methane monitoring from small unmanned aerial systems · rmotc storage facility movie_a:wells....
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Methane Monitoring from Small Unmanned Aerial Systems
Lance E. Christensen, Vlad Manzatianu, Georgios Matheou Jet Propulsion Laboratory, The California Institute of Technology, Pasadena, CA
YangQuan Chen, Brendan Smith, Garrett John
Univ. of California – Merced, Merced, CA
California Methane Symposium Jun. 6-7, 2016
Point of contacts: Lance Christensen (JPL) [email protected] Carrie Greaney (PRCI) [email protected]
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Background
JPL-TLS
Mars
Required NASA investment in:
• Tunable laser spectrometers
• Semiconductor lasers
To get:
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Before OPLS sniffer
Wind sensor + IMU
GPS
After
Data visualization
First, need a robust, miniature methane sensing instrument.
Open-Path Laser Spectrometer (OPLS)
Background
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RMOTC Storage Facility
Movie_A:WellsChristensen_movies\sim_wells.mp4
100 wells, 10 m/s well-to-well, 30-s surveillance at each well →
40 wells per flight.
< 2.5 kg VTOL
Fixed-wings & Hybrid fixed-wing/VTOL
Vision: Pipeline & facilities
Types of operations: • Surveillance • Localization • Quantification
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Vision: Neighborhood sUAS leak survey
Prescriptive operation ≈ Autonomous operation
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Detector
Methane
water
Raw data 1.2 Hz
Res
pons
e tim
e Li
near
ity
Stab
ility
Performance
Inte
r-co
mpa
rison
s
1 m/s
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<2
16.5
4.5 m
10
1.9 SCFH
Data: Foot surveys Learn behavior and signature of plumes in suburban setting
57 m
3.3 SCFH
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sUAS: Logistics
3DR Iris at Merced grassland Lockheed Indago at dry Lakebed
and Caltech
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sUAS: Prop-wash
Region of Sensor Sensitivity
Flight test with smoke sensor
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sUAS: Flight Data
Movie_B: OrbitalChristensen_movies\orbit_20151105_backtraj.mp4
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sUAS: Horizontal
Merced Vernal Pools
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50 m away Λ = 7.7 m
280 m Λ = 11.5 m
Define characteristic length, λ, as a measure of data ‘sharpness’
sUAS: Horizontal
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sUAS: Vertical
Distribution Between 250-280 m
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Sunset
Vertical mixing during day
Hong and Pan, Monthly Weather Rev., 1996
Noo
n
Sun
set
σv = 30 m
x = 300 m
No surface Roughness
Gaussian concentration profile
sUAS: Vertical
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sUAS: Gaussian plume model insufficient
Georgios Matheou (JPL) 5 m/s, mid-lat, noon, 6 SCFH. Passive scalar. Thermals are < 10% of area
Convection
2-m LES Modeling - Convection - Surface topology
50 m
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Conclusions
● Flown OPLS on two different VTOLS < 2.5 kg · Demonstrated 20 ppb s-1 noise · 250 g OPLS · Expect plug-n-play system by end of 2016 ● Building knowledge on how to deploy sUAS-OPLS · Right now, VTOLS; 2nd half of 2016, Fixed-wings/hybrids · Folding in understanding from LES modeling - convection - topology · Performing surveillance, localization, quantification