Náttúrufræðingurinn

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Náttúrufræðingurinn - 1970, Qupperneq 53

Náttúrufræðingurinn - 1970, Qupperneq 53
N ÁTTÚR U F RÆÐING U RI N N 195 Barnes, H. og A. li. Folkard 1951. The determination of nitrites. Analyst 76: 599-603. Carpenter, ./. H. 1960. New measurements of oxygen solubility in pure and natural water. Limnol. Oceanogr. 11:264-277. Hutchinson, G. E. 1957. A treatise on Limnolog)'. Vol. I. Geography, Physics and Chemistry. Jolin Wiley & Sons Inc. New York. Lamby, Karljosef 1941: Zur Fischereibiologie des Mývatn, Nord Island. Zeit- schrift f. Fischerei und Hilfswissenschaften, XXXIX, 5:749-805. Mullin, J. B. og J. P. lliley 1955. The colorimetric determination of silicate with special reference to sea and natural waters. Anal. Chirn. Acta 12: 162-176. Mullin, J. B. og J. P. Riley 1955 a. The spectrophotometric determination of nitrate in natural waters with particular reference to sea water. Anal. Chim. Acta /2:464-480. Murphy, J. og /. P. Riley 1962. Modified single solution method for the de- termination of pliosphate in natural waters. Anal. Chint. Acta 27(l):31-36. Ostenfeld, C. H. og Wesenberg-Lund 1906. A Regular Fortnightly Exploration of the Plankton of two Icelandic Lakes, Thingvallavatn and Mývatn. Pro- ceed. of the Roy. Soc. of Edinburgh, Session 1904—1905. XXV. Part 12: 1092-1167. Poulsen, E. M. 1924. Islandske Ferskvandsentomostraker. Vidensk. Meddel. fra Dansk naturhistorisk Forening i K0benhavn, 75:81-141. Richards, F. A. og R. A. Kletch 1964. The spectrophotometric determination of ammonia and labile amino compounds in fresh and seawater by oxidation to nitrite. Ken Sugawara Festival Volume, 65-81. Maruzen Com- pany Ltd. Tokyo. Strickland, J. D. H. og T. R. Parsons 1968. A practical handhook of seawater analysis. Fisheries Res. Board of Canada, Bull. No. 167. Ottawa. S U M M A R Y Chemical Observations in Lake Mývatn June 26—27, 1969 by Unnsleinn Stefánsson, Marine Research Institute, Reykjavík. Mývatn is considered one of the most productive lakes in Iceland. Biological- ly it is of enormous interest. The main sources of inflow are Grænilækur, a river entering the southern part ol' the lake, and warm and cold springs drain- ing into the eastern part. The outflow takes place at the westernmost part through Geirastaðakvísl into the river Laxá. In late June 1969 chemical observations were carricd out at 14 different
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