Natural Resources
Conservation Service
Ecological site R053AE067MT
Overflow (Ov) (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 in swales, drainageways, low terraces and flood plains where it receives extra moisture from run-in from adjacent land. The site does not have a permanent water table within 42 inches of the soil surface. 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)
Depression
(2) Swale (3) Flood plain |
---|---|
Flooding duration | Very brief (4 to 48 hours) to brief (2 to 7 days) |
Flooding frequency | Occasional to frequent |
Ponding duration | Long (7 to 30 days) |
Ponding frequency | None to frequent |
Elevation | 1,875 – 3,100 ft |
Slope | 2% |
Water table depth | 42 in |
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) | 12 in |
Figure 2. Annual precipitation pattern
Figure 3. Annual average temperature pattern
Influencing water features
The run-in moisture to this site occurs following rain or snowmelt. This site is not influenced by water from wetlands or streams.
Soil features
Soils are well drained and more than 60 inches deep to bedrock. Permeability varies from moderate to very slow. The surface layer of these soils vary from 0-12 inches in depth and are typically a loam, silt loam, clay loam, silty clay loam or fine sandy loam. Textures of underlying layers also vary since these are alluvial soils, having been deposited by flowing water. Soil ph varies from 6.1-8.4. Soils such as Trembles and Cherry are non-hydric. Other soils found on this site include Havre, Havrelon, and Hanly. However, soils (such as Dimmick and Nishon) that are typically found in depressions are hydric. Lallie is another hydric soil. It is typically found in old oxbows that have been cut off from the main stream channel.
Table 4. Representative soil features
Surface texture |
(1) Loam (2) Sandy loam (3) Clay loam |
---|---|
Family particle size |
(1) Loamy |
Drainage class | Moderately well drained to excessively drained |
Permeability class | Moderately rapid to very slow |
Soil depth | 20 – 72 in |
Surface fragment cover <=3" | Not specified |
Surface fragment cover >3" | Not specified |
Available water capacity (0-40in) |
6 – 8 in |
Calcium carbonate equivalent (0-40in) |
10% |
Electrical conductivity (0-40in) |
4 mmhos/cm |
Sodium adsorption ratio (0-40in) |
8 |
Soil reaction (1:1 water) (0-40in) |
6.1 – 8.4 |
Subsurface fragment volume <=3" (Depth not specified) |
5% |
Subsurface fragment volume >3" (Depth not specified) |
2% |
Ecological dynamics
This ecological site developed under Northern Great Plains climatic conditions, geological materials, fire, plants and animals. At the time that North America was settled by Europeans, the Glaciated Plains was the home of nomadic tribes of Native Americans and large numbers of bison, prairie dog, 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. However, research consistently shows that precipitation is the principal factor altering productivity on ecological sites in the Northern Great Plains (Heitschmidt et al. 2005). The same authors concluded that grazing reduces herbage standing crop, whereas its effects on above ground net primary production varies with timing of grazing and precipitation events, along with the functional and structural composition of the plant community.
It is theorized that these lands burned on a natural interval of 5-7 years, either as a result of lightning or Native Americans (Frost 1998). Most of the species present in the historic climax plant community (HCPL) are fire tolerant.
The HCPC is the basis for plant community interpretations. It is the plant community that is best adapted to the unique combination of factors associated with this ecological site. This site is highly resistant and resilient to disturbance. The HCPC has been determined by evaluating rangeland relic areas, and other areas protected from excessive disturbance.
.
The HCPC is dominated by a mixture of tall and medium height cool and warm season grasses and grasslike species. About 90% of the annual production is from grasses and grasslike plants. Forbs and shrubs each contribute about 5% to total annual production. Total vegetative production averages 2500 lbs/ac in normal years, 2000 lbs/ac in “unfavorable” years, and 3000 lbs/ac in “favorable” years.
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 colonization and recruitment, etc. Continual adverse impacts to the site over a period of years results in regression to lower seral stages. The deep-rooted cool season perennial grasses are replaced by warm season grasses (blue grama, sandberg bluegrass, etc), fringed sagewort, hoods phlox, threadleaf sedge, hairy gold aster, and annual grasses and forbs. The dominance of these short grasses, warm season forbs and half-shrubs, and low seral 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 can not satisfactorily describe the complex successional pathways of this site (Briske et al. 2005). As the HCPC regresses to an early seral state, it is theorized that a threshold is crossed somewhere within the mid-to-low seral state. Plant communities below this threshold are in a steady state. 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.”
