Natural Resources
Conservation Service

Ecological site F091XY009WI

Alfic Sandy Upland

Last updated: 9/27/2023
Accessed: 12/30/2024

Home / Esd catalog / MLRA 091X / Ecological site F091XY009WI

USC

Metric

General information

Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.

MLRA notes

Major Land Resource Area (MLRA): 091X–Wisconsin and Minnesota Sandy Outwash

The Wisconsin and Minnesota Sandy Outwash MLRA is the most extensive glacial outwash system in the northern half of Wisconsin. The total land area of the Wisconsin portion is just under 1.4 million acres (2,170 sq miles). The northern half is a former spillway for Glacial Lake Duluth. The flowing meltwater from the draining lake has left behind thick deposits of drift and carved a terraced river valley now occupied by the St. Croix and Bois Brule Rivers.
The northeastern section – the Bayfield hills – is a collapsed outwash plain where drift deposits are thick. Lacustrine materials from Glacial Lake Duluth line the northeastern tip. Moving southwest, the landscape transitions into a large pitted outwash plain. This is an area of extensive kettle holes, and, where the underlying till is less permeable, kettle lakes with some interspersed morainic hills and ridges. The glacial drift deposits are thinner in the southwestern section, although there is still no documented surface bedrock within this MLRA.

The St. Croix and Bois Brule rivers share a channel that lines much of the northwestern border of this MLRA. In some places, the underlying reddish-brown sandy loam till of the Copper Falls Formation is exposed along cut riverbanks, though most of it is covered by a mantle of outwash. Glacial lakes deposited pockets of fine-textured lacustrine materials, most of which were washed away or buried by glacial outwash and meltwater flowing through the channel. East of the channel, some of the silty and clayey lakebed deposits are found near the surface, where they impede drainage and contribute to the formation of extensive wetlands.

Historically, the area supported extensive jack pine (Pinus banksiana), scrub, and oak forests and barrens. The northern portion also supported stands of red pine (Pinus resinosa) and eastern white pine (Pinus strobus) as well. Marsh and sedge meadow, wet prairies, and lowland shrubs dominated the extensive wetland complexes in the southern tip of this MLRA (Finley, R., 1976).

Classification relationships

Relationship to Established Framework and Classification Systems:
Biophysical Settings (Landfire, 2014): This ES is largely mapped as Laurentian-Acadian Northern Hardwoods Forest, Boreal Aspen-Birch Forest, Laurentian Oak Barrens, Boreal Hardwood Forest, and Eastern Cool Temperate Pasture and Hayland

Habitat Types of N. Wisconsin (Kotar, 2002): The sites of this ES keyed out to one habitat type: Pinus strobus-Acer rubrum/Vaccinium-Amphicarpa (PArVAm)

WDNR Natural Communities (WDNR, 2015): This ES is most similar to the Northern Mesic Forest and Northern Dry-Mesic Forest communities.

Hierarchical Framework Relationships:
Major Land Resource Area (MLRA): Wisconsin and Minnesota Sandy Outwash (91X)

USFS Subregions: Bayfield Sand Plains (212Ka)
Small sections occur in the Mille Lacs Uplands (212Kb) subregion

Wisconsin DNR Ecological Landscapes: Northwest Sands, Northwest Lowlands

Ecological site concept

The Alfic Sandy Uplands ecological site is located throughout MLRA 91X on till, lake, and outwash plains, and on ground moraines. These sites are characterized by very deep, moderately well or well drained soils that formed in sandy till. These sites have a layer of significant clay accumulation: an argillic horizon is either present or forming. Precipitation and runoff from adjacent uplands are the primary sources of water. Soils range from strongly acid to slightly acid. These sites occur in higher landscape positions, sometimes where somewhat loamy morainal deposits protrude from the expansive outwash plain that makes up MLRA 91B. The presence of finer-textured parent materials allows the soils of Alfic Sandy Uplands to develop their characteristic argillic horizons.

