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Impact of Coal Mining on Vegetation: A Case Study in Jaintia Hills ...

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IMPACT OF COAL MINING ON VEGETATION: A CASE STUDY IN JAINTIA HILLS DISTRICT OF MEGHALAYA, INDIA1.5. Organisati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> the <strong>Study</strong>The present thesis <strong>on</strong> “<str<strong>on</strong>g>Impact</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> coal m<strong>in</strong><strong>in</strong>g <strong>on</strong> vegetati<strong>on</strong>: a case study <strong>in</strong> Ja<strong>in</strong>tia <strong>Hills</strong> district <str<strong>on</strong>g>of</str<strong>on</strong>g>Meghalaya, India” has been divided <strong>in</strong>to five chapters.1. Introducti<strong>on</strong>2. <strong>Study</strong> Area3. Materials and Methods4. Results and Discussi<strong>on</strong>5. General Discussi<strong>on</strong> and C<strong>on</strong>clusi<strong>on</strong>s1.6. Literature ReviewEcosystem disturbance may be def<strong>in</strong>ed as an event or series <str<strong>on</strong>g>of</str<strong>on</strong>g> events that alters the relati<strong>on</strong>ship <str<strong>on</strong>g>of</str<strong>on</strong>g>organisms and their habitat <strong>in</strong> time and space. Ecosystem disturbance by m<strong>in</strong><strong>in</strong>g is an evitable fall out<str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>in</strong>dustrializati<strong>on</strong> and modern civilizati<strong>on</strong>. With accelerat<strong>in</strong>g demand for fuel energy the world over,coal is certa<strong>in</strong>ly go<strong>in</strong>g to reta<strong>in</strong> its place <str<strong>on</strong>g>of</str<strong>on</strong>g> primacy well <strong>in</strong> to the future. <str<strong>on</strong>g>M<strong>in</strong><strong>in</strong>g</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> coal causesenormous damage to the flora, fauna, hydrological relati<strong>on</strong>s and soil biological systems. Destructi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g>the vegetal cover dur<strong>in</strong>g the m<strong>in</strong><strong>in</strong>g activity is <strong>in</strong>variably accompanied by an extensive damage andloss <str<strong>on</strong>g>of</str<strong>on</strong>g> the system. The disturbed and haphazardly mixed <strong>in</strong>fertile, c<strong>on</strong>solidated and unc<strong>on</strong>solidatedmaterials overly<strong>in</strong>g a coal seam are known as overburdens. These overburdens when dumped <strong>in</strong>unm<strong>in</strong>ed areas <strong>in</strong> the vic<strong>in</strong>ity <str<strong>on</strong>g>of</str<strong>on</strong>g> the coal m<strong>in</strong>es create m<strong>in</strong>e spoils. Nutrient deficient sandy spoils aregenerally hostile to plant growth and the regevetati<strong>on</strong> and reclamati<strong>on</strong> strategies other than naturalcol<strong>on</strong>izati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> m<strong>in</strong>e spoils are very tardy process. Some important researches <strong>on</strong> the study <str<strong>on</strong>g>of</str<strong>on</strong>g> theimpact <str<strong>on</strong>g>of</str<strong>on</strong>g> m<strong>in</strong><strong>in</strong>g <strong>on</strong> the vegetati<strong>on</strong> that relevant to the present study are be<strong>in</strong>g reviewed here.<str<strong>on</strong>g>Coal</str<strong>on</strong>g> m<strong>in</strong>e spoils when freshly tipped has a great range <str<strong>on</strong>g>of</str<strong>on</strong>g> particle size rang<strong>in</strong>g from large pieces <str<strong>on</strong>g>of</str<strong>on</strong>g>shale to silt and clay (Molyneux, 1963). These m<strong>in</strong>e spoils represent extremely rigid substrata for plantgrowth and development. Col<strong>on</strong>izati<strong>on</strong>, establishment and ma<strong>in</strong>tenance <str<strong>on</strong>g>of</str<strong>on</strong>g> vegetati<strong>on</strong> <strong>on</strong> these spoilsare enormously difficult. Am<strong>on</strong>g the factors which h<strong>in</strong>der the growth <str<strong>on</strong>g>of</str<strong>on</strong>g> plant species <strong>on</strong> these spoils,acidity merits special attenti<strong>on</strong>. Extreme acidity is caused due to the oxidati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> ir<strong>on</strong> pyrites(Chadwick, 1973). C<strong>on</strong>t<strong>in</strong>ued acidificati<strong>on</strong> for many years may lead to die back <str<strong>on</strong>g>of</str<strong>on</strong>g> well establishedvegetati<strong>on</strong> (Costigan et al., 1981). Besides acids, coal m<strong>in</strong>e spoils c<strong>on</strong>ta<strong>in</strong> toxic levels <str<strong>on</strong>g>of</str<strong>on</strong>g> solubleelements such as Fe, Al, Mn and Cu. The physical factors which limit plant establishment and survival<strong>in</strong>clude high temperature, moisture stress (Richards<strong>on</strong>, 1975), soil particle size (Down, 1974) andcompacti<strong>on</strong> (Hall, 1957, Richards<strong>on</strong>, 1975). Soil fertility is also a major factor regulat<strong>in</strong>g plant growth.The two limit<strong>in</strong>g nutrient <strong>on</strong> coal m<strong>in</strong>e spoils are nitrogen and phosphorus (William, 1975). Theshortage <str<strong>on</strong>g>of</str<strong>on</strong>g> organic matter is attributed to the absence <str<strong>on</strong>g>of</str<strong>on</strong>g> litter (Schafer et al., 1980). Power (1978)c<strong>on</strong>siders soil physico-chemical characteristics like texture, pH, electrical c<strong>on</strong>ductivity, soluble Ca,Mg, Na, B, cati<strong>on</strong> exchange capacity, exchangeable cati<strong>on</strong>s, gypsum and calcium carb<strong>on</strong>ateequivalents as be<strong>in</strong>g crucial to the predicti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> plant growth potential <str<strong>on</strong>g>of</str<strong>on</strong>g> m<strong>in</strong>e overburdens with waterhold<strong>in</strong>g capacity and <strong>in</strong>filtrati<strong>on</strong> rates as the other important variables. Bradshaw et al. (1975) and Belland Ungar (1981) found high temperature and low moisture <str<strong>on</strong>g>of</str<strong>on</strong>g> surface coal m<strong>in</strong>e spoils to be importantfactors limit<strong>in</strong>g plant growth.The col<strong>on</strong>izati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> plant species <strong>on</strong> coal m<strong>in</strong>e spoils is <strong>in</strong>fluenced by the particle size <str<strong>on</strong>g>of</str<strong>on</strong>g> the soilderived from the overburden and coal m<strong>in</strong>e wastes. This was c<strong>on</strong>clusively proved by Richards<strong>on</strong> et al.(1971). They reported that with high clay c<strong>on</strong>tent, the soils become water logged, whereas with high5

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