Two important plant communities and associated successional pathways for the reference state (State #1), are illustrated below for an Overflow 10-14” p.z. site in the Glaciated Plains. The transition from Plant Community A (State #1) across a threshold to Plant Community B (State #2), and the transition from Community B to Community C (State #3) are also shown.
State and transition model
More interactive model formats are also available.
View Interactive Models
More interactive model formats are also available.
View Interactive Models
Click on state and transition labels to scroll to the respective text
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). Cool season tall and mid-grasses (such as green needlegrass, western wheatgrass, thickspike wheatgrass, slender or bearded wheatgrass, basin wildrye and needleandthread grass) dominate the HCPC. These cool season grasses represent about 70% of the total annual plant production in the community. Warm and cool season short grasses and sedges (prairie junegrass, upland sedges, plains reed grass and blue grama) make up 10% of the total annual production. Goldenrods, scurfpeas, maximilian sunflower, cudweed sagewort, and western yarrow are important warm season forbs. American vetch, cinquefoil and penstemon are common cool season forbs. American vetch, milk vetch, prairie thermopsis, and scurfpea are important nitrogenous-fixing legumes. Total forb production normally represents less than 10% of the total annual production. Western snowberry, prairie rose, buffalo berry and chokecherry are common cool season shrubs. Silver sagebrush and fringed sagewort are common warm season shrubs. Overall, shrubs account for about 10% of the annual plant production. Annual production averages 2500 lbs/ac during “normal” years. Range inventory data collected (in 2001 and 2004) on the Fort Peck and Fort Belknap Indian Reservations indicate total above ground production averaged 2132 lbs/ac in plant communities associated with similarity indices of 45-65. Therefore, the 2500 lb/ac estimate is reasonable for the HCPC. Annual production is expected to increase and decrease, respectively on more mesic and xeric portions of the Glaciated plains. This plant community is well adapted to the Glaciated plains. Precipitation and run-in water are the most important factors influencing production. The functional and structural diversity of plant species (annuals, perennials, cool and warm season grasses, 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 non-drought conditions, more species found at HCPC will replace these lower successional species within a few years. Litter is in contact with 60% of the soil surface. Plant litter remains in place and is not moved by erosional forces. Plant basal canopy cover averages 40%. 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 (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
---|---|---|---|
Grass/Grasslike | 1600 | 2000 | 2400 |
Forb | 200 | 250 | 300 |
Shrub/Vine | 200 | 250 | 300 |
Total | 2000 | 2500 | 3000 |
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 | 0-1% |
Biological crusts | 0-1% |
Litter | 50-60% |
Surface fragments >0.25" and <=3" | 0-3% |
Surface fragments >3" | 0-2% |
Bedrock | 0% |
Water | 0-1% |
Bare ground | 0-1% |
Table 7. Soil surface cover
Tree basal cover | 0% |
---|---|
Shrub/vine/liana basal cover | 5-10% |
Grass/grasslike basal cover | 25-30% |
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 (ft) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
---|---|---|---|---|
<0.5 | – | 0-5% | 5-15% | 35-45% |
>0.5 <= 1 | – | 30-40% | 25-35% | 45-55% |
>1 <= 2 | – | 25-35% | 35-45% | 5-10% |
>2 <= 4.5 | – | 10-20% | 15-25% | 0-5% |
>4.5 <= 13 | – | 10-20% | – | – |
>13 <= 40 | – | – | – | – |
>40 <= 80 | – | – | – | – |
>80 <= 120 | – | – | – | – |
>120 | – | – | – | – |
