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Titlebook: Low Carbon Energy Supply; Trends, Technology, Atul Sharma,Amritanshu Shukla,Lu Aye Book 2018 Springer Nature Singapore Pte Ltd. 2018 Alter

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ds is largely a product of the past 15 years and has paralleled the development of modern analytical techniques such as combined gas chromatography-mass spectrometry. Although the identification of optical and geometric isomers needs more study, much progress has already been made in relating sedime
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Atul Sharma,Amritanshu Shukla,Karunesh Kantland this is Levander’s (1900) classification of archipelago fringe rock pools of shores of the northern Baltic Sea. The first contribution to applied limnology is Häyrén’s (1921) saproby classification of the polluted brackish water area off Helsinki, based on plant communities. Freshwater contribu
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Mukul Sharma,Om Prakash,Atul Sharma,Anil Kumarcapacities oflakes, deterioration of water quality and fisheries management. It is thus important to consider limnological aspects when making decisions in the field of water management. To further this attitude the Finnish Limnological Society considered ‘Lakes and Water Management‘ to be a suitabl
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K. Rajarajeswari,B. Hemalatha,A. Sreekumarean drainage basin. Lake Buir gained an area by 10.43 km. during the last 50 years between 1965 and 2015. This increase in area may have been related to the recent slight rise of the annual precipitation with peaks in 1968–1974, 1987–1998, and 2002–2018 as observed in the lake basin. The regression
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Salwa Bouadila,Rim Ben Alilution of Eurasia because it is situated at the southern border of eastern Siberia under the influences of the East Asian winter monsoon and westerlies. The region is unique with the presence of the high Khuvsgulmountains, perennial permafrost, large tectonic depressions (e.g., Darkhad), large river
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Anirshu Dev Roy,Om Prakash,Anil Kumar,A. K. Kaviti,Anukul Pandey be used as primary data source.Introduces lacustrine landsc.This book provides an overview of lakes in Mongolia from scientific, economic and scenic points of view, presenting lake area changes, their sedimentological and geochemical characteristics, valuable economic and geoheritage resources and
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Renu Singhn depends on climatic conditions that can guarantee the amount of surface water will exceed evaporation in the same region. In contrast, wetlands are able to develop in very shallow relief (and even on plains) where incoming water becomes stagnant. One important reason to the present day existence o
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R. N. Singh,D. Ashaiers and lakes become saline or brackish, occasionally transforming their character. Further inland, saline lakes accumulate salt content by freshwater inflow and river discharge that carries minimal amounts of salt, and as a consequence salt concentrations increase in a basin (and a lake) through e
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