Historically this Ecological Site was occupied by forest communities dominated by various mixtures of pine and oak species. Specific mixtures were largely dependent on frequency and severity of disturbances, particularly fire and subsequent seed-bed conditions and availability of seed sources. White pine (Pinus strobus) was the most persistent species in forest communities due to its biological and ecological characteristics of great longevity, resistance of old trees to fire damage and moderate tolerance to shade by seedlings and saplings. Red oak was often present as an associate species. Virtually all stands on this Ecological Site were harvested during the late 19th and early 20th centuries and post-logging fires were almost universal. Today’s forests are dominated by any mixture of, aspen, red maple (Acer rubrum), red oak (Quercus rubra), white oak (Q. alba), white pine (Pinus strobus) and red pine (Pinus resinosa). White birch (Betula papyrifera) and balsam fir (Abies balsamea) are common associates.

Alfic Sandy Uplands is differentiated from other ecological sites based on sandy deposits, drainage, and presence of accumulated clay in a subsurface horizon. The clay accumulation in the subsurface horizon may perch water and make it accessible to vegetation for longer than other sandy upland soils. The sandy material tends to have lower pH and available water capacity than loamy and clayey materials. The moderately well and well drained soil differs these sites from other sandy sites.

Associated sites

F091XY005WI	Wet Sandy and Loamy Lowland These sites occur on depressions and drainageways on outwash plains and lake plains. They primarily form in sandy outwash are subject to some flooding. Soils are very deep and poorly or very poorly drained. They are saturated for much of the year. They are wetter and occur lower on the drainage sequence than Alfic Sandy Uplands.
F091XY007WI	Moist Sandy and Loamy Lowland These soils formed in sandy outwash, sandy lacustrine deposits, sandy eolian deposits, or loess that is sometimes underlain by sandy or loamy till. Soils are very deep and somewhat poorly drained. They are wetter and occur lower on the drainage sequence than Alfic Sandy Uplands.
F091XY011WI	Sandy Upland These soils formed primarily in sandy outwash or sandy eolian deposits, but some sites formed in sandy lacustrine or loamy alluvium underlain by sandy outwash. Soils are very deep and are moderately well to somewhat excessively drained. They are neutral to extremely acid and lack a spodic horizon. They may be found in similar landscape positions adjacent to Alfic Sandy Uplands.

F091XY005WI

Wet Sandy and Loamy Lowland

These sites occur on depressions and drainageways on outwash plains and lake plains. They primarily form in sandy outwash are subject to some flooding. Soils are very deep and poorly or very poorly drained. They are saturated for much of the year. They are wetter and occur lower on the drainage sequence than Alfic Sandy Uplands.

F091XY007WI

Moist Sandy and Loamy Lowland

These soils formed in sandy outwash, sandy lacustrine deposits, sandy eolian deposits, or loess that is sometimes underlain by sandy or loamy till. Soils are very deep and somewhat poorly drained. They are wetter and occur lower on the drainage sequence than Alfic Sandy Uplands.

F091XY011WI

Sandy Upland

These soils formed primarily in sandy outwash or sandy eolian deposits, but some sites formed in sandy lacustrine or loamy alluvium underlain by sandy outwash. Soils are very deep and are moderately well to somewhat excessively drained. They are neutral to extremely acid and lack a spodic horizon. They may be found in similar landscape positions adjacent to Alfic Sandy Uplands.

Similar sites

F091XY010WI	Acidic Sandy Upland These soils formed primarily sandy outwash, but some sites formed in loamy alluvium over sandy outwash, and other sites are sandy outwash underlain by lacustrine deposits. Soils are very deep and are moderately well to somewhat excessively drained. These soils occupy the same positions on the landscape and have the same particle size class as Alfic Sandy Uplands but differ in that they are characterized by the presence of a spodic horizon.
F091XY011WI	Sandy Upland These soils formed primarily in sandy outwash or sandy eolian deposits, but some sites formed in sandy lacustrine or loamy alluvium underlain by sandy outwash. Soils are very deep and are moderately well to somewhat excessively drained. They are neutral to extremely acid and lack a spodic horizon. These soils occupy the same positions on the landscape and have the same particle size class as Alfic Sandy Uplands but differ in that they lack significant clay accumulation.
F091XY012WI	Loamy Upland These soils formed in loamy lacustrine, loamy alluvium, loamy till, sandy outwash, sandy eolian, or loess deposits. Some sites have underlying lacustrine deposits, till, or basalt bedrock. They are moderately well or well drained. These soils occupy the same landscape positions as Alfic Sandy Uplands but have finer particle size classes.

