remote sensing of eupatorium adenophorum spreng based on hj-a satellite data
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RESEARCH ARTICLE
Remote Sensing of Eupatorium Adenophorum Spreng Based
on HJ-A Satellite DataJun Chen & Wenting Quan & Kai Lu
Received: 24 October 2010 /Accepted: 25 May 2011 /Published online: 15 June 2011# Indian Society of Remote Sensing 2011
Abstract In the southwest of China, one of the
greatest threats to local ecosystem is the area
expansion of an invasive species, i.e., Eupatorium
adenophorum Spreng (EAS). In this study, the
remote-sensing technology was used to detect and
map the spatial distribution of EAS in Guizhou
Province, China. A series of vegetation indices,
including normalized difference vegetation index
(NDVI), simple ratio index (SRI) and atmospherically
resistant vegetation index (ARVI), were used to
identify EAS from HJ-A Chninese satellite data.According to the analysis results of fieldworks from
March 21 to 22, 2009, it was found that the vegetation
index of {1.9589SRI4.1095}{0.2359ARVI
0.5193} was the optimal remote-sensing parameter
for identifying EAS from HJ-A data. According to the
spatial distribution of EAS estimated from HJ-A data,
it was found that EAS was rather more in southwest of
Guizhou Province than in northeast. EAS became
sparse from southwest to northeast gradually, and the
central Guizhou Province was the ecological corridor
linking EAS in southwest to that in northeast. By
comparison with validated data collected by the
government of Guizhou Province, it was found that
the uncertainty of remote-sensing method was 18.52%,
29.31%, 8.77% and 9.46% in grassland, forest,
farmland and others respectively, and the mean
uncertainty was 13.29%. Owing to the lower heightof EAS than many plants in forest, the uncertainty of
EAS was the greatest in forest than that in grassland,
farmland and so on.
Keywords Remote sensing . Invasive species .
Eupatorium adenophorum Spreng
Introduction
Belonging to Asteraceae family, Eupatorium adenopho-rum Spreng (EAS) is mainly distributed in the tropical
and temperate zones of Central America (Sun et al.
2004). Owing to the superior endurance against various
environmental stresses, EAS has an advantage of
high ecological adaptation as well as an ability to
alter a natural ecosystem at an alarming rate (Wang
et al. 2007). In some fragile ecosystems, EAS is able
to change the biological diversity, alter the ecological
J Indian Soc Remote Sens (March 2012) 40(1):2936
DOI 10.1007/s12524-011-0133-z
J. Chen :K. LuThe key laboratory of marine hydrocarbon
resources and geology,
Qingdao 266071, China
J. Chen (*) :K. LuQingdao Institute of Marine Geosciences,
Qingdao 266071, China
e-mail: [email protected]
W. Quan
College of Resource Science and Technology,
Beijing Normal University,
Beijing 100875, China
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processes and services and even compete with other
native species. Additionally, EAS is a toxic species
causing serious damages to plants and animals
(Sharma et al. 1998; Katoch et al. 2000), e.g., the
foliage consumption by horses can lead to pulmonary
toxicity (OSullivan 1979); exposure of rats to feed
with the freeze-dried leaf powder of EAS may causehepatotoxicity (Ye 2001).
As its fruits introduced from Thailand to Yunnan
Province of China in 1940s (Xu and Wang 2004; Rymer
2008), EAS has dominated a large area of farmland,
national parks and forest land in Southeast China
during the past years (Ye 2001; Papes and Peterson
2003). If human beings still do nothing to solve this
problem, natural ecosystems may be replaced by a
monoculture of this invasive species. To effectively
prevent EAS spreading in Southeast China, compre-
hensive monitoring schemes for invasion detection arerequired. However, due to the lack of well-established
methods, EAS is rarely mapped on the large scale
spatial overview. Though providing accurate measure-
ments, traditional monitoring on EAS distribution is
costly, time consuming and often requires direct contact
with plants, which may result in further dispersal (Hestir
et al. 2008). Additionally, some land types are often
inaccessible or bring logistical difficulties to the field-
based monitoring methods. Satellite remote sensing
techniques may provide suitable tools to integrate
spectral data collected from traditional in situ measure-
ments. Since 1980s, with the improvement of sensor
spatial resolution, satellite remote sensing has been
widely used to monitor the spatial and temporal
changes of invasive plants in a large scale (Andrew
and Ustin 2008; Hestir et al. 2008).
