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Jefferson German Chain lake
Management Plan
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Table of Contents
1. Introduction............................................................................................................................ 1
2. Background.............................................................................................................................. 1
3. State of the Lakes..................................................................................................................... 1
4. Lake management goals........................................................................................................... 7
5. Bathtub model update............................................................................................................. 8
6. Implementation strategies..................................................................................................... 12
7. Grants Funding....................................................................................................................... 14
8. Conclusions and Recommendations...................................................................................... 16
The lakes within the Jefferson German Chain (JGC), West Jefferson, Middle Jefferson, East Jefferson, Swede’s Bay and German Lakes, do not meet State standards for due to excess nutrients and the presence of seasonal nuisance algae blooms. The Upper Canon Lakes Excess Nutrient Total Maximum Daily Load (TMDL) was published in 2014. The results of this study show the load reductions needed to meet state water quality standards. This report updates the information collected since the TMDL was developed, establishes goals, and provides recommendations for future projects and programs implementation. The purpose of the Jefferson German Chain Lake Management Plan (LMP) is to determine the appropriate course of action to improve the water quality of these lakes.
Watershed land cover plays a crucial role in the water quality of lakes. The watershed is the area of land that drains into a particular lake, river, or other water body. The types of land cover within a watershed, such as forests, urban areas, agricultural fields, and wetlands, greatly influence the quality of water that flows into the lake, see Section 3.A for more information.
The composition of land cover within a lake's watershed directly affects the quality of water entering the lake. Today, the percent developed in each of the JGC lakes subwatersheds ranges from 7% to 23% and the agricultural use ranges from 26% to 63%, Figure 1. Since 2013 there has been very little increase in development and some decrease in cultivated crops, Table 1. Many of the areas categorized in the 2013 land use report as Pasture/Hay are now classified as Grassland/Shrub. The natural areas of Forest, Wetland, and Grassland/Shrub have increased since 2013.
The largest two subwatersheds are the
German and Swede’s Bay watersheds which both have a large portion of their land
use categorized as cultivation. Agricultural production in the watershed is
primarily corn and soybean fields interspersed with pasture and some small wetlands and wooded
areas. Soil conservation and nutrient management programs are effective at
mitigating phosphorus loading. Options for these programs are expanded on in
Section 6. Development within the watershed includes single-family residential
areas, including parcels along the perimeter of the lake. The mowed lawns and
roadways runoff associated with these developed areas may contribute to
nutrient loading to the lakes. Open water accounts for approximately 21% of the
watershed area and wetland areas account for an additional 6% of the area.
About 8% of the watershed is forested/wooded. The land cover within the
watershed was used to develop a pollutant load model which is described in
further detail in Section 5.
Table 1: Land Use Classification by Lake Subwatershed.
|
Land Use Classification |
Lake Name |
Percent of Land Area (2013) |
Percent of Land Area (2023) |
Change |
|
Cultivated |
West Jefferson |
40 |
26 |
-36% |
|
|
Middle Jefferson |
61 |
63 |
4% |
|
|
Swede’s Bay |
47 |
53 |
14% |
|
|
East Jefferson |
21 |
28 |
31% |
|
|
German Lake |
41 |
37 |
-10% |
|
Developed |
West Jefferson |
25 |
23 |
-9% |
|
|
Middle Jefferson |
15 |
14 |
-9% |
|
|
Swede’s Bay |
7 |
4 |
-37% |
|
|
East Jefferson |
15 |
18 |
21% |
|
|
German Lake |
9 |
7 |
-21% |
|
Pasture/Hay |
West Jefferson |
21 |
32 |
50% |
|
|
Middle Jefferson |
13 |
11 |
-18% |
|
|
Swede’s Bay |
27 |
23 |
-17% |
|
|
East Jefferson |
41 |
23 |
-43% |
|
|
German Lake |
41 |
27 |
-34% |
|
Forest |
West Jefferson |
5 |
9 |
83% |
|
|
Middle Jefferson |
6 |
8 |
26% |
|
|
Swede’s Bay |
10 |
10 |
1% |
|
|
East Jefferson |
12 |
14 |
20% |
|
|
German Lake |
13 |
12 |
-10% |
|
Wetland |
West Jefferson |
7 |
9 |
31% |
|
|
Middle Jefferson |
3 |
3 |
3% |
|
|
Swede’s Bay |
5 |
8 |
68% |
|
|
East Jefferson |
9 |
16 |
74% |
|
|
German Lake |
7 |
14 |
98% |
|
Grassland/Shrub |
West Jefferson |
2 |
2 |
-22% |
|
|
Middle Jefferson |
1 |
2 |
89% |
|
|
Swede’s Bay |
3 |
1 |
-63% |
|
|
East Jefferson |
2 |
1 |
-55% |
|
|
German Lake |
4 |
4 |
-6% |

