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Ecological site R052XC210MT

Saline Upland (SU) 10-14" p.z.

Last updated: 1/24/2024
Accessed: 11/21/2024

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General information

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

MLRA notes

Major Land Resource Area (MLRA): 052X–Brown Glaciated Plains

The Brown Glaciated Plains, MLRA 52, is an expansive and agriculturally and ecologically significant area. It consists of approximately 14.5 million acres and stretches across 350 miles from east to west, encompassing portions of 15 counties in north-central Montana. This region represents the southwestern limit of the Laurentide Ice Sheet and is considered to be the driest and westernmost area within the vast network of glacially derived prairie pothole landforms of the northern Great Plains. Elevation ranges from 2,000 feet (610 meters) to 4,600 feet (1,400 meters).

Soils are primarily Mollisols, but Entisols, Inceptisols, Alfisols, and Vertisols are also common. Till from continental glaciation is the predominant parent material, but alluvium and bedrock are also common. Till deposits are typically less than 50 feet thick, and in some areas glacially deformed bedrock occurs at or near the soil surface (Soller, 2001). Underlying the till is sedimentary bedrock largely consisting of Cretaceous shale, sandstone, and mudstone (Vuke et al., 2007). The bedrock is commonly exposed on hillslopes, particularly along drainageways. Significant alluvial deposits occur along glacial outwash channels and major drainages, including portions of the Missouri, Teton, Marias, Milk, and Frenchman Rivers. Large glacial lakes, particularly in the western half of the MLRA, deposited clayey and silty lacustrine sediments (Fullerton et al., 2013).

Much of the western portion of this MLRA was glaciated towards the end of the Wisconsin age, and the maximum glacial extent occurred approximately 20,000 years ago (Fullerton et al., 2004). The result is a geologically young landscape that is predominantly a level till plain interspersed with lake plains and dominated by soils in the Mollisol and Vertisol orders. These soils are very productive and generally are well suited to dryland farming. Much of this area is aridic-ustic. Crop-fallow dryland wheat farming is the predominant land use. Areas of rangeland typically are on steep hillslopes along drainages.

The rangeland, much of which is native mixed-grass prairie, increases in abundance in the eastern half of the MLRA. The Wisconsin-age till in the north-central part of this area typically formed large disintegration moraines with steep slopes and numerous poorly drained potholes. A large portion of Wisconsin-age till occurring on the type of level terrain that would typically be optimal for farming has large amounts of less-suitable sodium-affected Natrustalfs. Significant portions of Blaine, Phillips, and Valley Counties were glaciated approximately 150,000 years ago during the Illinoisan age. Due to erosion and dissection of the landscape, many of these areas have steeper slopes and more exposed bedrock than areas glaciated during the Wisconsin age (Fullerton and Colton, 1986).

While much of the rangeland in the aridic-ustic portion of MLRA 52 is classified as belonging to the “dry grassland” climatic zone, sites in portions of southern MLRA 52 may belong to the “dry shrubland” climatic zone. The Dry Shrubland climatic zone represents the northernmost extent of the big sagebrush (Artemisia tridentata) steppe on the Great Plains. Because similar soils occur in both southern and northern portions of the MLRA, it is currently hypothesized that climate is the primary driving factor affecting big sagebrush distribution in this area. However, the precise factors are not fully understood at this time.

Sizeable tracts of largely unbroken rangeland in the eastern half of the MLRA and adjacent southern Saskatchewan are home to the Northern Montana population of greater sage-grouse (Centrocercus urophasianus), and large portions of this area are considered to be a Priority Area for Conservation (PAC) by the U.S. Fish and Wildlife Service (U.S. Fish and Wildlife Service, 2013). This population is unique among sage grouse populations because many individuals overwinter in the big sagebrush steppe (dry shrubland) in the southern portion of the MLRA and then migrate to the northern portion of the MLRA, which lacks big sagebrush (dry grassland), to live the rest of the year (Smith, 2013).

Areas of the till plain near the Bearpaw and Highwood Mountains as well as the Sweetgrass Hills and Rocky Mountain foothills are at higher elevations, receive higher amounts of precipitation, and have a typic-ustic moisture regime. These areas have significantly more rangeland production than the drier aridic-ustic portions of the MLRA and have enough moisture to produce crops annually rather than just bi-annually, as in the drier areas. Ecological sites in this higher precipitation area are classified as the Moist Grassland climatic zone.