The 4-channel HJ-A, a Peoples Republic of China
satellite launched on September 8, 2008, was selectedfor acquiring broad-band reflectance data by using the
following optical bands: blue-green (450520 nm),
green (520590 nm), red (630690 nm) and near
infrared (760900 nm). In this study, the HJ-A
satellite imageries were used to map the spatial
distribution of EAS. The main objectives of this
study were: (1) to develop the remote-sensing method
for identifying EAS from broad-band reflectance of
HJ-A satellite; (2) to extract EAS from HJ-A satellite
imageries; and (3) to use statistic data of field-based
reported in current literatures to access and validatethe accuracy of remote-sensing approach.
Materials and Methods
Study Area
Guizhou Province is the study area, located in Southeast
China (within 24372913N, 1033610935E) as a
representative region of EAS (Fig. 1). EAS has been
found in Guizhou Province since 1970s, of which the
Fig. 1 Study area
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distribution range has extended from 9 cities to 26
cities with an extension rate of 50 km/y from
southwest to northeast (Luo and Xiong 2005). Duringpast several years, EAS has resulted in considerable
economic losses in agriculture and forestry. At present,
Guizhou Province has become one of the regions with
severely endangered EAS in China (Lu et al. 2006).
Data Used
The dataset consisting of spectral data and 4-channel HJ-
A imageries was used to map the spatial distribution of
EAS in Guizhou Province in this study. Fieldworks were
carried out in Xichang City on March 21 and 22, 2009, inorder to measure and acquire spectral reflectance data of
typical terrestrial materials in Lu Mountain (2753N,
10214E) and Yuanjia Mountain (2748N, 10221E),
Xichang City (Fig. 1). The field observation involved the
acquisition of the following information: spectra and
coordinates of the observed sites. The spectral data was
shown in Fig. 2. At each observation point, spectral
measurements were recorded by a spectroradiometer
with a 25fore-optic, covering a spectral domain
(Analytic Spectral Devices, Boulder, Colorado) of 400
900 nm. ASD had a spectral resolution of 3 nm (full-
width at half maximum, FWHM) and a 1.4 nm sampling
interval across the spectral range of 400 nm900 nm
(ASD 1999). Maximum reflectance spectra were mea-sured from nadir at a height of 0.5 m above the material.
Measurements were performed within 2 h at local solar
noon on clear days to reduce the effect from changes in
solar angle. The 4-channel HJ-A data were acquired on
March 22, 2009, when the fieldworks were carried out.
The HJ-A data had a spatial resolution of 30 m. The data
strip covered most landscape of Guizhou Province,
China, except for its left boundary (the bad weather).