Figure 1. Jefferson German Chain of Lakes Watershed Land Cover.
The Jefferson German Chain Watershed (15,239 acres) is in Le Sueur County, in southwest Minnesota, within the Upper Cannon River HUC-8 (07040002) basin. The Jefferson German Chain consists of five main interconnected lakes: West Jefferson, Middle Jefferson, East Jefferson, German and Swede’s Bay. The surface water area totals 3,186 acres and outlets to the Northeast toward the Cannon River. The watershed to lake area ratio is 5:1.
The watershed has been subdivided into nine main subwatersheds, Figure 2. Three of these watersheds drain to Swede’s Bay, two to German Lake, and one each to West Middle and East Jefferson Lakes. The lakes with the largest drainage area are Swede’s Bay and German Lake which both have inputs from large agricultural areas to the south. Swede’s Bay flows into East Jefferson Lake and the rest of the chain flows east from West Jefferson Lake, i.e., West Jefferson à Middle Jefferson à East Jefferson à German à outlet.
Two creeks drain into Swede’s Bay. One drains a 3,043 acre watershed that is primarily agricultural land in the south and empties into Swede’s Bay at point JG6 or S004-155. The second drains an 898 acre area of primary agricultural land at point JG8 or S005-436. Both streams are hydraulically modified and have a 30-40 ft buffer with opportunities for improvement.
The West Jefferson watershed is the most upstream in the chain. The watershed is small and primarily consists of rural residential homes with forested lots around the lake. The watershed also picks up some small areas of agricultural runoff.
The Middle Jefferson subwatershed is larger than West Jefferson and consists of some forested residential lots surrounding the lake, but the majority of the subwatershed is agricultural land draining to the waterbody. There is a small stream that drains agricultural land from the north that discharges into Middle Jefferson at discharge point JG9 or S005-439. This small creek is directed through a pond just before discharging into the lake.
East Jefferson Lake receives input from Middle Jefferson Lake and Swede’s Bay. The subwatershed is primarily wooded residential lots with a small amount of agricultural land in the north. Within the north area there is also a large wetland complex.
German subwatershed has a large drainage area to the south that is a mix of agriculture and forested area flowing into the lake at discharge point JG7 or S004-154. The other drainage area surrounding the lake consists of a mix of both residential homes and a significant amount of wetland.
An external load is a nutrient load originating from outside of the lake which is then delivered to the lake. External loads can come from point and non-point sources. Point sources have a discrete point of discharge to the lake. Common point sources to lakes include stormwater pipes, municipal and industrial wastewater discharge, and Confined Animal feeding operations (CAFOs). Point source discharges are regulated through NPDES. Non-point sources are not from discrete sources. The most common non-point sources to lakes are watershed loads. Watershed loads are dependent on land cover. The types of land cover within a watershed, such as forests, urban areas, agricultural fields, and wetlands, greatly influence the quality of water that flows into the lake. Watershed land cover plays the following roles in determining water quality in downstream resources:
Internal
load is a phosphorus load which originates within the lake itself. There are
several types of internal load sources including vegetation senescence,
bioturbation, and legacy nutrients in the sediments. Sediment driven internal
load requires specific conditions to manifest. Phosphorus release from lake
sediments is influenced by various conditions. Due to past land uses,
phosphorus laden sediment has accumulated within the lake and continues to be
available for plant and algae growth. The following are key factors that can
contribute to phosphorus release:
Anoxic Conditions: Phosphorus release is commonly observed in sediments that lack oxygen (anoxic conditions). When oxygen is depleted, certain microorganisms in the sediments start conducting anaerobic processes that release phosphorus. Under anoxic conditions, phosphorus bound to iron and manganese oxides is released and becomes available in the water column. Anoxic conditions result through two primary mechanisms:
1. Thermal Stratification: Lakes often undergo a process called thermal stratification, where the water column separates into distinct layers based on temperature. During the warmer months, the upper layer (epilimnion) receives sunlight and becomes heated, while the lower layer (hypolimnion) remains cooler. This temperature difference prevents mixing between the layers, limiting oxygen transfer to the hypolimnion and promoting anoxia.
2. Nutrient Enrichment: Excessive nutrient inputs, particularly nitrogen and phosphorus from human activities such as agriculture or wastewater discharge, can cause excessive algal growth in lakes. This leads to the development of algal blooms. When these algae die and sink to the bottom, their decomposition consumes oxygen, depleting it in the bottom waters and creating anoxic conditions.
Sediment Disturbance: Human activities and natural processes can disturb lake sediments which can lead to phosphorus release. When sediments are resuspended, phosphorus that was previously bound to particles becomes available in the water column. In shallow areas of the lake, wind and wave action can disturb the bottom sediments.
Redox Potential: The redox potential, which indicates the oxidation-reduction conditions, affects phosphorus release. High redox potential (more oxidizing conditions) tends to keep phosphorus bound to sediments, while low redox potential (more reducing conditions) favors phosphorus release.
pH and Alkalinity: The pH and alkalinity of the lake water also influence phosphorus release. Lower pH and alkalinity can increase the solubility of phosphorus, leading to its release from sediments.
The potential internal loading rate in JGC lakes has yet to be quantified. In BATHTUB model, Section 5, internal load is estimated as the residual load that is not accounted for by the external load. Internal loading can be quantified by measuring sediment phosphorus release rate and the anoxic conditions measured in the lake. The sediment phosphorus release rate is measured in a laboratory by incubating intact sediment cores collected from the lake under oxic and anoxic conditions. Additionally, sediment phosphorus content should be quantified to inform the required sediment inactivation management plans. A feasibility study is outlined in Section 6.A which will inform the internal load control plan.
Curly
Leaf Pond Weed Senescence: Curly Leaf Pondweed (CLP) contributes to internal loading in two
ways to internal loading. 1) Actual senescence of aquatic plant material and
2)BOD resulting in night-time dissolved oxygen concentrations that approach
anoxic conditions in the absence of photosynthesis. CLP senescence occurs in
mid-summer which can lead to increases in TP into the water column.
Phytoplankton are microscopic, free-floating plants that play a critical role in the ecological health of lakes. It is important to note that the terms "phytoplankton" and "algae" are often used interchangeably, but there is a distinction between the two. While all phytoplankton are algae, not all algae are phytoplankton. Algae can refer to any type of aquatic, photosynthetic organism, including those that are attached to surfaces or are large enough to be visible to the naked eye. Phytoplankton specifically refers to those algae that are small enough to float freely in the water column.
Some of the key characteristics and roles of phytoplankton in lakes include:
· Primary production: Phytoplankton are the primary producers in lake ecosystems, converting energy from the sun into organic matter through photosynthesis.
· Nutrient cycling: Phytoplankton help regulate nutrient cycles in lakes by taking up and storing nutrients like nitrogen and phosphorus, which can help prevent excessive algal growth and improve water quality.
· Food source: Phytoplankton serve as a primary food source for many zooplankton and other aquatic organisms, which in turn provide food for fish and other larger predators.
Algae are a diverse group of aquatic organisms found in lakes, ranging from single-celled organisms to larger, multicellular forms. They are important in aquatic food webs and can also impact water quality and human health. Three main groups of algae are commonly found: green algae, blue-green algae, and diatoms. These groups can be distinguished by their growth form and pigmentation.
The Clean Water Act (CWA) is a federal law enacted in 1972 to regulate and improve the quality of the nation's waters, including lakes, rivers, streams, and wetlands. The CWA establishes a framework for setting water quality standards and implementing measures to achieve and maintain those standards. The CWA requires states to assess and identify impaired waters, i.e., those that fail to meet their designated uses, such as swimming, fishing, and maintaining a healthy aquatic ecosystem. States must then strive to restore impaired waters by developing a Total Maximum Daily Load (TMDL) which is a calculation of the maximum amount of a pollutant a water body can receive while still meeting water quality standards.
Minnesota’s impaired waters program is managed by the Minnesota Pollution Control Agency (MPCA) in collaboration with other state agencies, tribes, local governments, and citizens. Its main goal is to assess, monitor, and restore waters that do not meet water quality standards due to pollution or other factors. The MPCA compiles a list of impaired waters, known as the "Impaired Waters List," which is submitted to the U.S. Environmental Protection Agency (EPA) for approval.
The Jefferson German Chain lakes were placed on the impaired waters list for nutrients in 2008 at which time it was determined to be impaired for excess nutrients. The most recent assessment of the lakes, completed in 2022-2025, showed continued impairment. Minnesota's Water Quality Standards provide qualitative and quantitative goals for waters that are protective of Fishable, Swimmable conditions [Water Quality Standards and Classifications]. The applicable water quality standards are outlined below, Table 2.
Table 2: Water Quality Standards
|
Lake |
Lake Type |
TP Standard (ug/L) |
Chl-a (ug/L) |
Secchi (m) |
|
West Jefferson |
Deep |
40 |
14 |
1.4 |
|
Middle Jefferson |
Shallow |
60 |
20 |
1 |
|
East Jefferson |
Deep |
40 |
14 |
1.4 |
|
Swede's Bay |
Shallow |
60 |
20 |
1 |
|
German Lake |
Deep |
40 |
14 |
1.4 |
Lakes have been monitored at different frequencies over the years. Table 3 summarizes the data that has been collected to date for total phosphorus (TP). Figure 3 is a visual representation of all of the TP concentrations observed within the lake systems. Figure 4-Figure 8 show the time series of annual average for each eutrophication parameter. The phosphorus levels within Swede’s Bay are higher compared to the other lakes in the chain. German Lake has the lowest levels of phosphorus in the chain. However, all lakes are exceeding the standards, as seen in Table 3.
Table 3: Total Phosphorus Data Summary.
|
Lake Segment |
2015 to 2025 Average
Observed TP (ug/L) |
Lake Type |
TP Standard (ug/L) |
Years with
Observations between 2015 and 2025 |
|
West Jefferson |
97 |
Deep |
40 |
2022 |
|
Middle Jefferson |
88 |
Shallow |
60 |
2022, 2025 |
|
East Jefferson |
83 |
Deep |
40 |
2022, 2024, 2025 |
|
Swede's Bay |
304 |
Shallow |
60 |
- |
|
German Lake |
75 |
Deep |
40 |
2022, 2024, 2025 |