Ecological site concept

Saline Upland is an ecological site of limited extent occurring on fans, fan aprons, and terraces in MLRA 52. The distinguishing characteristic of this site is that saline, sodic, or saline-sodic conditions are evident in the upper 20 inches of soil. Soils for this ecological site are typically very deep (more than 60 inches), well drained, and derived from clayey alluvium or outwash deposits. Characteristic vegetation is western wheatgrass (Pascopyrum smithii), alkali sacaton (Sporobolus airoides), Nuttall’s saltbush (Atriplex nuttallii).

Associated sites

R052XC205MT	Clayey (Cy) 10-14" p.z. soils >20 inches in depth, higher production, and no hardpan, different species composition
R052XC216MT	Shallow to Gravel (SwGr) 10-14" p.z. similar position in landscape, soils with depth restriction that limits available moisture, soils 10-20” deep to sands or loamy sands
R052XC215MT	Shallow Clay (SwC) 10-14" p.z. soils 10-20” deep to bedrock’ soils are clayey over clayey shale
R052XC204MT	Claypan (Cp) 10-14" p.z. has 2-8” of soil over the hard argillic layer, less bare ground, and higher production
R052XC206MT	Dense Clay (DC) 10-14" p.z. has a hard restrictive layer in the soil at or near the surface, salt tolerant plants may be present but are rarely dominant

Similar sites

R052XN170MT	Saline Upland (SU) 10-14" p.z. R053AE071MT, same concept different climate and potential.

R052XN170MT

Saline Upland (SU) 10-14" p.z.

R053AE071MT, same concept different climate and potential.

Table 1. Dominant plant species

Tree	Not specified
Shrub	(1) Atriplex nuttallii
Herbaceous	(1) Pascopyrum smithii (2) Sporobolus airoides

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Physiographic features

This ecological site occurs on nearly level to moderately sloping fans and terraces in the uplands. It is associated with shale beds and soils have a clay loam to clay surface layer, subsoil, and underlying material. Soils contain salt and/or alkali accumulations and salt-tolerant species dominate the plant community. Slopes are usually less than 8%. Elevations normally vary from 2200 to 4000 feet.

Table 2. Representative physiographic features

Landforms	(1) Terrace (2) Fan (3) Fan apron
Runoff class	Medium to very high
Flooding frequency	None
Ponding frequency	None
Elevation	1,875 – 4,500 ft
Slope	8%
Aspect	W, NW, N, NE, E, SE, S, SW

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 (characteristic range)	85-123 days
Freeze-free period (characteristic range)	116-142 days
Precipitation total (characteristic range)	10-14 in
Frost-free period (average)	94 days
Freeze-free period (average)	125 days
Precipitation total (average)	12 in

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) SHELBY [USC00247500], Shelby, MT
(2) CHESTER [USC00241692], Chester, MT
(3) GLASGOW [USW00094008], Glasgow, MT
(4) HAVRE CITY CO AP [USW00094012], Havre, MT

Soil features

These deep, well drained soils formed in alluvium and glacial till. The soils usually contain a 2-3-inch surface layer, a 2-3 inch clay subsoil, and a strongly saline underlying material to a depth of > 60 inches. The surface texture is clay loam or silty clay; subsoil textures are usually clay or silty clay. Permeability is very slow. Salt tolerant plants dominate the site. Soil ph varies from 6.6 – 9.0. This site is characterized by the following taxonomic units: Benz and Nobe.

Table 4. Representative soil features

Parent material	(1) Alluvium – shale (2) Glaciofluvial deposits
Surface texture	(1) Clay loam (2) Silty clay (3) Loam
Family particle size	(1) Clayey
Drainage class	Well drained
Permeability class	Very slow
Soil depth	20 – 80 in
Surface fragment cover <=3"	Not specified
Surface fragment cover >3"	Not specified
Available water capacity (Depth not specified)	3 – 5 in
Calcium carbonate equivalent (Depth not specified)	10%
Electrical conductivity (Depth not specified)	4 – 16 mmhos/cm
Sodium adsorption ratio (Depth not specified)	10 – 70
Soil reaction (1:1 water) (Depth not specified)	6.6 – 9.6
Subsurface fragment volume <=3" (Depth not specified)	5%
Subsurface fragment volume >3" (Depth not specified)	5%