Vegetation Indices
More than 150 vegetation indices (VIs) have been
published in scientific literatures, but only a small
subset of them have a substantial biophysical basis
or has been systematically tested. The selection on
the most important vegetation categories and the
optimal representative indices within each category
was done by Asner et al. (2008). The oldest, the
most famous and the most frequently used VIs
included Normalized Difference Vegetation Index
(NDVI) (Rouse et al. 1973; Tucker 1979; Jackson
et al. 1983; Sellers 1985), Simple Ratio Index (SRI)
0
10
20
30
40
50
60
70
80
400 500 600 700 800 900
Wavelength (nm)
Reflectance
EAS EASEAS EASEAS EASEAS EASEAS EASEAS EASEAS EASTree canopy Tree canopyTree canopy PYF
COA BackgroundBackgroundBackground
BackgroundBackground
Fig. 2 Spectral data of
typical terrestrial materials
in Xichang City
Vegetation indices Formula Common range
NDVI NDVI RNIRRREDRNIRRRED 0.2 to 0.8
SRI SRIRNIR
RRED2 to 8
EVI EVI 2:5 RNIRRREDRNIR6RRED7:5RBLUE1
0.2 to 0.8
ARVI ARVI RNIR 2RREDRBLUE RNIR 2RREDRBLUE 0.2 to 0.8
Table 1 The commonly
using VIs
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(Rouse et al. 1973; Tucker 1979), Enhanced Vegeta-
tion Index (EVI) (Huete et al. 1997) and Atmospher-
ically Resistant Vegetation Index (ARVI) (Gitelson
and Merzlyak 1994; Kaufman and Tanre 1996; Sims
and Gamon 2002).
Due to the special absorption characteristics of
special plants at the near-infrared band, VIs are
usually designed for mapping the spatial distributionof plants species by using remote sensing approach
(Vogelmann et al. 1993). In this study, NDVI, SRI,
EVI and ARVI were used to construct the remote
sensing model for identifying EAS from HJ-A
satellite. Table 1 shows the equations and the common
green vegetation ranges of these four VIs. And then,
the focus of this study turned to finding out the
optimal threshold for these four VIs to detect EAS
from HJ-A satellite imageries.
Assessment Method for Selecting Optimal Parameters
It is assumed that
T X;Y 1
0
&VIMaxX VI
MinY
VIMinX VI
MaxY
< 0
VIMaxX VIMinY
VIMinX VI
MaxY
! 0
1
where, T(X,Y) is a parameter used to identify material
X from material Y; VIMaxX is the maximum VI of
material X; VIMinY is the minimum VI of material Y;
VIMinX is the minimum VI of material X; VIMaxY is the
maximum VI of material Y. According to Eq. (1), it is
found thatT(X,Y)=0 in case of the VI valued fields of
material Yintersected with that of material X, and T(X,
Y)=1 in case of the VI valued fields of material Y not
intersected with that of material X. Additionally, Eq.
(1) illuminates that it is possible to identify material X
from material Y by the values of VIs when T(X,Y)=1.
Conversely, it is difficult to identify material X from
material Y by the values of VIs if T(X,Y)=0.
In order to obtain optimal identification parameters
for EAS, the dividing degree of VIs, i.e., B(X,Y), was
used to illuminate the possibility that material Y
would be determined into material X.
B X;Y
VImaxX
VIminY
VIMaxX
VIMinX
VImax
Y
VImin
XVIMaxX
VIMinX
;whenVImaxX ! VI
minY
VImaxY > VImin
X
T X;Y 1
8>>>>>:
2
Results and Discussions
Atmospheric Correction
Atmospheric correction is an essential step in the
quantitative inversion of EAS based on remote
Table 2 NDVI
Sample size Minimum Maximum T B
EAS 15 0.3241 0.6086 /
Tree Canopy 3 0.6464 0.8372 1 13.29%
PYF 1 0.6113 0.6113 1 0.95%
COA 1 0.6686 0.6686 1 21.09%Background 4 0.1086 0.2287 1 33.53%
Table 3 SRI
Sample size Minimum Maximum T B
EAS 15 1.9589 4.1095 /
Tree Canopy 3 4.6554 11.281 1 25.38%
PYF 1 4.1456 4.1456 1 1.68%
COA 1 5.0341 5.0341 1 42.99%
Background 4 0.1086 0.2287 1 80.45%
Table 4 EVI
Sample size Minimum Maximum T B
EAS 15 0.7560 1.7826 /
Tree Canopy 3 1.7814 2.2919 0 /
PYF 1 1.7702 1.7702 0 /
COA 1 1.7972 1.7972 1 1.42%Background 4 0.1912 0.3552 1 39.04%
Table 5 ARVI
Sample size Minimum Maximum T B
