FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W50598887> ?p ?o ?g. }

• W50598887 abstract "The hydrology and water quality of Wind Lake-a recreational lake in a densely populated area of southeastern Wisconsin was studied from October 1, 1987 through September 30,1989. A drought in 1988 affected the hydrologic budget of Wind Lake in water years 1988-89. Precipitation was 5.9 inches less than normal in water year 1988 but was 2.3 inches greater than normal in water year 1989. Streamflows were near normal in water year 1988 and 25 percent less than normal in water year 1989 as indicated by data from a nearby streamflow-gaging station. Surface runoff was the dominant source of water to the lake in water year 1988 and 75 percent of the inflow was from Big Muskego Lake. The water level in Big Muskego Lake was 1.1 feet below the dam crest at the start of the 1989 water year because of the 1988 drought. About 2,510 acre-feet of water had to fill Big Muskego Lake before water could discharge to Wind Lake. In water year 1989, surface runoff was still the dominant source of water to the lake, but Big Muskego Lake only contributed 52 percent of the water inflow. Streamflow dominated the outflow budget for both years. In water year 1988, 88 percent of the outflow budget left by way of Wind Lake outlet and 12 percent evaporated from the lake surface. In water year 1989, 81 percent of the outflow budget left by way of Wind Lake outlet and 19 percent evaporated from the lake surface. On the basis of outflow from Wind Lake for water year 1988, the hydraulic residence time was 0.46 year; in water year 1989 it was 1.05 years. The total phosphorus input to Wind Lake from external sources was the same for both years, 3,160 pounds. The largest percentage of the phosphorus load came from Big Muskego Lake-- 70 percent in water year 1988 and 65 percent in water year 1989. Analysis of data by use of Vollenweider's model indicates that the phosphorus loadings for each year would cause eutrophic conditions. Data from a nearby gaging station indicate that phosphorus loading to Wind Lake was less than normal. Phosphorus retention in the lake is small and averages 14 percent of the incoming load for both years. Oxygen depletion occurs in the bottom waters during winter and summer months. A maximum anoxic zone was reached on July 18, 1988, when depths greater than 15 feet (about 21 percent of the lake bottom area) were anoxic. Total phosphorus concentrations at the lake surface for both years ranged from 11 to 78 micrograms per liter. Mean total phosphorus concentrations in June, July, and August that had averaged 49 micrograms per liter in 1985 through 1987 declined to 20 micrograms per liter in water year 1988 and 22 micrograms per liter in water year 1989. This reduction was related to the drought and reduced phosphorus loadings. Phosphorus concentrations 1.5 feet above the lake bottom increase during summer anoxic periods. The phosphorus concentration increased at a rate of 5.2 and 4.8 micrograms per liter per day for total and dissolved orthophosphate phosphorus. A maximum concentration of 760 micrograms per liter of total phosphorus and 650 micrograms per liter of dissolved orthophosphate phosphorus occurred on September 21, 1988, just before autumn turnover. Internal loading of phosphorus for the period October 15, 1987 through October 14, 1988, was estimated to be 2,890 pounds. This represents 48 percent of the combined internal and external total-phosphorus input of 5,960 pounds. Algal populations in water year 1988 ranged from 28,200 to 1,610,000 cells per milliliter. A total of 143 species were identified. Blue-green algae dominated the algal population and ranged from 56 percent (February 16, 1988) to 99 percent (five other sampling dates). Aphanocapsa delicatissima caused the largest algal bloom, which reached a maximum concentration of 934,000 cells per milliliter (September 7, 1988). Zooplankton populations in water year 1988 ranged from 52.5 to 686 organisms per liter. Eighteen species were identified. The cladoceran, Daphnia, dominated 12 of the 18 samples." @default.
• W50598887 created "2016-06-24" @default.
• W50598887 creator A5083226245 @default.
• W50598887 date "1993-01-01" @default.
• W50598887 modified "2023-09-26" @default.
• W50598887 title "Hydrology and water quality of Wind Lake in southeastern Wisconsin" @default.
• W50598887 cites W12428108 @default.
