Limnology of two lake systems of Katmai National Park and Preserve, Alaska : Part II. Light penetration and Secchi depth

Seven large lakes in the Naknek River drainage and four in the Alagnak River drainage within the Katmai National Park and Preserve, Alaska, were surveyed once a summer during the period 1990-92 to determine baseline limnological conditions. All of the lakes are oligotrophic based on Secchi depth (SD...

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Veröffentlicht in:Hydrobiologia 2000-01, Vol.418 (1-3), p.209-216
Hauptverfasser: LAPERRIERE, J. D, EDMUNDSON, J. A
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description Seven large lakes in the Naknek River drainage and four in the Alagnak River drainage within the Katmai National Park and Preserve, Alaska, were surveyed once a summer during the period 1990-92 to determine baseline limnological conditions. All of the lakes are oligotrophic based on Secchi depth (SD) transparency and light penetration. Overall, SD transparency varied from 4.4 m to 17 m, the vertical light extinction coefficient (K^sub d^) ranged from 0.411 m^sup -1^ to 0.070 m^sup -1^ and the depth of 1% light penetration (I^sub 1%^) varied from 11 m to 67 m. However, because of greater light scattering, the percent of photosynthetic radiation (PAR) at SD was nearly twice as much in Battle Lake (30.4%) and Naknek Lake (32.8%), compared with the other nine lakes (mean 16%). Consequently, the ratio of I^sub 1%^ to SD was about 4 in these two lakes compared to a mean value of 2.6 for the other lakes. However, Battle Lake is a 'deep blue' calcium sulfate lake with little phytoplankton, whereas Naknek Lake contains some inorganic glacial flour and volcanic ash, as well as planktonic algae, but where sampled exhibits minimal turbidity. Biomass of planktonic algae (indexed by total chlorophyll concentration) explained most of the variation in SD (r^sup 2^=0.66), K^sub d^ (r^sup 2^=0.75), and I^sub 1%^ (r^sup 2^=0.85). In contrast, neither color nor turbidity were significant predictors of any optical variable. Considering all 11 lakes, there was a significant linear relationship between SD and both K^sub d^ (r^sup 2^=0.80) and I^sub 1%^ (r^sup 2^=0.72); however, most of the unaccounted for variation was attributed to Battle Lake and Naknek Lake. Although changes in water transparency are often linked to changes in algal biomass (chlorophyll), simple measures of SD transparency alone may not be appropriate for assessing whole-scale watershed or regional changes toward oligotrophication or eutrophication in lakes of the remote and pristine Katmai National Park and Preserve.[PUBLICATION ABSTRACT]
doi_str_mv 10.1023/A:1003990600537
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Light penetration and Secchi depth</title><source>SpringerLink Journals</source><creator>LAPERRIERE, J. D ; EDMUNDSON, J. A</creator><creatorcontrib>LAPERRIERE, J. D ; EDMUNDSON, J. A</creatorcontrib><description>Seven large lakes in the Naknek River drainage and four in the Alagnak River drainage within the Katmai National Park and Preserve, Alaska, were surveyed once a summer during the period 1990-92 to determine baseline limnological conditions. All of the lakes are oligotrophic based on Secchi depth (SD) transparency and light penetration. Overall, SD transparency varied from 4.4 m to 17 m, the vertical light extinction coefficient (K^sub d^) ranged from 0.411 m^sup -1^ to 0.070 m^sup -1^ and the depth of 1% light penetration (I^sub 1%^) varied from 11 m to 67 m. However, because of greater light scattering, the percent of photosynthetic radiation (PAR) at SD was nearly twice as much in Battle Lake (30.4%) and Naknek Lake (32.8%), compared with the other nine lakes (mean 16%). Consequently, the ratio of I^sub 1%^ to SD was about 4 in these two lakes compared to a mean value of 2.6 for the other lakes. However, Battle Lake is a 'deep blue' calcium sulfate lake with little phytoplankton, whereas Naknek Lake contains some inorganic glacial flour and volcanic ash, as well as planktonic algae, but where sampled exhibits minimal turbidity. Biomass of planktonic algae (indexed by total chlorophyll concentration) explained most of the variation in SD (r^sup 2^=0.66), K^sub d^ (r^sup 2^=0.75), and I^sub 1%^ (r^sup 2^=0.85). In contrast, neither color nor turbidity were significant predictors of any optical variable. Considering all 11 lakes, there was a significant linear relationship between SD and both K^sub d^ (r^sup 2^=0.80) and I^sub 1%^ (r^sup 2^=0.72); however, most of the unaccounted for variation was attributed to Battle Lake and Naknek Lake. 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D</creatorcontrib><creatorcontrib>EDMUNDSON, J. A</creatorcontrib><title>Limnology of two lake systems of Katmai National Park and Preserve, Alaska : Part II. Light penetration and Secchi depth</title><title>Hydrobiologia</title><description>Seven large lakes in the Naknek River drainage and four in the Alagnak River drainage within the Katmai National Park and Preserve, Alaska, were surveyed once a summer during the period 1990-92 to determine baseline limnological conditions. All of the lakes are oligotrophic based on Secchi depth (SD) transparency and light penetration. Overall, SD transparency varied from 4.4 m to 17 m, the vertical light extinction coefficient (K^sub d^) ranged from 0.411 m^sup -1^ to 0.070 m^sup -1^ and the depth of 1% light penetration (I^sub 1%^) varied from 11 m to 67 m. 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source SpringerLink Journals
subjects Algae
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Calcium sulfate
Chlorophyll
Eutrophication
Fresh water ecosystems
Freshwater
Fundamental and applied biological sciences. Psychology
Lakes
Light
Light penetration
Light scattering
Limnology
National parks
Phytoplankton
Rivers
Synecology
Transparency
Turbidity
USA, Alaska
Water depth
title Limnology of two lake systems of Katmai National Park and Preserve, Alaska : Part II. Light penetration and Secchi depth
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