EAS 15 0.2359 0.5193 /
Tree Canopy 3 0.5731 0.7990 1 18.98%
PYF 1 0.5396 0.5396 1 7.16%
COA 1 0.5953 0.5953 1 26.82%
Background 4 0.0964 0.0156 1 7 7.73%
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sensing data. In this study, the dark target
atmospheric correction algorithm was used to
remove atmospheric influences on HJ-A data. Dark
targets usually refer to thick vegetation canopy,
clear water and dark soil. The light exiting the
atmosphere can be strongly polarized due to
Rayleigh scattering with effect ignored, leading to
significant errors in estimating remote sensing
reflectance. During correcting the HJ-A for removalof Rayleigh and aerosol scattering, Rayleigh scat-
tering with multiple scattering and polarization
correction has been computed and put into lookup
tables for all possible solar and viewing geometries
under a standard pressure (1,013.02 mbar) (Hu
and Carder 2002). Once Rayleigh scattering is
known, the problem is how to estimate aerosol
scattering and atmospheric diffuse transmittance.
And then, the aerosol lookup table constructed by
Gordon and Wang (1994) is used to estimate the
aerosol scattering from the reflectance of dark target
collected by HJ-A imageries.
Remote Sensing Model for EAS Identifying
Tables 2, 3, 4, and 5 show NDVI, SRI, EVI and ARVI
of the fieldwork respectively. According to the data
shown in Tables 2, 3, 4 and 5, NDVI, SRI and ARVI
characteristics of EAS were greatly different from
other materials. The differences existed as follows: (1)
NDVI of EAS was ranged from 0.3241 to 0.6086,
while those of other materials were beyond this range;
(2) SRI of EAS was ranged from 1.9589 to 4.1095,
while those of other materials did not show such
characteristics; (3) ARVI of EAS was ranged from
0.2359 to 0.5193, completely different from those ofother materials; and (4) EVI of EAS was ranged from
0.7560 to 1.7826, which was partly overlapped with
those of other materials.
To successfully map the spatial distribution of EAS
from HJ-A data, the VI dataset, composed of the VIs
with the maximum B(X,Y) for single material, was used
to identify EAS from other terrestrial materials. Table 6
shows the optimal VI dataset constructed by this study.
Table 6 Optimal combination of VIs identified parameters
Y Tree
canopy
COA Background PYF
VIs SRI SRI SRI ARVI
B(EAS,Y) 25.38% 42.99% 80.45% 7.16%
Threshold 1.9589SRI
4.1095
0.2359ARVI
0.5193
(a) Spatial distribution of EAS denoted by ARVI (b) Spatial distribution of EAS denoted by ARVI
Fig. 3 Regions detected from the HJ-A satellite data as having found EAS invading accidents
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According to Table 6, it was found that the maximum
B(X,Y) was 25.38%, 42.99%, 80.45% and 7.16% for
tree canopy, COA, background and PYF respectively,
and the corresponding VIs were SRI and ARVI. By
comparison with the study results as shown in Tables 2,
3, 4 and 5, the optimal parameters for EAS identified
from HJ-A data can be defined as follows:
0:2359 SRI 0:5193f g \ 0:2359 ARVI 0:5193f g
3
Mapping Spatial Distribution of EAS from HJ-A
Satellite Data
Equation (3) was used to map EAS from HJ-A
satellite data. Figure 3 shows the spatial distribution
of EAS denoted by VI values of ARVI and SRI.
According to Fig. 3, it was found that EAS was rather
more in southwest Guizhou Province than that in
northeast. EAS became sparse from southwest to
northeast gradually, and the central Guizhou Province
was the ecological corridor linking EAS in southwest
to that in northeast. Due to the tremendous space and
time of EAS propagation, traditional approaches
based on fieldworks were incapable for revealing the
distribution pattern and the propagation rules in such
a large mapping scale. However, the study results
showed that it was potential to use the remote sensing
approach to solve this problem.
