Sediment & Nutrient Sources
Sediment enters waterways by erosive forces that loosen soil particles are move them downstream. Non-point sources, both near-channel and upland fields, contribute the majority of the sediment and nutrient loading. Near-channel sources are locations where the force of water disturbs the soil underlying or bordering a water body, such as streambanks, bluffs, and ravines. Upland sources are areas where either water or wind erode soil from land surfaces into waterways, mainly agricultural fields. Some sediment also comes from point sources including wastewater and water treatment facilities, and municipal, industrial, and construction stormwater runoff. The overall dominant source of sediment has shifted over time, from upland agricultural erosion during the 1900s to predominantly near-channel erosion at the present time. Today, several hundred specific ravine and bluff sites in southern MN contribute a substantial portion of the sediment to Lake Pepin.
Excess nutrients also derive from point sources discussed above and nonpoint sources, such as agricultural runoff and seepage from individual treatment systems. Since phosphorus attaches to soil particles, the problems of increased phosphorus and sediment loading are highly interconnected. It is estimated that the accumulation of phosophorus in Lake Pepin sediments has increased 15-fold since 1830 due to greater input from upstream waterways and more efficient trapping of phosphours by lake bottom sediments. As such, addressing phosphorus accumulation in Lake Pepin depends to a substantial degree on addressing the accelerated sedimentation rate.
Although fed by three watersheds, 80-90% of the sediment and nutrients entering Lake Pepin come from the Minnesota River Basin (MRB). Multiple factors contribute to the MRB’s elevated sedimentation rate, including the natural geologic history, human land use changes, and climate change. Geologic processes started thousands of years ago continue to carve out waterways throughout the MRB, making the region highly susceptible to erosion naturally. Human land use changes since the European settlement have exacerbated the natural erosion at upland and near-channel sources. Finally, climate change is altering precipitation patterns and leading to higher streamflows with greater erosive force. This more nuanced picture of the landscape is extremely important for effectively exploring and prioritizing action steps to address the sedimentation problem. Protecting Lake Pepin will require management efforts aimed at upland and near-channel sediment sources as well as the underlying driving factors.
Learn more about the natural geologic history, human land use changes, and climate change effects below.
Natural Erosion Vulnerability
The geology and glacial history of the MRB has an unique role in watershed erosion and downstream sedimentation. The Minnesota River Valley was initially formed by the torrential drainage of Glacial Lake Agassiz around 10,000 years ago. The MRB landscape as a whole includes relatively flat upland areas and specific points of sharp elevation drop, called incision points, or “knickpoints,” where the glacial meltwaters initially formed waterfalls. The Minnesota River and its tributaries have been continuously carving out ravines at these migrating knickpoints for around 10,000 years. In fact, scientists have determined that the tributaries of the MRB are some of the fastest downcutting and thereby rivers in the world. In terms of sediment production, the knickpoints demarcate the MRB’s landscape. Above them, in the flatter upland regions, soil erosion from agricultural fields is the larger source of sediment to the Minnesota River and its tributaries. At or below the knickpoints, the majority of the sediment comes from near-channel sources, specifically bluffs and ravines (Gran et al. 2009).
Human Land Use Changes
Prior to European settlement, the MRB landscape was dominated by prairies with fine, glacially derived and poorly drained soils, and dotted with “pothole” wetlands that were seasonally or perpetually saturated. The settlers recognized the tremendous potential of these fertile lands and began dramatic land use changes that involved large scale row crop production, extensive wetland drainage, and installation of artificial drainage networks or tiling. Together, these human-induced changes to the landscape have profoundly altered the hydrological processes and lead to increased streamflows with higher erosive force.
Agricultural production has nearly converted the native prairie landscape. By 2006, approximately 78% of the MRB landscape was covered in agricultural row crops. Leaving croplands bare in the off-season, as is common agricultural practice, has dual negative effects. First, it makes fields more susceptible to erosion and the transportation of sediment to area water bodies. Second, it increases field runoff and thereby exacerbates high streamflows that greatly increase the amount of near-channel erosion.
Maximizing crop production required adequate soil drainage. Prior to current hydrological understanding, farmers were actually incentivized to drain wetlands and install drainage systems, such as subsurface tiling, that would get water off the land as quickly possible. While drainage systems are highly effective in boosting crop productivity, they have the unintended consequence of increasing streamflows and thus contributing to the complex sedimentation problem we now face. In a recent study surveying 21 Minnesota watersheds, seasonal and annual water flow has increased by over 50% since 1940, with artificial drainage identified as the largest contributor (Schottler et al., 2013). Similarly, the MPCA has determined that the average streamflow in the MN River near Jordan, MN nearly doubled when comparing the period 1977-2013 to 1935-1977. These numbers point to a dramatic increase in erosive force and soil loss at near-channel sources. As would be expected, many agricultural watersheds of the upper Midwest share a strong correlation between increased streamflows, streambank erosion, and channel widening.
Climate change is altering temperatures and precipitation, key components underlying local hydrological processes. Higher temperatures change evaporation rates, snowmelt timing, and ice out dates. Precipitation patterns are changing with storm events expected to increase in frequency and severity. With less water being stored as snow and ices and the increase of runoff from severe storms, it is expected that streamflows will increase and the erosion along them will continue to be problematic as water tries to cut new channels.
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