Figure 3: Total Phosphorus Overview
West
Jefferson
West Jefferson has total phosphorus concentrations that peak on average in July some years there is a peaks in May which may be due to large spring storm events washing phosphorus into the lake. The water quality parameters, though collected infrequently, are fairly consistent throughout the decades and are above the standards.



Figure 4:West Jefferson Lake Water
Quality Time Series
Middle
Jefferson
Middle Jefferson generally peaks in total phosphorus in July but can peak throughout the growing season as well. Middle Jefferson shows a steady improvement in Secchi depth starting in the early 00s and are below the TP and Secchi standard in the most recent sample.



Figure 5: Middle Jefferson Lake Water Quality Time Series
East
Jefferson
East Jefferson shows a peak in total phosphorus concentrations in August. The Secchi depth results are oscillating around the standard. TP and chlorophyll-a are consistently above the standard.



Figure 6: East
Jefferson Lake Water Quality Time Series
Swede’s
Bay
Swede’s Bay has concentrations peaking in July and September. The September peak may be a result of late season phosphorus being released from curly leaf pondweed that has died off. This lake has the highest total phosphorus values in the chain and is likely acting as a treatment system before water is discharged down the chain of lakes.



Figure 7: Swede’s Bay Water Quality Time Series
German
German Lake Secchi depth is often meeting the standard. However, historically chlorophyll-a concentrations are high. Total phosphorus concentrations peak on average in July. The TP concentrations are consistent with previous years.



