Title: Hyperspectral%20Environmental%20Monitoring%20of%20Waste%20Disposal%20Areas
1Hyperspectral Environmental Monitoring of Waste
Disposal Areas
- Jason Hamel
- Advisor Rolando Raqueño
- Digital Imaging and Remote Sensing Laboratory
- Chester F. Carlson Center for Imaging Science
- Rochester Institute of Technology
- Rochester, NY
2Overview
- Background
- Procedure/Results
- Spectra
- Classification
- Conclusions
3What are Landfills?
- Very common waste management technique
- They do not separate toxic wastes from the
environment - A water resistant clay cap is placed over the
landfill slows the spread of chemicals
4Clay Caps
Diagram of the material layers in the 2 major
clay cap technologies BGC.pdf for DOEs SRS
site
5Clay Cap Technology
- Caps are designed to last 40 years
- Replace with new technology that actually deals
with the waste - This lack of solution has given chemicals time to
leach into the environment - These problem areas must be found
6Why Look at Landfills?
- Currently, possible dangerous sites are manually
sampled and processed in a lab - This can be time and money consuming for larger
sites or a large number of sites - Chemicals are often dangerous even at very low
concentrations - Remote sensing with new hyperspectral detectors
may provide and economic alternative
7Example of Expected Imagery
Hyperspectral AVIRIS scene with 224 bands SRS
site
8Purpose of this Research
- Low concentrations make it very difficult to
directly detect a chemicals spectral signature - Determine if new hyperspectral sensors collect
enough information to identify materials - Determine the detectability of specific secondary
spectral effects of leachates (e.g.) - Vegetation health
- Soil water moisture
- Determine if atmospheric correction is necessary
9General Procedure
PROSPECT
Real Soil
Material Classification
OSP
SAM
SSM
Unmixing
Spectra
VEG S/U
Spectral Matching Algorithms
VEG/ Soil
Wavelength
Soil/ Soil
Atmosphere, Detectors, and Noise
Mix Spectra
10Vegetation Spectra
- PROSPECT leaf model and software
- Two varied inputs
- Chlorophyll concentration (mm/cm2)
- Equivalent water thickness (cm)
- Generated spectra
- Healthy leaf (high chlorophyll and water)
- Stressed leaf (low chlorophyll and water)
11Vegetation Spectra
Reflectance Spectra of Vegetation Green
Healthy Red Stressed
12Soil Spectra
- Ground measurements taken with spectrometer as
soil dried - Moisture in soil was not measured while spectra
was taken - Relative labels given to various spectra
- Wet Soil
- Moist Soil
- Dry Soil
13Soil Spectra
- Reflectance
- Spectra of Soil
- Brown Dry
- Orange Moist
- Black Wet
14Reflectance Data Set
- The 5 basic vegetation and soil spectra are mixed
by - This creates 10 additional mixed spectra
- 15 spectra in final data set
where R1 and R2 are 2 basic spectra
15Atmosphere and Detector Effects
- Light reflecting off material propagates through
atmosphere - Detector measures the radiance reaching the
detector at various narrow wavelength regions
called channels - Detector electronics record input signal in
digital counts (DC) - The hyperspectral AVIRIS detector has 224
channels from 400nm to 2500 nm
16Digital Count Spectral Data Set
- Radiance reaching the sensor, Lsen, calculated
from the Big Equation - Radiance variables supplied by MODTRAN
ES
Lu
LD
T1
T2
R
17Detector Effects
- All spectra converted to AVIRIS wavelength
regions - Lsen was multiplied at each wavelength by an
AVIRIS gain factor to calculate AVIRIS DCs
18AVIRIS Basic DC Spectra
19Realistic Data Set
- All detectors measure noise as well as signal
- Standard gaussian noise with standard deviation
of 1 added to DC spectra (not representative
AVIRIS noise value) - Noisy sensor radiance determined
- Noisy reflectance spectra calculated by removing
atmosphere effects
20Noisy Basic Reflectance Spectra
21Classification
- 6 classification algorithms used
- Linear Spectral Unmixing (ENVI)
- Orthogonal Subspace Projection (Coded)
- Spectral Angle Mapper (ENVI)
- Minimum Distance (ENVI)
- Binary Encoding (ENVI)
- Spectral Signature Matching (Coded)
- The 5 basic vegetation and soil spectra were used
as endmembers - Reflectance endmembers converted to DC before
classifying DC spectra
22Classification Algorithms
- Linear Spectral Unmixing (LSU)
- Generates maps of the fraction of each endmember
in a pixel - Orthogonal Subspace Projection (OSP)
- Suppresses background signatures and generates
fraction maps like the LSU algorithm - Spectral Angle Mapper (SAM)
- Treats a spectrum like a vector Finds angle
between spectra - Minimum Distance (MD)
- A simple Gaussian Maximum Likelihood algorithm
that does not use class probabilities - Binary Encoding (BE) and Spectral Signature
Matching (SSM) - Bit compare simple binary codes calculated from
spectra
23Classification Results
- The LSU and OSP fraction maps allow for the
calculation of sum of squared error
i endmember j wavelength
Sum of Square Errors Classifier Ground
Sensor DC Retrieved
Reflectance with Atmosphere Reflectance
LSU 4.81e-11 0.239
0.032 OSP 2.32e-6
0.237 0.038
24Classification Results
- The SAM, MD, BE, and SSM algorithms were not
designed to classify mixed pixels - Accuracy is the correct identification of one of
the fractions in a pixel
Percent Accuracy Classifier Ground Sensor
DC Retrieved
Reflectance with Atmosphere Reflectance
SAM 66.67 40.00
66.67 MD 66.67
80.00 66.67 BE
86.67 66.67 86.67
SSM 93.33 80.00
93.33
25Conclusions
- Atmosphere degrades performance of most of the
classification algorithms studied - Removal of the atmosphere is recommended
- The LSU and OSP fraction maps are more useful
- Provide very accurate material identification
without a large spectral library - Detects not just the material, but the amount of
material in a given pixel
26Follow Up Work
- There are many areas to expand on this research
- More realistic sensor noise
- Additional levels of vegetation health
- Broader range of atmospheres
- Incorporate background cloud effects
- Create a greater variety of mixed pixels
- Different percentages
- More than 2 materials
- Identification of actual secondary spectral
effects of leachates