F091XY010WI

Acidic Sandy Upland

These soils formed primarily sandy outwash, but some sites formed in loamy alluvium over sandy outwash, and other sites are sandy outwash underlain by lacustrine deposits. Soils are very deep and are moderately well to somewhat excessively drained. These soils occupy the same positions on the landscape and have the same particle size class as Alfic Sandy Uplands but differ in that they are characterized by the presence of a spodic horizon.

F091XY011WI

Sandy Upland

These soils formed primarily in sandy outwash or sandy eolian deposits, but some sites formed in sandy lacustrine or loamy alluvium underlain by sandy outwash. Soils are very deep and are moderately well to somewhat excessively drained. They are neutral to extremely acid and lack a spodic horizon. These soils occupy the same positions on the landscape and have the same particle size class as Alfic Sandy Uplands but differ in that they lack significant clay accumulation.

F091XY012WI

Loamy Upland

These soils formed in loamy lacustrine, loamy alluvium, loamy till, sandy outwash, sandy eolian, or loess deposits. Some sites have underlying lacustrine deposits, till, or basalt bedrock. They are moderately well or well drained. These soils occupy the same landscape positions as Alfic Sandy Uplands but have finer particle size classes.

Table 1. Dominant plant species

Tree	(1) Quercus rubra (2) Acer rubrum
Shrub	(1) Vaccinium
Herbaceous	(1) Amphicarpaea bracteata

Download full description

Physiographic features

These sites formed on till plains, lake plains, outwash plains, and ground moraines. Slopes range from 1 to 35 percent. Sites are on summit, shoulder, and backslope positions.

These sites are not subject to ponding or flooding. Some sites have a perched water table (episaturation), but most have apparent water tables (endosaturation). Seasonally high water table depths range from 18 to 30 inches below the soil surface. The water table can drop to greater than 60 inches during dry conditions. Runoff is negligible to medium.

Table 2. Representative physiographic features

Hillslope profile	(1) Summit (2) Shoulder (3) Backslope
Slope shape across	(1) Convex
Slope shape up-down	(1) Linear
Landforms	(1) Outwash plain (2) Lake plain (3) Till plain (4) Ground moraine (5) Disintegration moraine
Runoff class	Negligible to medium
Flooding frequency	None
Ponding frequency	None
Elevation	853 – 1,410 ft
Slope	1 – 35%
Water table depth	18 – 30 in
Aspect	Aspect is not a significant factor

Climatic features

The continental climate of the Wisconsin and Minnesota Sandy Outwash MLRA is typical of northern Wisconsin – colder winters and warmer summers. In general, the northern latitudes have cooler summers, colder winters, lower precipitation, and shorter growing seasons than the south; however, neither average annual precipitation nor average annual minimum and maximum temperatures vary greatly within this MLRA. The climate of the northernmost tip is somewhat affected by Lake Superior and receives higher annual precipitation in the form of lake effect snow.

Table 3. Representative climatic features

Frost-free period (characteristic range)	77-101 days
Freeze-free period (characteristic range)	111-133 days
Precipitation total (characteristic range)	30-32 in
Frost-free period (actual range)	73-108 days
Freeze-free period (actual range)	106-135 days
Precipitation total (actual range)	29-32 in
Frost-free period (average)	91 days
Freeze-free period (average)	122 days
Precipitation total (average)	31 in

Characteristic range

Actual range

Bar

Line

Figure 1. Monthly precipitation range

Characteristic range

Actual range

Bar

Line

Figure 2. Monthly minimum temperature range

Characteristic range

Actual range

Bar

Line

Figure 3. Monthly maximum temperature range

Bar

Line

Figure 4. Monthly average minimum and maximum temperature

Figure 5. Annual precipitation pattern

Figure 6. Annual average temperature pattern

Climate stations used

(1) DANBURY [USC00471978], Danbury, WI
(2) MINONG 5 WSW [USC00475525], Minong, WI
(3) SPOONER AG RES STN [USC00478027], Spooner, WI
(4) GORDON [USC00473186], Gordon, WI
(5) SOLON SPRINGS [USC00477892], Solon Springs, WI
(6) HAYWARD RS [USC00473511], Hayward, WI
(7) HAYWARD MUNI AP [USW00094973], Hayward, WI

Influencing water features

Water is received primarily through precipitation, runoff from adjacent uplands, and groundwater discharge. Water is discharged from the site primarily through runoff, evapotranspiration, and groundwater recharge.