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 colonization and recruitment, etc. As communities regress from HCPC, medium and short warm season grasses increase at the expense of mid and tall cool season grasses. Plant Community A (State #1): Total plant production averages about 1700 lbs/ac in this Plant Community. The tall, cool season grasses (green needlegrass, basin wildrye, switchgrass, big bluestem, and prairie cordgrass) persist in the community but have lost vigor with little evidence of successful regeneration. Western wheatgrass, prairie junegrass, blue grama and needleandthread grass have increased and contribute about 40% of the total annual production. Exact response of western wheatgrass and these lower successional species vary with the kind 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 gayfeather and American vetch tend to be replaced by cudweed sagewort, hoods phlox, etc. Shrubs account for about 15% of the total annual production. Species such as snowberry, fringed sagewort and silver sagebrush increase at the expense of chokecherry, golden currant and American plum. SI indicies from 35-65% are associated with this community. Litter cover decreases to 50% and bare ground increases to 5 – 10 %. 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, decreasing amount of litter, and increased presence of lower successional plants. The tall cool season grasses have poor vigor with little seed production. Most of the seedlings and young plants appear to represent short grasses and warm season forbs. Plant Community A is not highly resistant to disturbance. It can readily regress to a lower state from which upward succession is restricted. Because it is the “pre-threshold” community, it is critical that this community be recognized and strategies implemented to prevent further regression (UDSA and USDI, 2000). *Successional Pathway from Community A to HCPC: Successional processes can readily return Plant Community A to the HCPC. The process can be facilitated by prescribed grazing, the incorporation of the natural fire regime into the system, etc. *Transition from State #1 to Communities B (State #2) and C (State #3): Prolonged drought, non-prescribed grazing, and the removal of fire in the system will result in retrogression to State #2. The effects of drought and poor grazing management are readily apparent with careful observation. However, the influence of fire is more difficult to verify. Because of the continual interaction of these environmental factors, regression from State #1 may culminate in two distinct communities (Community B or C). Community B is dominated by snowberry, fringed sagewort, and silver sagebrush. Community C is comprised of mostly short grasses, Kentucky bluegrass and low successional forbs.
State 2
Plant Community B (State #2)
Community 2.1
Plant Community B (State #2)
Native shrubs such as snowberry, silver sagebrush, fringed sagewort, and prairie rose account for 25% or more of total annual production. A few western wheatgrass and green needlegrass plants persist with low vigor in the community. Needleandthread, blue grama, prairie junegrass, sandberg bluegrass and upland sedges dominate the graminoids, and represent about 30% of the total annual production. Cinquefoil, prairie thermopsis, scurfpeas, western yarrow, cudweed sagewort, and other native low successional forbs make up about 20% of the total annual production. Dandelions, salsify, cocklebur, hounds tongue, Canada thistle, and other noxious forbs are usually conspicuous in the community. SI indices for this community vary from 1-34%. Total vegetative production declines to about 900 lbs/ac in a normal precipitation year. Litter provides cover for about 15% of the ground, while bare ground increases to about 25%. Rills, water flow patterns and litter movement are evident on the site.
State 3
Plant Community C (State #3)
Community 3.1
Plant Community C (State #3)
Plant Community C (State #3) is dominated by Kentucky and Canada bluegrass, blue grama, prairie junegrass, sandberg bluegrass, and needleandthread. Allthough some western wheatgrass persists as single shoots with few seedstalks, it is difficult to find green needlegrass or any other high successional grass that dominated the HCPC. Japanese brome and cheatgrass often colonize disturbed sites (rodent mounds, etc.) in this community. Wooly plantain, hoods phlox, hairy goldenaster and western yarrow are common forbs. These low successional forbs contribute about 20% of the annual production. Fringed sagewort usually increases while snowberry and silver sagebrush decrease in abundance. There are very few seedlings of desirable species. SI indices of 0-34% are associated with Community C. Soil erosion is not a serious problem because of the cover provided by the introduced rhizomatous and short native warm and cool season 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 800 lbs/ac. In contrast to the reference state, range conservationists express moderate to extreme concerns about plant community composition, functional/structural groups, litter, annual production, and noxious 