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Ecological site R102CY058NE

Loamy Upland

Last updated: 6/28/2024
Accessed: 11/21/2024

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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.

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Figure 1. Mapped extent

Areas shown in blue indicate the maximum mapped extent of this ecological site. Other ecological sites likely occur within the highlighted areas. It is also possible for this ecological site to occur outside of highlighted areas if detailed soil survey has not been completed or recently updated.

MLRA notes

Major Land Resource Area (MLRA): 102C–Loess Uplands

Most of this area is in the Dissected Till Plains part of the Central Lowland Province of the Interior Plains. This MLRA has broad, undulating to rolling ridgetops and hilly to steep valley sides. The valleys are generally narrow, but broad flood plains and terraces are along the major rivers and the large tributaries. Elevation ranges from 335 to 610 meters (1,100 to 2,000 feet) increasing from southeast to northwest. Peorian age loess covers most of the area with depths ranging from 2 to 20 meters (6 to 70 feet). Glacial till underlies the loess in most areas. Bedrock can be found at or near the surface predominantly along the Missouri River valley found on the eastern side of the MLRA, but some bedrock can also be found in the northern part of 102C in Minnesota and South Dakota. The soils are predominantly Mollisols but Entisols are prominent in the floodplains of the area. Nearly all the area is farmed with 70% of the area being used as cropland for corn and soybeans. Feed grains and hay crops are also grown. The major resource concerns are wind erosion, water erosion, maintenance of organic matter and soil tilth, and soil moisture management. (USDA/NRCS 2006)

Classification relationships

"Silty" range sites for NE NRCS Vegetation Zones 3 & 4

NE Natural Heritage Program/NE Game & Parks Commission: "Upland Tallgrass Prairie"

Similar to R102BY010SD “Loamy”

General information for MLRA 102C:

*Fenneman (1916) Physiographic Regions*
Division - Interior Plains
East:
Province - Central Lowland
Section - Till Plains
West:
Province - Great Plains
Section - High Plains

*USFS (2007) Ecoregions*
Domain - Humid Temperate
Division - Prairie
Province - Prairie Parkland (Temperate)
Section - North-Central Glaciated Plains (251B)

*EPA Ecoregions (Omernik 1997)*
I - Great Plains (9)
II - Temperate Prairies (9.2)
III - Western Corn Belt Plains (9.2.3) IV - Loess Prairies (47a)
IV - Northeastern Nebraska Loess Hills (47k)
IV - Transitional Sandy Plain (47l)

Ecological site concept

This site occurs on higher, stable landscape positions and produces run-off, but gentler slopes generally allow for improved capture and storage of precipitation which produces well-developed soils with carbonates leached at least 25 centimeters (10 inches) below the soil surface.

Associated sites

R102CY050NE	Loamy Lowland Found in run-on positions, typically situated on upland drainages, foot slopes, and terraces.
R102CY059NE	Limy Upland Found in a similar run-off position but generally with steeper slopes.

R102CY050NE

Loamy Lowland

Found in run-on positions, typically situated on upland drainages, foot slopes, and terraces.

R102CY059NE

Limy Upland

Found in a similar run-off position but generally with steeper slopes.

Similar sites

R102CY059NE	Limy Upland Often intermixed, but steeper slopes reduce infiltration and soil development such that carbonates are not leached to the same degree and plant production is lower.
R102CY050NE	Loamy Lowland Species composition is very similar but with higher production due to additional run-on moisture.

R102CY059NE

Limy Upland

Often intermixed, but steeper slopes reduce infiltration and soil development such that carbonates are not leached to the same degree and plant production is lower.

R102CY050NE

Loamy Lowland

Species composition is very similar but with higher production due to additional run-on moisture.

Table 1. Dominant plant species

Tree	Not specified
Shrub	Not specified
Herbaceous	(1) Andropogon gerardii (2) Schizachyrium scoparium

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Physiographic features

This site predominantly occurs on nearly level to moderately steep hills, foot slopes, till plains, and interfluves (0-20% slopes). The slope generates runoff, has a water table greater than 203 centimeters (80 inches) deep, and does not flood or pond.

Table 2. Representative physiographic features

Landforms	(1) Hill (2) Interfluve (3) Till plain
Runoff class	Negligible to high
Elevation	1,150 – 1,800 ft
Slope	20%
Water table depth	80 in
Aspect	Aspect is not a significant factor

Climatic features

Most of the rainfall occurs as high-intensity, convective thunderstorms during the growing season. Peak precipitation occurs from the middle of spring to early in autumn. Winter precipitation occurs as snow (USDA/NRCS 2006).

The average annual temperature gradient trends higher from north (7°C / 45°F) to south (11°C/51°F).

The average annual precipitation gradient trends higher from northwest (64 centimeters / 25 inches) to southeast (79 centimeters / 31 inches).

The annual snowfall ranges from about 60 centimeters (24 inches) in the southern part of the area to 85 centimeters (34 inches) in the northern part.

