Mass-balance modeling of metal loading rates in the great lakes

2021 ◽  
pp. 112557
Author(s):  
Colton Bentley ◽  
Tassiane Junqueira ◽  
Alice Dove ◽  
Bas Vriens
2009 ◽  
Vol 35 (2) ◽  
pp. 272-284 ◽  
Author(s):  
Steven C. Chapra ◽  
Alice Dove ◽  
David C. Rockwell

2012 ◽  
Vol 38 (4) ◽  
pp. 741-754 ◽  
Author(s):  
Steven C. Chapra ◽  
David M. Dolan

2014 ◽  
Vol 40 (2) ◽  
pp. 336-346 ◽  
Author(s):  
Scott Jasechko ◽  
John J. Gibson ◽  
Thomas W.D. Edwards

1972 ◽  
Vol 29 (10) ◽  
pp. 1451-1462 ◽  
Author(s):  
K. Patalas

Fourteen copepod and 13 cladoceran species were found in the summer plankton of lakes Superior, Huron, Erie, and Ontario. Cyclops bicuspidatus thomasi was the most abundant species in lakes Huron, Ontario, and Erie, and Diaptomus sicilis in Lake Superior. A general trend was seen from oligotrophic Lake Superior to eutrophic Lake Erie: the diminishing significance of calanoids (Diaptomus sicilis and Diaptomus ashlandi) accompanied by the increasing predominance of cyclopoids and cladocerans (Cyclops bicuspidatus thomasi, Mesocyclops edax, Daphnia retrocurva, Daphnia galeata mendotae, Bosmina longirostris, and Bosmina coregoni coregoni). The average crustacean abundance varied from 43 individuals/cm2 in Lake Superior to 400/cm2 in Lake Erie, and was related to both the heat and chlorophyll content of the water.Total phosphorus loadings for the five Great Lakes were calculated using Vollenweider's criteria based on phosphorus exports from soils and human population densities in the drainage basins. They amounted to 0.03 g total P/m2∙year for Lake Superior, 0.15 for Lake Huron, 0.29 for Lake Michigan, 0.86 for Lake Ontario, and 0.98 for Lake Erie. The lake-average summer chlorophyll-a concentrations as well as Secchi disc visibilities were closely related to the phosphorus loading rates. Crustacean abundance was then indirectly related to the phosphorus loading rates. Based on the correlations found, predictions were made about changes in Secchi disc visibility and chlorophyll concentration with increasing human population densities in the drainage basin.


2018 ◽  
Vol 22 (5) ◽  
pp. 2739-2758 ◽  
Author(s):  
Katherine M. Ransom ◽  
Andrew M. Bell ◽  
Quinn E. Barber ◽  
George Kourakos ◽  
Thomas Harter

Abstract. This study is focused on nitrogen loading from a wide variety of crop and land-use types in the Central Valley, California, USA, an intensively farmed region with high agricultural crop diversity. Nitrogen loading rates for several crop types have been measured based on field-scale experiments, and recent research has calculated nitrogen loading rates for crops throughout the Central Valley based on a mass balance approach. However, research is lacking to infer nitrogen loading rates for the broad diversity of crop and land-use types directly from groundwater nitrate measurements. Relating groundwater nitrate measurements to specific crops must account for the uncertainty about and multiplicity in contributing crops (and other land uses) to individual well measurements, and for the variability of nitrogen loading within farms and from farm to farm for the same crop type. In this study, we developed a Bayesian regression model that allowed us to estimate land-use-specific groundwater nitrogen loading rate probability distributions for 15 crop and land-use groups based on a database of recent nitrate measurements from 2149 private wells in the Central Valley. The water and natural, rice, and alfalfa and pasture groups had the lowest median estimated nitrogen loading rates, each with a median estimate below 5 kg N ha−1 yr−1. Confined animal feeding operations (dairies) and citrus and subtropical crops had the greatest median estimated nitrogen loading rates at approximately 269 and 65 kg N ha−1 yr−1, respectively. In general, our probability-based estimates compare favorably with previous direct measurements and with mass-balance-based estimates of nitrogen loading. Nitrogen mass-balance-based estimates are larger than our groundwater nitrate derived estimates for manured and nonmanured forage, nuts, cotton, tree fruit, and rice crops. These discrepancies are thought to be due to groundwater age mixing, dilution from infiltrating river water, or denitrification between the time when nitrogen leaves the root zone (point of reference for mass-balance-derived loading) and the time and location of groundwater measurement.


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