Ecological dynamics

This site developed through time under the influence of climate, geological materials, fire, plants and animals. Research on upland ecological sites consistently shows that precipitation is the principal factor altering productivity (Heitschmidt et al. 2005). The same authors concluded that grazing reduces herbage standing crop, whereas its effects on aboveground net primary production vary with timing of grazing and precipitation events, along with the functional and structural composition of the plant community. Some ecologists believe that these lands may have burned on a natural interval of 10-12 years (Frost 1998). However, environmental characteristics of this site limit herbage production and subsequent fuel accumulation. Therefore, in comparison to normal upland range sites, the role of natural fire is probably less significant in the development of this site. The resultant historic climax plant community (HCPC) is the basis for plant community interpretations. The HCPC has been determined by evaluating rangeland relic areas, and other areas protected from excessive disturbance.
The HCPC is comprised of a mixture of cool and warm season grasses and shrubs. About 70% of the annual production is from grasses and sedges, most of which is produced during the cool season. Forbs and shrubs contribute 5% and 25%, respectively, to total annual production. Total vegetative production averages 500 lbs/ac in normal years, 350 lbs/ac in “unfavorable” years, and 600 lbs/ac in “favorable” years.
This site is moderately resilient to disturbance because soil characteristics limit plant growth. Departures from the HCPC generally result from management actions, drought, and/or a change in the natural fire regime. The site is considered fragile in the sense that vegetative vigor and composition will rapidly decline with continued adverse impacts. With favorable precipitation and/or prescribed grazing treatments, plant communities that are in the high seral state can return to the HCPC. In contrast, significant succession is unusual within early-seral communities.

Successional pathways of Saline Upland 10-14” p.z. ecological sites cannot be satisfactorily described using traditional theories of plant succession leading to a single climax community (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-seral state. Plant communities occurring below this threshold are in a steady state. Succession back to the HCPC does not occur within a reasonable length of time, and/or without a large input of energy.
Two plant communities and the successional pathways that commonly occur within the Reference State (State #1) are shown in the following diagram. The transitions from State #1 to State #2 (Plant Community B) and State #3 (Plant Community C) are also illustrated. Ecological processes are discussed in the plant community descriptions that follow the diagram.

State and transition model

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Ecosystem states

1. Reference State

2. Plant Community B

3. Plant Community C

T1A	-	Extended drought (>7 years), non-prescribed grazing, no fire
R2A	-	Prescribed grazing, fire, favorable precipitation
T2A	-	Prolonged drought (5-7 years), non-prescribed grazing, no fire
R3A	-	Fire, prescribed grazing

State 1 submodel, plant communities

1.1. Historic Climax Plant Community Western Wheatgrass-Alkali Sacaton-Saltbush

1.2. Saltbush/Western Wheatgrass-Alkali Sacaton

1.1a	-	No fire, non-prescribed grazing, drought (3-5 years)
1.2a	-	Fire, prescribed grazing

State 2 submodel, plant communities

2.1. Short-grass-Dominated

State 3 submodel, plant communities

3.1. Shrub-Dominated

State 1
Reference State

Community 1.1
Historic Climax Plant Community Western Wheatgrass-Alkali Sacaton-Saltbush

The cool season western wheatgrass and warm season alkali sacaton are the dominant plants on this ecological site. They account for about 60 percent of the total annual production in the Historic Climax Plant Community (HCPC). Drought and non-prescribed grazing reduces the competitiveness of the dominant species, and allows lower successional grasses (Nuttall’s alkali grass, inland saltgrass, plains reedgrass, blue grama and prairie junegrass) to increase on the site. About 10 percent of the total production is composed of a mix of warm and cool season short grasses and sedges. Forbs contribute about 5 percent of the total annual production. Poverty sumpweed, onion, hoods phlox, scarlet globemallow, wooly plantain, and biscuitroot are common forbs. The latter group contains a mix of warm and cool season species whose relative occurrence on the site is largely influenced by the timing and amount of precipitation. Nuttall saltbush and greasewood are two common shrubs on this site. Both species make most of their growth during the cool part of the growing season. While Nuttall saltbush is rated a valuable forage plant for livestock and wildlife, greasewood can be poisonous in some situations. Pricklypear cactus and fringed sagewort (a warm season half-shrub) can occur in the HCPC. Shrubs normally make up about 25 percent of the total annual production. Broom snakeweed, annual bromes, and annual forbs are not a part of the HCPC. Their presence indicates possible ecological deterioration, or downward trend. Trend is difficult to interpret because large areas of bare ground between plants are fairly common. Total annual production averages 500 lbs/ac during normal years. However, production declines as the site regresses from the HCPC to lower successional communities. Regression may result from grazing management strategies that do not allow adequate recovery periods between grazing events, drought, and/or the disruption of the normal fire sequence. The above disturbances favor the replacement of alkali sacaton and western wheatgrass by blue grama, sandberg bluegrass, prairie junegrass, poverty weed, hairy golden aster, and hoods phlox. Nuttall saltbush may also be replaced by broom snakeweed, fringed sagewort, etc. Cheatgrass and Japanese brome may invade the site. As the result of these vegetative changes, there is less litter to protect the soil and less infiltration. Hydrologic cycles are impaired when plant communities are unable to effectively use precipitation. Plant cover (litter and canopy of grasses, forbs and shrubs) is from 40 to 50 percent. Basal cover varies from 7 to 15 percent. Litter varies from 20 to 30 percent. Consequently, bare ground averages 50 percent. Thus, infiltration rates are lower, and runoff and erosion are higher than desired on this ecological site. Runoff and soil erosion normally increase as the HCPC regresses to earlier seral states. The major plant species composition and production by dry weight are shown for the HCPC in the following table. Total annual production has been derived from several sources, and has been adjusted to represent a typical annual moisture cycle.