The following data summary includes weather stations representing the full geographic extent of the MLRA, and is based on 70% probabilities (NOAA/UNL) meaning that actual observed climate conditions may fall outside these ranges 30% of the time. Furthermore, climatic events can manifest many different ways. For example, abnormally dry periods could occur as 3 consecutive drought years out of 10, 3 individual years separated by “normal” years, or some combination. Tree-ring records indicate that portions of the Great Plains have also historically experienced droughts lasting several decades, so plant community response will largely depend on the manner in which climatic variability is realized in interaction with past and current land management.

Table 3. Representative climatic features

Frost-free period (characteristic range)	125-129 days
Freeze-free period (characteristic range)	144-149 days
Precipitation total (characteristic range)	27-29 in
Frost-free period (actual range)	124-132 days
Freeze-free period (actual range)	143-158 days
Precipitation total (actual range)	27-30 in
Frost-free period (average)	127 days
Freeze-free period (average)	148 days
Precipitation total (average)	28 in

Characteristic range

Actual range

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Figure 2. Monthly precipitation range

Characteristic range

Actual range

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Figure 3. Monthly minimum temperature range

Characteristic range

Actual range

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Figure 4. Monthly maximum temperature range

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Figure 5. Monthly average minimum and maximum temperature

Figure 6. Annual precipitation pattern

Figure 7. Annual average temperature pattern

Climate stations used

(1) GENOA 2 W [USC00253185], Genoa, NE
(2) EWING [USC00252805], Ewing, NE
(3) WEST POINT [USC00259200], West Point, NE
(4) ROCK RAPIDS [USC00137147], Rock Rapids, IA
(5) FLANDREAU [USC00392984], Flandreau, SD
(6) SIOUX FALLS [USW00014944], Sioux Falls, SD

Soil features

These are predominantly very deep (moderately deep where residuum is present), well to somewhat excessively drained soils. The surface texture is predominantly silty clay loam, silt loam, or loam from 0 to 19 centimeters (0 to 8 inches) and the Subsurface Texture Group is Loamy from 19 to 203 centimeters (8 to 80 inches).

Rills and gullies are not inherent to this site. Water flow patterns, if present, should be irregular and disconnected, and pedestalling none to slight; although, both of these indicators may become more apparent as slope approaches the upper limit for the site. Soil aggregate stability should be high.

Major soils assigned to this site include Belfore, Dempster, Ihlen, Moody, and Nora

Table 4. Representative soil features

Parent material	(1) Loess (2) Till
Surface texture	(1) Silty clay loam (2) Silt loam (3) Loam
Family particle size	(1) Loamy
Drainage class	Well drained to somewhat excessively drained
Permeability class	Moderate to slow
Soil depth	20 – 80 in
Surface fragment cover <=3"	5%
Surface fragment cover >3"	2%
Available water capacity (0-40in)	4.9 – 9 in
Calcium carbonate equivalent (0-40in)	15%
Electrical conductivity (0-40in)	2 mmhos/cm
Sodium adsorption ratio (0-40in)	Not specified
Soil reaction (1:1 water) (0-40in)	5.6 – 9
Subsurface fragment volume <=3" (Depth not specified)	33%
Subsurface fragment volume >3" (Depth not specified)	3%

Ecological dynamics

While water is inherently limiting on most rangelands, relative to more arid regions energy capture (sunlight) is also a critical limiting resource, thereby making this site ideal for tallgrass communities. However, the favorable growing conditions and topography that historically made this the largest contributor to the “true prairie” habitat type in this MLRA have also made it one of the most extensively cropped in present time.

This site developed with fire as an integral part of the ecological processes and grassland maintenance. It is presumed that the historic fires generally occurred every 3-4 years, were randomly distributed, and ignited by lightning at various times throughout the summer when thunderstorms were likely to occur. Furthermore, it is also believed that pre-European inhabitants often used fire as a management tool for attracting herds of large migratory herbivores (bison, elk, and/or deer) as well as for warfare. However, the impact of fire over the past 100 years has been diminished due to human prevention and suppression of wildfire and the pervasive lack of cultural acceptance of prescribed fire as a surrogate (Helzer 2010).

The degree of herbivory (feeding on herbaceous plants) has a significant impact on the dynamics of the site. Historically, periodic grazing by herds of large migratory herbivores was a primary influence; however, herbivory by species such as insects, rodents, and root feeding organisms also impacted the vegetation historically and continue to this day (Helzer 2010). Human control of large herbivore impacts through grazing of domestic livestock and/or manipulation of wildlife populations has been a major contemporary influence on the ecological dynamics of the site (USDA/SCS 1977) and this management coupled with climate largely dictates the plant communities observed.

The reference state characterizes the historic natural condition, and has been determined by the study of rangeland relic areas, areas protected from excessive disturbance, and/or areas under compatible grazing regimes. Trends in plant community dynamics ranging from heavily grazed to unused areas, seasonal use pastures, and historical accounts have also been considered.

The following is a diagram illustrating predictable and recurring plant communities inherent to this site, and the pathways of change between them (Bestelmeyer 2010). The ecological processes will be discussed in more detail in the plant community descriptions following the diagram.

