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Ecological site R046XN230MT

Saline Lowland (SL) RRU 46-N 13-19 PZ

Last updated: 7/19/2023
Accessed: 11/24/2024

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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.

MLRA notes

Major Land Resource Area (MLRA): 046X–Northern and Central Rocky Mountain Foothills

Major Land Resource Area (MLRA) 46, Rocky Mountain Foothills, is approximately 11.6 million acres. MLRA 46’s extent has changed over recent years and is now primarily located in Montana and Wyoming with limited acres in Utah and Colorado. It spans from the Canadian border south to the Uinta Mountains of Northwest Colorado. MLRA 46 is a transitional MLRA between the plains and mountains of primarily non-forested rangeland. In Montana, 3 Land Resource Units (LRUs) exist based on differences in geology, landscape, soils, water resources, and plant communities. Elevations for this MLRA in Montana vary from a low of 3200 to 6500 feet (975 to 1981 m) however the elevations on the fringes of this MLRA may fall outside of that range in extremely small isolated areas where the boundaries between neighboring MLRAs are not easily defined. Annual precipitation ranges from 8 inches (254 mm) to, in very isolated areas, 42 inches (1083 mm). In general precipitation rarely exceeds 24 inches (610mm). Frost-free days are variable from 50 days near the Crazy and Beartooth Mountains to 130 days in the foothills south of the Bear’s Paw Mountains of Central Montana. The geology of MLRA 46 is generally Cretaceous and Jurassic marine sediments.

MLRA 46’s plant communities are dominated by cool-season bunchgrasses with mixed shrubs. This MLRA is rarely forested; however, ponderosa and limber pine do occupy areas. Portions of this MRLA may have a subdominance of warm-season mid-statured bunchgrasses like little bluestem; however, the general concept of the MLRA does not have a large component of warm season species. Wyoming big sagebrush, mountain big sagebrush, silver sagebrush, common snowberry, and shrubby cinquefoil tend to be the dominant shrub component. The kind and presences of shrubs tends to be driven by a combination of soils and climate. Due to the variable nature of the Land Resources Units, Climatic subsets will be necessary to describe the ecological sites and the variation of plant communities for this MLRA.

LRU notes

The Rocky Mountain Front Foothills LRU is the northernmost LRU of MLRA 46. The boundaries are the Canadian border to the north, MRLA 43B and the western extent of Continental Glaciation (MLRA 52). Boundaries between these MLRAs are extremely broad and often hard to distinguish.

Major watersheds of this LRU include the Missouri River, Sun River, Teton River, Marias River, and the Milk River. All of these river systems have been modified for the purpose of irrigation of pasture and crops.

The Rocky Mountain Front Foothills LRU’s geology is generally sedimentary in nature. Primary geological units include Two Medicine Limestone and Sandstone, Colorado Shale, Glacial Drift (alluvium), Terrace deposits (alluvium) and St Mary River formation (mudstone). Landforms include outwash terraces, escarpments, fan remnants, valleys, hillslopes, and drainage ways. Elevations of this landscape is from 3221 feet (982 m) to 6954 feet (2120 m).
Well drained soils are dominate in this LRU. Most areas vary from nearly level to 15 percent slope, while some areas do express steeper slopes near the 43B boundary. Soils are Slight to Moderate Alkaline. Soil mean clay percentages are mostly above 23 percent and are primarily very deep at approximately 70 percent of the LRU and moderately-deep to deep soils at approximately 30 percent of the LRU.

The climate of this LRU is highly variable however the average of 16.9 inches (429 mm) follows the typical MLRA concept. The major difference between this LRU and the others of MLRA 46 is the Chinook wind. These winds create massive temperature swings in the winter which can melt snow cover and initiate bud growth on shrubs. These changes may dry soil affecting plant production and species composition. The Rocky Mountain Front Foothills receives 10 inches (247 mm) to 42 inches (1083 mm) annually. However 42 inches is extremely limited extent. The average air temperature ranges from 36 degrees Fahrenheit (2.39 degrees C) to 46 degrees Fahrenheit (8.02 degrees C). The soil temperature regime is frigid with a soil moisture regime dominated by ustic with areas of udic. Average frost-free days is 70 to 110 days.

