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Report on Land Use /Vegetation Cover Mapping
of Singrauli Coalfield, NCL based on Remote Sensing Technique Year-2012-13
Submitted to COAL INDIA LIMITED
September 2012
Restricted
Contents Page No. Document Control Sheet ii List of Figures iii List of Tables iii List of Plates iii 1.0 Introduction 1 - 4
1.1 Project Reference 1.2 Project Background 1.3 Objectives 1.4 Location of the area and Accessibility 1.5 Physiography
2.0 Remote Sensing Concept & Methodology 5-17
2.1 Remote Sensing 2.2 Electromagnetic Spectrum 2.3 Scanning System 2.4 Data Source 2.5 Characteristics of Satellite/Sensor 2.6 Data Processing
2.6.1 Geometric Correction, rectification & geo-referencing 2.6.2 Image enhancement 2.6.3 Training set selection 2.6.4 Signature generation & classification 2.6.5 Creation / Overlay of vector database in GIS 2.6.6 Validation of classified image 2.6.7 Assessment of temporal changes
3.0 Land Use/ Vegetation Cover Monitoring 18-31
3.1 Introduction 3.2 Vegetation cover/ Land use Classification 3.3 Data Analysis & Change Detection 3.3.1 Vegetation Cover 3.3.2 Mining Area 3.3.3 Agricultural Land 3.3.4 Wasteland 3.3.5 Settlements
3.3.6 Water Bodies 3.3.7 Changes in Land Use/Vegetation Cover classes
4.0 Conclusion and Recommendations 33- 34
4.1 Conclusion 4.2 Recommendations
Document Control Sheet
(1) Job No. RSC/564607135
(2) Publication Date September 2012
(3) Number of Pages 34
(4) Number of Figures 12
(5) Number of Tables 9
(6) Number of Plates 2
(7) Title of Report Land Use/Vegetation Cover Mapping of Singrauli Coalfield, NCL. based on Remote Sensing Technique, Year 2012-13
(8) Aim of the Report To prepare Land Use/vegetation cover map on 1:50,000 scale for using Satellite Data of the year 2011 and assess the changes therein.
(9) Executing Unit Remote Sensing Cell, Geomatics Division, Central Mine Planning & Design Institute Limited, Gondwana Place, Kanke Road, Ranchi 834031
(10) User Agency Coal India Ltd (CIL), Kolkata and Northern Coalfields Ltd (NCL), Singrauli
(11) Authors Rajneesh Kumar, Sr Manager (RS)
(12) Security Restriction Restricted Circulation, for client use only
(13) No. of Copies CIL-3, NCL-3
(14) Distribution Statement Official
ii
List of Figures
1.1 Map of India showing Location of Singrauli Coalfield.
2.1 Remote Sensing Radiation System
2.2 Electromagnetic Spectrum
2.3 Expanded diagram of the visible and infrared regions (upper) and microwave
regions (lower) showing atmospheric windows.
2.4 Methodology for vegetation Cover mapping.
2.5 Geoid-Ellipsoid -Projection Relationship
3.1 Changes in vegetation cover Classes in Singrauli Coalfields during 2008 & 2011
3.2 Changes in Mining Areas in Singrauli Coalfields during 2008 & 2011
3.3 Changes in Agricultural Land in Singrauli Coalfields during 2008 & 2011
3.4 Changes in Waste Land in Singrauli Coalfields during 2008 & 2011
3.5 Changes in Built-up Land/Settlements in Singrauli Coalfields during 2008 & 2011
3.6 Changes in Waterbodies in Singrauli Coalfields during 2008 & 2011
3.7 Changes in Land Use/Vegetation Cover classes in Singrauli Coalfield during 2008 & 2011
List of Tables
2.1 Electromagnetic spectral regions
2.2 Characteristics of the satellite/sensor used in the present project work
3.1 Vegetation cover/land use classes identified in Singrauli Coalfield
3.2 Distribution of Vegetation Cover in Singrauli Coalfield During the year 2008 and
2011
3.3 Changes in Vegetation Cover in Singrauli Coalfield during the Year 2008 & 2011.
3.4 Changes in Mining Area in Singrauli Coalfield during the Year 2008 & 2011.
3.5 Changes in Agricultural Area in Singrauli Coalfield during the Year 2008 & 2011.
3.6 Changes in Wasteland in Singrauli Coalfield during the Year 2008 & 2011
3.7 Changes in Settlements in Singrauli Coalfield during the Year 2008 & 2011
iii
List of Plates
List of maps/plates prepared on a scale of 1:50,000 are given below:
1. Plate No. HQREMA101101: FCC of Singrauli Coalfield based on IRS –
Resourcesat 2, LISS IV data of May 2011
2. Plate No. HQREMA101103- Land Use/Vegetation Cover Map of Singrauli
Coalfield, NCL based on IRS – Resourcesat 2, LISS IV data of May 2011
iv
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Chapter 1
Introduction
1.1 Project Reference
HOD (WBP/Env/FP),Coal India Ltd issued a work order to CMPDI vide letter No
CIL/WBP/Env/2009/2428 dtd 29th December 2009 for monitoring of the status of
land reclamation in all major coalfields under CIL at an interval of every 3 years.
Accordingly Land Use/Vegetation Cover Mapping of Moher sub basin, Singrauli
coalfield of Northern Coalfields Ltd. Was carried out in the year 2008.
Subsequently, the present study was carried out at interval of three years based
on satellite data of the year 2011 to assess the regional impact of coal mining on
land use/vegetation cover in Singrauli Coalfield.
.