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. Native tallgrass

2. Native/invaded mix

3. Invasive dominant

4. Annual/pioneer

5. Evergreen dominant

States 1, 5 and 2 (additional transitions)

1. Native tallgrass

5. Evergreen dominant

2. Native/invaded mix

T1A	-	Reduced native grass competitiveness due to excessive defoliation intensity and frequency or drought
T1B	-	Severe disturbance
T1C	-	Cedar encroachment leading to woody plant dominance
R2A	-	Reduced invasive grass competitiveness allows for natives to dominant site
T2A	-	Reduced native competitiveness allows for introduced grass colonization and expansion
T2B	-	Severe disturbance; opportunistic species dominant
T2C	-	Cedar encroachment leading to woody plant dominance
T3A	-	Reduced invasive grass competitiveness allows for natives to increase
T3B	-	Severe disturbance; opportunistic species dominate
T3A	-	Cedar encroachment leading to woody plant dominance
R4A	-	Reduced invasive grass competitiveness allows for natives to dominant site
R5A	-	Restoration of plant community to native grasses

State 1 submodel, plant communities

1.1. Big bluestem-Little bluestem (Andropogon gerardii-Schizachyrium scoparium)

1.2. Little bluestem-Sideoats grama (Schizachyrium scoparium-Bouteloua curtipendula)

1.1A	-	Reduced tallgrass vigor due to excessive defoliation intensity and frequency; drought.
1.2A	-	Improved tallgrass vigor with adequate rest periods; return of normal precipitation.

State 2 submodel, plant communities

2.1. Subdominant Smooth brome-Kentucky bluegrass (Bromus inermis-Poa pratensis)

2.2. Codominant Smooth brome-Kentucky bluegrass (Bromus inermis-Poa pratensis)

2.1A	-	Cool-season grasses increase
2.2A	-	Native warm-season grasses increase in dominance

State 1
Native tallgrass

This state comprises the communities within the range of natural variability under historic conditions and disturbance regimes. Patterns created by wildlife use and fire would have created a mosaic of communities across the landscape; however, tall and/or mid warm-season grasses would remain dominant, with a subdominant contribution from native cool-season grasses, forbs, and shrubs. The cool-season contribution increases with latitude, with species such as needleandthread and green needlegrass becoming more prevalent northward. Fire and bison herbivory were the dominant disturbance regimes that historically maintained the tallgrass dominance with a diverse forb component. Furthermore, bison grazing was closely linked to fire patterns as the animals preferred grazing burned areas offering lush regrowth devoid of decadence and of higher nutritive quality. Thus, historic plant communities were subjected to occasional burning and grazing, with substantial rest/recovery periods as the fuel load rebuilt to eventually start the process again. Fire return intervals of 3-4 years served to suppress woody species, particularly non-sprouting eastern redcedar. The degree to which observed conditions represent this state largely depends on how closely the management has mimicked these past disturbance effects.

Dominant plant species

big bluestem (Andropogon gerardii), grass
little bluestem (Schizachyrium scoparium), grass

Community 1.1
Big bluestem-Little bluestem (Andropogon gerardii-Schizachyrium scoparium)

Figure 8. Loamy Upland 1.1

This is the reference plant community and can be found on areas that are managed to allow for adequate recovery periods following defoliation or drought stress. In addition to tallgrass vigor, suppression of woody species either through natural (e.g. fire) or artificial (e.g. chainsaw) methods is necessary to maintain herbaceous dominance. The plant community consists of 75-90% grasses and grass-likes, 5-10% forbs and 1-5% shrubs. Dominant grasses include big bluestem, little bluestem, porcupinegrass, and sideoats grama. Other grasses and grass-likes are indiangrass, blue grama, prairie junegrass, and sedges. Forb species are diverse and include prairieclovers, scurfpeas, and goldenrods. Common shrubs include leadplant and New Jersey tea (Kaul 2006, Steinauer 2010, USDA/NRCS 2012). This plant community is diverse, stable, and productive with nutrient and water cycles, and energy flow functioning near full potential. Plant litter is properly distributed with negligible movement off-site and natural plant mortality is very low. This community is resistant to many disturbances except continuous season-long heavy grazing, tillage, or non-use. Broadcast herbicide application will dramatically reduce non-target forb diversity and abundance. Total annual production, during an average year, ranges from 2400 to 4300 pounds per acre air-dry weight and will average 3500 pounds.

