Natural Resources
Conservation Service
Ecological site R053AE070MT
Subirrigated (Sb) (Legacy) RRU 53AE
Last updated: 6/14/2023
Accessed: 11/21/2024
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.
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.
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
Not specified |
Herbaceous |
Not specified |
Physiographic features
This site usually occurs on terraces and floodplain steppes, near springs or seeps, or other areas having a seasonal water table close enough to the surface to influence plant composition and production. These areas are rarely flooded or non-flooded. “Rare” indicates there is a 0- 5% chance of flooding in any year. The site has a seasonal water table at 24” – 42”. Slopes vary from 0-2% and occur on all exposures. Elevations generally range from 2,000 to 3,100 feet.
Table 2. Representative physiographic features
Landforms |
(1)
Terrace
(2) Hill (3) Flood plain |
---|---|
Flooding duration | Brief (2 to 7 days) |
Flooding frequency | None to rare |
Ponding frequency | None |
Elevation | 572 – 1,067 m |
Slope | 0 – 2% |
Water table depth | 61 – 107 cm |
Aspect | Aspect is not a significant factor |
Climatic features
A semi-arid, temperate climate characterizes the Glaciated Plains. The predominance of cool season species has evolved to take advantage of the precipitation regime that peaks in late spring-early summer (June). Seventy-five percent of the annual precipitation usually falls as steady, soaking, frontal system rains. Summer rains usually come with thunderstorms. Precipitation is the most important factor influencing production (Heitschmidt et al 2005). Severe drought occurs on average in two out of every ten years (Cooper, et al., 2001).
Table 3. Representative climatic features
Frost-free period (average) | 129 days |
---|---|
Freeze-free period (average) | 104 days |
Precipitation total (average) | 305 mm |
Figure 2. Annual precipitation pattern
Figure 3. Annual average temperature pattern
Influencing water features
Soil features
Soils are deep to very deep with a seasonal water table within about three feet of the surface. These soils are non-hydric. Soils are somewhat poorly drained, and more than 72 inches deep. Permeability varies from moderately slow to slow. The surface layer of these soils vary from 3-12 inches in depth and are typically a loam, silt loam, clay loam, or sandy loam. Textures of underlying layers also vary since these are alluvial soils, having been deposited by flowing water. Soil ph varies from 6.6-8.4. The following soil components characterize this site: Saypo and MacKenzie.
Table 4. Representative soil features
Surface texture |
(1) Loam (2) Sandy loam (3) Clay loam |
---|---|
Drainage class | Somewhat poorly drained |
Permeability class | Moderately slow to very slow |
Soil depth | 102 – 183 cm |
Surface fragment cover <=3" | 0% |
Surface fragment cover >3" | 0% |
Available water capacity (0-101.6cm) |
12.7 – 17.78 cm |
Calcium carbonate equivalent (0-101.6cm) |
0 – 10% |
Electrical conductivity (0-101.6cm) |
0 – 2 mmhos/cm |
Sodium adsorption ratio (0-101.6cm) |
0 – 8 |
Soil reaction (1:1 water) (0-101.6cm) |
6.6 – 8.4 |
Subsurface fragment volume <=3" (Depth not specified) |
0 – 1% |
Subsurface fragment volume >3" (Depth not specified) |
0 – 1% |
Ecological dynamics
This ecological site developed under Northern Great Plains climatic conditions. At the time that North America was settled by Europeans, the Glaciated Plains was the home of nomadic tribes and large numbers of bison, prairie dogs, elk, pronghorn, bighorn sheep and deer. These herbivores have been present on the plains since the retreat of the Pleistocene glaciers and greatly influenced the mixed grass prairie ecosystem. Much of the landscape burned at intervals of 5-7 years, either as a result of lightning or environmental manipulations by the Native Americans (Frost 1998).
Plant community interpretations are based on the Historic Climax Plant Community (HCPC). The HCPC is the plant community that is best adapted to the unique combination of factors associated with this ecological site. It was in a natural dynamic equilibrium with the historic biotic, abiotic, and climatic factors at the time of European immigration and settlement. This site is highly resilient to disturbance.