Project Background Northern coalfield Ltd. is an ISO 14001:1996 company, dedicated for maintaining
the ecological balance in the region, has initiated a massive plantation
programme on backfilled area, OB dumps and wasteland. The advent of high
resolution, multispectral satellite data has opened a new avenue in the field of
mapping and monitoring of vegetation cover. The present study has been taken
up to assess the changes in vegetation cover in Singrauli coalfield in a span of
last three years. While assessing the Land Use/ vegetation Cover in the coalfield,
changes in different categories Vegetation Cover are also analysed to formulate
the remedial measures, if any; required to be taken to maintain the ecological
balance in the region.
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1.3 Objectives
The objectives of the present study are:
- to prepare land use/vegetation cover map of Singrauli Coalfields on
1:50,000 scale based on Resourcesat/ LISS IV satellite data
- to assess the impact of coal mining on vegetation cover and analyse the
changes in span of last three years.
1.4 Location of the Area & Accessibility
The Singruali coalfield (Moher sub-basin) covers an area of about 300 sq km. it
is bounded by Lat 2407’ and 24012’N and Long 82030’ and 82052’E. The major
part of coalfield (about 220 sq km) lies in Singrauli district of Madhya Pradesh
and a small part (about 80 km) lies in Sonbhadra district of Uttar Pradesh.
Coalfield is connected by motorable road with Varanasi (220 km), Mirzapur (215
km), Rewa (206 km), Sidhi (100 km) and Satna (305 km). The nearest towns are
Waidhan (25 km) and Renukoot (50 km). The nearest railway station is Singrauli,
located on Chopan- Katni branch line which passes parallel to northern boundary
of the coalfield. The nearest railway station for going to Delhi and Ranchi is
Renukoot, which is on Garhwa-Chopan branch line. Nearest airstrip is at
Miyorpur (80 km) approachable by road from Singrauli. There is also a helipad at
Shaktinagar (20 km).
1.5 Physiography
Singrauli coalfield presents a typical erosional landscape with plain and plateau
topography. The general elevation above mean sea level varies from 280m on
the plain to over 500 m on plateau in steps alternating with three escarpment
faces which roughly correspond to the outcrop of the existing coal seams. The
plain country in the south and east has a gentle slope towards Govind Ballabh
Pant (GBP) Sagar reservoir. The important streams within this area are Baliya
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nala, Tippa Jahria nala, Bijul nala, Kachni and Mayar river. Bijul nala drains the
northern part of the plateau and joins Son river at Ghatihata near Chopan, while
southern part of the plateau is drained by number of streams which directly
discharge into Govind Ballabh Pant Sagar. Soil cover is very thin on the plateau.
Thick alluvial soil occurred in the valley which is loamy to sandy in nature. A map
of India showing the location of Singrauli Coalfield is given in Fig1.1.
.
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Fig 1.1 : Map of India Showing the Location of Singrauli Coalfields
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Chapter 2
Remote Sensing Concepts and Methodology
2.1 Remote Sensing
Remote sensing is the science and art of obtaining information about an object or
area through the analysis of
data acquired by a device
that is not in physical contact
with the object or area under
investigation. The term
remote sensing is
commonly restricted to
methods that employ electro-
magnetic energy (such as
light, heat and radio waves)
as the means of detecting
and measuring object
characteristics.
All physical objects on the
earth surface continuously
emit electromagnetic
radiation because of the
oscillations of their atomic
particles. Remote sensing is largely concerned with the measurement of electro-
magnetic energy from the SUN, which is reflected, scattered or emitted by the
objects on the surface of the earth. Figure 2.1 schematically illustrate the
generalised processes involved in electromagnetic remote sensing of the earth
resources.
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2.2 Electromagnetic Spectrum The electromagnetic (EM) spectrum is the continuum of energy that ranges from
meters to nanometres in wavelength and travels at the speed of light. Different
objects on the earth surface reflect different amounts of energy in various
wavelengths of the EM spectrum.
Figure 2.2 shows the electromagnetic spectrum, which is divided on the basis of
wavelength into different regions that are described in Table 2.1. The EM
spectrum ranges from the very short wavelengths of the gamma-ray region to the
long wavelengths of the radio region. The visible region (0.4-0.7µm wavelengths)
occupies only a small portion of the entire EM spectrum.
Energy reflected from the objects on the surface of the earth is recorded as a
function of wavelength. During daytime, the maximum amount of energy is
reflected at 0.5µm wavelengths, which corresponds to the green band of the
visible region, and is called the reflected energy peak (Figure 2.2). The earth also
radiates energy both day and night, with the maximum energy 9.7µm
wavelength. This radiant energy peak occurs in the thermal band of the IR region
(Figure 2.2).
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Table 2.1 Electromagnetic spectral regions Region Wavelength Remarks Gamma ray < 0.03 nm Incoming radiation is completely absorbed by the
upper atmosphere and is not available for remote sensing.
X-ray 0.03 to 3.00 nm Completely absorbed by atmosphere. Not employed in remote sensing.
Ultraviolet 0.03 to 0.40 µm Incoming wavelengths less than 0.3mm are completely absorbed by Ozone in the upper atmosphere.
Photographic UV band
0.30 to 0.40 µm Transmitted through atmosphere. Detectable with film and photo detectors, but atmospheric scattering is severe.
Visible 0.40 to 0.70 µm Imaged with film and photo detectors. Includes reflected energy peak of earth at 0.5mm.
Infrared 0.70 to 100.00 µm Interaction with matter varies with wavelength. Absorption bands separate atmospheric transmission windows.
Reflected IR band 0.70 to 3.00 µm Reflected solar radiation that contains no information about thermal properties of materials. The band from 0.7-0.9mm is detectable with film and is called the photographic IR band.