Dominant plant species

big bluestem (Andropogon gerardii), grass
little bluestem (Schizachyrium scoparium), grass

Figure 9. Annual production by plant type (representative values) or group (midpoint values)

Table 5. Annual production by plant type

Plant type	Low (lb/acre)	Representative value (lb/acre)	High (lb/acre)
Grass/Grasslike	2100	2975	3500
Shrub/Vine	150	262	400
Forb	150	263	400
Total	2400	3500	4300

Figure 10. Plant community growth curve (percent production by month). NE1021, 102C Warm-season. Warm-season grass, MLRA 102C.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
0	0	2	7	18	23	26	16	6	2	0	0

Community 1.2
Little bluestem-Sideoats grama (Schizachyrium scoparium-Bouteloua curtipendula)

Figure 11. Loamy Upland 1.2

This community largely resembles central Great Plains mixed-grass prairies where rainfall is more limiting and overall conditions are relatively drier. Tallgrasses remain an important component, but midgrasses - typically sideoats grama and little bluestem - dominate site structure and function. While still within the range of natural variability, energy capture, nutrient cycling, and hydrology are not functioning at their full potential relative to the reference condition. Reduced photosynthetic biomass does not capture as much light energy, less lignified plant material produces lower quality litter (e.g. less persistent, more easily transported), and reduced soil protection impairs the site''s ability to capture and retain moisture.

Dominant plant species

little bluestem (Schizachyrium scoparium), grass
sideoats grama (Bouteloua curtipendula), grass

Figure 12. Plant community growth curve (percent production by month). NE1021, 102C Warm-season. Warm-season grass, MLRA 102C.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
0	0	2	7	18	23	26	16	6	2	0	0

Pathway 1.1A
Community 1.1 to 1.2

Big bluestem-Little bluestem (Andropogon gerardii-Schizachyrium scoparium)

Little bluestem-Sideoats grama (Schizachyrium scoparium-Bouteloua curtipendula)

Events which remove tallgrass growing points and photosynthetic tissues without adequate recovery periods will shift community composition towards shorter statured species, particularly little bluestem and sideoats grama. Likewise, shortgrasses such as hairy and/or blue grama may also proliferate. As cattle grazing pressure increases/persists, rhizomatous grasses may assume a more sodbound growth habit which can further reduce overall diversity and adversely affect both infiltration and litter. Periods of extended drought can have similar impacts on species composition and bring about a shift towards mixed/shortgrass prairie species more tolerant of drier conditions.

Pathway 1.2A
Community 1.2 to 1.1

Little bluestem-Sideoats grama (Schizachyrium scoparium-Bouteloua curtipendula)

Big bluestem-Little bluestem (Andropogon gerardii-Schizachyrium scoparium)

Management that provides adequate recovery periods and does not annually prevent tallgrass seedset or otherwise impair vigor will facilitate a return to community phase 1.1. In the case of dought, the return to more typical precipitation patterns will promote shift towards tallgrass species.

State 2
Native/invaded mix

This state can manifest three ways: 1) the appearance of introduced cool-season grasses, 2) the expansion of deciduous shrubs and/or trees, or 3) some combination of these. Kentucky bluegrass and smooth brome are the primary cool-season grass invaders in this region, commonly found in roadsides, disturbed areas, and pastures intentionally seeded for cool-season forage. Management practices and/or environmental conditions that are not favorable to native grass vigor may allow introduced grasses to invade the site thereby decreasing native diversity and abundance, particularly of forbs. In the absence of the historic fire regime, woody deciduous species may also expand to become an influential component of the community. The invasive component tends to have very high reslience, is extremely difficult to eradicate, and what might be considered a new "contemporary" range of natural variability is seen as competition between the native grasses and introduced/woody species for space and resources.

Dominant plant species

little bluestem (Schizachyrium scoparium), grass
sideoats grama (Bouteloua curtipendula), grass
smooth brome (Bromus inermis), grass
Kentucky bluegrass (Poa pratensis), grass

Community 2.1
Subdominant Smooth brome-Kentucky bluegrass (Bromus inermis-Poa pratensis)

While native grasses still dominate the site, introduced cool-season species have established a foothold in the system and can be found interspersed throughout the stand. The stand may still have a native tallgrass appearance overall, but bluegrass and/or brome can be easily found. Deciduous shrub/tree species may also have begun to expand into areas where they did not persist historically, but the overall appearance can vary depending on the propagation method of a particular species. Seed propagated species, such as Siberian elm, tend to colonize further from the parent plant and affect larger areas, but in lower densities. In contrast, rhizomatous species such as smooth sumac tend to progress as a higher-density encroachment spreading directly from the parent plants.

Dominant plant species

little bluestem (Schizachyrium scoparium), grass
sideoats grama (Bouteloua curtipendula), grass
smooth brome (Bromus inermis), grass
Kentucky bluegrass (Poa pratensis), grass

Figure 13. Plant community growth curve (percent production by month). NE1022, Warm-season dominant, cool-season subdominant.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
0	0	2	9	19	23	24	13	7	3	0	0

Community 2.2
Codominant Smooth brome-Kentucky bluegrass (Bromus inermis-Poa pratensis)

This community is comprised of a relatively even mix of native grasses and invasive species overall. This may manifest as a well-distributed interspersion of natives and invaders, as distinct patches wherein competitors dominate locally, or some combination. Forb diversity and abundance is further diminished.

