IAPRS & SIS, Vol.34, Part 7, “Resource and Environmental Monitoring”, Hyderabad, India, 2002
STUDY AREA
The area selected for study is a part of Samastipur district of
Bihar occupying 86° 05’ to 86° 20° E longitude and 25° 40° to
25° 55’ N latitude. The study area is a part of Indo Gangetic
plain and is situated in the North of river Ganga.The area is
monotonously flat, the only diversities seen on the surface is
due to the action of rivers Gandak and Burhi Gandak. The
major constraints of the area are severe flooding and lack of
drainage network due to relatively flat terrain, clay and silty
soil. Thus, water spreads over the adjoining river area and
remains stagnant throughout the year. The water tolerant
capacity of surface and subsurface soil became saturated
resulting waterlogging in the area. The most important
characteristic feature of this region is formation of saucer
shaped black swamp landscape called “Tal”.
MATERIALS USED
Satellite Data:
Landsat TM — Kharif Season
Date of Pass — 27.10.1996
Path/Row — 140/42a
IRS IC LISS III — Rabi Season
Date of Pass — 04.03.1997
Path/Row — 105/53
Ancillary Data
a) Survey of India toposheets — No. 72K/1, K2, K5, K6 On
1:50,000 scales.
b) Watershed Atlas — Prepared by All India Soil Survey and
Land use Planning on 1:1,00,000 scale
c) Village Boundary Maps — From Population Census 1991
Since cloud free IRS data was not available for September
October hence Landsat TM data was used instead.
METHODOLOGY
Two-season satellite data available on CCT were loaded and
sub scene within which the study area falls were extracted. A
standard FCC was prepared by passing IR, Red and green to
Red, Green and Blue ranges respectively. Linear Contrast
stretch was performed on the data for optimum utilization of the
gray scales. The two sets of data were georeferenced to a
common base on 1:50,000 scale with a geographic co-ordinate
system and polyconic projection by selecting suitable Ground
Control Points both on image and reference map. The RMS
error was well within the limit (1/2 a pixel). The image was
resample to 23.5m pixel size. Image classification was done
using MLC. Waterlogged areas were easily identified by its
low reflectance value (DN value) and black-brown appearance
on satellite data. However, waterlogged covered with
vegetation showed deep brown-red color on standard False
Color Composite (FCC). Similar was the case with salt
affected land. The high reflectance of salt affected lands marks
a clear-cut separation with other categories of wastelands. Salt
affected lands were seen as white and bluish white tone with
fine texture. These were randomly distributed and were found
in patches along the streams. Scrublands were identified by
greenish blue tone and were in plenty in the study area.
Complete geographic database viz. administrative boundaries,
Cultural features like rail and road networks, drainage and
major settlements were generated using Arc/Info GIS software.
Since the village and watershed, boundaries were of concern in
the present study hence watershed boundaries and village
boundaries were marked as per the watershed atlas and village
census map respectively. Finally, the wasteland map was
intersected with villages and watersheds to get detailed village
and watershed wise area statistics. (Table-1 and Table-2).
RESULTS AND DISCUSSION
Since the prime objective of the present study was to delineate
and map the wastelands, which were compiled after the landuse
land cover classification. Among the eight Landuse classes
three were wastelands namely waterlogged, scrubland and Salt
affected land. The statistics pertaining to these classes is given
in Table 1. Table 2 and 3 show Village wise and Watershed
wise distribution of wastelands respectively.
Wastelands were extracted from the landuse/landcover map of
the area and statistics of each class was generated upto village
level for proper reclamation. Brief discussions of the
wasteland classes mapped under the two interpretation
techniques in the study area are given below.
Waterlogged land
The digital analysis showed an area of 6006 hectares, which is
nearly 18.20 % of the total study area. The results of
waterlogged area is mainly due to lack of drainage facilities
because of flat surface. In some of the waterlogged area, water
mud exists and area covered with weeds.
Waterlogged'weeds
These are those categories of land, which is permanently or
periodically inundated by water and is characterized by
vegetation which includes grasses and reeds. These appear as
dark colored patches on the FCC. These patches have been
found in close vicinity with rivers and cultivated fields.
However the statistics for these two categories have been have
been collectively calculated.
Scrub Land
Scrublands were scattered in the entire area in small patches.
The digital analysis showed area of 3256.94 hectares, which is
9.88% of the total study area.
Salt Affected Land
The digital analysis showed an area of 435.74 hectares, which
is about 11.32% of the total study area. The existence of salt-
affected land can be attributed to poor drainage facilities in the
area, which in turn, causes waterlogging and salt affected lands.
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