Figure 7. 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	245	350	420
Shrub/Vine	85	125	150
Forb	20	25	30
Total	350	500	600

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	20-30%
Surface fragments >0.25" and <=3"	0-1%
Surface fragments >3"	0-1%
Bedrock	0-1%
Water	0%
Bare ground	50-60%

Table 7. Soil surface cover

Tree basal cover	0%
Shrub/vine/liana basal cover	1-5%
Grass/grasslike basal cover	5-10%
Forb basal cover	1-2%
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	–	0-1%	0-20%	0-25%
>0.5 <= 1	–	0-40%	0-50%	0-50%
>1 <= 2	–	0-50%	0-25%	0-25%
>2 <= 4.5	–	0-10%	0-5%	–
>4.5 <= 13	–	–	–	–
>13 <= 40	–	–	–	–
>40 <= 80	–	–	–	–
>80 <= 120	–	–	–	–
>120	–	–	–	–

Community 1.2
Saltbush/Western Wheatgrass-Alkali Sacaton

Non-prescribed grazing and drought reduce plant height and plant litter. Surface runoff and soil temperature increases, infiltration decreases, and shallow-rooted short grasses (sandberg bluegrass, blue grama, and prairie junegrass) and sedges gain a competitive advantage over medium height, deep-rooted cool season perennial grasses (alkali sacaton and western wheatgrass). They are able to compete more successfully with the mid-grasses because of the ability of relatively shallow root systems to utilize shallowly penetrating moisture, characteristic of this site. In contrast to the Historic Climax Plant Community (HCPC), total annual production is 60 to 80 percent of potential production (400 versus 500 lbs/ac). Western wheatgrass and alkali sacaton contribute less than 50 percent of the annual production. They are less vigorous and individual plant growth is reduced from what it is in the HCPC. Production of the short grasses increases relative to their percentage contribution in the HCPC. Although a few annual forbs are present on disturbed areas, the forb component continues to contribute about 5 percent of the total annual production. Total shrub production remained at about 25 percent; however, production of fringed sagewort increased at the expense of Nuttall saltbush and greasewood. Plant community A is called the “pre-threshold community”. It is critical that this community be recognized and strategies implemented to prevent further regression. Compared to the HCPC, water flow patterns are more numerous than expected, there is slight to moderate active pedestalling, there is more bare ground than expected, there is moderate movement of smaller size litter deposits into depressions or against obstructions, infiltration is slightly to moderately affected by the shift toward more short grasses in the plant community, and the reproductive capability of alkali sacaton and western wheatgrass is somewhat limited relative to recent climatic conditions (USDI and USDA 2000). Although Community A can improve to the HCPC through successional processes, further disturbance will result in regression to a lower state. Once Plant Community 1.2 regresses to a lower state, normal successional processes are restricted.

Pathway 1.1a
Community 1.1 to 1.2

No fire, non-prescribed grazing, drought (3-5 years) Non-prescribed grazing, drought and/or a cessation of the natural fire regime will cause regression from HCPC to Community A.

