Monday, August 13, 2018

Lakeshore Property and Conservation: A Quick Dip in the Lakes of the Northern Red Cedar

I spent much of this summer driving around with my research partner, Lucia, listening to NPR and sharing our favorite playlists as we shuffled around the Red Cedar Watershed on our way to interviews. As someone who takes a keen interest in the experiences of others, I joined the LAKES REU to partake in qualitative research, which is a fancy way of saying research that focuses on ideas, opinions, and motivations rather than hard numbers. For our research, Lucia and I interviewed twenty-three stakeholders across the watershed: nine farmers and 23 property owners.

While I enjoyed immensely the time I spent with the farmers we interviewed, in terms of my final project, I focused on lakeshore property owners and other stakeholders on the lake. In our interviews with these folks, we asked about their history in the area, regular use and common maintenance practices, sense of community, sources of information, the impact of water quality, and wetland restoration.  We designed the interview guide with the hopes of learning more about how the private property around the watershed's lakes is being used and maintained in terms of land use and water quality. 

Can You C Yano Bacteria? (Can you see any bacteria?)

This summer, I researched how various sediments within the Red Cedar watershed effect the growth of cyanobacteria. Lake sediment was compared with bedrock sediment, meaning crushed rocks were used as sediment for treatment groups. The motive behind this was that if (climate change induced) storm events were to increase the weathering, or erosion of bedrocks, would this continue to increase cyanobacterial growth. The hope was to understand if all agricultural phosphorous runoff and urban runoff were to be completely stopped, would bedrock nutrients continue the growth of cyanobacteria in eutrophic lakes. This cyanobacteria I am referring to is also known as blue-green algae; however this name is misleading for they are bacteria a type of photosythetic bacteria. Not all species of cyanobacteria are indicators of poor water quality, but the ones that are can sometimes produce toxins hazardous to people and animals when they are in a high enough density and in the process of eutrophication they have the ability to unstabilize the balance of the once healthy aquatic ecosystem.

Sunday, August 12, 2018

Technology in the Lakes


This summer I worked with a wonderful group of people in efforts to clear the horrible smell that came with Lake Menomin.   While, of course, we did not eradicate the issue we all did continue to make strides towards this final goal.  Below the surface of the lake there is an accumulation of phosphorus rich sediment that we call the legacy.  It has been built up for such a long time that even if we completely eliminated the agricultural and domestic runoff occurring the phosphorus levels in the lake would still be just as high as they are now.  This legacy is something that needs to be recognized and investigated more because it is also an issue in the lakes.   


This summer my goal was to take the first steps towards bringing technology into the solution.  I first studied the varying sediment composition of lake sediment in devices that use bacterial metabolism to produce an electric potential.  These devices are called microbial fuel cells or MFCs.  MFCs are interesting cells that can be used to better the water quality but also to create the electric potential.  In my research I only looked at the creation of the electric potential, but future studies using larger cells could be used to better water quality on a smaller scale.  

Giving Plants the Power: Phosphorus Dynamics Along Wild Rice Beds


Plants need phosphorus to grow. The Red Cedar Watershed has plenty of excess phosphorus in the summer months, which promotes the growth of the green layer of cyanobacteria that residents have learned to see and smell so well. Why not use this phosphorus to promote the growth of a different plant, one that adds cultural significance to the water, rather than to fuel the growth of a slimy, green layer? Wild rice, a native aquatic plant to Wisconsin, should be this plant. Wild rice would add value to the Red Cedar Watershed as a natural and ecological approach to phosphorus mitigation.

Wild rice has the potential to thrive and support native wildlife in the Red Cedar Watershed due to its historic presence. To better understand the dynamics of a wild rice ecosystem, my team and I went straight to the source. We found and surveyed five sites in the Red Cedar and surrounding watersheds that had healthy wild rice stands. These visits alone were enough to prove that wild rice can both grow and thrive in north-western Wisconsin, so why not throughout Red Cedar Watershed too? Before jumping right into planting and seeding of this plant, it is important to understand how wild rice growth affects phosphorus in the water and sediment.