The vegetation potential for the Rocky Mountain Front Foothills LRU can be variable but is dominated by rangeland. Forested extents are typically minimal and consist primarily of Douglas fir, limber pine, ponderosa pine, and Rocky Mountain juniper with mixed grassland understory. The rangeland of this LRU follows the general concept of the MLRA. The dryer sites are dominated by bluebunch wheatgrass and as the precipitation increases and temperatures decrease rough fescue increases. In areas that receive the highest precipitation, Columbia and Richardson’s needlegrass may exist. Shrub cover is limited in this area and is generally silver sagebrush and shrubby cinquefoil with areas of chokecherry and buffaloberry (both Russet and silver). The glacial drift areas will often have wetland associated vegetation in potholes as well as large areas of quaking aspen with mixed meadows.

Conversion from rangeland to cropland has been the largest land use change of this relatively intact grassland system. Small grain (barley and wheat) production is the most common crop produced in this area. Forage crops such as hay barley, perennial grass pasture, and alfalfa hay are also common. Irrigation from the area's extensive water resources facilitates highly productive farming practices.

MLRA 46 has experienced high conversion from rangeland to urban development where larger expanses of land have been separated into smaller ranchette subdivisions. Often these ranchettes experience extremely high grazing pressure from companion animals.

Classification relationships

EPA Ecoregion Level III: Canadian Rockies
Level IV: Northern Front
Southern Carbonate Front

EPA Ecoregion Level III: Northwestern Glaciated Plains
Level IV: Rocky Mountain Front Foothill Potholes
Sweetgrass Uplands
Foothills Grasslands
Glaciated Northern Grasslands

EPA Ecoregion Level III: Northwestern Great Plains
Level IV: Limy Foothill Grassland
Judith Basin Grassland

Ecological site concept

• Site receives additional effective moisture because of run-in or stream overflow
• Seasonal water table greater than or equal to 40 inches from ground surface
• Soil saline (EC greater than 4 within surface 4 inches)
• Salt tolerant plants dominate site

Associated sites

R046XN629MT	Saline Upland (SU) RRU 46-N 10-14 PZ Saline Upland is higher on the landscape

R046XN629MT

Saline Upland (SU) RRU 46-N 10-14 PZ

Saline Upland is higher on the landscape

Similar sites

R046XN629MT	Saline Upland (SU) RRU 46-N 10-14 PZ Saline Upland has similar plant community however lower production

R046XN629MT

Saline Upland (SU) RRU 46-N 10-14 PZ

Saline Upland has similar plant community however lower production

Table 1. Dominant plant species

Tree	Not specified
Shrub	(1) Atriplex gardneri (2) Krascheninnikovia lanata
Herbaceous	(1) Sporobolus airoides (2) Pascopyrum smithii

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Physiographic features

This ecological site occurs on overflow lands where salt and/or alkali accumulations are apparent and salt-tolerant species dominate the plant community. It is associated mainly with ephemeral streams (those that flow only in response to a precipitation event or snow melt, and the water table is lower than the channel bottom).

The site is nearly level to gently sloping; rarely exceeding 5 percent slope.

Table 2. Representative physiographic features

Landforms	(1) Foothills > Slough (2) Foothills > Stream terrace (3) Foothills > Fan (4) Foothills > Swale (5) Foothills > Pothole
Flooding duration	Extremely brief (0.1 to 4 hours) to brief (2 to 7 days)
Flooding frequency	None to rare
Elevation	1,097 – 1,768 m
Slope	0 – 5%
Water table depth	102 cm
Aspect	Aspect is not a significant factor

Climatic features

The climate of the Saline Lowland ecological site falls into Climatic Subset B. The central concept of Climatic Subset B is 13 to 19 inches Relative Effective Annual Precipitation (REAP) and 70 to 110 days frost free. Calculated averages based on climate stations suggest that this ecological site receives 16 inches of precipitation with 70 to 115 Frost Free Days.