Figure 8: German Lake Water Quality Time Series
In 2008 and 2009 all 4 tributaries and the one outlet of the Jefferson German chain of lakes were monitored during the growing season. The results, seen in Table 3 and Figure 9 show phosphorus concentrations well above the Class 2B stream standard of 100ug/L. The inlet flowing into Middle Jefferson from the north shows consistently very high Total Phosphorus concentrations over all the years it was monitored. The land use is primarily agriculture which accounts for high phosphorus load, but it should be further investigated what is causing the exceptionally high TP concentrations at S005-439.
Table 4: Total Phosphorus Sampling Statistics for each stream sample point
|
Location |
Total Phosphorus (ug/L) |
Years Sampled |
Count |
|||
|
Min |
Max |
Average |
Standard |
|||
|
North Inlet to Middle German (S005-439) |
265 |
3,440 |
1,183 |
100 |
2002-2003, 2008-2009 |
63 |
|
Southwest Inlet to Swede's Bay (S004-155) |
52 |
1,110 |
226 |
100 |
2002, 2008-2009 |
46 |
|
Southeast Inlet to Swede's Bay (S005-436) |
51 |
950 |
252 |
100 |
2002, 2008-2009 |
44 |
|
South Inlet to German (S004-154) |
52 |
886 |
262 |
100 |
2002, 2008-2009 |
37 |
|
Outlet from German (S005-440) |
11 |
132 |
45 |
100 |
2008-2009 |
42 |
Aquatic macrophytes, or underwater plants, play an important role in the ecological health of lakes. Some of the key ecological benefits provided by these plants include:
· Oxygen production: Aquatic macrophytes produce oxygen through photosynthesis, which helps maintain healthy oxygen levels in the water and supports aquatic life.
· Habitat creation: These plants provide important habitat and cover for fish, invertebrates, and other aquatic organisms, which can improve overall biodiversity in the lake.
· Nutrient cycling: Aquatic macrophytes help regulate nutrient cycles by taking up and storing nutrients like nitrogen and phosphorus, which can help prevent excessive algal growth and reduce the risk of harmful algal blooms.
· Sediment stabilization: The root systems of aquatic macrophytes help stabilize lake sediments, which can help reduce erosion and improve water clarity.
· Water filtration: These plants can help filter out pollutants and other contaminants from the water, improving water quality and reducing the risk of harmful effects on aquatic life and human health.
Overall, the presence of aquatic macrophytes in lakes can help promote a healthy and balanced ecosystem, especially in shallow lakes. However, excessive growth of these plants can also have negative impacts on lake use which can be a concern for lake users.
A survey of the plant diversity in each of the lakes was conducted in 2009. Figure 10 – Figure 14 show the extent of curly leaf pondweed. Table 5 compares the lakes FQI values. An FQI value takes into account the vegetation found in the lake including its rarity or harmfulness to the ecosystem to create a comparable value between lakes. An FQI score of below 20 is indicative of degraded habitats. Despite Swede’s Bay having a large amount of Curly Leaf pond weed, many high value species were also found during the point intercept survey which increased the FQI score of Swede’s Bay. West Jefferson and Middle Jefferson have the worst FQI scores of the lakes in the chain. For the full summary of Aquatic Invasive Species in the Jefferson German Chain see Upper Cannon Lakes Excess Nutrient TMDL - Jefferson-German Lake Chain Pages 95-108.
While aquatic plants are vital to maintaining the ecologically-preferred clear water state, Figure 15, invasive species like Curly-leaf pondweed (CLP) can quickly alter the ecology of a shallow lake and prevent or restrict lake users from enjoying certain recreational activities such as boating and swimming. Senescence of Curly-leaf pondweed in mid-summer particularly contributes to internal nutrient loading and sub-optimal conditions for native aquatic plants, contributing to a turbid anoxic state. Therefore, the challenge for JGC lakes is to concurrently reduce CLP coverage and protect lake water quality by maintaining a clear-water, aquatic plant dominated state.

Figure 10: West Jefferson Lake Curly Leaf Distribution May 2009.

Figure 11: Middle Jefferson Lake Curly Leaf Distribution May 2009

Figure 12: Swede’s Bay Curly Leaf Pondweed Distribution May 2009

Figure 13: East Jefferson Lake Curly Leaf Pondweed Distribution May 2009

Figure 14: German Lake Curly Leaf Pondweed Distribution May 2009
Table 5: FQI Scores by lake
|
Lake |
FQI Score May |
FQI Score August |
|
West Jefferson |
9.82 |
12.02 |
|
Middle Jefferson |
2.68 |
-- |
|
Swede’s Bay |
15.75 |
20.51 |
|
East Jefferson |
12.21 |
19.5 |
|
German |
14.4 |
22.8 |

Figure 15. Cascading biological communities in shallow lakes under clear and turbid water states.
· Water Quality Mitigation: The riparian area acts as a natural buffer zone, filtering and absorbing pollutants, sediments, and nutrients from runoff before they enter the lake. Plants in the riparian zone contribute to nutrient cycling by taking up excess nutrients like nitrogen and phosphorus from runoff. This can help prevent over-enrichment of the lake with nutrients, which can lead to issues like harmful algal blooms.
· Habitat and Biodiversity: Riparian zones provide important habitats for various plant and animal species. They offer food, shelter, and breeding sites for aquatic and terrestrial organisms, contributing to the overall biodiversity of the ecosystem.
· Bank Stabilization & Erosion Control: The roots of riparian plants help anchor the soil, preventing bank erosion and maintaining the structural integrity of the shoreline. This is particularly important during storms or high-water events. The vegetation in riparian areas, including trees, shrubs, and grasses, helps stabilize the soil along the shoreline. This prevents soil erosion and reduces sedimentation in the lake, which can negatively impact water quality and aquatic habitats.
Overall, the health and integrity of the lake riparian area are closely linked to the water quality and ecological balance of the lake itself. Proper management and conservation of these zones are essential for preserving the long-term health and sustainability of lake ecosystems. The state of the JGC shoreline has not been determined.