To study how wild rice growth impacts phosphorus concentration and deposition along the bed, we took samples from the start to end of the wild rice bed. There was a noticeable difference in the sediment as we sampled throughout the zones just by the appearance of the muck as it oozed out of the corer. The sediment before the bed was barely penetrable sand while throughout the stand, the sediment was a black-brown, fibrous muck. There was an obvious difference in the sediment along the wild rice bed- a complex environment connected with wild rice that was waiting to be explored.

 To quantify the apparent differences in the sediment, my team and I took to the lab where we analyzed phosphorus concentrations and texture of the sediment from the samples. The phosphorus was measured as soluble reactive phosphorus (SRP), a form of phosphorus readily available to plants. There was an increase in SRP concentration in the downstream direction of the bed. Increasing SRP levels are likely related to high levels of nutrient sediment as well as decaying plant matter from previous years. In addition, the sediment with the highest sand content was found before the bed began and the sediment with the highest content of fine particles, like clay and silt, was found in the most upstream portion of the bed. This expected sedimentation from coarse to fine particles in the downstream direction is most likely caused a decrease in flow velocity due to the presence of wild rice. Since phosphorus is attached to particles floating in the water, sedimentation allows for the settling of phosphorus.

The increasing SRP levels in the sediment along the length of the wild rice bed and evidence of sedimentation provide initial data to phosphorus dynamics among the plant, water, and sediment. An increasing concentration of phosphorus in the sediment may be sourced from the water column. A decrease in phosphorus in the water column would lead to decreased phosphorus available for algae growth. To further understand the transport of SRP at the sediment-water interface, water measurements of SRP concentration along wild rice beds should be investigated. Data that revealed a decrease in SRP in the water column as the SRP in the sediment decreased would better support that wild rice removes phosphorus from the water column.

Wild rice nutrient uptake throughout the growing season is also important to understand because the plant takes up and released varying levels of phosphorus throughout the year to support growth.  For instance, wild rice holds the most nutrients in the sediment in mid-July to August so that the nutrients are ready to support the later stage of grain formation in late-August to September. Since the maximum nutrient uptake of wild rice occurs at the same time of algae blooms, wild rice may be an optimal plant for eutrophication mitigation. Further studies may measure SRP concentrations in the sediment throughout the year to understand phosphorus intake by the growing plant and phosphorus release by the decaying plant.

This study provides the initial evidence that wild rice affects phosphorus levels at the water-sediment interface and can be a part of the solution to decreasing algae blooms. Members of the community have asked me, “Why not just throw some scum suckers on the lake to clean up the mess?” While this machine and other forms of artificial technology may seem like the desired quick fix for algae blooms, they are by no means a long-term solution. Human activity and change to the landscape of Dunn County has led to the disruption of the lakes, but a natural process like plant growth can be used to balance the nutrients in the water bodies. It is time for us to rely on the restoration of wild rice, an ecosystem approach, to return the lakes their historic, clean state.

Policies for the People


On the surface, many issues that society faces seem like they may have a one and done solution. However, as we continue on the road of technological advancement, modern life becomes much more complex, and a solution is not always what it seems. Throughout the summer, I have had the opportunity to work alongside seven incredible women from many academic disciplines. All in an effort to find an interdisciplinary approach that will allow us to keep our fresh water bodies swimmable and fishable for the generations to come.

In Wisconsin, we have a long and proud tradition of “doing what needs to be done”, we also benefit from a midwestern sense of community and a fierce gratitude for the natural resources that provide our way of life. This attitude gives us a unique opportunity to combat problems and create policies together in the hopes for a more community-oriented solution. The Red Cedar Watershed, home to some of the most genuine and enthusiastic people I have ever encountered, has been fighting against nutrient pollution that creates algal blooms in our fresh water bodies for decades.