Changes in the HCPC are brought about by frequency, timing and intensity of past grazing use, series of dry or wet years, or disturbances by fire, insect infestations, noxious weed invasions, etc. Continual adverse impacts to the site over a period of years results in a departure from the HCPC. As the HCPC regresses to lower seral stages, the deep-rooted perennial grasses are replaced by the introduced bluegrasses (Kentucky and Canada) and lower successional species (Baltic rush, sedges, foxtail barley, curlydock, and annual forbs). The dominance of these short grasses, low successional warm season forbs and half-shrubs, and invasive species in the plant community disrupts ecological processes, impairs the biotic integrity of the site, and adversely affects resiliency. The system’s ability to recover to higher seral states is restricted or impeded.
State and Transition Diagram
Traditional theories of plant succession leading to a single climax community are inadequate for understanding the complex successional pathways of Subirrigated 10-14” p.z. ecological sites in the Glaciated Plains. The ecological site is more aptly described using state-and-transition vegetation dynamics in a non-linear framework. A “state” is an alternative, persistent vegetation community that is not simply reversible in the linear successional framework (Stringham 2003). States are depicted as seral stages, while pathways between states are “transitions.” The latter can be transient or persisting (crosses a threshold). Transitions are triggered by climatic events, fire, grazing, farming, burning, etc.
Three important plant communities and associated successional pathways for the Reference state (State #1) are illustrated below for the Subirrigated 10-14” p.z. ecological site in the eastern Glaciated Plains. The diagram also depicts a transition from Plant Community B to State 2 (Community C) and a possible transition from the Reference State to State 3 (Community D).
State and transition model
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State 1 submodel, plant communities
State 2 submodel, plant communities
State 3 submodel, plant communities
State 1
State #1: Historic Climax Plant Community (HCPC)
Community 1.1
State #1: Historic Climax Plant Community (HCPC)
The interpretive plant community for this site is the Historic Climax Plant Community (HCPC). Warm and cool season tall and mid-grasses (such as switchgrass, prairie cordgrass, big bluestem, western wheatgrass, slender wheatgrass, bearded wheatgrass, mat muhly, and tall reedgrasses) dominate the HCPC. These grasses represent about 80% of the total annual plant production in the community. Short grasses, sedges and rushes make up another 5% of the total annual production. Dotted blazing-star, meadow hawksbeard, lance-leaf goldenweed, goldenrods, maximilian sunflower, cinquefoil, and blue-eyed grass are important forbs. Total forb production normally represents less than 10% of the total annual production. Buffaloberry, willows, chokecherry, snowberry, shrubby cinquefoil, and rose are important shrubs. Overall, shrubs account for about 10% of the annual plant production. Historic NRCS data indicate that total annual production on this site varies from 5000 lbs/ac in favorable years to 3500 lbs/ac in unfavorable years. Annual production averages 4000 lbs/ac. This site was rarely sampled in the range inventory (in 2001 and 2004) on the Fort Peck and Fort Belknap Indian Reservations. Therefore, the production estimate for the HCPC could not be refined with more recent data. Average annual production is expected to be slightly higher or lower, respectively on more mesic and xeric portions of the eastern Glaciated Plains. This plant community is well adapted to the climatic conditions of the glaciated plains and to the presence of a permanent water table. The diversity of plant species helps make the site resistant to environmental changes. The functional and structural diversity of plant species (perennials, cool and warm season grasses, sedges, forbs and shrubs) optimize the capture of solar energy and maximize subsequent plant growth through the efficient use of available soil water and nutrient cycling. Continued adverse disturbances reduce the competitiveness of perennial plants, and precipitate the replacement of high successional species with lower successional grasses, forbs, shrubs, and annual species. With proper grazing management and a “natural” fire regime, more species found at HCPC will replace these lower successional species within a few years. Litter is in contact with 55% of the soil surface. Plant litter remains in place and is not moved by erosional forces. Less than 1% of the soil surface should be bare, or unprotected by litter, rock, moss, and plant canopy. Rills should not be present and water flow patterns should be barely observable.
