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Energy and Materials Exchange between Terrestrial
and Aquatic Ecosystems at the UM Biological Station
Paul Drevnick <drevnick@umich.edu>
“The large lens of groundwater under in the thick, sandy/gravelly glacial
deposits overlying sandstone and limestone bedrock interacts with all manner
of surface water, vegetation, and various life forms in the ‘tip of the mitt’
region at the confluence of the three largest of the Great Lakes” – Knute N.
groundwater in = change in lake volume - precipitation - surface
water in + evaporation + surface water out + groundwater out
For a 54-day period from winter 2013-2014, in units of million cubic feet per day:
51 - 48 - 39 + 0 + (139 at end, 212 at beginning) + 65 = 168 to 241 million cubic feet per day.
Groundwater input is the biggest term in the hydrologic budget!
BVK
In the Cheboygan River watershed:
Groundwater-dominated headwater
streams support valuable cold-water
fisheries and serve as constant sources
of clean water for lakes that are the
economic engines for northern MI
tourism.
Groundwater seepage (i.e, subsurface,
nonchannelized flow) may be more
important than streams as a renewable
water source for lakes.
Management decisions regarding land development and uses of
groundwater must take into account the importance of groundwater
for maintaining high water quality in streams and lakes.
Also in the Cheboygan River watershed:
A mercury problem!
Crooked, Pickerel, Burt, and Mullett Lakes are listed as federally
impaired for exceeding the U.S. EPA water quality criterion for
methylmercury in fish tissue for the protection of human health.
MI DNR
9151
8806
9456
8911
9149
9127
Establish watershed studies to monitor inputs and outputs of mercury
Must understand hydrology before we can understand energy or
materials exchange between terrestrial and aquatic ecosystems
-Define topographic and phreatic boundaries
-Monitor precipitation, evapotranspiration, stream discharge, storage
Characterize ecosystem components, i.e., above- and belowground
biomass, soils and parent material, and quantify mercury stocks therein
Watershed-scale studies to understand
inputs, outputs, retention of mercury
Plot-scale studies to understand
processes that affect retention
Goal is to understand forest management
practices that maximize retention.
Opportunities for collaboration
Hydrology
Energy or materials exchange

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  • 1. Energy and Materials Exchange between Terrestrial and Aquatic Ecosystems at the UM Biological Station Paul Drevnick <drevnick@umich.edu> “The large lens of groundwater under in the thick, sandy/gravelly glacial deposits overlying sandstone and limestone bedrock interacts with all manner of surface water, vegetation, and various life forms in the ‘tip of the mitt’ region at the confluence of the three largest of the Great Lakes” – Knute N.
  • 2. groundwater in = change in lake volume - precipitation - surface water in + evaporation + surface water out + groundwater out For a 54-day period from winter 2013-2014, in units of million cubic feet per day: 51 - 48 - 39 + 0 + (139 at end, 212 at beginning) + 65 = 168 to 241 million cubic feet per day. Groundwater input is the biggest term in the hydrologic budget! BVK
  • 3. In the Cheboygan River watershed: Groundwater-dominated headwater streams support valuable cold-water fisheries and serve as constant sources of clean water for lakes that are the economic engines for northern MI tourism. Groundwater seepage (i.e, subsurface, nonchannelized flow) may be more important than streams as a renewable water source for lakes. Management decisions regarding land development and uses of groundwater must take into account the importance of groundwater for maintaining high water quality in streams and lakes. Also in the Cheboygan River watershed: A mercury problem! Crooked, Pickerel, Burt, and Mullett Lakes are listed as federally impaired for exceeding the U.S. EPA water quality criterion for methylmercury in fish tissue for the protection of human health. MI DNR
  • 4. 9151 8806 9456 8911 9149 9127 Establish watershed studies to monitor inputs and outputs of mercury Must understand hydrology before we can understand energy or materials exchange between terrestrial and aquatic ecosystems -Define topographic and phreatic boundaries -Monitor precipitation, evapotranspiration, stream discharge, storage Characterize ecosystem components, i.e., above- and belowground biomass, soils and parent material, and quantify mercury stocks therein
  • 5. Watershed-scale studies to understand inputs, outputs, retention of mercury Plot-scale studies to understand processes that affect retention Goal is to understand forest management practices that maximize retention. Opportunities for collaboration Hydrology Energy or materials exchange