The soil temperature regime for this Saline Lowland ecological site is frigid and the soil moisture regime is ustic

Table 3. Representative climatic features

Frost-free period (characteristic range)	61-84 days
Freeze-free period (characteristic range)	109-122 days
Precipitation total (characteristic range)	330-432 mm
Frost-free period (actual range)	39-110 days
Freeze-free period (actual range)	70-129 days
Precipitation total (actual range)	330-483 mm
Frost-free period (average)	70 days
Freeze-free period (average)	115 days
Precipitation total (average)	406 mm

Characteristic range

Actual range

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Figure 1. Monthly precipitation range

Characteristic range

Actual range

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Figure 2. Monthly minimum temperature range

Characteristic range

Actual range

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Figure 3. Monthly maximum temperature range

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Figure 4. Monthly average minimum and maximum temperature

Figure 5. Annual precipitation pattern

Figure 6. Annual average temperature pattern

Climate stations used

(1) BABB 6 NE [USC00240392], Babb, MT
(2) CUT BANK MUNI AP [USW00024137], Cut Bank, MT
(3) FAIRFIELD [USC00242857], Fairfield, MT
(4) AUGUSTA [USC00240364], Augusta, MT
(5) ROGERS PASS 9 NNE [USC00247159], Wolf Creek, MT
(6) ST MARY [USC00247292], Babb, MT
(7) DEL BONITA [USC00242301], Cut Bank, MT

Influencing water features

Site is located at the bottom third of the slope where run-in or stream overflow brings saline or alkali water to or near the surface where salt accumulate. This site may have a seasonal water table as close as 40 inches from the surface. Seasonal water flows as a result of high precipitation events or spring snowmelt. These areas may also be associated near springs or seeps that travel through salt laden material.

Wetland description

Site is not considered a wetland

Soil features

The soils on this site are moderately to strongly saline, medium- to fine-textured, moderately deep to deep, but poorly developed. This site has a seasonal high water table that is deeper than 40 inches. Soils tend to be saline or sodic. Soluble salt accumulations are often apparent at or near the surface. Most herbaceous roots extend less than 20 inches below the soil surface. Surface textures are mainly silty clay, silty clay loam, clay loam and loam. Permeability varies with surface texture and the amount of salt and/or sodium present. Soil ph varies from 7.4 – 9.0.

Table 4. Representative soil features

Parent material	(1) Alluvium – sedimentary rock
Surface texture	(1) Clay loam (2) Loam (3) Silty clay loam (4) Silty clay
Family particle size	(1) Fine (2) Fine-loamy
Drainage class	Moderately well drained to somewhat poorly drained
Permeability class	Moderately slow to very slow
Electrical conductivity (0-101.6cm)	4 – 16 mmhos/cm
Sodium adsorption ratio (0-101.6cm)	5 – 25
Soil reaction (1:1 water) (0-101.6cm)	7.4 – 9

Table 5. Representative soil features (actual values)

Drainage class	Not specified
Permeability class	Not specified
Electrical conductivity (0-101.6cm)	Not specified
Sodium adsorption ratio (0-101.6cm)	3 – 35
Soil reaction (1:1 water) (0-101.6cm)	Not specified

Ecological dynamics

The Saline Lowland (SL) Ecological Site is characterized by the production and composition of the Reference Plant Community, which is defined by soils, precipitation, and the temperature regime influencing the site. The Saline Lowland ecological site receives
additional effective moisture from offsite runoff from precipitation events or stream overflow. The site has saline or saline-sodic conditions within 4 inches of the soil surface which is expressed as an Electrical Conductivity of 4-30 mmhos/cm. This site may also have a seasonal water table within 40 inches of the soil surface.

In the Rocky Mountain Foothills of Northern Montana, MLRA 46X LRU B is found where an Ustic soil moisture regime occurs. This area is typified by a frigid soil temperature phase which receives a yearly representative value of 15 to 19 inches of relative effective annual precipitation and between 70 and 110 consecutive frost-free days annually.

Much of the precipitation comes in May and June. Primary plant growth typically occurs between May and early July however due to the increased soil moisture the growing season is extended longer into the summer than other sites in this MLRA. Dominant plants are those that have adapted to these conditions. A period of fall “green-up” can occur amongst this cool season dominated plant community if adequate precipitation is present.