Figure 16. Loss of natural ground cover reduces infiltration and evapotranspiration, increasing stormwater and pollutant runoff into nearby waterbodies
Goals for the future of Jefferson German Chain of Lakes were established with input from the GJGLA.
The primary water quality goals are based on standards the State of Minnesota established for recreational use of lakes in the North Central Hardwood Forest Ecoregions. The presence of nuisance algae blooms is the primary basis for Minnesota recreational-use standards. The numeric criteria provided in the state standard are essentially proxies for the presence of algae or the conditions which lead to algal blooms. It is important to note that these standards apply to growing season measurements. Additional goals are included to address the primary sources of nutrient loading to the lake. The JGC goals are listed below:
1. Establish a monitoring program to evaluate water quality trends and improvements after management.
a. Three years of data should be collected to establish water quality trends and a baseline for pre-management conditions. See Section 6 for a detailed monitoring plan.
2. Meet the Minnesota’s standards (growing season averages) for each lake in order to remove from the impaired waters list.
3. Reduce the internal and external loads based on the TMDL and updated models, Table 6.
a. See Section 6 for an outline of the necessary feasibility study to address load reduction strategies.
Table 6: TMDL Load Reduction Summary.
|
Lake |
Internal Load Reduction (lbs/yr) |
External Load Reduction (lbs/yr) |
Upstream Load (lbs/yr) |
Total Load Reduction (lbs/yr) |
|
West Jefferson |
37 |
527 |
- |
564 |
|
Middle Jefferson |
756 |
1631 |
5 |
2,393 |
|
East Jefferson |
20 |
1664 |
886 |
2,571 |
|
Swede's Bay |
807 |
6424 |
- |
7,231 |
|
German Lake |
732 |
1078 |
159 |
1,969 |
4. Reduce the frequency and magnitude of seasonal algal blooms by 50% for 10 years after load reduction goals are met.
5. Support the Soil and Water Conservation District (SWCD) with their mission to implement agricultural best management practices (BMPs).
The aquatic invasive species (AIS) goals are based on controlling the resident populations of AIS and preventing the spread AIS amongst the chain of lakes.
1. Control the populations non-native aquatic invasive species.
a. See Section 3 above for specific species
2. Determine the existence and persistence of AIS in each lake
a. See Section 6 for more information on the recommended assessment.
3. Support local government programs regarding the public awareness of AIS efforts.
1. Establish 75% shoreline as native habitats in shoreline, emergent, and submergent habitats to promote populations of natural mussels and other species that improve the lake ecosystem.
2. Establish the current condition of shoreline on each lake.
a. See Section 6 for information on the recommended assessment.
3. Educate and support local stakeholders about vegetation management best practices
a. See implementation section for information
1. Support safe and balanced recreational use of the lakes
A TMDL study completed in 2011 and
published in 2014 by the Water Resources Center (WRC) at Minnesota State
University, Mankato (MSU,M) on the JGC developed a BATHTUB model. This section
outlines the updates that were incorporated from the original model. In
general, we updated the information in the model to 2015-2024 date. Lake
characteristics were kept the same as the TMDL. The Observed in-lake TP
Concentrations were averaged for all available TP concentration values between
2015 and 2024. Data years available:
·
West Jefferson: 2022
·
Middle Jefferson: 2022, 2025
·
East Jefferson: 2022, 2024, 2025
·
German: 2022, 2024, 2025
·
Swede’s Bay: No new data, so kept same as TMDL
The atmospheric load was 30 kg/km2-yr
in TMDL, but we updated to 43.2 kg/km2-yr based on state database.
In TMDL, the P decay calibration factor was kept as 1, then
internal loading factor was used to calibrate the model. For new data, we kept P
decay calibration factor as 1, then scaled either the internal loading or
watershed loading values or both from the TMDL values until observed matched
predicted TP concentration:
·
West Jefferson - Watershed is small, so it only calibrated
with internal loading while keeping watershed loading the same.
·
Middle Jefferson: Not possible to calibrate by reducing the
watershed loading alone, so scaled both the watershed loading and internal
loading from TMDL to match TP.
·
East Jefferson: Added outflows from Swede’s Bay and Middle
Jefferson together as the inflow to East Jefferson. Kept internal loading the
same as TMDL, but scaled watershed loading from TMDL.
·
German: Kept internal loading the same as TMDL, but scaled
watershed loading from TMDL.
·
Swede’s Bay: No new data on TP, but we increased atmospheric
loading as mentioned previously, so scaled watershed loading from TMDL to
compensate for the increase. Kept internal loading the same.
It is important to note that these models are based on
limited data, and the internal load can be quantified by following the
recommended feasibility study in Section 6.
The results of the phosphorus load budget from each lake can be seen in Figure 17 – Figure 21. Though the concentrations at the stream inputs are high, the primary driver for phosphorus levels in the lakes are ultimately internal loading. A large portion of the loading to East Jefferson Lake is through the outflow from Swede’s Bay as well. Swede’s Bay has phosphorus loads primarily driven by internal loading. Middle Jefferson Lake has a notable contribution of phosphorus load from the inflow but still is primarily driven by internal loading. The primary phosphorus load for West Jefferson is driven by internal loading. German Lake has phosphorus loads primarily driven by internal loading and Inflow site JG7 or S004-154.

Figure 17: West Jefferson Loading Summary

Figure 18: Middle Jefferson Loading Summary

Figure 19: East Jefferson Loading Summary

Figure 20: Swede’s Bay Loading Summary

Figure 21: German Loading Summary
Table 7: Implementation Summary.
|
Timeline |
||||||||||||
|
Priority |
2026 |
2027 |
2028 |
2029 |
2030 |
2031 |
2032 |
2033 |
2034 |
2035 |
||
|
Eutrophication |
|
|
|
|
|
|
|
|
|
|
|
|
|
In-Lake Monitoring |
High |
$1,500-$2,000/year |
$1,500-$2,000/year |
|||||||||
|
Internal Load
feasibility |
High |
$65,000-$75,000 |
||||||||||
|
Internal Load Control* |
High |
TBD |
||||||||||
|
Education and
Outreach* |
Medium |
|
|
|
|
|
|
|
|
|
|
|
|
AIS |
|
|
|
|
|
|
|
|
|
|
|
|
|
AIS Macrophyte
Assessment |
Medium |
$2,500-$5,000/lake |
$2,500-$5,000/lake |
|
||||||||
|
Education and
Outreach* |
High |
|
|
|
|
|
|
|
|
|
|
|
|
Habitat |
|
|
|
|
|
|
|
|
|
|
|
|
|
Shoreline assessment |
Medium |
$2,000-$3,500/lake |
||||||||||
|
Education and
Outreach* |
High |
|
|
|
|
|
|
|
|
|
|
|
|
Recreation and Safety |
|
|
|
|
|
|
|
|
|
|
|
|
|
Boat Capacity Survey |
Low |
$3,500-$5,000/lake |
||||||||||
|
Outreach for Wake
Boats** |
Medium |
|
|
|
|
|
|
|||||
|
Outreach for Safe
boating ** |
High |
|
|
|
|
|
|
|
|
|
|
|
*The cost of the Internal load control will be determined by the Internal load feasibility study.
**Outreach activities can be determined by the outreach and education plan
The first goal for eutrophication is to establish a monitoring program to evaluate water quality baseline and improvements after management.
In-lake sampling of JGC lakes have been done sporadically over the years. The following monitoring plan is recommended to set baseline conditions. The monitoring plan is built from past data sets and models. EOR recommends the GJGLA complete this plan for three consecutive years pre-in-lake treatment to meet the goal.
The
recommended monitoring plan is outlined in Table 8, below. The monitoring
locations are illustrated in Figure 22. The in-lake monitoring
includes dissolved oxygen and temperature profiles and routine water quality
monitoring. The dissolved oxygen and temperature profiles will inform mixing
conditions and anoxia within JGC lakes. The routine water quality monitoring at
the deep hole will inform temporal dynamics of mixing, nutrients, algae growth,
and water clarity.
There has been no long-term monitoring of the water flowing from Swede’s Bay to East Jefferson. This information is important for prioritizing management activities amongst the chain. For example, Swede’s Bay may be acting a sink of phosphorus from the watershed load but may be acting as a source of phosphorus downstream because of high internal load. Monitoring at the Swede’s Bay outlet will allow us to determine the load from Swede’s Bay downstream.
The cost range for this monitoring plan is $1,500-$2,000/year incorporating the cost of equipment rental (DO and temperature probe) and lab costs for data analysis. The cost of the monitoring relies on volunteers to collect the data. If volunteers cannot be used then the cost will increase.
Table 8: Recommended Monitoring Plan Summary
|
Parameter |
Timing |
Frequency |
Monitoring Depth |
Station Location |
Methodology |
|
Swede’s Bay outlet Monitoring |
|||||
|
Flow |
May-October |
Continuous |
_ |
Swede’s Bay outlet |
Flow meter |
|
React
P, Total P |
May-October |
Biweekly |
Surface outflow |
Samples will need to be shipped to a certified lab for analysis |
|
|
In-lake Monitoring |
|||||
|
Dissolved
Oxygen (DO) and Temperature Profiles |
May-October |
Biweekly |
Every 0.5m from surface to bottom |
In lake Sampling: Deep-hole |
Multi-probe |
|
React
P, Total P |
May-October |
Biweekly |
0.5 ft from the bottom and at the surface |
Grab samples collected using a van dorne sampler. Samples will
need to be shipped to a certified lab for analysis |
|
|
Chlorophyll-a |
May-October |
Biweekly |
Surface |
Samples will need to be shipped to a certified lab for analysis |
|
|
Secchi
Depth |
May-October |
Biweekly |
|
Secchi Disk |
|

