Abstract
An optics theory-based mechanistic model for Secchi disk depth (Z SD) is advanced, tested, and applied for Cayuga Lake, NY. Robust data sets supported the initiative, including for (1) Z SD, (2) multiple light attenuation metrics, most importantly the beam attenuation (c) and particulate scattering (b p) coefficients, and (3) measures of constituents responsible for contributions to b p by phytoplankton (b o) and minerogenic particles (b m). The model features two serially connected links. The first link supports predictions of b p from those for b o and b m. The second link provides predictions of Z SD based on those for b p, utilizing an earlier optical theory radiative transfer equation. Recent advancements in mechanistically strong estimates of b m, empirical estimates of b o, and more widely available bulk measurements of c and b p have enabled a transformation from a theory-based conceptual to this implementable Z SD model for lacustrine waters. The successfully tested model was applied to quantify the contributions of phytoplankton biomass, and minerogenic particle groups, such as terrigenous clay minerals and autochthonously produced calcite, to recent b p and Z SD levels and dynamics. Moreover, it has utility for integration as a submodel into larger water quality models to upgrade their predictive capabilities for Z SD.
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Acknowledgments
Funding for portions of this study was provided, in part, by Cornell University, a grant on aquatic optics from NASA (award NNX14AB80G), and the Upstate Freshwater Institute (UFI). The program of sampling and field and laboratory measurements was conducted by UFI. This is contribution number 337 of the Upstate Freshwater Institute.
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Effler, S.W., Strait, C., O’Donnell, D.M. et al. A Mechanistic Model for Secchi Disk Depth, Driven by Light Scattering Constituents. Water Air Soil Pollut 228, 153 (2017). https://doi.org/10.1007/s11270-017-3323-7
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DOI: https://doi.org/10.1007/s11270-017-3323-7