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- W401484008 abstract "Big Soda Lake, Nevada, is a terminal, volcanic crater lake whose water level is maintained exclusively by groundwater. The crater is composed of volcanic, basaltic sand and the lake is ~60 m deep (Rush, 1972). The lake is meromictic with a distinct chemocline (Kimmel et al. 1978). The chemocline currently rests at ~40 m and is reflected in both specific conductivity and salinity measurements. Below the chemocline a redox gradient develops with highly reducing conditions. The pH is consistent throughout the depth of the lake at ~9.5, proving that it is alkaline in nature. It is further stratified by both a thermocline and oxycline. The existing conditions at Big Soda Lake make it the perfect setting for studying a diverse array of microbial activities and their interactions within a varying geochemical regime. Our goal was to perform an observational survey of Soda Lake to infer the inherent biogeochemical processes. The data collected by YSI displays how temperature, light, dissolved oxygen and specific conductive strong stratification. Coincident with the distinct chemocline at 40 m there is a dramatic increase in reducing potential. There is a rapid increase at the monimolimnion of cations, anions and nutrients. And reduced compounds ammonia, sulfides and nitrite." @default.
- W401484008 created "2016-06-24" @default.
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- W401484008 date "2010-01-01" @default.
- W401484008 modified "2023-09-27" @default.
- W401484008 title "Biogeochemical investigation of Soda Lake" @default.
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