Figure 22: Approximate locations for water quality monitoring.

Figure 23: West Jefferson Lake Proposed Sediment Core Locations.

Figure 24: Middle Jefferson Lake Proposed Sediment Core Locations.

Figure 25: East Jefferson Lake Proposed Sediment Core Locations.

Figure 26: Swede’s Bay Proposed Sediment Core Locations.

Figure 27: German Lake Proposed Sediment Core Locations.
Eutrophication goals 2-4 all relate to meeting nutrient reductions goals to reverse eutrophication on the JGC lakes. The driving phosphorus load on each lake is internal load. A feasibility study for internal loading on each lake must be conducted to determine the appropriate management. If an alum treatment were recommended, the prescribed dose could reduce the internal load by up to 90% and last at least 10 years.
Since most of the lakes have internal load as the majority load. The next step is internal load feasibility study. This includes understanding the sediments and the oxygen and mixing dynamics collected from the recommended monitoring plan above. The sediment cores will be collected at locations at varying depths, as indicated in Figure 23-Figure 27. The sediment cores will be collected to quantify the phosphorus content and potential phosphorus release from the sediments into the water column which is used to quantify the internal load. The sediment cores will also be used to prescribe a sediment inactivation plan if internal loading control is deemed necessary.
Sediment cores should be taken from areas of anoxia or areas that are feasible for sediment activation application. The recommended locations can be further refined based on the results of the DO monitoring. The convention for selecting the locations of the sediment core was determined by the lake bathymetry and morphology. More complex lakes require more sediment core locations to resolve internal load dynamics. Sediment cores should be segmented into six sections: 0-2cm, 2-4cm, 4-6cm, 6-8cm, 8-10cm, 10-20cm. Each section should be analyzed for loosely bound P, iron-bound P, labile organic P, and aluminum-bound P. The phosphorus content is used to prescribe the internal load control dose. In addition, sediment core will be analyzed for soluble reactive phosphorus release rates. Incorporating release rate analysis is imperative to understanding the internal load. The P release rate in conjunction with the DO data will be used to update the internal load estimate.
Table 9: Recommended Sediment Core Summary
|
Lake Sediment Cores |
No. cores
fractionation |
No. cores flux |
Cost |
|
East Jefferson Lake |
8 |
3 |
$14,500 |
|
Middle Jefferson Lake |
3 |
3 |
$6,750 |
|
West Jefferson Lake |
4 |
3 |
$8,250 |
|
Swede's Bay |
4 |
4 |
$9,000 |
|
German Lake |
6 |
3 |
$11,500 |
The cost of the internal load feasibility study includes $50,000 of laboratory costs for sediment core analysis plus an additional $15,000-$25,000 in consultant fees to analyze data, update the P budget, and create an internal loading control plan. The total cost of this feasibility study is $65,000-$75,000.
The fifth eutrophication goal is to support the Soil and Water Conservation District (SWCD) with their mission to implement agricultural best management practices.
A wide array of conservation practices is available to manage nutrient loading from agricultural land. Roughly 20% of the Jefferson German Chain watershed is currently used for row crop production and another 20% for pastureland. Agricultural conservation practices that promote soil health are recommended for the Jefferson German Chain watershed. Soil health practices are a set of sustainable farming techniques and management strategies designed to protect and improve the overall health and quality of soil in agricultural ecosystems. These practices aim to enhance soil fertility, structure, and resilience, while minimizing erosion, nutrient depletion, and environmental degradation. They are critical for maintaining long-term agricultural productivity and sustainability. In many cases, these practices are cost-neutral (reduce expenses) and may be eligible for funding through the Le Sueur Soil and Water Conservation District cost share program.
Cover
Crops
Cover crop is a term to describe any crop grown primarily for the benefit of the soil rather than the crop yield. Cover crops are typically grasses or legumes (planted in the fall between harvest and planting of spring crops) but may be comprised of other green plants. Cover crops prevent erosion, improve the physical and biological properties of soil, supply nutrients, suppress weeds, improve the availability of soil water, and break pest cycles, in addition to a wide range of additional benefits. The Le Sueur SWCD offers cost share programs for agricultural BMPs, and Cover Crops are currently being incentivized at a rate of $45/acre for single species and $50/acre for multispecies.
No-till
No-till is a way of growing crops or pasture from year to year without disturbing the soil through tillage. No-till increases the amount of water that infiltrates into the soil, the soil's retention of organic matter and its cycling of nutrients. It can also reduce soil erosion and increase the amount and variety of life in and on the soil. The most powerful benefit of no-tillage is improvement in soil biological fertility, making soils more resilient. The Le Sueur SWCD offers cost share programs for agricultural BMPs and No-till is currently being incentivized at a rate of $20/acre.
4Rs
of Nutrient Management
The 4Rs of nutrient management refer to fertilizer application techniques focused on minimizing the risk of nutrient loss from the field. The principles of the 4R framework include:
• Right Source – Ensure a balanced supply of essential nutrients, considering both naturally available sources and characteristics of specific products in plant available forms.
• Right Rate – Assess and make decisions based on soil nutrient supply and plant demand.
• Right Time – Assess and make decisions based on the dynamics of crop uptake, soil supply, nutrient loss risks, and field operation logistics.
• Right Place – Address root-soil dynamics and nutrient movement and manage spatial variability within the field to meet site-specific crop needs and limit potential losses from the field. Nutrient management plans are tailored by farmers and/or crop consultants to maximize yields and minimize nutrient inputs.