The colors of EAS flowers are white, and the seeds
are hidden at the bottom of the f lowers l ike
Taraxacum. During the florescence, the fruits can be
easily carried by the south-west monsoon from
southwest to northeast of Guizhou Province. With
the high ecological adaptation, EAS gradually invades
farmland, forest, and grassland from southwest to
northeast of Guizhou Province. Figure 4 shows the
landscape pattern of Guizhou Province, China.
According to Figs. 3 and 4, it was found that EAS
was widely distributed in farmland, forest, wetland
and so on. Owing to human disturbance, EAS in
farmland and grassland was rather less than that in
other regions. Because of the serious impact on the
biodiversity and stability of ecosystems, critical
habits, nutrient cycles and environmental qualities
Landuse type Grass land Forest land Farm land Others Total
Estimated by Field words 0.0027 0.1184 0.0775 0.4315 0.63
Estimated by Remote Sensing 0.0032 0.1531 0.0843 0.4731 0.7137
Estimation Errors 18.52% 29.31% 8.77% 9.64% 13.29%
Table 7 EAS cover fraction
in Guizhou Province, China
Fig. 4 Landscape in
Guizhou Province, China
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should not be ignored. It is necessary to pay more
attention on supervising and controlling the propa-
gation trend of EAS.
Accuracy Validation
The landscape patterns in Guizhou Province, China, aredivided into four different types-grassland, forestland,
farmland and others. The landscape characteristics of
Guizhou Province of China were collected by the
government of Guizhou Province, as shown in Fig. 4.
The cover fraction of EAS was collected from in situ
measurement conducted by statistical departments of
the county governments in Guizhou Province. The
fieldwork mainly involved the investigation of the
cover fraction of EAS in these four different landscape
types. Table 7 shows the cover fraction of EAS, which
was estimated from the fieldworks and the remotesensing approach respectively, as shown in Fig. 3.
According to Table 7, it was found that the uncertainty
of the remote sensing method was 18.52%, 29.31%,
8.77% and 9.46% in grassland, forest, farmland and
others respectively, and the mean uncertainty was
13.29%. In general, the height of EAS plant was no
more than 1 m, but lower than those of many plants in
forest. As a result, the uncertainty of remote sensing
approach was the greatest in forest than those in
grassland, farmland and so on.
Conclusions
The initial results of an exploratory project on remote
sensing of the invasive speciesEAS were reported
in this study. Broadband multi-spectral methods were
successfully applied to map EAS for representing the
unique life forms in the ecological environment they
invaded. The following conclusions were obtained
from investigations:
(1) EAS was generally different from those native
plants in terms of their reflectance, NDVI, SRI and
ARVI. According to the study results, it was found
that the optimal spatial distribution of EAS
extracted from the remote sensing data was
{1.9589SRI4.1095}{0.2359ARVI0.5193}.
(2) The HJ-A CCD imageries were successfully
used to map EAS for representing the unique
life forms in the ecological environment they
invade. The spatial distribution pattern of EAS
obtained from HJ-A data showed that EAS was
rather more in southwest Guizhou Province than
that in northeast. EAS became sparse from
southwest to northeast gradually and the central
Guizhou Province was the ecological corridor
linking EAS in southwest to that in northeast.(3) The uncertainty of the remote sensing method
was 18.52%, 29.31%, 8.77% and 9.46% in
grassland, forest, farmland and others respec-
tively, and the mean uncertainty was 13.29%.
Owing to the lower height of EAS than those of
many plants in forest, the uncertainty of EAS
was the greatest in forest than those in grassland,
farmland, and so on.
Acknowledgements This study is supported by the China
National Great Geological Survey (GZH200900504).
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