The reference plant community is dominated by alkali sacaton (Sporobolus airoides), basin wildrye (Leymus cinereus), western wheatgrass (Pascopyrum smithii), alkali cordgrass (Spartina gracilis), and Sandberg bluegrass (Poa secunda). Subdominant species may include black greasewood (Sarcobatus vermiculatus), big sagebrush (Artemisia tridentata), winterfat (Krascheninnikovia lanata) and Gardner's saltbush (Atriplex gardnerii).

As the community changes away from reference, cool season shortgrasses tend to increase. If allowed to continue non-native grasses (cheatgrass, field brome, and ventenata) tend to take over the site. Throughout this time bare ground increases exponentially. The short rooted nature of the sodforming grasses erosion can occur rapidly.

Historical records indicate, prior to the introduction of livestock (cattle and sheep) during the late 1800’s, elk and bison grazed this ecological site. Due to the nomadic nature and herd structure of bison, areas that were grazed received periodic high intensity short duration grazing pressure.

Livestock grazing has occurred on most of this ecological site for more than 150 years. The gold boom in the 1860s brought the first herds of livestock overland from Texas, and homesteaders began settling the area. During this time cattle were the primary domestic grazers in the area.

Natural fire was a frequent ecological driver of this Ecological Site however due to the relatively low plant density and fire resistant plants (saltbush and greasewood) stand replacement was rare. The reference community with a high amount of herbaceous growth as a result of favorable growing conditions has the highest susceptibility to extreme fire. A herbaceous invaded community that contains high amounts of exotic annual grasses can greatly increase risk of fire frequency and intensity resulting in potential removal of native species.

Some of the major invasive species that can occur on this site include (but not limited to) spotted knapweed (Centaurea stoebe), leafy spurge (Euphorbia esula), cheatgrass (Bromus techtorum), Canada thistle (Cirsium arvense), dandelion (Taraxicum spp), and Kentucky
bluegrass (Poa pratensis). Invasive weeds have a high impact on this Ecological Site.

Plant Communities and Transitions
A State and Transition Model for this ecological site is depicted below. Thorough descriptions of each state, transition, plant community, and pathway follow the model. This model is based on available experimental research, field data, field observations, and interpretations by experts. It is likely to change as knowledge increases.

The plant communities within the same ecological site will differ across the MLRA due to the naturally occurring variability in weather, soils, and aspect. The biological processes on this site are complex; therefore, representative values are presented in a land management context. The species lists are representative and are not botanical descriptions of all species occurring, or potentially occurring, on this site. They are intended to cover the core species and known range of conditions and responses. Both percent species composition by weight and percent canopy cover are referenced in this document. Canopy cover drives the transitions between communities and states because of the influence of shade, interception of rainfall and competition for available water. Species composition by dry weight remains an important descriptor of the herbaceous community and of the community as a whole. Woody species are included in species composition for the site. Calculating similarity index requires use of species composition by dry weight.

Although there is considerable qualitative experience supporting the pathways and transitions within the State and Transition Model (STM), no quantitative information exists that specifically identifies threshold parameters between grassland types and invaded types in this ecological site. For information on STMs, see the following citations: Bestelmeyer el al. 2003, Bestelmeyer et al. 2004, Bestelmeyer and Brown 2005, Stringham et al. 2003.

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

State 1
Reference State

The Reference State of this ecological site consists of 2 known potential plant communities 1.1 Reference Bunchgrass Community and 1.2 Wheatgrass Community. These are described below but are generally characterized by a mid-statured, cool season grass community with limited shrub production. Community 1.1 is dominated by a mix of western wheatgrass, winterfat, basin wildrye, alkali sacaton, alkali cordgrass. Community 1.1 is considered the reference while Community 1.2 has a codominance of western wheatgrass, alkali sacaton, saltbush, Sandberg bluegrass, and other shrubs including big sagebrush and black greasewood.