The ultimate AIS goals is to control the populations non-native aquatic invasive species. The first step in controlling AIS is to determine the existence and persistence of AIS in each lake via a diagnostic study.
The diagnostic study determines the health of the aquatic vegetation community. The monitoring plan includes point intercept surveys and delineation of aquatic invasive species (AIS). Point-Intercept surveys include systematic assessment of the vegetation community over time. The point-intercept method is considered the standard protocol by MNDNR for sampling macrophytes because it offers a methodology that is quantitative (e.g., frequency of occurrence), repeatable (can be used to track trends in aquatic plant communities over time), and georeferenced (can be used to compare plant communities within different areas of a lake). A small lake should include 60-80 sampling points in the littoral zone. For larger lakes, a 100 x 100 meter point-intercept sampling grid over the total surface area of the lake is recommended. It is assumed that there will be up to approximately 300 sampling points in the littoral zone. At each sampling point the aquatic plants and plant density for each species are identified. The survey will yield the distribution, density, and floristic quality of the aquatic plant community. A Floristic Quality Index (FQI) will also be calculated for each survey. The FQI calculation is based on both the quantity of species observed (species richness) as well as the quality of each individual species. Another monitoring method, specific to AIS, is to precisely delineate the total acreage infested with AIS. The timeline for these surveys is dependent on species. The estimated cost for the survey includes labor for the survey and data analysis of $2,500-$5,000 per lake.
The final goal is to support existing governmental programs AIS education and outreach programs and to put signs up by lake entrances. Further discussion about partnerships and outreach activities in sections below.
The ultimate habitat goal is to establish 75% of native shorelines. However, at this time, the current shoreline status has yet to be determined for each lake.
The zone of land adjacent to a lake's shoreline or lake riparian area plays a crucial role in maintaining and influencing the quality of the lake ecosystem. In particular, the riparian area acts as a natural buffer zone, filtering and absorbing pollutants, sediments, and nutrients from runoff before they enter the lake. Plants in the riparian zone contribute to nutrient cycling by taking up excess nutrients like nitrogen and phosphorus from runoff.
Lakeshore improvements entail planting of native vegetation along lakeshore and in emergent zone of the lake as a way of restoring the natural transition from lake to upland. The goal of a lakeshore improvement effort is a dense stand of vegetation growing throughout the riparian area to trap and filter pollutants. Beyond addressing water quality, lakeshore improvements provide additional ecosystem services such as habitat for birds, spawning and refuge for fish, wave-erosion protection, and pollinator habitat.
To assess the current condition of the shoreline and identify areas for shoreline improvements, a diagnostic study is recommended. The diagnostic study determines extent of shoreline erosion along the lake. The monitoring plan includes targeting areas from visual lakeshore survey using Score Your Shore (Department of Natural Resources). Score Your Shore is a tool to assess habitat conditions. The protocol is designed for use by lakeshore property owners to self-assess habitat or by organizations, such as lake associations and county staff, to assess multiple sites on a lake. Score Your Shore provides an objective and systematic method to assess the type, quantity, and quality of the existing shoreland habitat.
The Score Your Shore tool will enable you to:
· Assess the amount of habitat at developed lake sites
· Generate awareness of what makes a high quality functioning shoreline buffer
· Provide a system to recognize landowners with functioning shoreline buffers.
The cost for the shoreline assessment study is estimated to be $2,000-$3,500 per lake. The cost to complete the diagnostic study includes conducting lakeshore surveys, i.e., Score Your Shore.
The Cannon River Watershed JPO offers shoreland owners $500 per parcel for planting a minimum of 150 sq ft of native vegetation. This program should be promoted to shoreline owners as part the lake association outreach programing
The goal for recreation and safety is to support safe and balanced recreational use of the lakes. In order to achieve this goal, it is important to determine the safe boat capacity for each lake.
The diagnostic study for recreation and safety
includes evaluating the lakes’ boating carrying capactiy. The boating carrying
capacity is the number of watercaraft that can simultaneously operate on the
lake without: compromising user safety, causing significant user displacement
or dissatisfaction, and causing environmental harm to the lake. The
methodology for the boat capacity survey includes the following steps:
The monitoring plan includes
identifying boats type and density and number of Boat slips over 6 days, selecting
3 peaks days, 1 average day, and 2 non-peak days.
The estimated cost for the completing the boat carrying capacity survey is $3,500-$5,000 per lake. The cost to complete the diagnostic study includes labor for the boat capacity survey.
The outreach goals for wake boating can be achieved by educating boaters on safe practices. Wake Boating is only safe in 20ft of water and 500ft from shore. Only a small portion of East Jefferson and German fall into this Category. To help residents and visitors to understand, consider posting on social media, educating at meetings, and creating signs for boat launches with information around wake boat safety and environmental impact. Possible partnerships for this work include MN Coalition of Lake Associations and Minnesota Lakes and Rivers.
Each implementation category includes an education and outreach component. EOR recommends developing a separate education and outreach plan to broadly address the comprehensive program. The following activities are important to consider for education and outreach programing.
· Consider joining MN Cola ($50/annual)
· Create subcommittees
· Promote on Social media
· Dedicate time during meetings for rotating topics
· Engage with business on the lakes
· Give materials to AIS inspectors