• W50598887 cites W142599993 @default.
• W50598887 cites W1510659591 @default.
• W50598887 cites W1869573013 @default.
• W50598887 cites W1967353470 @default.
• W50598887 cites W1972311421 @default.
• W50598887 cites W2064299399 @default.
• W50598887 cites W2084896680 @default.
• W50598887 cites W2273370527 @default.
• W50598887 cites W2908765440 @default.
• W50598887 doi "https://doi.org/10.3133/wri914107" @default.
• W50598887 hasPublicationYear "1993" @default.
• W50598887 type Work @default.
• W50598887 sameAs 50598887 @default.
• W50598887 citedByCount "1" @default.
• W50598887 crossrefType "report" @default.
• W50598887 hasAuthorship W50598887A5083226245 @default.
• W50598887 hasBestOaLocation W505988871 @default.
• W50598887 hasConcept C107054158 @default.
• W50598887 hasConcept C111368507 @default.
• W50598887 hasConcept C126645576 @default.
• W50598887 hasConcept C127313418 @default.
• W50598887 hasConcept C153294291 @default.
• W50598887 hasConcept C187320778 @default.
• W50598887 hasConcept C18903297 @default.
• W50598887 hasConcept C205649164 @default.
• W50598887 hasConcept C2776132308 @default.
• W50598887 hasConcept C2780797713 @default.
• W50598887 hasConcept C39432304 @default.
• W50598887 hasConcept C50477045 @default.
• W50598887 hasConcept C53739315 @default.
• W50598887 hasConcept C58640448 @default.
• W50598887 hasConcept C76886044 @default.
• W50598887 hasConcept C86132830 @default.
• W50598887 hasConcept C8625798 @default.
• W50598887 hasConcept C86803240 @default.
• W50598887 hasConcept C87717796 @default.
• W50598887 hasConceptScore W50598887C107054158 @default.
• W50598887 hasConceptScore W50598887C111368507 @default.
• W50598887 hasConceptScore W50598887C126645576 @default.
• W50598887 hasConceptScore W50598887C127313418 @default.
• W50598887 hasConceptScore W50598887C153294291 @default.
• W50598887 hasConceptScore W50598887C187320778 @default.
• W50598887 hasConceptScore W50598887C18903297 @default.
• W50598887 hasConceptScore W50598887C205649164 @default.
• W50598887 hasConceptScore W50598887C2776132308 @default.
• W50598887 hasConceptScore W50598887C2780797713 @default.
• W50598887 hasConceptScore W50598887C39432304 @default.
• W50598887 hasConceptScore W50598887C50477045 @default.
• W50598887 hasConceptScore W50598887C53739315 @default.
• W50598887 hasConceptScore W50598887C58640448 @default.
• W50598887 hasConceptScore W50598887C76886044 @default.
• W50598887 hasConceptScore W50598887C86132830 @default.
• W50598887 hasConceptScore W50598887C8625798 @default.
• W50598887 hasConceptScore W50598887C86803240 @default.
• W50598887 hasConceptScore W50598887C87717796 @default.
• W50598887 hasLocation W505988871 @default.
• W50598887 hasLocation W505988872 @default.
• W50598887 hasOpenAccess W50598887 @default.
• W50598887 hasPrimaryLocation W505988871 @default.
• W50598887 hasRelatedWork W1965193919 @default.
• W50598887 hasRelatedWork W2039023150 @default.
• W50598887 hasRelatedWork W2067490953 @default.
• W50598887 hasRelatedWork W2151185233 @default.
• W50598887 hasRelatedWork W2333685733 @default.
• W50598887 hasRelatedWork W2368868807 @default.
• W50598887 hasRelatedWork W2747372171 @default.
• W50598887 hasRelatedWork W2808172528 @default.
• W50598887 hasRelatedWork W2981013795 @default.
• W50598887 hasRelatedWork W3026564026 @default.
• W50598887 isParatext "false" @default.
• W50598887 isRetracted "false" @default.
• W50598887 magId "50598887" @default.
• W50598887 workType "report" @default.