Permeability of these sites is very slow, moderately slow, or moderate. Hydrologic group is A.

Wetland description

Hydrogeomorphic Wetland Classification: None
Cowardin Wetland Classification: None

Soil features

These sites are represented by the Ashwabay, Fremstadt, and Keewenaw soil series. Ashwabay is classified as an Alfic Oxyaquic Haplorthod; Fremstadt is an Arenic Hapludalf; and Keweenaw is an Alfic Haplorthod.

These soils formed in sandy or loamy till, or in sandy outwash underlain by till. Soils are very deep and are moderately well or well drained. Soils do not meet hydric soil requirements.
Surface textures are loamy sand and sandy loam. Subsurface textures include loamy sand, sandy, sandy loam, and clay. Soil pH ranges from strongly acid to neutral with values of 5.2 to 6.7. Carbonates are absent.

Figure 7. Fremstadt Soil Series sampled on 07/10/2019 in Jefferson County, WI.

Table 4. Representative soil features

Parent material	(1) Till (2) Outwash
Surface texture	(1) Loamy sand (2) Sandy loam
Drainage class	Moderately well drained to well drained
Permeability class	Very slow to moderate
Soil depth	80 in
Surface fragment cover <=3"	Not specified
Surface fragment cover >3"	2%
Available water capacity (0-60in)	4.47 – 5.69 in
Soil reaction (1:1 water) (0-40in)	5.2 – 6.7
Subsurface fragment volume <=3" (0-40in)	7 – 20%
Subsurface fragment volume >3" (0-40in)	5%

Ecological dynamics

Perhaps the most important ecological characteristic of this Ecological Site, in terms of influence on forest community dynamics, is its limited capacity to support the high to moderate soil moisture and nutrient requiring species such as sugar maple (Acer saccharum), basswood (Tilia americana) and white ash (Fraxinus Americana). These are the shade-tolerant species, commonly known as the northern hardwoods, that typically dominate the more productive sites throughout northern Wisconsin. Although some of these species do occur sporadically on this Ecological Site, their regeneration capacity and growth rates are sub-optimal, thus precluding their canopy dominance.

In pre-European settlement time wild fire was the main controlling factor of forest community dynamics. Following a severe, stand-replacing fire, any of the naturally occurring species could become established, depending on the seed source and specific conditions of post-fire seedbed. The newly established young stands of any species were easily eliminated by recurring fires, but differences in fire-resisting properties among the species began to play a role in any species’ survival success. White pine is best adapted for long-term success on this Ecological Site. Although vulnerable to damage or elimination by fire in early life it eventually develops thick fire-resistant bark which helps to extend its longevity, in some cases for up to four centuries or more. These survival properties assure the species’ relatively continuous seed source in the region as a whole. White pine is also moderately shade-tolerant in early life which means that it can become established in some pioneer communities, such as aspen – white birch stands, or in poorly stocked oak and red maple dominated communities. Red pine had in the past been a common associate of white pine stands. It shares some of the fire-resisting properties of white pine, but it lacks shade-tolerance and does not become established in the understory. For this reason, it has not maintained its presence in current stands and its seed source has been greatly reduced throughout its natural range following the unset of fire suppression.

In his reconstruction of pre-European settlement vegetation of Wisconsin, Finley (1976) did not identify red maple (Acer rubrum) as a prominent component of pine forests, but the species is a prominent member of current stands. Absence of fire since the end of the original logging era is probably the main reason. Red maple is extremely sensitive to fire, but is a prolific and early seed producer. Stems of 2-4 inches in diameter can produce large amounts of seed (USDA Forest Service, 1990). It is sufficiently shade-tolerant to become established in the understories of most communities on sandy soils. On this Ecological Site it behaves similarly to white pine, but because of its much smaller stature at maturity, it does not compete with white pine in the upper canopy.