Thermal IR band 3.00 8.00
to to
5.0014.00
µm µm
Principal atmospheric windows in the thermal region. Images at these wavelengths are acquired by optical-mechanical scanners and special Videocon systems but not by film.
Microwave 0.10 to 30.00 cm Longer wavelengths can penetrate clouds, fog and rain. Images may be acquired in the active or passive mode.
Radar 0.10 to 30.00 cm Active form of microwave remote sensing. Radar images are acquired at various wavelength bands.
Radio > 30.00 cm Longest wavelength portion of electromagnetic spectrum. Some classified radars with very long wavelength operate in this region.
The earth's atmosphere absorbs energy in the gamma-ray, X-ray and most of the
ultraviolet (UV) region; therefore, these regions are not used for remote sensing. Details
of these regions are shown in Figure 2.3. The horizontal axes show wavelength on a
logarithmic scale; the vertical axes show percent atmospheric transmission of EM
energy. Wavelength regions with high transmission are called atmospheric windows and
are used to acquire remote sensing data. The major remote sensing records energy
only in the visible, infrared and micro-wave regions. Detection and measurement of the
recorded energy enables identification of surface objects (by their characteristic
wavelength patterns or spectral signatures), both from air-borne and space-borne
platforms.
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2.3 Scanning System
The sensing device in a remotely placed platform (aircraft/satellite) records EM
radiation using a scanning system. In scanning system, a sensor, with a narrow
field of view is employed; this sweeps across the terrain to produce an image.
The sensor receives electromagnetic energy radiated or reflected from the terrain
and converts them into signal that is recorded as numerical data. In a remote
sensing satellite, multiple arrays of linear sensors are used, with each array
recording simultaneously a separate band of EM energy. The array of sensors
employs a spectrometer to disperse the incoming energy into a spectrum.
Sensors (or detectors) are positioned to record specific wavelength bands of
energy. The information received by the sensor is suitably manipulated and
transported back to the ground receiving station. The data are reconstructed on
ground into digital images. The digital image data on magnetic/optical media
consist of picture elements arranged in regular rows and columns. The position
of any picture element, pixel, is determined on a x-y co-ordinate system. Each
pixel has a numeric value, called digital number (DN), which records the intensity
of electromagnetic energy measured for the ground resolution cell represented
by that pixel. The range of digital numbers in an image data is controlled by the
radiometric resolution of the satellite’s sensor system. The digital image data are
further processed to produce master images of the study area. By analysing the
digital data/imagery, digitally/visually, it is possible to detect, identify and classify
various objects and phenomenon on the earth surface.
Remote sensing technique provides an efficient, speedy and cost-effective
method for assessing the changes in vegetation cover certain period of time due
to its inherited capabilities of being multi-spectral, repetitive and synoptic aerial
coverage.
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2.4 Data Source
The following data are used in the present study:
Primary Data –Raw satellite data, obtained from National Remote Sensing
Centre (NRSC), Hyderabad, as follows, was used as primary data source for
the study.
IRS Resourcesat 2/ LISS IV; Band 2,3,4 Path # 102, Row # 055; Date of
pass 23.05.2011.
The detail specification of the data is also given in Table 2.2.
Secondary Data
Secondary (ancillary) and ground data constitute important baseline
information in remote sensing, as they improve the interpretation accuracy
and reliability of remotely sensed data by enabling verification of the
interpreted details and by supplementing it with the information that cannot be
obtained directly from the remotely sensed data.
2.5 Characteristics of Satellite/Sensor
The basic properties of a satellite’s sensor system can be summarised as:
(a) Spectral coverage/resolution, i.e., band locations/width; (b) spectral
dimensionality: number of bands; (c) radiometric resolution: quantisation;
(d) spatial resolution/instantaneous field of view or IFOV; and (e)
temporal resolution. Table 2.2 illustrates the basic properties of IRS-
Resourcesat 2 satellite/sensor that is used in the present study.
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Table 2.2 Characteristics of the satellite/sensor used in the present project work
Platform Sensor Spectral Bands in µm Radiometric Resolution
Spatial Resolution
Temporal Resolution
Country
IRS- Resourcesat 2
LISS-IV
B2 B3 B4
0.52 0.62 0.77
- - -
0.590.680.86
Green Red NIR
10-bit
5.8 m 5.8 m 5.8 m
5 days
India
NIR: Near Infra-Red
2.6 Data Processing The methodology for data processing carried out in the present study is shown in
Figure 2.4. The processing involves the following major steps:
(a) Geometric correction, rectification and geo-referencing;
(b) Image enhancement;
(c) Training set selection;
(d) Signature generation and classification;
(e) Creation/overlay of vector database;
(f) Validation of classified image;
(g) Layer wise theme extraction using GIS
(g) Final vegetation map preparation.
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Data Source Secondary Data Basic Data
IRS – Resourcesat 2 (LISS – IV)
Surface Plan (Scale 1:50,000)
Pre-processing, geometric correction, rectification & georefrencing
Creation of Vector Database (Drainage, Road network Railway network)
Image Enhancement
Training set Identification
Signature Generation
Pre-Field Classification
Validation through Ground Truthing
Final Land Use/ Vegetation Cover Map
Integration of Thematic Information using GIS
Report Preparation
Training Set Refinement
Pass
Fail
Geocoded FCC Generation
Fig 2.4 : Methodology for Land Use / Vegetation Cover Mapping
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2.6.1 Geometric correction, rectification and georeferencing
Inaccuracies in digital imagery may occur due to ‘systematic errors’ attributed to
earth curvature and rotation as well as ‘non-systematic errors’ attributed to
intermittent sensor malfunctions, etc. Systematic errors are corrected at the
satellite receiving station itself while non-systematic errors/ random errors are
corrected in pre-processing stage.
