    Temperature

  • Temperature (oF)

    30 40 50 60 70 80 90 100 110Rela

    tive D

    rivin

    g F

    orc

    e for

    Convers

    ion

    of A

    queous N

    H3 to G

    aseous N

    H3

    1

    2

    3

    4

    5

    Effect of Temperature on Conversion of

    Aqueous NH3 to Gaseous NH3

  • Soil

    +

    Effect of Temperature on NH3 Volatilization

    NH4+Urea NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    ½ inch

    Temperature

  • Soil

    Wind speed

    +

    Effect of Wind Speed on NH3 Volatilization

    NH4+Urea

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    Atmosphere

    ½ inch

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

  • Am

    monia

    Loss (

    % o

    f A

    pplie

    d N

    )

    0

    5

    10

    15

    20UAN UREA Nitamin

    51mm

    Replication II0

    5

    10

    15

    20 UAN UREA Nitamin

    51mm

    Replication I

    Days After Application

    0 20 40 60 80 100 1200

    5

    10

    15

    20UAN UREA Nitamin

    51mm

    Replication III Time00:00:00 08:00:00 16:00:00 00:00:00

    Win

    d S

    pe

    ed

    (m

    s-1

    )

    0

    1

    2

    3

    4

    5

    High

    Low

    Time

    00:00:00 08:00:00 16:00:00 00:00:00

    Win

    d S

    pe

    ed

    (m

    s-1

    )

    0

    1

    2

    3

    4

    5

    High

    Low

  • Optimum Conditions for

    Volatilization

    • Small diffusion depth into soil

    • RH > CRH

    • High temperature

    • High wind speed

    • Low pH buffering capacity

  • Overview

    • Urea Consumption

    • Definitions

    • UAN Solution Reactions

    • Urea Dissolution and Diffusion

    • Urea Hydrolysis

    • Ammonia Volatilization

    • Research Results

    • Summary

  • Urea Applied to Pasture - Fall 2004

    Days after application

    NH

    3lo

    ss (

    % o

    f applie

    d N

    )

    0

    10

    20

    30

    40

    50

    0.1

    0.2

    0.3

    0.4

    10

    20

    30

    40

    50

    Soil

    wa

    ter

    conte

    nt

    (g g

    -1)

    20 40 60 80 100 120

    Rain

    fall

    (mm

    )

    Nitamin®

    UAN

    Urea

    Rainfall

    Soil water content

    Temp = 47oF

  • Days after application

    NH

    3lo

    ss (

    % o

    f applie

    d N

    )

    0

    10

    20

    30

    40

    50

    10

    20

    30

    40

    50 Nitamin®

    UAN

    Urea

    0.1

    0.2

    0.3

    0.4

    Soil

    wa

    ter

    conte

    nt

    (g g

    -1)

    20 40 60

    Rain

    fall

    (mm

    )

    Rainfall

    Soil water content

    Temp = 63oF

    Urea Applied to Pasture – Spring 2005

  • UreaNH4+

    Atmosphere

    Clay

    OM

    NH3

    Urea Urea Urea

    Urea UreaNH4+

    NH4+

    (aq)+

    Equilibrium

    NH4+

    (aq)NH3 H+

  • Days after application

    NH

    3lo

    ss (

    % o

    f applie

    d N

    )

    0

    10

    20

    30

    40

    50

    10

    20

    30

    40

    50Nitamin®

    UAN

    Urea

    Rainfall

    Soil water content

    0.1

    0.2

    0.3

    0.4

    Soil

    wa

    ter

    conte

    nt

    (g g

    -1)

    20 40 60

    Rain

    fall

    (mm

    )Temp = 62oF

    Urea Applied to Pasture - Fall 2005

  • Time of RH above CRH in the first 30 d

    Tim

    e o

    f R

    H >

    CR

    H (

    h)

    0

    5

    10

    15

    20

    25

    0 5 10 15 20 25 30

    Total: RH > CRH =19 days63 %

    Days after application

  • Urea Urea Urea

    Atmosphere

    Urea Urea Urea

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    Soil water content (0.07 g g-1)

    RH > CRH (80%)

    Permanent wilting point (0.04 g g-1)

    Fescue thatch

    NH4+

    NH4+

    NH4+

    NH4+NH4

    +NH4+NH4

    +

  • Days after application

    NH

    3lo

    ss (

    % o

    f applie

    d N

    )

    0

    10

    20

    30

    40

    50

    10

    20

    30

    40

    50Nitamin®

    UAN

    Urea

    0.1

    0.2

    0.3

    0.4

    Soil

    wa

    ter

    conte

    nt

    (g g

    -1)

    20 40 80

    Rain

    fall

    (mm

    )

    60

    Rainfall

    Soil water content

    Temp = 69oF

    Urea Applied to Pasture – Spring 2006

  • Urea Urea Urea

    Urea Urea UreaNH4+

    Atmosphere

    NH4+

    NH4+

    (aq)+

    Equilibrium

    NH4+

    (aq)NH3 H+

    NH3

    NH3 NH3

    NH3

    NH3

    NH3NH3

    NH3

    Soil water content (0.15 g g-1)

    Field capacity (0.18 g g-1)CEC

  • Ammonia volatilization losses under field conditions

    Fertilizer

    --------------- Ammonia loss (% of applied N) -----------------

    Fall 2004

    Urea

    UAN

    Nitamin®

    19 a*

    6 b

    6 b

    Spring 2005

    12 a

    13 a

    14 a

    •Within a column, values followed by the same letter are not significantly different according to

    Fisher’s LSD at p=0.05

    Summary of Pasture Results

    Fall 2005 Spring 2006

    46 a

    33 b

    34 b

    24 a

    18 a

    18 a

  • Summary for Pastures/No-Till

    Dry Soil, Dry Residue, RH < CRH: OK

    Dry Soil, Dry Residue, RH > CRH: not OK

    Wet Soil, Wet Residue: not OK

    • Apply on dry soil, dry residue, expected low RH, and

    hope for 1 inch of rain whenever it rains.

    • Apply on wet soil if 1 inch rain/irrigation is expected.

  • Summary for Clean-Till Crops

    Dry Soil: OK

    Wet Soil: not OK

    • Apply on dry soil and hope for 1 inch of rain whenever

    it rains.

    • Apply on wet soil if 1 inch of rain/irrigation is expected.

  • Summary for Pastures/CropsKnifed or disked in

    Dribbled

    Broadcast

    • Knifed or disked in better than Dribbled

    • Dribbled better than Broadcast

  • Laboratory Results (77oF, 90% RH)

    NH3 volatilization in the lab

    Days after application0 10 20 30

    NH

    3Lo

    ss (

    % o

    f A

    pplie

    d N

    )

    0

    10

    20

    30 Urea

    UAN

    Nitamin®

    a

    bb

  • Some Results from Central Great

    Plains, Manhattan, Kansas

  • Topdress N on Wheat

    Kansas State Univ., NE KS

    N, pounds/acre N Source Yield, Bu/acre

    0 45.3

    30 Urea 60.2

    60 Urea 68.1

    90 Urea 71.0

    30 Amm. Nitrate 59.1

    60 Amm. Nitrate 64.0

    90 Amm. Nitrate 70.1

  • Ammonia loss from N uptake by

    Coastal Bermudagrass- Temple, TX

    Bill Hargrove – 1975, 1976

    Treatment N rate, pound/A NH3 Loss (%)

    Urea 100 0

    Urea 200 0

    Urea 400 3

    UAN 100 8

    UAN 200 2

    UAN 400 0

  • Questions?