Dominant plant species

little bluestem (Schizachyrium scoparium), grass
smooth brome (Bromus inermis), grass
sideoats grama (Bouteloua curtipendula), grass
Kentucky bluegrass (Poa pratensis), grass

Figure 14. Plant community growth curve (percent production by month). NE1023, Warm-season, cool-season codominant.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
0	0	3	10	23	26	16	10	7	4	1	0

Pathway 2.1A
Community 2.1 to 2.2

Management and/or environmental conditions have afforded a persisting competitive advantage to introduced cool-season grasses, and they begin to dominate the ecological dynamics of the site. The robust invasive component is able to quickly and effectively exploit opportunities to outcompete and displace natives. Repeated summer use of an area will place the bulk of stressor impacts on native plants, reducing native vigor and allowing invaders to thrive. Likewise, a climate pattern limiting natural moisture to the spring and fall months coincides with peak cool-season growth and may support a similar process.

Pathway 2.2A
Community 2.2 to 2.1

The native component remains in an abundance that can facilitate a return towards more historic conditions if management is modified to shift stressor impacts to the invasive species, and promote warm-season grass vigor. Environmental conditions and/or disturbance regimes that strongly favor warm-season grasses can also trend the site towards the reference.

State 3
Invasive dominant

Introduced cool-season invasion has progressed to the point that native species comprise a negligible portion of the community and the aggressively rhizomatous invasives preclude native germination and seedling survival. The native component may be completely absent, and the site resembles a seeded pasture. Alternatively, the dominant invasives may be deciduous woody species. Woody competitiveness for sunlight, water, space, and other resources continues to increase as desirable herbaceous species are shaded out, crowded out, or otherwise suppressed.

Dominant plant species

smooth brome (Bromus inermis), grass
Kentucky bluegrass (Poa pratensis), grass

Community 3.1
Smooth brome-Kentucky bluegrass (Bromus inermis-Poa pratensis)

Figure 15. Loamy Upland 3.1

This community is typically composed of smooth brome with bluegrass interspersed among the brome tillers. Warm-season natives, if present, are sparse yet often conspicuous due to pronounced differences in growth habits and metabolic pathways. Community structure and function have been dramatically simplified relative to the reference condition, and very few biotic functional groups are represented in amounts that would influence ecological function. The invasive grass root skein provides good site stability; however, replacement of the deeper roots and complex bunchgrass canopy with the shallower roots and erect tiller canopy of the invaders results in reduced interception and infiltration rates.

Dominant plant species

smooth brome (Bromus inermis), grass
Kentucky bluegrass (Poa pratensis), grass

Figure 16. Plant community growth curve (percent production by month). NE1024, Cool-season. Smooth brome/Kentucky bluegrass.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
0	0	4	13	25	28	8	6	9	5	2	0

State 4
Annual/pioneer

Nutrient cycling, hydrologic function, and/or soil stability have been severely altered, and possibly compromised. This is a highly variable state in which the specific plants observed will depend largely on the original community and the nature of the disturbance. This condition encompasses (but is not necessarily limited to) events such as severe fire impacts, heavy continuous grazing, heavy nutrient inputs, and abandoned cropland.

Dominant plant species

snow on the mountain (Euphorbia marginata), other herbaceous
ragweed (Ambrosia), other herbaceous
Texas croton (Croton texensis), other herbaceous
nightshade (Solanum), other herbaceous
thistle (Cirsium), other herbaceous

Community 4.1
Variable native and introduced

Figure 17. Loamy Upland 4.1

This community is heavily dominated by annual plants that thrive in disturbed areas and often includes snow-on-the-mountain, annual ragweed, Texas croton, nightshades, and/or hoary verbena. It is also particularly vulnerable to noxious weed invasion with the most common species being plumeless, musk, and Canada thistles. Leafy spurge becomes more common northward in the MLRA.

Dominant plant species

snow on the mountain (Euphorbia marginata), other herbaceous
ragweed (Ambrosia), other herbaceous
Texas croton (Croton texensis), other herbaceous
nightshade (Solanum), other herbaceous
thistle (Cirsium), other herbaceous

State 5
Evergreen dominant

Left unchecked, the spatial extent of eastern redcedar encroachment has expanded, and the individual trees have grown substantially. The areas under and near individual cedars experience profoundly altered function through shading, evergreen litter, and suppressed herbaceous understory. The woody overstory now dictates certain disturbance responses, and prescribed fire options become increasingly problematic as any fire will be largely carried by the volatile evergreen canopy instead of the herbaceous understory.

Dominant plant species

eastern redcedar (Juniperus virginiana), tree

Community 5.1
Eastern redcedar (Juniperus virginiana)

Figure 18. Loamy Upland 5.1

Cedars have reached stature and abundance that is beyond the range of natural variability, and the remaining herbaceous component is restricted to cedar interspaces. Evergreen canopy and litter serve to dramatically increase interception, capture, and eventual evaporation of precipitation thereby further reducing the resources available for grasses and forbs. Without intervention, woody canopy will progress towards complete closure under which herbaceous species will eventually disappear completely.