Figure 4. Annual production by plant type (representative values) or group (midpoint values)
Table 5. Annual production by plant type
Plant type | Low (kg/hectare) |
Representative value (kg/hectare) |
High (kg/hectare) |
---|---|---|---|
Grass/Grasslike | 3335 | 3811 | 4764 |
Forb | 392 | 448 | 560 |
Shrub/Vine | 196 | 224 | 280 |
Total | 3923 | 4483 | 5604 |
Table 6. Ground cover
Tree foliar cover | 0% |
---|---|
Shrub/vine/liana foliar cover | 0% |
Grass/grasslike foliar cover | 0% |
Forb foliar cover | 0% |
Non-vascular plants | 0-5% |
Biological crusts | 0-2% |
Litter | 50-55% |
Surface fragments >0.25" and <=3" | 0-1% |
Surface fragments >3" | 0-1% |
Bedrock | 0% |
Water | 0-1% |
Bare ground | 0% |
Table 7. Soil surface cover
Tree basal cover | 0% |
---|---|
Shrub/vine/liana basal cover | 1-5% |
Grass/grasslike basal cover | 30-35% |
Forb basal cover | 5-10% |
Non-vascular plants | 0% |
Biological crusts | 0% |
Litter | 0% |
Surface fragments >0.25" and <=3" | 0% |
Surface fragments >3" | 0% |
Bedrock | 0% |
Water | 0% |
Bare ground | 0% |
Table 8. Canopy structure (% cover)
Height Above Ground (m) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
---|---|---|---|---|
<0.15 | – | 0-10% | 5-15% | 5-15% |
>0.15 <= 0.3 | – | 20-30% | 1-15% | 25-35% |
>0.3 <= 0.6 | – | 25-35% | 35-45% | 35-45% |
>0.6 <= 1.4 | – | 25-35% | 30-40% | 15-25% |
>1.4 <= 4 | – | 5-15% | 0-10% | – |
>4 <= 12 | – | – | – | – |
>12 <= 24 | – | – | – | – |
>24 <= 37 | – | – | – | – |
>37 | – | – | – | – |
Community 1.2
Plant Community A (State #1)
*Successional pathway from HCPC to Community A (State #1): Successional pathways from the HCPC are influenced by frequency, timing and intensity of grazing, precipitation patterns, fire, insect infestations, noxious weed invasions, etc. As communities regress from HCPC, medium and short grasses increase at the expense of mid and tall, cool season grasses. Total annual production decreases. Plant Community A (State #1): Total plant production averages about 3200 lbs/ac in this Plant Community. Annual production of the tall, more palatable grasses (prairie cordgrass, big bluestem, and switchgrass) declines by about 20%. In response, western wheatgrass, mat muhly, and lower successional sedges have increased. Exact response by these lower successional species varies with the kind and intensity of disturbance (drought, grazing, etc.) and with precipitation (amount and timing). Production of native forbs increases relative to the HCPC and now accounts for more than 10% of the total production. Dotted blazing-star and Maximilian sunflower decrease in abundance while meadow hawksbeard, prairie thermopsis, and cinquefoil increase. Shrubs account for about 5% of the total annual production. Species such as snowberry, rose and shrubby cinquefoil increase at the expense of chokecherry and willows. Litter cover decreases to 50% and bare ground increases to about 5%. In contrast to the HCPC, range conservationists have slight to moderate concerns regarding lower infiltration rates and potentially higher runoff rates, plant functional/structural group shifts, and decreasing amount of litter. There shouldn’t be any, or only a trace of invasive plants present. The tall cool season grasses have poor vigor, with reduced seed production. Most of the seedlings and young plants appear to represent short grasses and warm season forbs. *Successional Pathway from Community A to HCPC: Plant Community A is highly resistant to disturbance. It is also resilient. With prescribed grazing, the high successional species are able to replace the lower-successional species and also expand into the bare areas. *Successional Pathway from Community A to Community B: Non-prescribed grazing, prolonged or extended drought, and the prolonged elimination of the natural fire regime from the system results in regression to Plant Community B. The effects of poor grazing management are readily apparent with careful observation. However, the influence of fire is more difficult to verify. It is believed that these sites burned naturally at 5 – 7 year intervals (Frost 1998). Without fire and/or grazing, litter accumulation becomes excessive and adversely impacts plant vigor, seedling establishment, and nutrient cycling.