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, blue grama, and prairie junegrass), the ability 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 is 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 compromised. *Successional Pathways between Communities B & C: Plant communities B & C are 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. However, dominant status is less variable. Changes in climate, fire patterns and frequency, and grazing all play a role in determining which of the plant communities will be expressed. Plant Community B regresses to Community C with non-prescribed grazing and/or a wildfire that removes the dominant shrubs from the community. The shift from Community C to Community B might occur with a combination of a natural fire regime, prescribed grazing and an extended period of favorable precipitation. The possibility of this succession is depicted with a dashed arrow in the state and transition diagram. *Transition from Community B (State #2) to State #1: The implementation of prescribed grazing and a favorable precipitation pattern normally will not induce succession from State #2 to State #1. Succession normally requires significant economic inputs. However, the Overflow 10-14” p.z. ecological site is productive. It is theorized that succession from Community B to State #1 may occur with the combination of a natural fire regime, prescribed grazing, and an extended period of favorable precipitation. This potential is depicted as a dashed arrow in the state and transition model. The Overflow 10-14” p.z. is a productive site with deep soils on landscapes with less than 2% slope. Although the potential of using mechanical treatments to promote plant succession is limited because this site often occurs as small and irregularly shaped tracts, mechanical treatments are feasible in some places (See NRCS Conservation Practice 548). Following mechanical treatment, it is critical that grazing is deferred one or two growing seasons. Length of grazing deferment varies with precipitation and response of vegetation. Furthermore, prescribed grazing must be implemented following the deferment. Failure to do will result in economic losses and potential ecological damage to the site. With prescribed grazing and plant succession, the effective life of treatment should be greater than 10 years. Prescribed burning may be a useful tool for promoting succession in the State #2 Plant Communities. Fire would reduce the shrubs in Community B, and also adversely impact the shallow-rooted Kentucky and Canada bluegrasses in Community C. The opening of the community will favor the establishment of new plants, if seed (and/or rhizomes) of desired plants are available. If not, range seeding may be necessary following mechanical treatment or fire.
Additional community tables
Table 9. Community 1.1 plant community composition
Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
---|---|---|---|---|---|---|
Grass/Grasslike
|
||||||
1 | Native perennial grasses and grasslikes | 1–2000 | ||||
green needlegrass | NAVI4 | Nassella viridula | 375–750 | – | ||
western wheatgrass | PASM | Pascopyrum smithii | 375–750 | – | ||
basin wildrye | LECI4 | Leymus cinereus | 250–500 | – | ||
Canada wildrye | ELCA4 | Elymus canadensis | 125–250 | – | ||
bluegrass | POA | Poa | 125–250 | – | ||
prairie cordgrass | SPPE | Spartina pectinata | 125–250 | – | ||
beardless wheatgrass | PSSPI | Pseudoroegneria spicata ssp. inermis | 65–125 | – | ||
switchgrass | PAVI2 | Panicum virgatum | 1–125 | – | ||
slender wheatgrass | ELTR7 | Elymus trachycaulus | 65–125 | – | ||
needle and thread | HECOC8 | Hesperostipa comata ssp. comata | 1–125 | – | ||
big bluestem | ANGE | Andropogon gerardii | 1–125 | – | ||
2 | Native perennial grasses and grasslikes | 1–250 | ||||
Grass-like, perennial | 2GLP | Grass-like, perennial | 1–90 | – | ||
Grass, perennial | 2GP | Grass, perennial | 1–90 | – | ||
blue grama | BOGR2 | Bouteloua gracilis | 1–90 | – | ||
threadleaf sedge | CAFI | Carex filifolia | 1–90 | – | ||
plains reedgrass | CAMO | Calamagrostis montanensis | 1–90 | – | ||
prairie Junegrass | KOMA | Koeleria macrantha | 1–90 | – | ||
Sandberg bluegrass | POSE | Poa secunda | 1–90 | – | ||
Forb
|
||||||
3 | Native perennial forbs | 125–250 | ||||
Maximilian sunflower | HEMA2 | Helianthus maximiliani | 125–250 | – | ||
dotted blazing star | LIPU | Liatris punctata | 125–250 | – | ||
American vetch | VIAM | Vicia americana | 125–250 | – | ||
