Название: Sustainable Development Practices Using Geoinformatics
Автор: Группа авторов
Издательство: John Wiley & Sons Limited
Жанр: Экономика
isbn: 9781119687122
isbn:
2.2 Study Area
The study area comprising 381 km2 in the Survey of India (SOI) topographical sheet no. 73 E/6, on a scale of 1:50,000, is situated in Ramgarh and Hazaribagh district of Jharkhand (Figure 2.1). It lies between longitude 85° 15’ to 85° 27’ and latitude 23° 35’ to 23° 44’ at an altitude of 348 m above mean sea level (MSL). The South Karanpura coalfield forms an elongated strip along the Chingara fault. It occupies different formations of the Lower Gondwana system such as Talchir, Karharbari, Barakar, Barren Measure, and Raniganj Formation that overlie with the Precambrian basement. The Coalfield considerably recognized for its excellent quality non-coking coal used by various industries such as power station, steel, cement, fertilizer, bricks-manufacturing, and many other medium and small-scale industries. The general climate of the area is tropical with maximum temperatures between 40°C and 2°C. The area receives an average rainfall between 1,102 mm and 1472 mm with significant seasonal variation. From November to the middle of February, there is the occasional cold weather, which follows rain. The Damodar River drains the area with the Nalkari River as its chief tributary. The main urban settlements in the area are Patratu, Bhurkunda, Barkakana, Saunda, Gidi, Lapanga, Dari, and Simratanr. Patratu is the leading industrial town, and it is well known for coal mining activity and thermal power. Various other medium and small-scale industries also present here are responsible for the degradation of air quality and land degradation in the area.
Figure 2.1 Location map of the study area showing village boundaries along with water bodies and coal mining areas.
2.3 Methodology and Data Used
In the present study, a satellite image of Landsat TM (pertaining to year 2011) was used for the preparation of LU/LC map. The Landsat Thematic Mapper (TM) data was downloaded from the website of the United States Geological Survey (USGS) (http://glovis.usgs.gov). The topographical map pertaining to sheet number 73 E/6 provides the details of the study area and was obtained from the SOI on 1:50,000 scale for ground reference. Visual interpretation techniques were used for delineating and mapping of LU/LC classes of the study area. Categorization of various LU/LC classes such as built-up land (urban/rural), industrial settlement, cropland/fallow land, forest, wasteland, water body within coal mine, water body/river/reservoir, and coal mining area are envisaged based on classification scheme developed by National Remote Sensing Agency (NRSA) [24]. The minor modification in the categories at Level-II is done because of coal mining activity in the area. Further, the hazard rating (1 to 4) was assigned in each LU/LC class based on their relative influence toward inducing geo-environmental hazards.
Aerosol optical depth (AOD), also called aerosol optical thickness (AOT), PWV, and ambient temperature were simultaneously measured using MICROTOPS-II Sunphotometer instrument during January 2011. The Sunphotometer has five accurately aligned optical collimators, viz., 340, 500, 870, 936, and 1,020 nm with a full field view of 2.5° [25]. The finer wavelength, i.e., 340 nm was used to assess the status of atmospheric pollution in and around the coal mining area. The observation revealed considerable variation in AOT at the wavelength of 340 nm. The PWV is estimated from the measurements of solar intensity at 936 and 1020 nm. Ambient temperature was measured during day time to assess the vulnerability condition over industrial, mining, urban and forest area. The inverse distance weightage (IDW) technique was used to interpolate the AOT, PWV, and temperature concentration over the study area. This technique applies the spatial correlation of variables and based on observed values predicts the variables at unobserved locations [26].
For the preparation of the geo-environmental index model, each subclass of indicator maps assigns a numerical rating within a scale of 1–4 according to their relative influence of hazard proneness. Finally, a composite geo-environmental hazard map was prepared by the addition of the entire ratings assigned to different hazard inducing factor maps and divided by total number of parameters in GIS environment. For each of the above four geo-environmental hazard indicators, four classes of hazard such as low, moderate, high, and very high were defined. The composite geo-environmental hazard index (GHI) of the integrated layers is calculated by using the following formula:
Where AOT(340 nm)r represents ratings assigned to AOT; PWVr represents ratings assigned to PWV concentration in the winter season; Tr,represents the ratings assigned to temperature in the winter season; LULCr represents ratings assigned to LU/LC map; and n represents the number of indicators.
Census data of the year 2011 were used for computation of village-wise socio-economic indicators of PD, workers, literacy rate, and children below ages 0–6 years. Numerical ratings within a scale of 1 to 4 were assigned to each indicator class according to their assumed vulnerability to geo-environmental hazards. A composite vulnerability map was generated by integrating the village level thematic maps of all socio-economic indicators and divided by total numbers. For the socio-economic vulnerability map, four classes of vulnerability such as low, moderate, high, and very high were defined. The composite socio-economic vulnerability index (SVI) of the integrated layers is calculated by using the following formula:
where PDr represents the ratings assigned to population density; TWr represents ratings assigned to total worker density; CAGr represents ratings assigned to the population of children in the age group 0–6 years; LRr represents ratings assigned to percentage population of literacy rate; and n represents the number of indicators.
Risk is the probability of adverse consequences or expected losses resulting from interactions between hazards and vulnerable conditions [20, 27, 28]. The final coal mining risk index (CMRI) is prepared by multiplication of both GHI and SVI in the GIS domain using the following formula:
where CMRI represents coal mining risk index; GHI represents village level geo-environmental hazard index; and SVI represents the village level socio-economic vulnerability index.
All thematic layers were converted into a raster format, maintaining the same resolution (30 m) and coordinate system before they are taken into the GIS environment. The software, ArcGIS (version 10.5) and ERDAS Imagine (version 2015) were, respectively, used for GIS analysis and image processing in the digital framework. The details of the overall methodology adopted for the present study are depicted in Figure 2.2.