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[TP Metro ]Chl1/SDAHODTP e PP e TDP e DOP e SRP e %time SRP e < 1µgP·L -1 [TP Metro ] Chl SD AHOD TP e PP e TDP e DOP e SRP e %time SRP e < 1µgP·L -1 Correlation Matrix: TP Metro, Trophic State Metrics, and Forms of P parameters correlated parameters not correlated
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Bible Study “And I looked, and behold a pale horse: and his name that sat on him was Death, and Hell followed with him.”
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As Considered Here … “And I looked, and behold a pale horse: and his name that sat on him was AHOD, and Hell followed with him.”
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Martin T. Auer, Phillip A. DePetro, and Kevin A. Bierlein Department of Civil & Environmental Engineering Michigan Technological University Steven C. Chapra Department of Civil & Environmental Engineering Tufts University 11 th Onondaga Lake Scientific Forum, Syracuse, New York, November 2009 SINS OF THE MOTHERS AND FATHERS: WHITHER REDEMPTION? UNTO HOW MANY GENERATIONS: LEGACY ORGANIC CARBON IN ONONDAGA LAKE SEDIMENTS
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Let’s Get One Thing Straight …
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Why? Time Concentration what extent when The question is not whether lakes will improve following external loading reductions, but when and to what extent. Restoration & Management of Lakes and Reservoirs; Cooke et al. (2005)
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sediment water burial flushing with a rapid flushing rate, the fast eigenvalue for Onondaga Lake is fast indeed. the slow eigenvalue … not so much. It’s the Slow Eigenvalue, Stupid
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sediment water burial flushing Eigenvalues and Lake Recovery fast eigenvalue effect slow eigenvalue effect C water C sediment Time (yr)
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Whatever Became of Shagawa Lake? Ely, Minnesota Shagawa Lake Larsen, D.P. and Malueg, K.W. 1980. Whatever became of Shagawa Lake? pp. 67-72, In: Restoration of Lakes and Inland Waters, U.S. Environmental Protection Agency. water column TP of 50 ppb tertiary treatment reduced load by 80% not so much; they missed the slow eigenvalue a fast eigenvalue-based model predicted that water column TP would reach 12.5 ppb within 1.5 years
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Whatever Became of Shagawa Lake? Ely, Minnesota Shagawa Lake Chapra, S.C. and R.P. Canale. 1991. Long-term phenomenological model of phosphorus and oxygen in stratified lakes. Water Research, 25(6): 707-715. “supply from the sediments had not diminished since treatment began … further recovery … will depend upon how long feedback from the sediments continues.”
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So … What’s in the Bottom of Onondaga Lake? win a UFI t-shirt text your answers to 22422 (1)Pere Lemoyne’s hat
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So … What’s in the Bottom of Onondaga Lake? (1)Pere Lemoyne’s hat (2)A Cornell coxswain
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So … What’s in the Bottom of Onondaga Lake? (1)Pere Lemoyne’s hat (2)A Cornell coxswain (3) Ben Schwartzwalder’s comb
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So … What’s in the Bottom of Onondaga Lake? (1)Pere Lemoyne’s hat (2)A Cornell coxswain (3) Ben Schwartzwalder’s comb (4) The veil of Onondaga
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So … What’s in the Bottom of Onondaga Lake? (1)Pere Lemoyne’s hat (2) A Cornell coxswain (3) Ben Schwartzwalder’s comb (4)The veil of Onondaga (5) Le Soup d’Yesterjour NH 3 PO 4 CH 4 H2SH2S SOD MeHg SND
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The Path to Recovery Runs Through the Soup … when and to what extent? Le Soup d’Yesterjour … with organic carbon fueling the fire.