In spite of ‘System / Bulk correction’ carried out at supplier end; some residual
errors in respect of attitude attributes still remains even after correction.
Therefore, fine tuning is required for correcting the image geometrically using
ground control points (GCP).
Raw digital images contain geometric distortions, which make them unusable as
maps. A map is defined as a flat representation of part of the earth’s spheroidal
surface that should conform to an internationally accepted type of cartographic
projection, so that any measurements made on the map will be accurate with
those made on the ground. Any map has two basic characteristics: (a) scale and
(b) projection. While scale is the ratio between reduced depiction of geographical
features on a map and the geographical features in the real world, projection is
the method of transforming map information from a sphere (round Earth) to a flat
(map) sheet. Therefore, it is essential to transform the digital image data from a
generic co-ordinate system (i.e. from line and pixel co-ordinates) to a projected
co-ordinate system. In the present study geo-referencing was done with the help
of Survey of India (SoI) topo-sheets so that information from various sources can
be compared and integrated on a GIS platform, if required.
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An understanding of the basics of projection system is required before selecting
any transformation model. While maps are flat surfaces, Earth however is an
irregular sphere, slightly flattened at the poles and bulging at the Equator. Map
projections are systemic methods for “flattening the orange peel” in measurable
ways. When transferring the Earth and its irregularities onto the plane surface of
a map, the following three factors are involved: (a) geoid (b) ellipsoid and (c)
projection. Figure 2.5 illustrates the relationship between these three factors. The
geoid is the rendition of the irregular spheroidal shape of the Earth; here the
variations in gravity are taken into account. The observation made on the geoid is
then transferred to a regular geometric reference surface, the ellipsoid. Finally,
the geographical relationships of the ellipsoid (in 3-D form) are transformed into
the 2-D plane of a map by a transformation process called map projection. As
shown in Figure 2.5, the vast majority of projections are based upon cones,
cylinders and planes.
Fig 2.5 : Geoid – Ellipsoid – Projection Relationship
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In the present study, Polyconic projection along with Modified Everest
Ellipsoidal model was used so as to prepare the map compatible with the SoI
topo-sheets. Polyconic projection is used in SoI topo-sheets as it is best suited
for small-scale mapping and larger area as well as for areas with North-South
orientation (viz. India). Maps prepared using this projection is a compromise of
many properties; it is neither conformal perspective nor equal area. Distances,
areas and shapes are true only along central meridian. Distortion increases away
from central meridian. Image transformation from generic co-ordinate system to a
projected co-ordinate system was carried out using ERDAS Imagine 9.3 digital
image processing system.
2.6.2 Image enhancement
To improve the interpretability of the raw data, image enhancement is necessary.
Most of the digital image enhancement techniques are categorised as either
point or local operations. Point operations modify the value of each pixel in the
image data independently. However, local operations modify the value of each
pixel based on brightness value of neighbouring pixels. Contrast
manipulations/stretching technique based on local operation were applied on the
image data using ERDAS Imagine 9.3 s/w. The enhanced and geocoded FCC
(False colour composite) image of Singrauli Coalfield is shown in Plate No. 1 for
the year 2011.
2.6.3 Training set selection The image data were analysed based on the interpretation keys. These keys are
evolved from certain fundamental image-elements such as tone/colour, size,
shape, texture, pattern, location, association and shadow. Based on the image-
elements and other geo-technical elements like land form, drainage pattern and
physiography; training sets were selected/ identified for each land use/cover
class. Field survey was carried out by taking selective traverses in order to
collect the ground information (or reference data) so that training sets are
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selected accurately in the image. This was intended to serve as an aid for
classification. Based on the variability of land use/cover condition and terrain
characteristics and accessibility, 90 points were selected to generate the training
sets.
2.6.4 Signature generation and classification
Image classification was carried out using the minimum distance algorithm. The
classification proceeds through the following steps: (a) calculation of statistics
[i.e. signature generation] for the identified training areas, and (b) the decision
boundary of maximum probability based on the mean vector, variance,
covariance and correlation matrix of the pixels.
After evaluating the statistical parameters of the training sets, reliability test of
training sets was conducted by measuring the statistical separation between the
classes that resulted from computing divergence matrix. The overall accuracy of
the classification was finally assessed with reference to ground truth data. The
aerial extent of each land use class in the coalfield was determined using
ERDAS Imagine 9.3 s/w. The classified image for the year 2011 for Singrauli
Coalfield is shown in Drawing No. HQREMA11102.
2.6.5 Creation/overlay of vector database in GIS Plan showing leasehold areas of mining projects supplied by NCL are
superimposed on the image as vector layer in the GIS database. Road network,
rail network and drainage network are digitised on different vector layers in GIS
database. Layer wise theme extraction was carried out using ArcGIS s/w and
imported the same on GIS platform for further analysis.
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2.6.6 Validation of classified image Ground truth survey was carried out for validation of the interpreted results from
the study area. Based on the validation, classification accuracy matrix was
prepared.
The overall classification accuracy for the year 2011 was found to be 88.59%.
2.6.7 Assessment of temporal changes Change detection in Land Use/vegetation cover was carried out through GIS by
analysing the Land Use/ vegetation Cover map of the year 2008 and 2011. Final
Land Use/vegetation cover maps (on 1:50,000 scale) were printed using HP
Design jet 4500 Colour Plotter.