Community 1.1
Reference Bunchgrass Community

In the Reference Bunchgrass Community, basin wildrye, alkali sacaton, and western wheatgrass are dominant. On the wettest of sites, alkali cordgrass will increase. Alkalie bluegrass (now known as Sandberg bluegrass), Inland saltgrass, and prairie Junegrass are also component of the reference state. Big sagebrush, black greasewood, Gardner's saltbush, and winter fat are dominant shrubs. Forbs tend to be restricted to salt tolerant succuents such as seepweed (Suaeda) and poverty sumpweed (Iva axillaris) however several goosefoot species (Chenopodium ssp) may also be present. About 90 percent of the annual production is from grasses and sedges, most of which is produced during the cool season. Forbs and shrubs each contribute about 5 percent to total annual production. Total vegetative production averages 3000 lbs/ac in normal years, 4500 lbs/ac in favorable years, and 1750 lbs/ac in “unfavorable” years.

Community 1.2
Mixed Grass Community

The Mixed Grass Community is defined by a plant community formed primarily of a codominance of midstatured bunchgrasses and rhizomatous grasses with an increase in forbs and shrubs. This is typically a result of non-prescribed grazing removing some of the basin wildrye and alkali sacaton. If present, basin wildrye may be in such low density it no long contributes to the structural integrity of the community. This community is extremely susceptible to invasive non-native species due to an increase in bare ground is expected due to a reduction of basal area occupied by the larger bunchgrasses. In this community, cheatgrass possibly exists as a trace amount which poses a risk to the hydrologic function, biotic integrity, and site stability due to its shallow rooting structure and ability to overtake areas.

Pathway 1.1a
Community 1.1 to 1.2

The community pathway from the Reference Bunchgrass Community (1.1) to the Mixed Grass Community (1.2) is primarily driven by improper grazing. When vigor declines enough for plants to die or become smaller, species with higher grazing tolerance, such as western wheatgrass and Sandberg bluegrass, increase in vigor and production as they access the resources previously used by green needlegrass and other tall grasses. Decrease of species composition by weight of the tall grasses to be equal to that of rhizomatous grasses specifically western wheatgrass and thickspike wheatgrass indicates that the reference plant community has shifted to the Mixed Grass Community (1.2). The driver for community shift 1.1A is improper grazing management or prolonged drought. This shift is triggered by the loss of vigor of tall grasses, soil erosion, or prolonged drought coupled with improper grazing. Blaisdell (1958) stated that drought and warmer than normal temperatures are known to advance plant phenology by as much as one month. During drought years, plants may be especially sensitive or in a critical stage of development earlier than expected.

Pathway 1.2a
Community 1.2 to 1.1

The Mixed Grass Community (1.2) will return to the Reference Bunchgrass Community (1.1) with proper grazing management and appropriate grazing intensity. Favorable moisture conditions will facilitate or accelerate this transition. It may take several years of favorable conditions for the community to transition back to a basin wildrye and alkali sacaton dominated state. The driver for this community shift (1.2a) is increased vigor of the tall grasses resulting in increase biomass production and dominance of plant community. The trigger for this shift is the change in grazing management favoring basin wildrye. In general, conservative grazing management styles such as deferred or rest rotations utilizing moderate grazing (less than 50% use) coupled with favorable growing conditions like cool, wet springs are these triggers. These systems tend to promote increases in soil organic matter which promotes microfauna and can increase infiltration rates. Inversely, long periods of rest at a time when this state is considered to be stable may not result in an increase in native bunchgrasses and it has been suggested (Noy-Meir 1975) that these long periods of rest or underutilization may actually drive the system to a lower level of stability by creating large amounts of standing biomass, dead plant caudex centers, and gaps in the plant canopy.

State 2
Shortgrass State

State 2, Shortgrass State, has been altered by long term unmanaged, heavy grazing. In this State, drought conditions may speed the departure from reference.

Community 2.1
Shortgrass Community

The Shortgrass Community (2.1) receives its name by the overall dominance of shortgrasses such as inland saltgrass, sand dropseed, sandberg bluegrass, bottlebrush squirreltail, foxtail barley, and sedges. The mid and tall warm season perennial grasses (alkali sacaton, western/thickspike wheatgrasses, alkali cordgrass, etc.) are either significantly reduced or absent. Poverty weed, knotweed, seepweed, curlycup gumweed and other forbs account for about 10% of the annual production. Winterfat is removed from this plant community and replaced by a dominance of black greasewood, saltbush, and plains pricklypear cactus. This is a result of a combination of long term drought and overgrazing (grazing that exceeds 50 percent utilization without proper rest period and/or repeated seasonal use). Amount of bare ground is moderately higher than expected. Surface salts are quite extensive.

