PICOPHYTOPLANKTON BIOMASS IN RELATION TO LAKE TROPHIC STATE AND THE TN:TP RATIO OF LAKE WATER IN JAPAN1

1994 ◽  
Vol 30 (3) ◽  
pp. 439-444 ◽  
Author(s):  
Noriko Takamura ◽  
Yukihiro Nojiri
2008 ◽  
Vol 8 ◽  
pp. 558-572 ◽  
Author(s):  
Yoshimasa Amano ◽  
Motoi Machida ◽  
Hideki Tatsumoto ◽  
Dennis George ◽  
Sharon Berk ◽  
...  

We evaluated the relationship between TN:TP ratio andMicrocystisgrowth via a database that includes worldwide lakes based on four types of lake origin (dammed, tectonic, coastal, and volcanic lakes). We used microcosm and mesocosm for the nutrient elution tests with lake water and four kinds of sediment (nontreated, MgO sprinkling treated, dissolved air flotation [DAF] treated, and combined treated sediment) in order to control TN:TP ratio and to suppressMicrocystisgrowth.Microcystisgrowth was related to TN:TP ratio, with the maximum value at an optimum TN:TP ratio and the minimum values when the TN:TP ratios reached to 0 or ∞. The kurtosis of the distribution curve varied with the type of lake origin; the lowest kurtosis was found in dammed lakes, while the highest was found in volcanic lakes. The lake trophic state could affect the change in the kurtosis, providing much lower kurtosis at eutrophic lakes (dammed lakes) than that at oligotrophic lakes (volcanic lakes). The relationship between TN:TP ratio andMicrocystisgrowth could be explained by the nutrient elution tests under controlled TN:TP ratios through the various sediment treatments. A significant suppression ofMicrocystisgrowth of 70% could be achieved when the TN:TP ratios exceeded 21. Lake origin could be regarded as an index including morphological and geographical factors, and controlling the trophic state in lakes. The origin rather than trophic state for lakes could be considered as an important factor of TN:TP influences on Microcystis growth.


1980 ◽  
Vol 37 (4) ◽  
pp. 640-646 ◽  
Author(s):  
R. P. Reid ◽  
C. H. Pharo ◽  
W. C. Barnes

Apatite is a common accessory mineral in the source rocks for the glacial debris supplying sediments to many Canadian lakes. A method has been developed which uses scanning electron microscopy and energy dispersive X-ray emission spectrometry for direct identification of apatite. This method has been used to examine the apatite content of various size fractions in Kamloops Lake sediments. Apatite concentrations obtained by this direct examination correlate well (r > 0.999) with apatite concentrations determined by chemical analyses and indicate that, in addition to comprising as much as 70% of the total phosphorus load, apatite may comprise as much as one-third of the "dissolved" (< 0.45 μm) inorganic phosphorus load. Consequently the use of classical (e.g. Vollenweider 1968; Vollenweider and Dillon 1974) methods of estimating lake trophic state from inorganic phosphorus concentrations in lake water must be done with care, recognizing that the bulk of inorganic phosphorus in lakes deriving sediment from glaciated igneous or metamorphic terrains may be in the form of apatite.Key words: apatite, lake, trophic state, phosphorus load, scanning electron microscopy


Hydrobiologia ◽  
1996 ◽  
Vol 319 (3) ◽  
pp. 213-223 ◽  
Author(s):  
Ray W. Drenner ◽  
J. Durward Smith ◽  
Stephen T. Threlkeld

1992 ◽  
Vol 1 (3) ◽  
pp. 173-197 ◽  
Author(s):  
Eugene B. Welch ◽  
Richard P. Barbiero ◽  
Debra Bouchard ◽  
Clain A. Jones

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