4 | Native perennial forbs | 1–250 | ||||
Forb, perennial | 2FP | Forb, perennial | 1–30 | – | ||
common yarrow | ACMI2 | Achillea millefolium | 1–30 | – | ||
pussytoes | ANTEN | Antennaria | 1–30 | – | ||
white sagebrush | ARLU | Artemisia ludoviciana | 1–30 | – | ||
aster | ASTER | Aster | 1–30 | – | ||
milkvetch | ASTRA | Astragalus | 1–30 | – | ||
bastard toadflax | COUM | Comandra umbellata | 1–30 | – | ||
buckwheat | ERIOG | Eriogonum | 1–30 | – | ||
northern bedstraw | GABO2 | Galium boreale | 1–30 | – | ||
hairy false goldenaster | HEVI4 | Heterotheca villosa | 1–30 | – | ||
beardtongue | PENST | Penstemon | 1–30 | – | ||
spiny phlox | PHHO | Phlox hoodii | 1–30 | – | ||
scurfpea | PSORA2 | Psoralidium | 1–30 | – | ||
Missouri goldenrod | SOMI2 | Solidago missouriensis | 1–30 | – | ||
scarlet globemallow | SPCO | Sphaeralcea coccinea | 1–30 | – | ||
prairie thermopsis | THRH | Thermopsis rhombifolia | 1–30 | – | ||
Shrub/Vine
|
||||||
5 | Native shrubs and half-shrubs | 70–250 | ||||
chokecherry | PRVI | Prunus virginiana | 90–200 | – | ||
golden currant | RIAU | Ribes aureum | 90–200 | – | ||
American plum | PRAM | Prunus americana | 70–100 | – | ||
6 | Native shrubs and half-shrubs | 1–100 | ||||
silver sagebrush | ARCA13 | Artemisia cana | 1–25 | – | ||
prairie sagewort | ARFR4 | Artemisia frigida | 1–25 | – | ||
rose | ROSA5 | Rosa | 1–25 | – | ||
snowberry | SYMPH | Symphoricarpos | 1–25 | – | ||
Shrub, broadleaf | 2SB | Shrub, broadleaf | 0–1 | – | ||
7 | Native shrubs and half-shrubs | 0–1 | ||||
plains pricklypear | OPPO | Opuntia polyacantha | 0–1 | – |
Interpretations
Animal community
Livestock Management
This site evolved with trampling, defoliation (ungulates, grasshoppers and jackrabbits, and other herbivores), fire and drought. Potholes in ephemeral drainages tend to store run-off water following storm events, which would be accessible to animals grazing on adjacent sites. Therefore, it is theorized that this site evolved with more animal impact than did the adjacent upland ecological sites. This site is highly resistant to disturbances which may alter its ecological processes. Within the Reference State (State #1) it is also resilient. Following perturbations such as drought, which allows blue grama and other warm season, lower successional species to increase at the expense of the mid and tall cool season grasses, succession occurs with subsequent rainfall and run-in. Thus, the HCPC and Community A may be present at any given time in State #1. The site has the potential to produce 2000 – 3000 lbs of vegetation per acre.
Annual production shows far greater variations in response to changes in annual precipitation than to different grazing intensities (Hutchings and Stewart 1953). However, proper stocking rates and prescribed grazing are needed to ensure that the site remains in a high seral or HCPC state. Without proper grazing management the mid-to-tall grass community regresses to a blue grama, prairie junegrass, Kentucky bluegrass and low-successional forb community. Data from the recent range inventories indicate a significant Kentucky bluegrass population on nearly 20% of these sites.
Kentucky bluegrass may be a mixed blessing. It produces high quality forage (but not much of it), it grows as a sod and its rhizomes protect the soil from erosion (but it provides less protection than species in the HCPC). Unless stressed by drought, the Kentucky bluegrass is resistant to grazing systems with limited rest periods. Additional ecological concerns are its tendencies to form a monoculture and persist as a steady state. Plant succession is slow to non-existent in Kentucky bluegrass communities on the Overflow site. In comparison to the high seral state, suggested stocking rates on sites dominated by Kentucky bluegrass represent a 2-fold reduction. Prescribed grazing is recommended to prevent further deterioration in States #2 and #3. Non-prescribed grazing reduces plant cover and litter, increases surface runoff, and often leads to gully formation and active head cutting. Down-cutting lowers water tables and/or reduces the effectiveness of run-in moisture. Thus, the Overflow site crosses a conservation threshold, where most or all of its ecological processes are severely impacted. Once the ecological processes (hydrologic cycle, nutrient cycling, and conversion of solar energy into carbohydrates for plant growth) are disrupted, significant plant succession will not occur within a reasonable time period.