These efforts will require a pool of volunteers for consider engaging with your membership to participate in Citizen science, subcommittees, and boat surveys. GJGLA should explore partnerships with area organizations to provide education and outreach for each area of interest. The recommended partnerships per implementation item is summarized in Table 10. The following partnerships will be important for education content to provide to members and function as guest speakers.
•Farmers for Agricultural BMPs
•Minnesota Collation of Lake Associations (MN COLA)
•Partner with Frank Breen Memorial Wildlife Management area
•Potential partnership with Dove Lake Wildlife Management Area for restoration project
•Resorts/Camps
•County
•Soil and Water Conservation District (SWCD)
•Department of Natural Resources (DNR)
•Local Sportsman Club
•Fishing tournaments
•Cleveland school district partnership – possible volunteers
•Universities and colleges – Mankato State, Gustavus, Water Resource Center
•County Commissioners to seek funding for water quality improvement projects
•Canon River Watershed Joint Powers Organization
Table 10: Partnership Summary
|
Priority |
Lead Organization |
Partners |
||
|
Eutrophication |
|
|
|
|
|
In-Lake Monitoring |
High |
GJGLA |
SWCD |
|
|
Internal Load
feasibility |
High |
Consultant |
||
|
Internal Load Control |
High |
Consultant |
||
|
Education and Outreach |
Medium |
|||
|
AIS |
|
|
|
|
|
AIS Macrophyte
Assessment |
Medium |
GJGLA |
AIS inspectors |
|
|
Education and Outreach |
High |
GJGLA |
MN COLA, MAISRC |
|
|
Habitat |
|
|
|
|
|
Shoreline assessment |
Medium |
Consultant |
||
|
Education and Outreach |
High |
GJGLA |
MN COLA, University
Partners, Canon River Watershed |
|
|
Recreation and Safety |
|
|
|
|
|
Boat Capacity Survey |
Low |
Consultant |
DNR |
|
|
Outreach for Wake
Boats |
Medium |
GJGLA |
MN COLA, County,
Minnesota Lakes, and Rivers |
|
|
Outreach for Safe
boating |
High |
GJGLA |
MN COLA, County, DNR |
|
Table 11 summarizes the implementation projects and applicable grant information. In general, there are few grants that assist with education and outreach capabilities but will rely on the partnerships discussed in Section 6.E. It is important note that funding from BWSR is shifting from an open competitive process to priorities given to the projects priorities as part of the One Watershed One Plan. Currently the only priority project relevant for JGC is German-Jefferson Chain-of-Lakes Septic Inventory and Feasibility Assessments. EOR recommends engaging with the Cannon River Watershed Joint Powers Organization (CRWJPO) to incorporate the high priority projects identified in this plan into the priority projects to future plan amendments to increase funding opportunities.
Table 11: Grant Summary
|
Eutrophication |
Priority |
Grant |
Level of support |
Funder |
Timeline |
|
|
In-Lake Monitoring |
High |
Surface Water
Assessment |
TBD |
MPCA |
2027 |
|
|
Internal Load
feasibility |
High |
Surface Water
Assessment |
TBD |
MPCA |
2027 |
|
|
Clean Water Fund:
Project and Program |
10% match required |
BWSR |
2027 |
|||
|
Internal load control |
High |
Clean Water Fund:
Accelerated Implementation |
10% match required |
BWSR |
2027 |
|
|
Education and Outreach |
||||||
|
AIS |
|
|
|
|
|
|
|
Macrophyte AIS
Assessment and Control |
High |
Invasive Species
Control |
fund control of CLP, EAW,
or flowering rush |
MN DNR |
February Annually |
|
|
Education and Outreach |
High |
|||||
|
Habitat |
|
|
|
|
|
|
|
Shoreline assessment |
Medium |
Native Planting Cost
Share |
$500/ landowner |
Canon River JPO |
Rolling |
|
|
Shoreline improvements |
Medium |
Land Conservation
Grant |
$360,000 Typically 3-5
projects funded annually |
Midwest Glacial Lakes
Partnership |
First of the Year
Annually |
|
|
Bass Pro Shops US Open
Grant Program |
no limit or match |
National Fish Habitat
Partnership |
May Annually |
|||
|
Partners for Fish and
Wildlife Program |
$25,000, no match
required |
US Fish and Wildlife
Service |
||||
|
Education and Outreach |
High |
|||||
|
Recreation and Safety |
|
|
|
|
|
|
|
Boat Capacity Survey |
Low |
|||||
|
Outreach for Wake
Boats |
High |
|||||
|
Outreach for Safe
boating |
High |
|||||
The lake management plan updated the lake ecology and water quality information since the TMDL was developed in 2011. EOR collaborated with the stakeholders to prescribe goals addressing the following management strategies: eutrophication, aquatic vegetation, lake habitat, and recreation and safety.
For eutrophication goals, it is important to note, although data is available and discussed above, it is sporadic both spatially and temporarily. Overall, Jefferson German Chain of Lakes are eutrophic lakes in a plant dominated state. The available data informed phosphorus budgets which demonstrate the lakes are dominated by internal loading. However, the specific management is dependent on the results from the recommended monitoring plan which will more directly quantify internal loading. At this time, our primary recommendations are to pursue the comprehensive monitoring plan and internal load feasibility study, which will inform load reduction strategies to address eutrophication goals.
Aquatic vegetation, habitat, and recreation and safety require further diagnostic study to establish baseline conditions to determine future management feasibility and management success. Aquatic vegetation goals are related to control of AIS. The primary implementation strategy is to determine the current vegetation population. Habitat goals are related to shoreline restoration. Similar to the aquatic vegetation goals, the primary implementation strategy is to assess the existing condition of the shoreline for each lake. Finally, the recreation and safety activity is to determine the boat carrying capacity of each lake to determine safe recreation conditions.
Each of the management categories also includes an education and outreach goal. GJGLA should explore developing a comprehensive education and outreach plan and seek strong partnerships with agencies and relevant organizations to achieve the goals outlined in this lake management plan.
There are several grants available to implement lake management activities. The primary recommendation is for the GJGLA to engage with the Cannon River Watershed Joint Powers Organization (CRWJPO) to incorporate the high priority projects identified in this plan into the priority projects to future plan One Watershed One Plan amendments to increase funding opportunities.