State and transition model

More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective text

Ecosystem states

1. Reference State

2. Early to Mid-Successional Forest

3. Livestock Grazed Forest

4. Agricultural State

T1A	-	Stand replacing disturbance e.g., blow-down and fire, or clear-cutting followed by fire. Regeneration by natural seeding or planting.
R2A	-	Fire control, time, natural succession.
T2A	-	Grazing by livestock. Disruption of tree regeneration and ground vegetation.
T2B	-	Removal of natural vegetation, plowing, fertilizing, irrigating, planting agricultural crops.
R3A	-	Removal of livestock from stands.
T3A	-	Removal of natural vegetation, plowing, fertilizing, irrigating, planting agricultural crops.

State 1 submodel, plant communities

1.1. Advanced Succession Phase

1.2. Old Mixed Pine-Oak Forest Phase

1.1A	-	Light to moderate intensity fires, reducing or eliminating advance tree regeneration.
1.2A	-	White pine and red oak regeneration re-establishes.

State 2 submodel, plant communities

2.1. White Pine - Red Pine Forest

2.2. Red Pine Plantation

2.3. Jack Pine Forest

2.4. Aspen Forest

2.5. Mixed Species Phase

Communities 1, 5 and 2 (additional pathways)

2.1. White Pine - Red Pine Forest

2.5. Mixed Species Phase

2.2. Red Pine Plantation

2.1B	-	Removal of White Pine
2.5B	-	Time without disturbance, natural succession
2.5C	-	This pathway occurs with fire when Jack pine seed sources is available or when planted.
2.5A	-	Repetitive clearcutting and burning of earlier stands

State 1
Reference State

In the long-term absence of stand replacing disturbance, tree species composition of forest communities on this ecological site fluctuates among white pine (Pinus strobus), red pine (P. Resinosa), red oak (Quercus rubra) and red maple (Acer rubrum). This fluctuation is due to many factors. There is a differential response to a range of common, but not stand-replacing disturbances, such as light fire, snow and ice brakeage and natural mortality in the canopy. There are differences in regeneration requirements among the species and in seedling tolerance of understory conditions. While the resulting community species composition and structure can be viewed as a continuum, two distinct community phases can be described as representing the opposite ends of a continuum.

Dominant plant species

eastern white pine (Pinus strobus), tree
red pine (Pinus resinosa), tree
northern red oak (Quercus rubra), tree

Community 1.1
Advanced Succession Phase

White pine, with varying admixtures of red pine and red oak, constitutes the dominant overstory. The shrub layer typically is well-developed and is dominated by beaked- and american hazel, (Corylus cornuta and C. americana)). Other important species are juneberry (Amalenchier spp.) and blueberry, (Vaccinium angustifolum). Herbaceous layer typically is dominated by high cover of bracken fern (Pteridium aquilinum) and large-leaf aster (Eurybia macrophylla). Other well represented species include wild lily of-the valley (Maianthemum canadense), wood anemone (Anemone quinquefolia) and starflower (Trientalis borealis).

Dominant plant species

eastern white pine (Pinus strobus), tree
red pine (Pinus resinosa), tree
northern red oak (Quercus rubra), tree
balsam fir (Abies balsamea), tree
beaked hazelnut (Corylus cornuta), shrub
lowbush blueberry (Vaccinium angustifolium), shrub
western brackenfern (Pteridium aquilinum), other herbaceous
bigleaf aster (Eurybia macrophylla), other herbaceous

Community 1.2
Old Mixed Pine-Oak Forest Phase

Pathway 1.1A
Community 1.1 to 1.2

Periodic moderate intensity fires, eliminating or reducing advance regeneration, but leaving at least the oldest and fire-resistant pines and oaks.

Pathway 1.2A
Community 1.2 to 1.1

Canopy species re-establish regeneration layer.

State 2
Early to Mid-Successional Forest

Community 2.1
White Pine - Red Pine Forest

Even-aged, naturally regenerated, mixed pine forest, some times with admixture of red oak of sprout origin. These stands often contain considerable amount of white pine regeneration, but with only sporadic presence of young red pine in locations with large canopy openings and absence of other competing vegetation.

Dominant plant species

eastern white pine (Pinus strobus), tree
red pine (Pinus resinosa), tree

Community 2.2
Red Pine Plantation

Planted red pine with varying spacing. Plantations with close spacing e.g. less than 8 x 8 feet typically are devoid of significant understory vegetation. However, if thinning is applied the shrub component, dominated by beaked hazelnut (Corylus cornuta), increases significantly. Other common shrubs may include blackberries and raspberries (Rubus spp.), juneberry (Amelanchier spp.) and blueberries (Vaccinium spp.). Depending on the proximity of seed sources, white pine regeneration may be common. Herbaceous layer also increases, often dramatically, with bracken fern (Pteridium aquilinum) and large-leaf aster (Eurybia macrophylla) attaining strong dominance.