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Chapter 3
Land Use/ Vegetation Cover Monitoring
3.1 Introduction
The need for information on land use/ vegetation cover has gained importance
due to the all-round concern on environmental impact of mining. The information
on land use/cover inventory that includes spatial distribution, aerial extent,
location, rate and pattern of change of each category is of paramount importance
for assessing the impact of coal mining on vegetation cover. Remote sensing
data with its various spectral and spatial resolutions, offers comprehensive and
accurate information for mapping and monitoring of land use/cover over a period
of time. Since production from the mines are increasing and hence the mining
areas also keep on increasing, therefore it is has become very important to
reclaim the areas where the mining operations have been completed to reclaim
the surface of the earth to its original form along with the vegetation cover.
Realising the need of monitoring of land use/ vegetation cover and land
reclamation in Singrauli coalfield; CIL requested the services of CMPDI to
prepare land use/vegetation cover map of all coalfields at an interval of 3 years,
including Singrauli coalfield for assessing the impact of coal mining on land use
pattern and vegetation cover using remote sensing data. The first report in this
series was prepared in year 2008 to analyse the changes in land use/ vegetation
cover over the 3 year period. The data which emerged out of the 2008 analysis
was compared for temporal changes with the results of the study done earlier in
2005. Currently the findings of analysis of the data of year 2011 is now compared
for temporal changes with the results of the analysis of 2008, for the changes in
land use / vegetation cover during the 3 year interval. This will help in formulating
the mitigative measures, if any required for environmental protection in the coal
mining area.
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3.2 Land Use / Vegetation Cover Classification
The array of information available on land use/cover requires be arranging or
grouping under a suitable framework in order to facilitate the creation of
database. Further, to accommodate the changing land use/vegetation cover
pattern, it becomes essential to develop a standardised classification system that
is not only flexible in nomenclature and definition, but also capable of
incorporating information obtained from the satellite data and other different
sources.
The present framework of land use/cover classification has been primarily based
on the ‘Manual of Nationwide Land Use/ Land Cover Mapping Using Satellite
Imagery’ developed by National Remote Sensing Agency, Hyderabad, which has
further been modified by CMPDI for coal mining areas. Land use/vegetation
cover map was prepared on the basis of image interpretation carried out based
on the satellite data for the year 2011. Following land use/cover classes are
identified in the Singrauli coalfield region (Table 3.1).
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-
3.3Data Analysis & Change Detection Satellite data of the year 2011 was processed using ERDAS Imagine v.9.3 image
processing s/w in order to interpret the various land use and vegetation cover
classes present in the Singrauli coalfield. The analysis was carried out for entire
coalfield covering about 284 sq. km.
The area of each class was calculated and analysed using ERDAS Digital Image
Processing s/w and ArcGIS s/w. Analysis of land use / vegetation cover pattern in
Singrauli Coalfield and changes therein for the year 2008 and 2011 was carried
out, details are and shown in table 3.2.
Table 3.1 Land use / Vegetation Cover classes identified in Singrauli Coalfield
LEVEL –I LEVEL-II
1 Vegetation Cover
3.1 Dense Forest 3.2 Open Forest 3.3 Plantation under Social Forestry 3.4 Plantation on OB Dumps
2 Scrubs 3.1 Scrubs
2 Mining Area
5.1 Active Mining Area 5.2 Advance Quarry Site 5.3 Barren OB Dump 5.4 Barren Backfilled Area 5.5 Coal Dump 5.6 Water Filled Quarry
3 Agricultural Land 2.1 Crop Land 2.2 Fallow Land
4 Wasteland 4.1 Waste upland with/without scrubs 4.2 Fly Ash Pond
5 Settlements 1.1 Urban 1.2 Rural 1.3 Industrial
6 Water Bodies 6.1 River/Streams /Reservoir
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TABLE – 3.2 STATUS OF VEGETATION COVER & LANDUSE PATTERN IN SINGRAULI COALFIELD
DURING YEAR 2008 & 2011 Area in Sq km
Land Use Classes Year 2008 Year 2012 Change
Area % of total Area % of
total Area % of
total Reasons
VEGETATION COVER Dense forest 23.48 8.28 21.45 7.57 -2.03 -0.71 Mine advance in dip
side Open Forest 47.78 16.85 45.36 16.00 -2.42 -0.85 -do-
Total Forest 71.26 25.13 66.81 23.57 -4.45 -1.56 Social Forestry 41.91 14.78 42.90 15.13 0.99 0.35 Due to efforts of NCL
Plantation on OB Dump 28.94 10.21 29.84 10.53 0.90 0,32 Due to NCL efforts towards land reclamation
Total Plantation 70.85 25.00 72.74 25.66 1.89 0.66
Total Vegetation Cover 142.11 50.13 139.55 49.23 ‐2.56 ‐0.90 Due to rapid pace of coal mining
Scrubs 36.83 12.99 29.15 10.28 ‐7.68 ‐2.71
MINING AREA Coal Quarry 13.38 4.72 10.62 3.75 -2.76 -0.97 Due to backfilling
Barren Backfilled Area 12.71 4.48 21.27 7.50 8.56 3.02 Efforts of NCL towards Land reclamation
Coal Dump 0.32 0.11 0.42 0.15 0.10 0.04 Water Filled Quarry 1.24 0.44 1.60 0.56 0.36 0.12 Advance Quarry Site 6.17 2.18 5.54 1.95 -0.63 -0.23
Barren OB Dump 6.13 2.16 9.49 3.35 3.36 1.19 Due to high technical reclamation
Sub Total 39.95 14.09 48.94 17.26 8.99 3.17 AGRICULTURAL LAND Crop Land 8.86 3.13 8.58 3.03 -0.28 -0.10 Fallow Land 17.38 6.13 17.50 6.17 0.12 0.04
Sub Total 26.24 9.26 26.08 9.20 ‐0.16 ‐0.06 Due to industrialization
WASTELAND Wasteland 21.36 7.53 20.40 7.20 -0.96 -0.33 Fly-Ash Pond 0.29 0.10 0.06 0.02 -0.23 -0.08
Sub Total 21.65 7.64 20.46 7.22 ‐1.19 ‐0.42 Due to Mining & Industrialization
SETTLEMENTS Urban 12.24 4.32 14.87 5.25 2.63 0.93 Rural 0.84 0.30 1.09 0.38 0.25 0.08 Industrial 2.38 0.84 2.32 0.82 -0.06 -0.02
Sub Total 15.46 5.45 18.28 6.45 2.82 1.00 Due to industrialization
WATER BODIES 1.24 0.44 1.91 0.67 0.67 0.23 TOTAL 283.48 100.00 283.48 100.00 0.00 0.00
CMPDI
Job No 564607135 Chapter-3 Page 22
3.3.1 Vegetation Cover
Vegetation cover in the coalfield area has been found to be predominantly of five classes.