Dominant plant species

eastern redcedar (Juniperus virginiana), tree

Transition T1A
State 1 to 2

In the presence of introduced cool-season grasses, environmental conditions and/or management that reduces native vigor and stand resilience, and frees up resources (space, sunlight, nutrients, water) will allow for colonization of Kentucky bluegrass and smooth brome. Likewise, similar processes may also allow for deciduous woody shrubs and trees such as smooth sumac, roughleaf dogwood, and Siberian elm to expand.

Transition T1B
State 1 to 4

There are many possible triggers for this transition that may occur as acute events (e.g. plowing) or cumulative impacts of chronic events (e.g. long-term undermanaged grazing.) The absence of deep-rooted perennial cover exposes the site to topsoil loss, open nutrient cycle, and free space which collectively allow for opportunistic annual species to dominate.

Transition T1C
State 1 to 5

The presence of an invasion source coupled with fire exclusion allows cedar seeds to germinate and establish within the herbaceous stand. This typically begins near fencerows, woody draws, etc, and accelerates outward as propagules increase. Lack of intervening action allows cedar expansion to continue, and tree sizes to increase. Cedar will eventually modify site function in ways that promote further encroachment such as rainfall interception and stemflow, heavy duff litter, and shading of the herbaceous understory.

Restoration pathway R2A
State 2 to 1

Eradication of introduced cool-season grasses from this site will require long-term, targeted management efforts to create an adverse environment during the spring and late fall when bluegrass and brome are most actively growing, with favorable conditions during the summer to promote native warm-season species. Targeted practices such as prescribed burning, flash grazing, and herbicide are often employed at strategic times of the year to set back undesirable species. The combination of practices should strive to mimic the historic disturbance regimes to which the desirable native species are best adapted.

Transition T2A
State 2 to 3

If the conditions which initiated and fomented the colonization and expansion of cool-season invasion are not removed or mitigated, stand composition will continue to shift in this direction and begin to resemble a monoculture of bluegrass and/or brome. Due to the dense rhizomatous root mat of brome and bluegrass, native species suffer decreasing opportunities to contribute propagules, and individual plants lost are not replaced by desirable natives.

Transition T2B
State 2 to 4

Transition T2C
State 2 to 5

Transition T3A
State 3 to 2

Aggressive intervening actions will be required to simultaneously recolonize native grasses and suppress vigor in undesirable species. Restoration follows the same principles as the R2A pathway, but may also require native range seeding if the latent seedbank is inadequate.

Transition T3B
State 3 to 4

Transition T3A
State 3 to 5

Restoration pathway R4A
State 4 to 1

With favorable weather and site stability, it may take just a few years for the site to naturally return to a perennial community. Range seeding can “jump start” the recolonization of desirable species and may re-establish a near reference grass community; although, forb diversity may take longer to recover. Depending on the nature of the disturbance(s), additional ameliorative efforts may be necessary to mitigate accelerated erosion and weedy competition until the seeded perennial community has stabilized. It is possible for a disturbance and/or subsequent processes (e.g. accelerated erosion) to profoundly, and even permanently, alter fundamental soil properties in such a way that the site may never again exhibit its historic structure or function without extraordinary restoration inputs.

Restoration pathway R5A
State 5 to 1

Tree mortality is required to restore a grassland state, however the herbaceous response will depend on many factors such as method(s) used, mortality rates, and the remnant herbaceous species. Mechanical and chemical methods can remove cedars but will have little if any notable impact on the herbs. Reintroducing the historic fire regime will provide the most profound and beneficial effects, and seasonal timing and burn intensity can have significant influence on the herbaceous outcome. As a general rule, hot spring burns will not only kill trees but also stress shallower-rooted invasive cool-season grasses and promote a ahift in favor of the reference community.