Dominant plant species

red pine (Pinus resinosa), tree

Community 2.3
Jack Pine Forest

Unless planted, this community develops only if fire was included in the destruction of preceding community and mature Jack pine trees were present to provide seed source. Young jack pine communities often are very dense. Over time, natural mortality thins the stand and shrub and herb layers develop similarly as described for Community Phase 2.2.

Dominant plant species

jack pine (Pinus banksiana), tree

Community 2.4
Aspen Forest

Like the naturally developed jack pine forest, the aspen forest community most often requires fire disturbance for establishment. Once in place it can be perpetuated by clear cutting. Understory communities develop in a similar way as described in communities 2.2 and 2.3, but more quickly, because aspen mortality leads to faster self-thinning of stands and light penetration in aspen canopy is greater that that in conifer stands.

Dominant plant species

quaking aspen (Populus tremuloides), tree
bigtooth aspen (Populus grandidentata), tree

Community 2.5
Mixed Species Phase

Figure 8. Image courtesy of UWSP taken on 07/11/2019 in Jefferson County, WI.

This is a mid-successional community. The oldest tree cohort is made up of remnants of the pioneer communities of either Jack pine, red pine, or aspen. This cohort is in the process of being replaced by more shade tolerant white pine. Red oak is also frequent associate. In absence of major disturbance this community phase transitions into Reference State Community.

Dominant plant species

jack pine (Pinus banksiana), tree
red pine (Pinus resinosa), tree
quaking aspen (Populus tremuloides), tree
eastern white pine (Pinus strobus), tree
northern red oak (Quercus rubra), tree

Pathway 2.1B
Community 2.1 to 2.2

Stand replacing disturbance e.g., blow-down and fire, or logging of white pine followed by fire. Regeneration by natural seeding or planting.

Pathway 2.1A
Community 2.1 to 2.5

White pine regeneration in mixed stand of white, red, and sometimes Jack pine.

Pathway 2.2A
Community 2.2 to 2.1

White pine seeding in from natural seed source or under-planted.

Pathway 2.2B
Community 2.2 to 2.5

White pine seeding in from natural seed source or under-planted.

Pathway 2.3A
Community 2.3 to 2.5

White pine seeding in from natural seed source or under-planted.

Pathway 2.4A
Community 2.4 to 2.5

White pine seeding in from natural seed source or under-planted.

Pathway 2.5B
Community 2.5 to 2.1

Elimination of repetitive clearcuttng and burning of stands. Lack of disturbance over time will cause this transition.

Pathway 2.5C
Community 2.5 to 2.3

This pathway occurs with fire when Jack pine seed sources is available or when planted.

Pathway 2.5A
Community 2.5 to 2.4

Aspen becomes established following repetitive clearcuttng and burning of early stages of pine and oak. These stands are being perpetuated through clear cutting.

State 3
Livestock Grazed Forest

Livestock grazed forests are more often referred to as woodlands rather than forests because this long-term land use significantly changes some soil characteristics and nature of vegetative community. Species composition is altered by selective browsing and grazing as well as by distribution of seeds and other propagules by grazing animals. In addition, soil compaction differentially affects germination and establishment of plant species, including trees.

State 4
Agricultural State

Production of agricultural crops, most often oats or hay. Routine usage of tillage, fertilizer, and other field practices.

Transition T1A
State 1 to 2

Stand-replacing disturbance, such as blow-down, or ice storm, followed by fire, or clear-cut logging, followed by natural regeneration or site preparation and planting.

Restoration pathway R2A
State 2 to 1

Time (50-100 years) and natural succession by white pine will lead back to the reference state. Minimal disturbance during the successional period.

Transition T2A
State 2 to 3

Prolonged grazing by livestock

Transition T2B
State 2 to 4

Elimination of forest cover and introduction of tilling, fertilizing an/or irrigation.

Restoration pathway R3A
State 3 to 2

Removal of livestock, natural succession. Results may be sped up by planting and initial outcomes will be heavily influenced by seed source and adjacent plant communities.