Dense Forest
Open Forest
Plantation on Over Burden(OB) Dumps / Backfilled area, and
Social Forestry
Scrubs have been put into a separate class.
There has been significant variation in the land use under the vegetation classes within
the area as shown below in Table 3.3.
TABLE – 3.3
Changes in Vegetation Cover in Singrauli Coalfield during the year 2008 & 2011
Dense forest – Forest having crown density of above 40% comes in this class. Dense
forest over the area has decreased, basically due advance of the mines on their dip sides
where there were forest areas such as Moher reserve forest etc. A total decrease in
dense forest is estimated to be 2.03 sq km, i.e. 0.71% of the coalfield area.
Open Forest – Forest having crown density between 10% to 40% comes under this
class. Open forest cover over the area has also reduced in the coalfield. There is some
Year 2008 Year 2011 Change Analysis
Vegetation Cover Area
(sq km)
% of total
Area
(sq km)% of total
Area
(sq km) % of total
Dense forest 23.48 8.28 21.45 7.57 -2.03 -0.71 Open Forest 47.78 16.85 45.36 16.00 -2.42 -0.85
Total Forest 71.26 25.13 66.81 23.57 -4.45 -1.56 Social Forestry 41.91 14.78 42.90 15.13 0.99 0.35 Plantation on OB Dump 28.94 10.21 29.84 10.53 0.90 0.32
Total Plantation 70.85 25.00 69.74 24.60 -1.11 -0.40 Scrubs 36.83 12.99 29.15 10.28 ‐7.68 ‐2.71
CMPDI
Job No 564607135 Chapter-3 Page 23
area line east to Block B, where the open forest has reduced due to mining activities.
Some of the reduction is also due to deforestation outside the mining areas. The total
decrease observed in open forest is 2.42 sq km, i.e. 0.85% of the coalfield area..
Social Forestry – Plantation which has been carried out on wastelands, along the
roadsides and colonies on green belt come under this category. Analysis of data reveals
that there is an increase of 0.99 sq km, which is 0.35% of the coalfield area.
Plantation over OB Dump and backfilled area – Analysis of the data reveals that NCL
has carried out massive plantation on OB dumps as well as backfilled areas during the
period for maintaining the ecological balance of the area. There is an increase of 0.90 sq
km, ie 0.32% of the coalfield area in respect to the year 2008.
Scrubs – Scrubs are vegetation with crown density less than 10%.Scrubs in the coalfield
has also decreased. This is because of advance of the mines in dip side and some scrubs
being converted into settlements.. There has been decrease of 7.68 sq km, ie 2.71% of
land with scrubs in the coalfield area.
It is significant to note that the vegetation cover in Singrauli Coalfield has decreased by
2.56 sq km which is about 0.90% % of the coalfield area. This decrease is mainly due to
advance of mine in Amlohri and Nigahi. Also significant depletion of forest is seen at
Krishnashila where the mining activity is progressing rapidly.
The variation in the vegetation classes which took place during year 2008 and 2011 within
the area are shown in bar diagram in Figure – 3.1.
Figures represent area in sq km
CMPDI
Job No 564607135 Chapter-3 Page 24
FIGURE - 3.1CHANGES IN VEGETATION COVER IN SINGRAULI COALFIELD DURING 2008 & 2011
23.48 21.45
47.7845.36
36.83
29.15
41.91 42.9
28.94 29.84
0
10
20
30
40
50
60
2008 2011
YEAR
AR
EA
(Sq
Km
)
Dense Forest
Open Forest
Scrubs
Social Forestry
Plantation on OBDump/backfilled area
3.3.2 Mining Area
The mining area was primarily been categorized as follows:
• Coal Quarry
• Advance Quarry Site, and
• Barren OB Dump
• Barren Backfilled Area
• Coal Dumps
• Water filled Quarry
The change in land use pattern in the mining area is shown in Table-3.4. Analysis of the
data reveals that the mining area which was 39.95 sq km in the year 2008 has increased
to 48.94 sq km in the year 2011. The increase of 8.99 sq km, i.e. 3.17% of the coalfield
area is primarily due to the increase in coal production.
CMPDI
Job No 564607135 Chapter-3 Page 25
TABLE – 3.4
Changes in Mining Area in Singrauli Coalfield during the year 2008 & 2011
Year 2008 Year 2011 Change Analysis
Mining Area Area
(sq km) % of total
Area
(sq km) % of total
Area
(sq km) % of total
Coal Quarry 13.38 4.72 10.62 3.75 -2.76 -0.97
Barren Backfilled Area 12.71 4.48 21.27 7.50 8.56 3.02
Coal Dump 0.32 0.11 0.42 0.15 0.10 0.04
Water Filled Quarry 1.24 0.44 1.60 0.56 0.36 0.12
Advance Quarry Site 6.17 2.18 5.54 1.95 -0.63 -0.23
Barren OB Dump 6.13 2.16 9.49 3.35 3.36 1.19
Sub Total 39.95 14.09 48.94 17.26 8.99 3.17
The variation in the Mining areas which took place during year 2008 and 2011 within the
coalfield area are shown in bar diagram in Figure – 3.2.
