Studying the processes of transport and transformation of lignosulfonates in Onega Lake water

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Author(s):  
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N. E. Kulakova

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Vol 18 (1) ◽  
pp. 107-115 ◽  
Author(s):  
Kwang-Hee Lee ◽  
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Min-Ho Kim ◽  
Nam-Woo An ◽  
Chul-hwi Park


Reproduction ◽  
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Vol 31 (3) ◽  
pp. 506-507 ◽  
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T. Cooper ◽  
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Vol 3 (4) ◽  
pp. 448-450 ◽  
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Vol 50 (6) ◽  
pp. 32-40
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Yu. A. Shustov ◽  
I. A. Tyrkin ◽  
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Author(s):  
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N. John Anderson

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Brodersen, K. P., & Anderson, N. J. (2000). Subfossil insect remains (Chironomidae) and lake-water temperature inference in the Sisimiut–Kangerlussuaq region, southern West Greenland. Geology of Greenland Survey Bulletin, 186, 78-82. https://doi.org/10.34194/ggub.v186.5219 _______________ Climate and water temperature have an important influence on the functioning of lake ecosystems. From limnological and palaeolimnological studies of lakes, information on biological diversity and climate variability in time and space can be gleaned from physical, chemical and biological indicators preserved in the lake sediments. The lakes in southern West Greenland are particularly useful for this purpose – they are numerous, diverse and have minimal anthropogenic impact (Anderson & Bennike 1997). Palaeolimnological data are fundamental for understanding the functioning and development of modern lakes and for understanding the causes of climatic change as well as the effect on lake biota.





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