Community 1.3
Plant Community B (State #1)
Mid and short grasses and grasslike plants dominate this Community. A few western wheatgrass, tufted hairgrass plants persist with reduced vigor in the community. Mat muhly, sedges and Baltic rush are common species. Grasses and grass-like plants contribute 75% of total annual production. Arrowgrass, white-prairie aster, cudweed sagewort, cinquefoil, prairie thermopsis, and other native low successional forbs make up about 15% of the total annual production. Dandelions, salsify, Canada thistle, and other invasive forbs may be present in this community. Total vegetative production declines to about 2000 lbs/ac in a normal year. Litter provides cover for about 40% of the ground, while bare ground increases to about 10%. Rills, water flow patterns and litter movement are evident on the site. *Succession and Regression from Plant Community B: Plant Community B should be recognized as the pre-threshold community. It is generally resilient but it is not highly resistant to stress. Under prescribed grazing this Community can return to Community A through succession. However, it will regress under the influence of NPG to lower successional Plant Community C (State #2). Regression also occurs to Community D (State #3). However, it is theorized that the pathways for this transition originate from within the Reference State, and not necessarily from Community B.
State 2
Plant Community C (State #2)
Community 2.1
Plant Community C (State #2)
Baltic rush, western wheatgrass, clustered field sedge, ticklegrass, mat muhly, Kentucky bluegrass, meadow barley and other short grasses and grass-like plants dominate this Community. HCPC dominant species such as prairie cordgrass and switchgrass may persist as individual plants. Normally there is minimal regeneration of these species. Wooly plantain, cudweed sagewort, arrowgrass, cinquefoil, dandelion, and western yarrow are common forbs. These low successional forbs contribute about 20% of the annual production. In comparison to the HCPC, fringed sagewort, snowberry and rose tend to increase and may contribute about 10% of the total annual production. Soil erosion is not a serious problem because of the cover provided by the short native grasses and the rhizomatous grasses. However, the loss of the tall cool season bunchgrasses, results in a simplification of the compositional and structural plant communities. The hydrologic cycle (capture, storage and redistribution of precipitation), energy flow, and nutrient cycles are believed to be adversely impacted. Total vegetative production averages about 1500 lbs/ac. In contrast to the HCPC, range conservationists express moderate concerns about plant community composition, functional/structural groups, litter, annual production, and invasive plants. Each of the primary processes: 1) hydrology (the capture, storage and redistribution of precipitation), 2) energy capture (conversion of sunlight to plant and animal matter), and 3) nutrient cycling (the cycle of nutrients through the physical and biotic components of the environment) has been degraded beyond the point of self-repair within a reasonable length of time. For example, when tall, high producing, cool season grasses are replaced by short grasses (Kentucky bluegrass, mat muhly and Baltic rush), the abilities of the plant community to maximize the conversion of solar energy to plant biomass and efficiently utilize available precipitation are impaired. Less solar energy is captured and converted to carbohydrates for plant growth. Plant growth declines, and there are less plant canopy and less litter to protect the soil. As bare ground increases, infiltration decreases and/or surface runoff and soil evaporation increases. Because ecological processes of the site are no longer balanced and sustained, shallow rooted, warm season species continue to gain a competitive advantage over the deep rooted, cool season species. The biotic integrity of the site is degraded. Thus, the transitions from Plant Community B in State #1 to either Communities C (State #2) or D (State #3) represent thresholds. Thresholds are defined as a point in space and time at which one or more of the primary ecological processes responsible for maintaining the sustained equilibrium of the state degrades beyond the point of self-repair. *Transition from Plant Community C to Community B: Succession from Community C to Community B is not likely without significant input of energy into the system. Many of the rhizomatous species are resistant to fire and grazing. Therefore, it is not logical for nutrient cycling and other ecological processes to be restored after a single fire or immediately following the implementation of prescribed grazing. *Successional Pathways from Community C to Community D: Plant community C is not a precise assemblage of species that remain constant from place to place or from year to year. Variability is apparent in productivity and occurrence of individual species. Changes in climate, fire patterns and frequency, and grazing all play a role in determining which plant species express dominance. Plant community C can regress into Community D with non-prescribed grazing and/or the absence of a natural fire regime.