CMPDI
Job No 564607135 Chapter-3 Page 26
FIGURE - 3.2CHANGES IN MINING AREAS IN SINGRAULI COALFIELD DURING 2008 & 2011
13.38
10.6212.71
21.27
0.32 0.42
6.17 6.13
9.49
5.54
0
5
10
15
20
25
2008 2011YEAR
AREA
(Sq
Km)
Coal QuarryBarren Backfilled AreaCoal DumpAdv Quarry SiteBarren OB Dump
3.3.3 Agricultural Land
Land primarily used for farming and production of food, fibre and other commercial and
horticultural crops falls under this category. It includes crop land (irrigated and unirrigated)
and fallow land (land used for cultivation, but temporarily allowed to rest)
Total agricultural land which was 26.24 sq km in year 2008 has marginally decreased to
26.08 sq km in the year 2011. The reduction of 0.16 km (0.06%) in agricultural land in the
coalfield is due to development of infrastructure and residential complexes for mining
industry. The details are shown below in Table 3.5.
CMPDI
Job No 564607135 Chapter-3 Page 27
TABLE – 3.5
Changes in Agricultural Land in Singrauli Coalfield during the year 2008 & 2011
Year 2008 Year 2011
Change
Analysis
Agricultural
Land Area
(sq km) % of total
Area
(sq km) % of total
Area
(sq km) % of total
Crop Land 8.86 3.13 8.58 3.03 -0.28 -0.10
Fallow Land 17.38 6.13 17.50 6.17 0.12 0.04
Sub Total 26.24 9.26 26.08 9.20 ‐0.16 ‐0.06
The variation in the Agricultural Land which took place during year 2008 and 2011 within
the coalfield area are shown in bar diagram in Figure – 3.3.
FIGURE - 3.3CHANGES IN AGRICULTURAL LAND IN SINGRAULI COALFIELD DURING 2008 & 2011
8.86 8.58
17.38 17.5
02468
101214161820
2008 2011YEAR
AREA
(Sq
Km)
Crop LandFallow Land
CMPDI
Job No 564607135 Chapter-3 Page 28
3.3.4 Wasteland
Wasteland is degraded and unutilised class of land which is deteriorating on account of
natural causes or due to lack of appropriate water and soil management. Wasteland can
result from inherent/imposed constraints such as location, environment, chemical and
physical properties of the soil or financial or management constraints. There are two types
of wastelands predominant within the coalfield area, viz waste upland and fly ash pond.
There has been a slight reduction of 1.19 sq km, ie 0.42% of the coal field area. Some of
the waste lands have been converted in to vegetated areas due to social forestry. Some
wasteland has been converted to mining areas too.
The land use pattern within the area for waste lands is shown below in Table – 3.6.
TABLE – 3.6
Changes in Wastelands in Singrauli Coalfield during the year 2008 & 2011
Year 2008 Year 2011 Change
Analysis
Waste land Area
(sq km)
% of total
Area
(sq km)
% of total
Area
(sq km)
% of total
Wasteland with/without Scrubs
21.36 7.53 20.40 7.20 -0.96 -0.33
Fly Ash Pond 0.29 0.10 0.06 0.02 -0.23 -0.08
Sub Total 21.65 7.64 20.46 7.22 ‐1.19 ‐0.42
The variation in the Waste Land which took place during year 2008 and 2011 within the
coalfield area are shown in bar diagram in Figure – 3.4
CMPDI
Job No 564607135 Chapter-3 Page 29
FIGURE - 3.4CHANGES IN WASTE LAND IN SINGRAULI COALFIELD DURING 2008 & 2011
21.36 20.4
0.29 0.060
5
10
15
20
25
2008 2011
YEAR
AR
EA
(Sq
Km
)WastelandFlyAsh Pond
3.3.5 Settlements
All the man-made constructions covering the land surface are included under this
category. Built-up land has been further divided in to rural, urban and industrial
classes. In the present study, industrial settlement indicates only industrial
complexes excluding residential facilities.
The details of the land use under this category are shown in Table 3.7 as follows:
TABLE- 3.7.
CMPDI
Job No 564607135 Chapter-3 Page 30
Changes in Settlements in Singrauli Coalfields during the year 2008 & 2011
Year 2008 Year 2011 Change Analysis
Settlements Area
(sq km)
% of total
Area
(sq km)
% of total
Area
(sq km)
% of total
Urban 12.24 4.32 14.87 5.25 2.63 0.93
Rural 0.84 0.30 1.09 0.38 0.25 0.08
Industrial 2.38 0.84 2.32 0.82 -0.06 -0.02
Sub Total 15.46 5.45 18.28 6.45 2.82 1.00
It is observed that the settlements within the coalfield have grown by 2.82 sq km,
which is about 1.00% of the coalfield area. It is observed that the rural settlements
have been also grown marginally by 1.09 sq km which is 0.38% of the coalfield area.
The Urban settlement within the coalfield has grown by about 2.63 sq km, i.e.
0.93%. This increase is due to some population from rural areas shifting to urban
areas to seek livelihood in the mining areas. It may be noted that the major industrial
settlements, i.e. the thermal power plants in the area are out of the coalfield area.