Transition T3A
State 3 to 4

Elimination of forest cover and introduction of tilling, fertilizing an/or irrigation.

Additional community tables

Supporting information

Inventory data references

Plot and other supporting inventory data for site identification and community phases is located on a NRCS North Central Region shared and one drive folder. University Wisconsin-Stevens Point described soils, took photographs, and inventoried vegetation data at community phases within the reference state. The data sources include WI ESD Plot Data Collection Form - Tier 2, Releve Method, NASIS pedon description, NRCS SOI 036, photographs, and Kotar Habitat Types.

Other references

Cleland, D.T.; Avers, P.E.; McNab, W.H.; Jensen, M.E.; Bailey, R.G., King, T.; Russell, W.E. 1997. National Hierarchical Framework of Ecological Units. Published in, Boyce, M. S.; Haney, A., ed. 1997. Ecosystem Management Applications for Sustainable Forest and Wildlife Resources. Yale University Press, New Haven, CT. pp. 181-200.

County Soil Surveys from Douglas, Bayfield, Washburn, Burnett, Polk, and Sawyer.

Curtis, J.T. 1959. Vegetation of Wisconsin: an ordination of plant communities. University of Wisconsin Press, Madison. 657 pp.

Finley, R. 1976. Original vegetation of Wisconsin. Map compiled from U.S. General Land Office notes. U.S. Forest Service, North Central Forest Experiment Station, St. Paul, Minnesota.

Hvizdak, David. Personal knowledge and field experience.

NatureServe. 2018. International Ecological Classification Satandard: Terrestrial Ecological Classifications. NautreServe Centreal Databases. Arlington, VA. U.S.A. Data current as of 28 August 2018.

Kotar, J. 1986. Soil – Habitat Type relationships in Michigan and Wisconsin. J. For. and Water Cons. 41(5): 348-350.

Kotar, J., J.A. Kovach and G. Brand. 1999. Analysis of the 1996 Wisconsin Forest Statistics by Habitat Type. U.S.D.A. For. Serv. N.C. Res. Stn. Gen. Tech. Rept. NC-207.

Kotar, J., J. A. Kovach, and T. L. Burger. 2002. A Guide to Forest Communities and Habitat Types of Northern Wisconsin. Second edition. University of Wisconsin-Madison, Department of Forest Ecology and Management, Madison.

Kotar, J., and T. L. Burger. 2017. Wetland Forest Habitat Type Classification System for Northern Wisconsin: A Guide for Land Managers and landowners. Wisconsin Department of Natural Resources, PUB-FR-627 2017, Madison.

Schulte, L.A., and D.J. Mladenoff. 2001. The original U.S. public land sur¬vey records: their use and limitations in reconstructing pre-European settlement vegetation. Journal of Forestry 99:5–10.

Schulte, L.A., and D.J. Mladenoff. 2005. Severe wind and fire regimes in northern forests: historical variability at the regional scale. Ecology 86(2):431–445.

Schulte, L.A., and D.J. Mladenoff. 2005. Severe wind and fire regimes in northern forests: historical variability at the regional scale. Ecology 86(2):431–445.

Soil Survey Staff. Input based on personal experience. Tim Miland, Scott Eversoll, Ryan Bevernitz, and Jason Nemecek.

United States Department of Agriculture, Natural Resources Conservation Service. 2022. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture, Agriculture Handbook 296.

Wisconsin Department of Natural Resources. 2015. The ecological landscapes of Wisconsin: An assessment of ecological resources and a guide to planning sustainable management. Wisconsin Department of Natural Resources, PUB-SS-1131 2015, Madison.

Contributors

Jacob Prater, Associate Professor at University of Wisconsin Stevens Point
John Kotar, Ecological Specialist- independent contract
Bryant Scharenbroch, Assistant Professor at University of Wisconsin Stevens Point

Approval

Suzanne Mayne-Kinney, 9/27/2023

Acknowledgments

NRCS contracted UWSP to write ecological sites for MLRA 91. Completed in 2021.

Rangeland health reference sheet

Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.

Author(s)/participant(s)
Contact for lead author
Date	09/27/2023
Approved by	Suzanne Mayne-Kinney
Approval date
Composition (Indicators 10 and 12) based on	Annual Production