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Diagenesis and the Slow Eigenvalue in Onondaga Lake P, NH 3, Hg slow eigenvalue burial; Hg diagenesis; NH 3, P
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The Slow Eigenvalue in Onondaga Lake P (mgP∙m -2 ∙d -1 )P slow eigenvalue They weren’t supposed to do this until I was dead. Chapra (2009)
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The Slow Eigenvalue in Onondaga Lake 0.0 0.2 0.4 0.6 0.8 1.0 0 10 20 30 40 50 Depth in Sediment (cm) Total Nitrogen (%DW) NH 3 NH 3 -N (mg∙m -2 ∙d -1 ) slow eigenvalue
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The Slow Eigenvalue in Onondaga Lake 1997 Total Hg Depth in Sediment (cm) Total Mercury (µg∙gDW -1 ) MeHg HAR (ng∙m -2 ∙d -1 ) Hg, MeHg slow eigenvalue
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Carbon Diagenesis and Water Quality The Engine P NH 3 H 2 S MeHg CH 4 The Fuel The Gatekeepers O2O2 NO 3 external loads management variable
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Carbon Diagenesis and Water Quality The Engine P NH 3 H 2 S MeHg CH 4 The Fuel external loads internal loads management variable
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Organic Carbon Diagenesis in Sediments: The Slow Eigenvalue C slow eigenvalue operative processes burial diagenesis P NH 3 H 2 S MeHg CH 4
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DIAGENESIS with constant deposition Total Organic Carbon (%DW) Depth in Sediment (cm) Quantifying Legacy Carbon
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DIAGENESIS with variable deposition Total Organic Carbon (%DW) Depth in Sediment (cm) Quantifying Legacy Carbon
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LABILITY ASSAYS under oxic conditions Oxygen Consumed (mgO 2 ∙gDW -1 ) by oxidative metabolism Z = 2.0-2.5 cm Z = 58-60 cm Incubation Time (d) Quantifying Legacy Carbon
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Oxygen Consumed (mgO 2 ∙gDW -1 ) by fermentative metabolism Z = 21 cm Z = 49 cm Incubation Time (d) Quantifying Legacy Carbon LABILITY ASSAYS under anoxic conditions
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LABILITY AT DEPOSITION by fermentative metabolism 56% by oxidative metabolism 90% Quantifying Legacy Carbon
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EXPECTATIONS for downcore changes in lability Total Organic Carbon (%DW) Depth in Sediment (cm) Quantifying Legacy Carbon
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LABILITY PROFILE under oxic conditions Labile Organic Carbon (%TOC) Depth in Sediment (cm) oxidative metabolism Quantifying Legacy Carbon Total Organic Carbon (%DW) Depth in Sediment (cm) No Redemption
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Labile Organic Carbon (%TOC Depth in Sediment (cm) fermentative metabolism Quantifying Legacy Carbon Total Organic Carbon (%DW) Depth in Sediment (cm) No Redemption LABILITY PROFILE under anoxic conditions
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electron donor electron acceptor CO 2 + reduced species end product + various Quantifying Legacy Carbon MAPPING DIAGENESIS
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ETSA and the localization of oxidative processes region of oxidative metabolism ~0-10 cm Quantifying Legacy Carbon
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MAPPING DIAGENESIS localization of methanogenesis region of fermentative metabolism ~10-20 cm Depth in Sediment (cm) Quantifying Legacy Carbon
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om rm Depth in Sediment (cm) Total Organic Carbon (%DW) LITANY OF LEGACY 14 years in the mud
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Preservation (think iceman) Mayer et al. 1994a,b, 2004; Zimmerman et al. 2004; Curry et al. 2007 MECHANISMS surface adsorption on mineral particles encapsulation in the mineral microfabric biological protection (necromass) humification (enzyme resistance) Thompsen et al. 2002; Arnarson and Keil 2007; Curry et al. 2007 Ladd and Paul 1973; Mayer 2004 Hedges 1988; Hedges et al. 1999; Hedges and Keil 1995 b. 3300 BCE Ötzi the Iceman
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Does this mean … ? om rm Depth in Sediment (cm) Total Organic Carbon (%DW) preservation
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Total Organic Carbon (%DW) Depth in Sediment (cm) Ah … yes … redemption!
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SINS OF THE MOTHERS AND FATHERS: WHITHER REDEMPTION?
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Carbon Diagenesis and Water Quality The Model The Engine P NH 3 H 2 S MeHg CH 4 The Fuel The Gatekeepers O2O2 NO 3 external loads management variable THE load driven water column linked coupled flux predictingMODEL
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