Willow River (10 MI to 140 St), Lower Willow River Watershed (SC02)
Willow River (10 MI to 140 St), Lower Willow River Watershed (SC02)
Willow River (10 MI to 140 St) (2606900)
1.93 Miles
11.81 - 13.75
Cool-Warm Mainstem
2022
Good
 

Overview

Willow River flows southwest into Lake St. Croix. Five flowages are impounded on this stream: the New Richmond (16 foot head darn), Mounds (50'), Burkhardt (101'), Little Falls Flowage (27') and Mallileau Lake (20'). Over half the stream is considered trout water with the main species being brown trout. Brook and rainbow trout are also present. Fish species found in the stream include northern pike, walleyes, largemouth bass, bluegills, perch, black crappies, pumpkinseeds, green sunfish and a variety of forage fish.

Feeder streams include Black Brook, South Fork Willow River, Ten Mile Creek, Anderson Spring and a small spring feeder stream that flows into the Willow from Section 9, Township 30 North, Range 17 West. Mallards, blue- winged teal, wood ducks and hooded mergansers may be found nesting in the 1,410 acres of predominantly wooded wetlands. Muskrats and beaver are also present.

Public land consists of 0.3 miles of county-owned frontage with 20 road bridges also providing access to the stream. Private development is limited to 20 cottages and homes.

From: Sather, LaVerne M. and Threinen, C.W., 1961. Lake and Stream Classification Project. Surface Water Resources of St. Croix County, Wisconsin Department of Natural Resources, Madison, WI.

Date  1961

Author   Aquatic Biologist

Historical Description

Water quality and fisheries surveys in 1992 indicate that nonpoint source pollution degrades water quality and fish populations in the Willow River. Ammonia and total phosphorus concentrations were significantly increased during high flow conditions. A fisheries study indicated that fish populations lacked a diversity of species.

Monthly grab sampling of Willow River water quality was initiated in July 1990 at four sites from New Richmond to the Little Falls Dam. Two additional ammonia sampling sites were added in November 1990 and February 1991. Grab samples for ammonia were collected at a few locations in the reach in August 1984, October 1984 and August 1988. Continuous recording dissolved oxygen (DO) equipment was deployed at three locations in the reach in August 1988 and in July and August 1991. Equipment failure resulted in the loss of some recording DO data.

Date  1992

Author   Aquatic Biologist

Historical Description

When examining the data, special consideration was given to three important factors affecting water quality:
1. The New Richmond Flowage was drawn down in late June and early July of 1991.
2. The 1988 data was collected during unusually low flow conditions, although still four times above the Q,.,, flow.
3. Known sources of pollutant loading to the river reach being evaluated were the New Richmond WWTP, the Friday Canning spray irrigation site and the past spills of fertilizer to groundwater by Blue Ribbon Feeds in New Richmond.

DISSOLVED OXYGEN
The water quality standard for DO was not met in the Willow River at all three monitoring locations between Hwy 64 and Boardman in 1988 (Figure 1). The portion of the reach classified as a warmwater fishery did not maintain the minimum DO standard of 5 mg/l, measured at Hwy 64 and at a point 0.75 miles below the WWTP. DO leaving the reach classified trout stream (Boardman site) did not maintain the minimum DO standard of 6 mg4. Monitoring in 1991 found no violations of the DO standard (Figure 2). However, examination of the river DO data expressed as percent saturation indicated that the river had lower DO levels at Hwy 64 and at the downstream site than at the New Richmond Dam. This condition was present to a greater extent in 1988.

Both the 1988 and 1991 data were collected under stable, non-event flow conditions. Based on the gauged flow of other rivers in the region, Willow River flow was estimated to be about 50% higher during the 1991 sampling than the 1988 sampling. The difference between the 1988 and 1991 DO was likely linked to the response of river water quality to different flows or to a change due to the loss of the upstream impoundment. Top draw impoundments can adversely affect downstream DO if they contribute significant BOD, in the form of algae passing over thedam. With the impoundment drawn down, this source of BOD, would be eliminated. The slightly depressed DO below the New Richmond Dam in 1991 may be the result of oxygen demand of sediments scoured out of the former impoundment as a new river channel was being formed. The river experienced higher suspended solids in the summer of 1991, after the impoundment was drawn down, than the previous summer.

