The Dynamic World of Ammonia 1 NH 3 in the Environment HNO 3(g) - - PowerPoint PPT Presentation

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The Dynamic World of Ammonia 1 NH 3 in the Environment HNO 3(g) - - PowerPoint PPT Presentation

The Dynamic World of Ammonia 1 NH 3 in the Environment HNO 3(g) Deposition Eutrophication? NH 3(g) Acidification? H 2 SO 4 Emissions 65 Tg N yr -1 ~5 ~6 ~37 ~2 ~4 ~9 2 Sutton et al. (2013) Phil. Trans. R. Soc. B. Changes in


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SLIDE 1

The Dynamic World of Ammonia

1

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SLIDE 2

NH3 in the Environment

NH3(g)

H2SO4 HNO3(g) ~9 ~5 ~37 ~2 ~4 ~6 Emissions ≈ 65 Tg N yr-1 Sutton et al. (2013) Phil. Trans. R. Soc. B. Deposition… Eutrophication? Acidification?

2

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SLIDE 3

Changes in precipitation N

  • In all but one state, NO3
  • wet deposition fluxes decreased (average 29%)
  • In 37 of 45 states, NH4

+ wet deposition fluxes increased (average 22%)

Li et al., PNAS, 2016

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SLIDE 4

NHx also comprises majority of total inorganic nitrogen deposition

Li et al., PNAS, 2016

Biggest uncertainty lies with bidirectional NH3 deposition

Pleim et al., JGR, 2013

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SLIDE 5

Spring overview

  • Strong

concentration gradient

  • Low

concentrations west of RMNP

  • High

concentrations east of RMNP

  • Ammonia peaks

in NE Colorado

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SLIDE 6

A closer look…

  • Ammonium nitrate episodes

associated with upslope flow from east of RMNP

20 40 60 80 100 120 140 4/20 4/21 4/22 4/23 4/24 4/25 4/26 4/27 Date neq/m3 90 180 270 360 WD (Degree) SO4= NO3- NH4+ WD 30 per. Mov. Avg. (WD)

precip

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SLIDE 7

6 4 2 NH3 (ppb) 12:00 AM 2015-06-25 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-26 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-27 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-28 Time (local)

NH3 emissions

Adapted from Benedict et al. (2013a)

RMNP Denver

NH3 in Rocky Mountain National Park

RMNP morning NH3 often increases prior to upslope flow from eastern Colorado

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SLIDE 8

What is dew?

Radiative cooling of surfaces at night can drop their temperature below the air dewpoint leading to condensed water (dew) formation

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https://www.flickr.com/photos/steve wall/4680114666/in/photostream/

Ersa, Greek goddess of dew

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SLIDE 9

9

𝑂𝐼3(𝑕) ↔ 𝑂𝐼3 ∙ 𝐼2𝑃 ↔ 𝑂𝐼4 + + OH-

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SLIDE 10

Motivation and Goals

No quantitative studies on NH3 emission from dew

  • 1. Is dew a significant NH3 reservoir?
  • 2. What happens to NH4

+ (dew) upon evaporation?

  • 3. Can dew evaporation explain the NH3 morning spike?

NH3(g)

𝐹𝑛𝑗𝑡𝑡𝑗𝑝𝑜𝑂𝐼3 = 𝑂𝐼4

+ ∗ 𝑊 𝑒𝑓𝑥

𝑢𝑓𝑤𝑏𝑞𝑝𝑠𝑏𝑢𝑗𝑝𝑜 ∗ 𝐺𝑠𝑏𝑑𝑂𝐼3

(in μmol m-2 s-1)

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Verified in lab studies

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SLIDE 11

RMNP Dew Field Work

  • Dew collector w/

IC analysis

  • Dew meter to

monitor dew formation and evaporation

  • Picarro Cavity

Ringdown Analyzer to monitor gaseous NH3

  • Meteorological

measurements

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Dew meter based on Price and Clark (2014) Electronic balance with artificial turf surface

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SLIDE 12

Results – RMNP Dew Composition

Average FracNH3 = 0.94

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Wentworth et al., 2016

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SLIDE 13

Results – Dew and NH3

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Wentworth et al., 2016

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Results – NH3 in the Morning

Dew No Dew

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Wentworth et al., 2016

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SLIDE 15

Assuming a 150 m boundary layer…

  • ~Mass closure for NH3(g) lost to NH4

+ gained

  • NH4

+ (dew):NH3(BL) = 1.6 ± 0.7 at dawn

Results – NH3 Mass Closure

15

Wentworth et al., 2016

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Conclusions

  • 1. Ammonia is an abundant and dynamic beast
  • Gas-particle-partitioning
  • Bidirectional atmosphere-surface exchange
  • 2. Dew is an important temporary reservoir for ammonia
  • ~60% NH3 in RMNP BL goes to dew overnight
  • ~94% of dew NH4

+ is re-released as NH3 in RMNP

  • Dynamics are environment/dew composition dependent!

Implications for…

  • Other gases (acetic acid, formic acid, HONO, …)
  • Reduction in overnight NH3 dry deposition
  • Permanence of NH4

+ wet deposition…?

16

Caters News Agency

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SLIDE 17

Acknowledgments

17 http://www.fotocommunity.de/photo/the-light-pours-out-of-me- jens-kolk/3960881

– Katie Benedict and Yi Li, CSU – Greg Wentworth and Jen Murphy, Univ. of Toronto – Bret Schichtel and Tony Prenni, NPS

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SLIDE 18

Evidence of NH3 volatilization during rain evaporation…

  • Is this significant? Only in dry regions?
  • Does fractional loss decrease with larger rain events?

NH4

+ loss from wet deposition?

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SLIDE 19

NH4

+ % of wet

inorganic N dep

  • NO3
  • dominated

U.S. wet N dep in 70s and 80s

  • NH4

+ now

comprises > 50%

  • f wet inorganic

nitrogen deposition across most of the U.S.

Li et al., PNAS, 2016

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SLIDE 20

NH3 and NH4

+ Annual Timelines

0.0 0.2 0.4 0.6 0.8 1.0

Concentration (µmol/m3) NH3

Brush Loveland RMNP

RMNP

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6 4 2 NH3 (ppb) 12:00 AM 2015-06-25 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-26 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-27 6:00 AM 12:00 PM 6:00 PM 12:00 AM 2015-06-28 Time (local)

NH3 Morning Spike

Dew Evaporation? Wichink Kruit et al. (2007) Gong et al. (2011) Wentworth et al. (2014) Plant/Soil Emissions? Bash et al. (2010) Ellis et al. (2011) Traffic Emissions? Löflund et al. (2002) Nowak et al. (2006) Whitehead et al. (2007) Gong et al. (2011) Mixing Down? Walker et al. (2006)

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