Additional community tables

Table 6. Community 1.1 plant community composition

Group	Common name	Symbol	Scientific name	Annual production (lb/acre)	Foliar cover (%)
Grass/Grasslike
1	Tall warm-season			1575–2100
	big bluestem	ANGE	Andropogon gerardii	700–1050	–
	switchgrass	PAVI2	Panicum virgatum	175–350	–
	Indiangrass	SONU2	Sorghastrum nutans	175–350	–
	composite dropseed	SPCO16	Sporobolus compositus	0–175	–
	prairie dropseed	SPHE	Sporobolus heterolepis	0–175	–
2	Mid warm-season			875–1750
	little bluestem	SCSC	Schizachyrium scoparium	525–1050	–
	sideoats grama	BOCU	Bouteloua curtipendula	175–525	–
	purple lovegrass	ERSP	Eragrostis spectabilis	0–175	–
3	Shortgrasses			0–350
	blue grama	BOGR2	Bouteloua gracilis	0–350	–
	buffalograss	BODA2	Bouteloua dactyloides	0–175	–
4	Cool-season			300–1050
	porcupinegrass	HESP11	Hesperostipa spartea	0–525	–
	needle and thread	HECO26	Hesperostipa comata	0–350	–
	western wheatgrass	PASM	Pascopyrum smithii	175–350	–
	Scribner's rosette grass	DIOLS	Dichanthelium oligosanthes var. scribnerianum	0–175	–
	fall rosette grass	DIWI5	Dichanthelium wilcoxianum	0–175	–
	Canada wildrye	ELCA4	Elymus canadensis	0–175	–
	prairie Junegrass	KOMA	Koeleria macrantha	0–175	–
	green needlegrass	NAVI4	Nassella viridula	0–175	–
5	Grass-like			175–350
	heavy sedge	CAGR4	Carex gravida	0–175	–
	sun sedge	CAINH2	Carex inops ssp. heliophila	0–175	–
	Mead's sedge	CAME2	Carex meadii	0–175	–
	sedge	CAREX	Carex	0–175	–
Forb
6	Forb			175–350
	Baldwin's ironweed	VEBA	Vernonia baldwinii	35–175	–
	hoary verbena	VEST	Verbena stricta	0–105	–
	western yarrow	ACMIO	Achillea millefolium var. occidentalis	0–105	–
	Cuman ragweed	AMPS	Ambrosia psilostachya	0–105	–
	candle anemone	ANCY	Anemone cylindrica	0–105	–
	field pussytoes	ANNE	Antennaria neglecta	0–105	–
	white sagebrush	ARLU	Artemisia ludoviciana	0–105	–
	groundplum milkvetch	ASCR2	Astragalus crassicarpus	0–105	–
	false boneset	BREU	Brickellia eupatorioides	0–105	–
	white prairie clover	DACA7	Dalea candida	0–105	–
	purple prairie clover	DAPU5	Dalea purpurea	0–105	–
	Illinois ticktrefoil	DEIL2	Desmodium illinoense	0–105	–
	blacksamson echinacea	ECAN2	Echinacea angustifolia	0–105	–
	Maximilian sunflower	HEMA2	Helianthus maximiliani	0–105	–
	stiff sunflower	HEPA19	Helianthus pauciflorus	0–105	–
	dotted blazing star	LIPU	Liatris punctata	0–105	–
	rush skeletonplant	LYJU	Lygodesmia juncea	0–105	–
	stiff goldenrod	OLRI	Oligoneuron rigidum	0–105	–
	western marbleseed	ONBEO	Onosmodium bejariense var. occidentale	0–105	–
	purple locoweed	OXLA3	Oxytropis lambertii	0–105	–
	prairie groundsel	PAPL12	Packera plattensis	0–105	–
	silverleaf Indian breadroot	PEAR6	Pediomelum argophyllum	0–105	–
	large Indian breadroot	PEES	Pediomelum esculentum	0–105	–
	large beardtongue	PEGR7	Penstemon grandiflorus	0–105	–
	upright prairie coneflower	RACO3	Ratibida columnifera	0–105	–
	prairie blue-eyed grass	SICA9	Sisyrinchium campestre	0–105	–
	compassplant	SILA3	Silphium laciniatum	0–105	–
	Missouri goldenrod	SOMI2	Solidago missouriensis	35–105	–
	white heath aster	SYER	Symphyotrichum ericoides	0–105	–
	aromatic aster	SYOB	Symphyotrichum oblongifolium	0–105	–
Shrub/Vine
7				175–350
	Jersey tea	CEHE	Ceanothus herbaceus	0–175	–
	prairie rose	ROAR3	Rosa arkansana	0–175	–
	western snowberry	SYOC	Symphoricarpos occidentalis	0–175	–
	smooth sumac	RHGL	Rhus glabra	0–105	–
	leadplant	AMCA6	Amorpha canescens	0–105	–

Interpretations

Animal community

This site is well adapted to managed grazing by domestic livestock. The predominance of herbaceous plants across all plant community phases best lends these sites to grazing by cattle but browsing livestock such as goats or sheep that will more heavily utilize invasive forbs and brush. Carrying capacity and production estimates are conservative estimates that should be used only as guidelines in initial stages of grazing lands planning.

Often, the plant community does not entirely match any particular plant community (as described in the ecological site description). Because of this, a resource inventory is necessary to document plant composition and production. Proper interpretation of this inventory data will permit the establishment of a safe, initial stocking rate for the type and class of animals and level of grazing management. Grazing by domestic livestock is one of the major income-producing industries in the area. Rangeland in this area may provide year-long forage for cattle, sheep, or horses. During the dormant period, the protein levels of the forage may be lower than the minimum needed to meet livestock (primarily cattle and sheep) requirements.

Suggested stocking rates (carrying capacity*) for cattle under continuous season-long grazing under normal growing conditions are listed below:

- 1.1 Big bluestem-Little bluestem; 3500 lbs/acre production and 0.96 AUM/acre

- 1.2 Little bluestem-Sideoats grama; 3000 lbs/acre production and 0.82 AUM/acre

- 2.1 Subdominant smooth brome-KY bluegrass; 2700 lbs/acre production and 0.74 AUM/acre

- 2.2 Codominant smooth brome-KY bluegrass; 2400 lbs/ac and 0.66 AUM/acre with 50% or more introduced cool-season component

- 3.1 Smooth brome-KY bluegrass; 2750 lbs/ac and .75 AUM/ac, unfertilized, non-irrigated naturalized community. Refer to Forage Suitability Groups for cool-season pasture under a higher management level.

