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Explore the relationship between dissolved oxygen, system metabolism, and natural disasters in flowing waters. Includes insights from GLOF events. Data and isopleths analysis from Reid, CIEP, and the University of Montana.
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DISSOLVED OXYGEN and system metabolism in flowing waters Including a bonus natural disaster (GLOF) B.L. Reid Centro de Investigación en Ecosístemas de la Patagonia (CIEP) Flathead Lake Biological Station The University of Montana
DO Isopleths: Surficial Groundwater
0 2 4 6 8 10 0 3 6 9 12 0 2 2 4 4 6 6 8 0 Jun 04 2 Aug 04 Nov 04 4 Jan 05 6 May 05 8 DO Isopleths: Surficial Groundwater
12 9 Mean DO (mg/l) 6 3 0 30 20 10 Flowpath Residence Time - Tau (d) DO Isopleths: Surficial Groundwater
12 DO (mg/l) 8 4 0 Jun-04 Sep-04 Dec-04 Mar-05 Jun-05 Sep-05 Dec-05 Mar-06
Recharge - river Horizontal Flow Zone 8 Discharge Zone 6 Resp (μg O2/lsed/hr) 4 2 0
“A skillful limnologist can probably learn more about the nature of a lake from a series of oxygen determinations than from any other kind of chemical data” – G. Evelyn Hutchinson 300 300 River 250 wells 250 y = 18.119x - 13.929 200 2 R = 0.8848 R 2 = 0.704 DSi (μmol/l) avg NOx (ug/l) 150 200 100 50 150 0 0 2 4 6 8 10 12 avg DO (mg/l) 100 0 100 200 300 400 DO (μmol/l)
BGC along aquifer flowpaths: threshold response…. 500 River Wells 400 300 2 R = 0.9183 Specific Conducrance (uS/cm-2s-1) 200 100 0 9 pH 8 2 R = 0.703 7 0 2 4 6 8 10 12 mean DO (mg/l)
Daytime: DO = P – R + Raer Nightime: DO = – R + Raer 9 Sep 2008
Assumptions on Ecosystem Metabolism? 25 Nov 2008
Is this Robust Pattern? Saturation (270m)
Metabolism in the Landscape: Rivers vs. Lakes? From A. Stehr, EULA U de Concepcion
Outlet LG Carrera Balsa Baker (km 50) Tortel (km 150)
Outlet: Lago Traiguen Lago Sauce Grande Outlet: Lago Yulton