PHOSPHORUS
Total phosphorus in the Willow River generally fell between 0.05 and 0.15 mgil. The highest values were associated with high river flow in the spring (Figures 5&6). The minimum total phosphorus level was higher at Hwy A (0.07 mgl) than at the other sites (0.04 mgil). Phosphorus loading from the New Richmond WWTP may be the cause. Since substantial increases in river flow occur between the WWTP and Hwy A, the minimum total phosphorus concentration immediately below the WWTP may be substantially higher the minimum documented at Hwy A.

AMMONIA
A high concentration of ammonia nitrogen was documented in the Willow River at Hwy 64 in 1984. The concentration was only slightly less than the level toxic to warmwater aquatic life in a chronic exposure. Since no sample was taken in the downstream river section classified as a trout stream, it is unknown if the lower trout stream water quality standard was met in that reach. The river seems to have been on a downward trend in low flow ammonia nitrogen since that sample was taken. No violations of the water quality standard have been documented.

Date  1992

Author   Aquatic Biologist

Historical Description

The possible causes for the high ammonia levels in 1984 include large spills of high nitrogen fertilizer into the groundwater near the New Richmond Dam by Blue Ribbon Feeds in 1981 and 1983 and Friday Canning's spray irrigation field. Groundwater monitoring at the Friday Canning site, which is located on the banks of the river, has shown decreases in pollutant levels since 1985, when loading to the field was reduced. Down gradient monitoring wells still indicate an significant increase in groundwater ammonia nitrogen levels as comparcii to up gradient wells. The sources of ammonia nitrogen in the Willow River near New Richmond can be evaluated by examining Figure 7, which includes only data collected when river ammonia levels were high. On 6/3/91, ammonia levels, as well as suspended solid levels, were elevated entering the reach. This occurred during a time of high flow and was probably the result of nonpoint sources in the watershed above New Richmond Flowage.

On 01/10/91 and again on0 2/05/91 a rise in river ammonia occurred as it flowed past the Friday Canning site. This was during winter low flow conditions, when impacts by ammonia in groundwater on streams would be at the maximum. At this time of year many streams experience a rise in ammonia associated with the onset of cold weather. This may be responsible for the above normal ammonia levels at the New Richmond Dam. The increase in ammonia near the Friday Canning site is in addition to this natural occurrence. On 2/5/91 and again on 3/14/91 a rise in river ammonia occurred between Hwy 64 and Boardman. Loading from the New Richmond WWTP is a possible cause for this rise.

BACTERIA
The Willow River was sampled for fecal coliform bacteria at four sites on eight dates during May - October of 1990 and 1991. Of the 29 samples collected, six were above 200 bacteria per 100ml and three were above 400 bacteria per 100ml. The highest bacteria per 100ml at each site were 570 at Odanah Road, 600 at Hwy 64, 3200 at Hwy A and 110 at Little Falls Dam, all recorded on 6/3/91.

Date  1992

Author   Aquatic Biologist

Natural communities (stream and lake natural communities) represent model results that use predicted flow and temperature based on landscape features and related assumptions. Ranges of flow and temperature associated with specific aquatic life communities (fish, macroinvertebrates) help biologists identify appropriate resource management goals. Wisconsin Natural Communities.
This is the most recent date of monitoring data stored in SWIMS. Additional surveys for fish and habitat may be available subsequent to this date.
Trout Waters are represented by Class I, Class II or Class III waters. These classes have specific ecological characteristics and management actions associated with them. For more information regarding Trout Classifications, see the Fisheries Trout Class Webpages.
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