Item talk:Q246305
From geokb
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"name": "Modeling spatial and temporal variations in temperature and salinity during stratification and overturn in Dexter Pit Lake, Tuscarora, Nevada, USA",
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"abstract": "This paper examines the seasonal cycling of temperature and salinity in Dexter pit lake in arid northern Nevada, and describes an approach for modeling the physical processes that operate in such systems. The pit lake contains about 596,200\u00a0m3\u00a0of dilute, near neutral (pHs 6.7\u20139) water. Profiles of temperature, conductivity, and selected element concentrations were measured almost monthly during 1999 and 2000. In winter (January\u2013March), the pit lake was covered with ice and bottom water was warmer (5.3\u00a0\u00b0C) with higher total dissolved solids (0.298\u00a0g/L) than overlying water (3.96\u00a0\u00b0C and 0.241\u00a0g/L), suggesting inflow of warm (11.7\u00a0\u00b0C) groundwater with a higher conductivity than the lake (657 versus 126\u2013383\u00a0\u03bcS/cm). Seasonal surface inflow due to spring snowmelt resulted in lower conductivity in the surface water (232\u2013247\u00a0\u03bcS/cm) relative to deeper water (315\u2013318\u00a0\u03bcS/cm). The pit lake was thermally stratified from late spring through early fall, and the water column turned over in late November (2000) or early December (1999). The pit lake is a mixture of inflowing surface water and groundwater that has subsequently been evapoconcentrated in the arid environment. Linear relationships between conductivity and major and some minor (B, Li, Sr, and U) ions indicate conservative mixing for these elements.",
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