Death camas, horsetail, milkvetch and a few additional species of plants occurring on this site may be poisonous to livestock. 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, the site is better-suited for cattle, rather than sheep grazing.
Wildlife Interpretations
The Overflow 10-14” p.z. ecological site creates biodiversity in the Glaciated Plains. The run-in moisture and diversity of shrubs, grasses and forbs provides food and cover for resident and migratory wildlife species. The narrow irregular, meandering landforms serve as a corridor allowing big game and other species to move between adjacent upland habitats.
State #1 (reference state) includes the HCPC and one additional community. This state 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.
Communities that are in 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, there is less cover, structure and food resources for upland birds and mammals. Springs and seeps may partially dry up.
Hydrological functions
Soils associated with this ecological site are in Hydrologic Soil Groups A, B, C and D. Infiltration rates are generally moderate. The runoff potential is usually negligible to very low, but varies with landscape and ground cover.
Good hydrologic conditions exist on these sites when they are either in the Reference State (HCPC or Community A). Canopy cover (grass, forbs and shrubs) is greater than 90% in these communities, which is conducive to high infiltration rates and minimizes runoff and erosion.
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 grass sod restricts the ability of the desirable tall and mid-grasses to utilize available moisture. When rills develop into a gully, erosion threatens resource productivity. Therefore, it is recommended that grazing management strategies be implemented to address the problem of rills and litter movement -- do not wait until the formation of gullies to change management strategies.
Recreational uses
Hunters are probably the most common recreational user of this ecological site. The site is also used by hikers and photographers.
Wood products
This site has no significant value for wood products.
Other information
The following is an example of how to calculate the recommended stocking rate. This example does not use production estimates from this specific ecological site. You will need to adjust the annual production values and run the calculations using total annual production values from the ecological sites encountered on each individual ranch/pasture. Before making specific recommendations, an on-site evaluation must be made.
Supporting information
Inventory data references
SCS-Range-417 (#515,#520) 1991-1992 MT Phillips
ECS-1
Modified Double Sampling 24 2001-2004 MT Blaine, Roosevelt, Sheridan, Phillips, Valley
USDA-SCS-MT 1981 Technical Range Site Descriptions
Other references
Briske, D. D., S. D. Fuhlendorf, and F. E. Smeins. 2005. State-and-transition models, thresholds, and rangeland health: a synthesis of ecological concepts and perspectives. Rangeland Ecol.Manage.58:1-10.
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.
Heitschmidt, R. K., K. D. Klement, and M. R. Haferkamp. 2005. Interactive effects of drought and grazing on Northern Great Plains rangelands. Rangeland Ecol. Manage. 58:11-19.
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 HCPC or in plant community A. -
Presence of water flow patterns:
Water flow patterns should not be observable in HCPC or in plant community A. -
Number and height of erosional pedestals or terracettes:
Pedestals or terracettes would essentially be nonexistent in HCPC and in plant community A. -
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. -
Number of gullies and erosion associated with gullies:
Gullies are not associated with either 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 either of the State 1 reference plant communities. -
Amount of litter movement (describe size and distance expected to travel):
Litter movement is not expected with HCPC or plant community A. -
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 is 0-12” deep. The color ranges from light brownish gray, brownish gray, to gray as the soil becomes hydric. Surface textures include loam, silt loam, clay loam, silty clay loam or fine sandy loam. Soil organic matter ranges from 2-4% with a high of 8% and a low of 1%. -
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. -
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, cool season bunch grasses > mid-stature, cool season bunch grasses > mid-stature cool season rhizomatous grasses > tall warm season rhizomatous grasses > forbs =shrubs. Plant community A: Mid-stature, cool season rhizomatous grasses> > mid-stature cool season bunch grasses > tall, cool season bunch grasses > shrubs > forbs.Sub-dominant:
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, shrubs 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):
2000 - 3000 #/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:
Needle and thread, western snowberry, smooth bromegrass, Kentucky bluegrass, Canada bluegrass, silver sagebrush, 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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