Title
Mixing of the Metro Wastewater Treatment Plant effluent with the Mississippi River below St. Paul
Abstract
As a result of this study the following description of the Metro
Wastewater Treatment Plant (WWTP) effluent zone in the Mississippi River
below St. Paul can be given:
• The shape and the size of the mixing zone changes with season.
Only summer conditions were analyzed specifically.
• The longest mixing zone can be expected in fall or spring when the
mixing is controlled by transverse spreading under neutrally
buoyant conditions. Such conditions may also exist at very high
flows during other seasons.
o Between June and August the Metro WWTP effluent plunges below the
water surface before reaching the end of the diverging outlet channel.
The process also occurs in May and ends sometime in September.
The effluent water therefore enters the Mississippi River
as a submerged flow (underflow). Water temperatures and higher
dissolved solids content in the effluent relative to the oncoming
Mississippi River water are the cause of the plunging phenomenon
and the underflow.
• The river becomes vertically stratified below the outlet due to the
sinking of the effluent into the deepest part of the river main
channel.
• The spread of the effluent underflow across the river bottom during
June, July and August appears essentially completed within 0.3 miles or less from the outlet, the actual distance depending on
river flow rate. An analysis of the initial transverse spreading process (nearfield) has not been .made.·
• The most appropriate model for the summer Metro WWTP effluent
mixing zone is therefore a model which considers the plunging,
transverse underflow and vertical mixing in the river.
Funding information
Prepared for
Metropolitan Waste Control Commission
Division of Quality Control
St. Paul, Minnesota
Suggested Citation
Stefan, Heinz G..
(1982).
Mixing of the Metro Wastewater Treatment Plant effluent with the Mississippi River below St. Paul.
Retrieved from the University of Minnesota Digital Conservancy,
https://hdl.handle.net/11299/110003.