State 3
Invaded State

Site is invaded by nonnative herbaceous species primarily cheatgrass, field brome, ventenata, and halogeton. This is often a result of reduced vigor in States 1 and 2. The reduced vigor may be attributed to overgrazing however longterm drought may also trigger reduced vigor of these communities

Community 3.1
Invaded Community

The Invaded Community consists primarily of non-native grasses and forbs. The primary species is cheatgrass however ventenata is known to be present in this MLRA allowing for rapid invasion. There tends to be an increase in sagebrush and greasewood cover. Native grasses are often limited to short bunchgrasses although some taller grasses may exist in the protective bases of shrubs. The increase of annual grasses can increase the intensity and severity of wildfire. The transition to this community is driven by 2 likely disturbances. The first being repeated heavy, unmanaged grazing and the other is intense fire. These often occur in combination which creates bare ground, depletes organic matter, and increases evapotranspiration. Extensive restoration practices are needed to make this community resemble the reference state however it will never return to reference due to the severe departure and often loss of soil resources needed to maintain reference. Restoration to a community that resembles reference will require extensive and expensive inputs such as pest management, brush management and range seeding however removal of existing species may actually accelerate erosion of the soil surface if not properly managed.

Transition T1
State 1 to 2

This transition is often triggered by long term overgrazing or other human disturbances. Long term drought or altered hydrologic function is also a factor. This system is seasonally wet and if a drying cycle lasts long enough health and vigor of the species present is reduce which allows short grasses to take advantage of limited water resources on the potentially reduced salinity of the soil surface.

Transition T3
State 1 to 3

Invasion of the community by nonnative herbaceous species including cheatgrass, field brome, and halogeton (Halogeton glomerata). Often as a result of long term overgrazing and/or intense fire which reduces vigor of native herbaceous species. This transition is often irreversible to due the high salinity as well as seasonally wet soil conditions.

Restoration pathway R1
State 2 to 1

Improved grazing management with favorable growing conditions may allow deep rooted bunchgrasses to reestablish dominance. Limited prescribed fire may reduce vigor of shortgrasses and shrubs temporarily. Due to the potentially wet soil conditions associated with this site mechanical alteration of the soil and vegetation is not recommended.

Transition T2
State 2 to 3

Additional community tables

Interpretations

Animal community

The Saline Lowland Ecological site provides for a variety of wildlife habitat for an array of species. Prior to the settlement of this area, large herds of antelope, elk and bison roamed. Though the bison that once utilized this landscape have been replaced with domestic livestock, wildlife still utilize this largely intact landscape for habitat The relatively high grass component of the Reference Community provides excellent nesting cover for multiple neotropical migratory birds as well as provide hiding habitat for larger animals.
Greater Sage Grouse likely utilize most states of this ecological site as there are high amounts of forbs and insects as a result of the favorable soil moisture. Even in the Shortgrass State, sage grouse will utilize the increased forb and shrub cover for both foraging and hiding cover. This site would be considered critical habitat for most lifestages of Greater Sage Grouse.

Managed livestock grazing is suitable on this site due to the potential to produce an abundance of high quality forage. This is often a preferred site for grazing by livestock, and animals tend to congregate in these areas. In order to maintain the productivity of this site,grazing on adjoining sites with less production must be managed carefully to be sure utilization on this site is not excessive. Management objectives should include maintenance or improvement of the native plant community. Careful management of timing and duration of grazing is important. Shorter grazing periods and adequate deferment during the growing season are recommended for plant maintenance, health, and recovery.
Continual non-prescribed grazing of this site will be injurious, will alter the plant composition and production over time, and will result in transition to the Shortgrass State. Transition to other states will depend on duration of poorly managed grazing as well as other circumstances such as weather conditions and fire frequency. Further degradation will result in transition to the Invaded State. Management should focus on grazing management strategies that will prevent further degradation, such as seasonal grazing deferment or winter grazing where feasible. Communities within this state are still stable and healthy under proper management. Forage quantity and/or quality may be substantially decreased from the Reference State.