The figure above represents only the industrial structures which are within the
coalfield area.
The variation in the Built-up Land/Settlements which took place during year 2008 and 2011
within the coalfield area are shown in bar diagram in Figure – 3.5
CMPDI
Job No 564607135 Chapter-3 Page 31
FIGURE - 3.5CHANGES IN BUILT-UP LAND IN SINGRAULI COALFIELD DURING 2008 & 2011
12.24
14.87
0.84 1.092.38 2.32
0
2
4
6
8
10
12
14
16
2008 2011YEAR
AREA
(Sq
Km)
Urban SettlementsRyral SettlementsIndustrial Settlements
3.3.6 Water bodies
It is the area of impounded water includes natural lakes, rivers/streams and man made
canal, reservoirs, tanks etc. The water bodies in the study area have been found to be
increased from 1.24 sq km in year 2008 (0.44%) to 1.91 sq km (0.67%) in 2011. The
variation in area under various water bodies within the coalfield area is shown in Bar
Diagram 3.6
FIGURE - 3.6CHANGES IN WATERBODIES IN SINGRAULI COALFIELD DURING 2008 & 2011
1.24
1.91
0
0.5
1
1.5
2
2.5
2008 2011
YEAR
AR
EA
(Sq
Km
) Waterbodies
CMPDI
Job No 564607135 Chapter-3 Page 32
142.11
70.85
39.95 26.24
21.65
15.46
1.24
139.55
72.74
48.94
26.08
20.46
18.28
1.91
0
20
40
60
80
100
120
140
160
2008
2011
3.3.7 Changes in Land Use/Vegetation Cover Classes
The overall variation in various Land Use /Cover classes in Moher sub-basin of Singrauli
Coalfield during the year 2008 and 2011 is shown in the Bar Chart below:
Year
Area (Sq km)
Fig 3.7 Overall Changes in Land Use/Cover Classes in Singrauli Coalfield in the Year 2008 & 2011 It can be seen from the chart above that there is a decrease in vegetation cover in the
coalfield area mainly because of deforestation in dip side of the mines where the mines
have advanced. However, the plantation carried out by NCL has increased in the 3 year
period. It can also be seen that there is significant increase in Mining areas which is due to
increase in coal production. Agricultural land has reduced marginally which may be due to
some agricultural land in dip side of mining has been used for mining activities. Wasteland
has also reduced marginally. This is also due to increase in mining activities. Settlements
have also increase which is due to more population coming for livelihood to mining areas.
CMPDI
Job No 564607135 Chapter-3 Page 33
Chapter 4
Conclusion & Recommendations
4.1 Conclusion
In the present study, land use/vegetation cover map of Singrauli coalfield (Moher
Sub-basin) is prepared based on IRS-Resourcesat 2/ LISS IV data of February
2011 in order to generate the database on vegetation cover and land use pattern to
detect the changes in respect to the year 2008 for effective natural resource
management and its planning. The Land use/vegetation cover analysis will help to
analyse and monitor the impact of mining and other industrial activities in the area.
Study reveals that vegetation cover has decreased by 2.56 sq km which is 0.90% of
the coalfield area in span of last 3 years. The major factor for decrease in vegetation
cover has been found to be loss of natural forests in the dip side where mines are
advancing. The plantations carried out under social forestry and on OB dumps and
backfilled areas have increased over this period. Social forestry has increased by
0.35% and plantation on OB dump and backfilled areas have increased by 0.32%.
the overall increase in plantation is 0.90% in the coalfield. Scrubs have been kept as
separate entity from the forests in line with the practice adopted by Forest Survey of
India (FSI). The Scrubs have decreased by 2.71 % in the coalfield area because of
the mine advancement. This shows that NCL’s afforestation programme is
progressing in an effective way. Study reveals that decrease in dense forest (-
2.03%) and open forests (-2.48%) is mostly due felling of forest to pave the way for
mine advance in the dip side.
Besides vegetation cover, other land use classes were also analysed and it was
observed that in span of 3 years mining area has increased from 39.95 sq km to
48.95 sq km. This increase of 8.99 sq km (3.17%) in mining area is due to rapid
increase in coal production.
CMPDI
Job No 564607135 Chapter-3 Page 34
Further study reveals that agricultural land in study area has marginally reduced
from 26.24 sq km to 26.08 sq km. This reduction of 0.16 sq km in agricultural land is
mainly due to its conversion in mining area. The area of wasteland has also
decreased very marginally from 21.65 sq km to 20.46 sq km during the last 3 years.
This reduction of 1.19 sq km is mainly due to conversion of wasteland into mining
and building the infrastructure. Area of settlement has increased from 15.46 sq km
to 18.28 sq km. this increase of 2.82 sq km in settlement area has taken place
mainly due to migration of rural population to urban mining settlements in the region
The detail change analysis is given under Table-3.2.
4.2 Recommendations
Keeping in view the sustainable development together with coal mining in the area,
it is recommended that;
a. To combat the effect of rapid mining and subsequent deforestation
associated with it, NCL should make the afforestation programme more
comprehensive to balance the ecological changes.
b. Efforts should be made to protect the vegetated dumps. Fresh dumping
should be avoided on the already stabilized and vegetated dumps.
c. Plantation should be avoided in dip side of the mine.
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NIGAHIAMLOHRIBINA
JAYANT
KAKRIBLOCK-B
Central Mine Planning & Design Institute Limited (A Subsidiary of Coal India Ltd)
Gondwana Place, Kanke Road, Ranchi - 834 031, Jharkhand, India Phone:(+91) 651 2231850/51/52/53 Fax:(+91) 651 2231447/2230826
Email: [email protected] ; website : www.cmpdi.co.in