Upload
others
View
5
Download
0
Embed Size (px)
Citation preview
Measurement of Ammonia Fluxes at a Cattle Feedlot Using Relaxed Eddy Accumulation
Patrick O’Keeffe
Shelley PressleyEugene AllwineBrian Lamb
Kris JohnsonJennifer MichalSarah Spogen
MotivationNH3 impacts:
• atmosphere - major contributor to secondary aerosol formation
• aquatic ecosystems - deposition can lead to eutrophication
Atmospheric NH3 Sources • livestock operations,
fertilizer/soils, wastewater treatment facilities, industrial sources, mobile sources
Ammonia in our air
Global budget for NH3
Source Amount Tg/yr
Agricultural (livestock, fertilizers, crops) 37.4 (65%)
Natural or biogenic (oceans, undisturbed soils, animals)
10.7 (19%)
Biomass burning 6.4 (11%)
Other (industrial, wastewater facilities, fossil fuel combustion, mobile sources)
3.1 (5%)
Total 57.6
Why at a feedlot?
• Recent requirements under EPA mandate all CAFO’s (>1000 hd) must report NH3 and H2S emissions under the Emergency Planning and Community Right to Know Act (EPCRA)
• Because no officially adopted emission factors are currently available to use for this purpose, the final rule allows reports to reflect “good faith estimates.” - users are provided a worksheet
Simple emission estimates using a worksheet
The field campaign
• Mid-sized cattle feedlot (30,000 head)
• Mid-west feedlot containing growing and finishing steers
• Measurements conducted during two weeks in spring– Cooler temperatures; periodic rainfall; dusty
• Techniques: relaxed eddy accumulation (REA), ultraviolet DOAS, horizontal profiling system and mobile van outfitted with various instruments
Measurement SiteInstrumentation
location
Mobile Vanroute
Feed Storage
Manure Compost
N
Predominant Winds (either SW or SE)
DOAS• Differential Optical Absorption Spectrometer
• NH3 concentrations measured via Beer’s law
Short path (110m)
line-averaged
200-240 nm wavelength
TGAPS• Trace Gas Analytical Profiling System
• N2O analyzed with GC-electron capture detector (ECD) technique• Same path as DOAS, time-averaged N2O concentrations• 7 inlets, runs continuously, 5 min avg. DOAS
Retro-reflectors
TGAPSSamplinglines
Mobile Van• Mobile Van
• Stationary or mobile sampling for• CO2, CH4, NH3, NO, NO2
• Mobile transects (line-averaging) or fixed time series
REA Relaxed Eddy Accumulation
TGAPS inlets
3D SonicAnemometerREA system
REA is a micrometeorological flux measurement technique, in this case used for NH3 flux measurements
REA Method• High frequency sampling of wind with time averaged
NH3 concentrations
• Up and down wind gusts are conditionally sampled through honeycomb denuders
• Denuders capture NH3 over 1 hr period and air volume sampled is known
• Colorimetric analysis used to determine NH3 conc.
• Fluxes calculated with mean ‘up’ and ‘down’ concentrations of NH3 and standard deviation of wind speed ( )−+ −= CCF wβσ
3D sonic Anemometer
CO2/H2O Analyzer
Thermo ScientificHoneycomb Denuders
REA NH3 system
Results
• REA NH3 Fluxes collected over 4 days
• Wind directions dictate which portion of the feedlot was sampled
• Footprint lengths important, primarily dependent on stability of the atmosphere
• Operational parameters also important –still working to incorporate this data
Run 11: evening E-SE winds
Light winds, evening time, temperatures ~20 C
NH3 flux = 105 µg/m2s
Run 13: mid-day, S-SW winds
higher winds, mid-day, temperatures ~25 C
NH3 flux = 253 µg/m2s
Run 14: mid-day, S-SW winds
Note – not to scale
Meterological Conditions - April 23
0
5
10
15
20
25
30
0:00 3:00 6:00 9:00 12:00 15:00 18:00 21:00
Tem
pera
ture
(C)
0
1
2
3
4
5
6
Win
d Sp
eed
(m/s
)temperaturewind speed
higher winds, mid-day, temperatures ~25 C
NH3 flux = 352 µg/m2s
Run 11
Runs 13-14
Summary• NH3 fluxes during warm spring conditions
averaged 142±87 µg/m2s
• Emissions were from an upwind fetch of ~100 m which typically encompassed 225 hd of 400 kg growing and finishing steers.
• Acknowledgements– USDA for research funding
– Jay Ham, Colorado State, for help developing REA
– CAFO’s for allowing us to make measurements
Future Work
• Further refine the REA results • Look at turbulence/atmospheric stability
parameters
• Calculate footprint size for each run
• Use WindTrax – atmospheric dispersion model• Determine NH3 fluxes using WindTrax and DOAS
for comparison with REA results
• Integrate results with other datasets (i.e. feedlot operations, additional measurements)