State 3
Plant Community D (State #3)
Community 3.1
Plant Community D (State #3)
This plant community is dominated by invasive forbs, Kentucky and Canada bluegrasses, and noxious weeds. Some native short grasses and sedges remain in the Community. *Transition from Plant Community D to Community C: The noxious weeds and introduced rhizomatous grasses are competitive. Succession to Plant Community C is not likely to occur without a pro-active management of a significant input of energy into the natural system. Practical experience indicates that Garrison Creeping Foxtail (GCF) can be introduced into this community by feeding livestock GCF on the site, or by scattering seed and allowing livestock to trample it into the soil. Within a few years, the GCF often dominates the community. The seasonal water table and extensive below ground biomass that characterizes this restricts the use of conventional tillage. Research suggests that desirable species can be seeded into the site with a no-till drill following the application of RoundupR to control undesirable plants. In most situations, these agronomic approaches are usually economically and ecologically prohibitive.
Additional community tables
Table 9. Community 1.1 plant community composition
Group | Common name | Symbol | Scientific name | Annual production (kg/hectare) | Foliar cover (%) | |
---|---|---|---|---|---|---|
Grass/Grasslike
|
||||||
1 | Native perennial grasses and grasslikes | 1–3811 | ||||
prairie cordgrass | SPPE | Spartina pectinata | 448–1345 | – | ||
western wheatgrass | PASM | Pascopyrum smithii | 448–897 | – | ||
switchgrass | PAVI2 | Panicum virgatum | 336–897 | – | ||
slender wheatgrass | ELTR7 | Elymus trachycaulus | 224–673 | – | ||
slimstem reedgrass | CASTS5 | Calamagrostis stricta ssp. stricta | 224–673 | – | ||
mat muhly | MURI | Muhlenbergia richardsonis | 1–448 | – | ||
bulrush | SCIRP | Scirpus | 224–448 | – | ||
Grass, perennial | 2GP | Grass, perennial | 224–448 | – | ||
rough bentgrass | AGSC5 | Agrostis scabra | 1–448 | – | ||
big bluestem | ANGE | Andropogon gerardii | 168–448 | – | ||
sedge | CAREX | Carex | 224–448 | – | ||
Forb
|
||||||
2 | Native perennial forbs | 1–448 | ||||
Forb, perennial | 2FP | Forb, perennial | 1–168 | – | ||
fiddleleaf hawksbeard | CRRU3 | Crepis runcinata | 1–168 | – | ||
Maximilian sunflower | HEMA2 | Helianthus maximiliani | 45–168 | – | ||
Rocky Mountain blazing star | LILI | Liatris ligulistylis | 45–168 | – | ||
lanceleaf goldenweed | PYLAL | Pyrrocoma lanceolata var. lanceolata | 1–168 | – | ||
prairie thermopsis | THRH | Thermopsis rhombifolia | 1–168 | – | ||
arrowgrass | TRIGL | Triglochin | 1–168 | – | ||
Shrub/Vine
|
||||||
3 | Native shrubs and half-shrubs | 1–224 | ||||
Shrub, broadleaf | 2SB | Shrub, broadleaf | 1–112 | – | ||
shrubby cinquefoil | DAFRF | Dasiphora fruticosa ssp. floribunda | 1–112 | – | ||
chokecherry | PRVI | Prunus virginiana | 45–112 | – | ||
rose | ROSA5 | Rosa | 1–112 | – | ||
willow | SALIX | Salix | 45–112 | – | ||
buffaloberry | SHEPH | Shepherdia | 1–112 | – | ||
snowberry | SYMPH | Symphoricarpos | 1–112 | – |
Interpretations
Animal community
Livestock Management
This site evolved with trampling, defoliation (ungulates, grasshoppers and jackrabbits, and other herbivores), fire and drought. In comparison to upland ecological sites, water is relatively more accessible to grazing animals on this site. Therefore, it is theorized that this site evolved with more animal impact than did the normal upland ecological sites. This site has the potential to produce an abundance of high quality forage. Total annual production varies from 3500 – 5000 lbs/ac.