*Carrying capacity based on continuous season-long grazing by cattle under average growing conditions, 25% harvest efficiency. Air dry forage requirements based on 3% of animal body weight, or 912 lbs/AU/month.

If grazing distribution problems occur, stocking rates must be reduced to maintain plant health and vigor. Carrying capacity and production estimates are conservative estimates that should be used only as guidelines in the initial stages of the conservation planning process. Utilizing a rotational grazing system that allows for adequate rest and recovery will increase plant vigor and carrying capacity. Often, the current plant composition does not entirely match any particular plant community (as described in this ecological site description). Because of this, a field visit is recommended to document plant composition and production. More precise carrying capacity estimates can be calculated based on actual site information along with animal preference data, particularly when livestock other than cattle are involved. With consultation of the land manager, more intensive grazing management may result in improved harvest efficiencies and increased carrying capacity.

Supporting information

Inventory data references

Information presented here has been derived from RANGE-417 archives, Rangeland NRI, and other inventory data. Field observations from range-trained personnel were also used. In addition to the multitude of NRCS field office employees and private landowners that helped with site visits and local knowledge, those involved in developing this site include:

Nebraska NRCS:
Nadine Bishop, State Rangeland Management Specialist
Patrick Cowsert, Resource Soil Scientist
Cassidy Gerdes, Biologist
Dirk Schultz, Soil Conservationist
Dan Shurtliff, Asst State Soil Scientist

South Dakota NRCS:
Stan Boltz, State Rangeland Management Specialist
Shane Deranleau, Area Rangeland Management Specialist
Kevin Luebke, State Biologist

Iowa NRCS:
Jess Jackson, Area Grazing Specialist

Minnesota NRCS:
Lance Smith, Area Grazing Specialist

MLRA Office 10:
Stu McFarland, Ecological Site Inventory Specialist, QC
Stacey Clark, Ecological Site Inventory Specialist, QA
Michael Whited, Soil Data Quality Specialist
Jo Parsley, Soil Scientist/10-3 MSSO Leader

National Soil Survey Center:
Mike Kucera, National Agronomist, Soil Quality & Ecosystems
Steve Peaslee, GIS Specialist, Soil Survey Interpretations

Nebraska Game & Parks Commission:
Gerry Steinauer, Botanist
Scott Wessel, Biologist
Russ Hamer, Biologist
Rebekah Jessen, Biologist

Nebraska Forest Service:
Steve Rasmussen, District Forester

Other references

Bestelmeyer, Brandon, et al. 2010. Practical Guidance for Developing State-and-transition Models. Rangelands 32:6 pp 2-64. Wheat Ridge, CO: Society for Range Management.

Fenneman, Nevin M. 1916. Physiographic Subdivision of the United States. Annals of the Association of American Geographers.

Helzer, Chris. 2010. The Ecology and Management of Prairies in the Central U.S. Iowa City, IA: University of Iowa Press/The Nature Conservancy.

Kaul, Robert B., David Sutherland, and Steven Rolfsmeier. 2006. The Flora of Nebraska. Lincoln, NE: University of Nebraska – Lincoln (Conservation and Survey Division, School of Natural Resources.)

NOAA/UNL – High Plains Regional Climate Center. Historical Data Summaries: http://www.hprcc.unl.edu/data/historical/

Omernik, J.M. 1997. Ecoregions of the Conterminous United States. Annals of the Association of American Geographers, v.77, no. 1, p.118-125.

Steinauer, Gerry and Steve Rolfsmeier. 2010. Terrestrial Ecological Systems and Natural Communities of Nebraska. Lincoln, NE: Nebraska Natural Heritage Program and Nebraska Game and Parks Commission.

USDA/USFS. 2007. Ecological Subregions: Sections and Subsections for the Conterminous United States. Washington, DC: USDA - Forest Service.

USDA/SCS. 1977. Rangeland Resources of Nebraska. Lincoln, NE: Society for Range Management. USDA/NRCS. 2011. ESD User Guide. Fort Worth, TX: Central National Technology Support Center.

USDA/NRCS 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.

USDA/NRCS. 2012. Field Office Technical Guide (Nebraska, Natural Resources Information, Statewide Soil and Site Information, Rangeland Interpretations, Nebraska Range Site Descriptions – Vegetative Zones 3 and 4), U.S. Department of Agriculture, Natural Resources Conservation Service, Nebraska Ecological Sciences.

Contributors

Greg Clark (Greg.Clark@usda.gov) Soil Survey Office Leader, USDA-NRCS, Stanton NE
Stu McFarland

Approval

Suzanne Mayne-Kinney, 6/28/2024

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)	Stu McFarland, Nadine Bishop
Contact for lead author
Date	08/01/2013
Approved by	Suzanne Mayne-Kinney
Approval date
Composition (Indicators 10 and 12) based on	Annual Production