Grazing is possible in the Invaded State. Invasive species are generally less palatable than native grasses. Forage production is typically greatly reduced in this state. Due to the aggressive nature of invasive species, sites in the Invaded State face increased risk for further degradation. Grazing has to be carefully managed to avoid further soil loss and degradation and possible livestock health issues.

Prescriptive grazing can be used to manage invasive species. In some instances, carefully targeted grazing (sometimes in combination with other treatments) can reduce or maintain species composition of invasive species.

Supporting information

Inventory data references

Information presented was derived from NRCS inventory data, National Resources Inventory (NRI) data, literature, field observations, and personal contacts with range-trained personnel (i.e., used professional opinion of agency specialists, observations of land managers, and outside scientists).

Other references

McLean, A. and S. Wikeem. 1985. Influence of season and intensity of defoliation on bluebunch wheatgrass survival and vigor in southern British Columbia. Journal of Range Management 38:21–26.

Ross, R.L., E.P. Murray, and J.G. Haigh. July 1973. Soil and Vegetation of Near-pristine sites in Montana.

Colberg, T.J. and J.T. Romo. 2003. Clubmoss effects on plant water status and standing crop. Journal of Range Management 56:489–495.

Walker, L.R. and S.D. Smith. 1997. Impacts of invasive plants on community and ecosystem properties. Pages 69–86 in Assessment and management of plant invasions. Springer, New York, NY.

Barrett, H. 2007. Western Juniper Management: A Field Guide.

Miller, R.F., T.J. Svejcar, and J.A. Rose. 2000. Impacts of western juniper on plant community composition and structure. Journal of Range Management 53:574–585.

Masters, R. and R. Sheley. 2001. Principles and practices for managing rangeland invasive plants. Journal of Range Management 38:21–26.

Hobbs, J.R. and S.E. Humphries. 1995. An integrated approach to the ecology and management of plant invasions. Conservation Biology 9:761–770.

DiTomaso, J.M. 2000. Invasive weeds in Rangelands: Species, Impacts, and Management. Weed Science 48:255–265.

Dormaar, J.F., B.W. Adams, and W.D. Willms. 1997. Impacts of rotational grazing on mixed prairie soils and vegetation. Journal of Range Management 50:647–651.

Smoliak, S., R.L. Ditterlin, J.D. Scheetz, L.K. Holzworth, J.R. Sims, L.E. Wiesner, D.E.
Baldridge, and G.L. Tibke. 2006. Montana Interagency Plant Materials Handbook.

Wilson, A.M., G.A. Harris, and D.H. Gates. 1966. Cumulative Effects of Clipping on Yield of Bluebunch wheatgrass. Journal of Range Management 19:90–91.

Blaisdell, J.P. 1958. Seasonal development and yield of native plants on the Upper Snake River Plains and their relation to certain climate factors.

Whitford, W.G., E.F. Aldon, D.W. Freckman, Y. Steinberger, and L.W. Parker. 1989. Effects of Organic Amendments on Soil Biota on a Degraded Rangeland. Journal of Range Management 41:56–60.

Stavi, I. 2012. The potential use of biochar in reclaiming degraded rangelands. Journal of Environmental Planning and Management 55:1–9.

Bestelmeyer, B., J.R. Brown, J.E. Herrick, D.A. Trujillo, and K.M. Havstad. 2004. Land Management in the American Southwest: a state-and-transition approach to ecosystem complexity. Environmental Management 34:38–51.

Bestelmeyer, B. and J. Brown. 2005. State-and-Transition Models 101: A Fresh look at vegetation change.

Stringham, T.K., W.C. Kreuger, and P.L. Shaver. 2003. State and Transition Modeling: an ecological process approach. Journal of Range Management 56:106–113.

Stringham, T.K. and W.C. Krueger. 2001. States, Transitions, and Thresholds: Further refinement for rangeland applications.