The Subirrigated 10-14” p.z. site is normally highly resistant to disturbances which may alter its ecological processes. However, grazing early in the season when the upper part of the soil is wet can cause compaction and hummocks. Proper stocking rates, along with adequate recovery periods following grazing events, are needed to ensure that this site remains in a high seral or HCPC state. Following perturbations such as drought or poor grazing management, which allows mat muhly and other low successional species to increase at the expense of the mid and tall grasses, succession occurs with subsequent rainfall and prescribed grazing.
Forage production is greatly reduced in Plant communities C and D. Once these communities occupy this site, the presence of non-native grasses and undesirable plants significantly impede succession. Species such as Kentucky bluegrass, leafy spurge and Canada thistle are difficult to remove from the site.
Arrowgrass, death camas, and horsetail are poisonous plants that often occur on this site. However, livestock losses are unusual unless the range is overstocked and livestock are forced to consume the poisonous plants.
This site is suitable for livestock grazing from May through October. Because of topographic position, proximity to water, and species composition (grasses comprise about 85% of the production) the site is better-suited for cattle, rather than sheep grazing.
Wildlife Interpretations
The Subirrigated 10-14” p.z. ecological site has high biodiversity in the Glaciated Plains. High forage yields and the diversity of shrubs, grasses and forbs provide food and cover for resident and migratory wildlife species. The narrow irregular, meandering drainage patterns serve as a corridor allowing big game and other species to move between upland habitats.
State #1 supports the highest abundance of insects, invertebrates, amphibians, reptiles, upland game birds and small mammals. It also provides forage for mule deer and antelope during most of the year.
States #2 and #3 are much less suitable for big game, upland birds and most species of small mammals. The simplification of the plant community reduces the number of wildlife habitat niches. Because of less plant growth and litter, soil surface temperatures rise and soil moisture decreases. As the site becomes more xeric the insect and invertebrate population becomes less diverse, and there are less cover and food resources for upland birds, and mammals.
Plant Preferences by Animal Kind
Refer to NRCS Field Office Technical Guide, Section IIE, General Information, for tables displaying plant preferences by livestock and wildlife.
Hydrological functions
Soils associated with this ecological site are in Hydrologic Soil Groups B and C. Infiltration rates are generally moderate. The runoff potential is negligible to low, varying with landscape and ground cover.
Good hydrologic conditions exist on overflow sites that are either in a high seral state or are at HCPC (State #1). Canopy cover (grasses, forbs and shrubs) is greater than 100% in these communities, which is conducive to high infiltration rates and minimal runoff and erosion.
Communities in the early seral state (Communities B & C) are generally considered to be in poor hydrologic condition. Concerns are valid, not because of the amount of bare ground, but because the short grasses have replaced the tall high yielding species. Thus, there is much less opportunity for the plant community to effectively utilize available moisture.
Recreational uses
Hunters are probably the most common recreational user of this ecological site. The site is also used by hikers and photographers and birdwatchers.
Wood products
This site has no significant value for wood products.
Other information
At high seral states, the Subirrigated 10-14” p.z. site in the eastern Glaciated Plains is resistant to perturbations. However, the site loses its resiliency when the plant community regresses from State #1 to State #2. Reproductive capability of desirable plants declines and annual production decreases as the site moves toward the threshold separating State #1 from State #2. Production in the latter state is less than 50% of the potential at HCPC. Thus, litter and the number of structural/functional groups are adversely affected.
The Montana Natural Heritage Program (Heidel, Cooper and Jean 2000) conducted an inventory in Sheridan County for plant associations and plant species of special concern. They found that the eastern end of Sheridan County had the greatest diversity of high quality plant associations. The wetland types that they inventoried included several plant communities in the Subirrigated 10-14” p.z. site. Many of these communities had over 100% canopy cover and were dominated by switchgrass. Prairie cordgrass, clustered field sedge and mat muhly were common species. Their report contains legal locations, environmental descriptions, and cover estimates by species.