Stavi, I 2012. The potential use of biochar in reclaiming degraded rangelands. Journal of Environmental Planning and Management 55:1-9

Humphrey, L. David. 1984. Patterns and mechanisms of plant succession after fire on Artemisia-grass sites in southeastern Idaho Vegetation. 57: 91-101.

Tirmenstein, D. 1999. Gutierrezia sarothrae. In: Fire Effects Information System, [Online]. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory (Producer). https://www.fs.fed.us/database/feis/plants/shrub/gutsar/all.html [2022, March 30].

Approval

Kirt Walstad, 7/19/2023

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)	Grant Petersen
Contact for lead author	grant.petersen@usda.gov
Date	08/05/2020
Approved by	Kirt Walstad
Approval date
Composition (Indicators 10 and 12) based on	Annual Production

Indicators

Number and extent of rills:
Rills are not present in the reference state
Presence of water flow patterns:
Water flow patterns will not be present in the Reference State
Number and height of erosional pedestals or terracettes:
Pedestals and terracettes will not be present in the Reference State
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is extremely limited due to high amounts of herbaceous growth and litter. Bare ground may be expressed in very small patches of up to 5 percent.
Number of gullies and erosion associated with gullies:
Gullies will not be present in the Reference State
Extent of wind scoured, blowouts and/or depositional areas:
Wind scoured, blowouts, and/or depositional areas will not be present in the Reference State.
Amount of litter movement (describe size and distance expected to travel):
No litter movement is expected in the Reference State.
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
This site is stable due to deep rooted nature of the bunchgrass dominated community. Stability ratings of 5 to 6 under both canopy and ratings of 3-5 in plant interspaces are expected. .
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Soil Structure at the surface is weak subangular blocky to weak fine granular. A Horizon should be 4-8 inches thick with color, when wet, typically ranging in Value of 5 or less and Chroma of 4 or less.

Local geology may affect color, it is important to reference the Official Series Description (OSD) for characteristic range. https://soilseries.sc.egov.usda.gov/osdname.aspx
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
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):
A compaction layer is not present in the reference condition. Soil profile may contain an abrupt transition to an Argillic horizon which can be misinterpreted as compaction, however, the soil structure will be fine to medium subangular blocky, where a compaction layer will be platy or structureless (massive).
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:
Tall, warm season bunch grasses = mid-stature, cool season bunch grasses> mid-stature cool season rhizomatous grasses > sedges and rushes > short, warm season rhizomatous grasses

Sub-dominant:
forbs = shrubs.

Other:

Additional:
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Mortality in herbaceous species is not evident. Species with bunch growth forms may have some natural mortality in centers is 3% or less.
Average percent litter cover (%) and depth ( in):
Litter cover is high and ranges from 50-65 percent. Litter depth is highly variable from nearly immeasurable in plant interspaces to very thick (1 inch) under plants. Averages are 0.25 to 0.5 inches deep.
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Total vegetative production averages 3000 lbs/ac, 4500 lbs/ac as a high, and 1750 lbs/ac as a low

Production varies based on effective precipitation and natural variability of soil properties for this ecological site.
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:
Potential invasive (including noxious) species (native and non-native). Invasive species on this ecological site include (but not limited to): annual brome spp., spotted knapweed, leafy spurge, crested wheatgrass, salsify, and halogeton

Native species such as rocky mtn Juniper, ponderosa pine, pricklypear cactus, broom snakeweed, Sandberg’s bluegrass, etc. when their populations are significant enough to affect ecological function, indicate site condition departure.
Perennial plant reproductive capability:
In the reference condition, all plants are vigorous enough for reproduction either by seed or rhizomes in order to balance natural mortality with species recruitment.

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Natural ResourcesConservation Service

Ecological site R046XN230MT

Saline Lowland (SL) RRU 46-N 13-19 PZ

Last updated: 7/19/2023 Accessed: 11/24/2024

General information

MLRA notes

LRU notes

Classification relationships

Ecological site concept

Associated sites

Similar sites

Table 1. Dominant plant species

Ecosystem states

State 1 submodel, plant communities

State 2 submodel, plant communities

State 3 submodel, plant communities

Natural Resources
Conservation Service

Last updated: 7/19/2023
Accessed: 11/24/2024