Supporting information
Inventory data references
SCS-Range-417
ECS-1
Modified Double Sampling 1 2001 MT Valley
USDA-SCS-MT 1981 Technical Range Site Description
Other references
Frost, Cecil C. 1998. Presettlement fire frequency regimes of the United States: a first approximation. Pages 70-81 in Teresa L. Pruden and Leonard A. Brennan (eds.). Fire in ecosystem management: shifting the paradigm from suppression to prescription. Tall Timbers Fire Ecology Conference Proceedings, No. 20. Tall Timbers Research Station, Tallahassee, Fl.
Heidel, B. S.,V. Cooper, and C. Jean. Plant species of special concern and plant associations of Sheridan County, Montana. Report to the U.S. Fish and Wildlife Service. Montana Natural Heritage Program, Helena. 22pp. plus appendices.
Stringham, T. k., W. C. Krueger, and P. L. Shaver. 2003. State and transition modeling: an ecological process approach. J. Range Manage. 56(2):106-113.
USDI BLM USGS and USDA NRCS. 2000. Interpreting indicators of rangeland health. Tech. Ref. 1734-6.
Approval
Kirt Walstad, 6/14/2023
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) | Dr. John Lacey, Maxine Rasmussen, Jon Siddoway & Rick Bandy |
---|---|
Contact for lead author | |
Date | 03/30/2005 |
Approved by | Kirt Walstad |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
Rills should not be present in any of the State 1 reference plant communities. -
Presence of water flow patterns:
Water flow patterns should not be observable in any of the State 1 reference plant communities. -
Number and height of erosional pedestals or terracettes:
Pedestals or terracettes would essentially be nonexistent in any of the State 1 reference plant communities. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground would essentially be nonexistent in HCPC. Bare ground should be less than 2” in diameter. If in plant community A, less than 5% of the soil surface can be exposed. In plant community B, 10% bare ground may be exposed. -
Number of gullies and erosion associated with gullies:
Gullies are not associated with any of the State 1 reference plant communities. -
Extent of wind scoured, blowouts and/or depositional areas:
Wind scoured, blowouts and/or depositional areas are not associated with any of the State 1 reference plant communities. -
Amount of litter movement (describe size and distance expected to travel):
Litter movement is not expected with any of the State 1 reference plant communities. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Stability class anticipated to be 5 or 6 under plant canopy. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
The surface layer varies from 0-3” deep to 0-12” deep. The color is usually dark brown. Surface textures include loam, silt loam, clay loam, or sandy loam. Soil organic matter ranges from 2-4%. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
In HCPC, 90-95% plant canopy and 80-85% basal cover with small gaps between plants should reduce raindrop impact and slow overland flow, providing increased time for infiltration to occur. Healthy, deep rooted native grasses enhance infiltration and reduce runoff. Infiltration rate is moderate to very slow. If in plant community A, 90-95% plant canopy and 70-80% basal cover with small gaps between plants will still reduce raindrop impact and decrease overland flow. If in plant community B, 40-70% plant canopy and 50-75% basal cover with moderate gaps between plants, intensifies raindrop impact and increases overland flow. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
No compaction layer or soil surface crusting should be evident in either of the State 1 plant communities. -
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
HCPC: Tall, warm season rhizomatous grasses > mid-stature, cool season rhizomatous grasses > mid-stature cool season bunch grasses > forbs >shrubs. Plant community A: Mid-stature, cool season rhizomatous grasses> mid-stature cool season bunch grasses > tall, cool season bunch grasses > forbs > shrubs.Sub-dominant:
Plant community B: Mid-stature, cool season rhizomatous grasses > mid-stature cool season bunch grasses > sedges and rushes > forbs > shrubs.Other:
Additional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Plant mortality and decadence very low in HCPC and Plant community A. In periods of drought, all plants would exhibit decadence in the state 1 reference communities. -
Average percent litter cover (%) and depth ( in):
Litter cover is in contact with soil surface. Litter decreases in Plant community A to 40-50% and depth is reduced to 0.5 inch. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
3500 - 5000 #/acre from Plant community A to HCPC in the State 1 reference community. -
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
Smooth bromegrass, Kentucky bluegrass, Canada bluegrass, Baltic rush, leafy spurge and Canada thistle. -
Perennial plant reproductive capability:
All species are capable of reproducing in HCPC. In Plant community A, plant seedlings will be weighed in favor of marginal and undesirable species. Replacement of desirable species will be very few.
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
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