Pathway 1.2a
Community 1.2 to 1.1

Fire, prescribed grazing Favorable growing conditions, the implementation of prescribed grazing, or periodic fire will move Plant Community A to the HCPC. This succession is possible within a couple of years.

State 2
Plant Community B

Community 2.1
Short-grass-Dominated

This Community is dominated by a mix of cool and warm season short grasses. Blue grama, threadleaf sedge, sandberg bluegrass and other low successional grasses expanded their influence in the community by replacing most of the alkali sacaton and western wheatgrass. A few “stunted” western wheatgrass plants persist in this community. Poverty weed, hoods phlox, and other low successional forbs contribute more than 5 percent of the total annual production. The density of fringed sagewort and broom snakeweed (warm season half-shrubs) increase relative to their presence in the State 1 Communities. Pricklypear cactus is usually conspicuous in this community. Total annual production averages 300 lbs/ac. In comparison to the HCPC, total plant basal cover averages about 10 percent. Litter varies from 10 to 15 percent. Bare ground increases to more than 60 percent. Thus, pedestalling, rills, flow patterns and litter deposits are visible.

State 3
Plant Community C

Community 3.1
Shrub-Dominated

Plant Community C is dominated by Nuttall saltbush, greasewood, fringed sagewort, and broom snakeweed. There has been a significant reduction in percentage of western wheatgrass. The remaining wheatgrasses produce few seed heads and lack vigor. Inland saltgrass, sandberg bluegrass, blue grama and other low-successional grasses and sedges contribute about 50 percent of the total annual production. Annual bromes and pricklypear cactus are conspicuous in the community. An increase in chenopod species is possible, but not enough sites have been inventoried to be certain. Total annual production averaged 200 lbs/ac, a 33 percent reduction from Community B. Litter cover averages about 10 percent. Water flow patterns are numerous and there is moderately active pedestalling. Bare ground is moderately to much higher than expected. Compared to the Historic Climax Plant Community (HCPC), there has been a structural shift from medium height to short grasses, and a functional shift from cool to warm season plants, and an increase in shrub species. Reproductive capability of cool season plants is greatly reduced relative to recent climatic conditions.

Transition T1A
State 1 to 2

Extended drought (>7 years), non-prescribed grazing, no fire Plant Community A will regress to Community B (State 2) under non-prescribed grazing, prolonged drought, or following periodic wildfire (which would reduce competitiveness of shrubs). Regression rates vary with the intensity and frequency of the disturbances. Severe drought may cause retrogression within a couple years.

Transition T1B
State 1 to 3

Non-prescribed grazing, prolonged drought (5-7 years) Plant Community A will regress to Plant Community C (State 3) under non-prescribed grazing and an extended period lacking a natural fire regime. The absence of fire would allow the shrubs to remain competitive against the short grasses. This transition is shown with a dashed arrow in the state and transition model. Regression rates vary with the intensity and frequency of the disturbances. Severe drought may cause retrogression within a couple years.

Restoration pathway R2A
State 2 to 1

Prescribed grazing, fire, favorable precipitation Plant community B is not noted for its resiliency. Plant Community B is a steady state and significant succession is not expected to occur. However, succession to State 1 may be possible with the combination of prescribed grazing and a prolonged period of favorable moisture. This potential succession is indicated by a dashed line in the state and transition diagram.

Transition T2A
State 2 to 3

Prolonged drought (5-7 years), non-prescribed grazing, no fire Community B is much less resistant to disturbance than Community A. Lower production, lower vegetative cover, less litter, and increased bare ground increases Community B’s susceptibility to disturbance. Extended drought and non-prescribed grazing can cause regression to State 3 (Community C).

Restoration pathway R3A
State 3 to 2

Fire, prescribed grazing Community C is resistant to significant succession. It is theorized that another threshold separates Communities B and C. Blue grama and the other short grasses and sedges form a competitive community. The adverse soil conditions characteristic of this site, and a theorized shortage of wheatgrass and alkali sacaton seeds in the seed bank greatly restrict potential for significant succession. Succession is not expected to occur within a reasonable length of time. However, succession may be possible with the combination of fire to reduce shrub competition, prescribed grazing to allow preferred species the opportunity to regain vigor and set seed, and a prolonged period of favorable precipitation. This potential succession is indicated by a dashed line in the state and transition diagram. Mechanical treatments and range seeding are not normally recommended on this site. Ecological processes will be adversely affected by poorly planned range improvement efforts.

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	Rhizomatous Wheatgrasses			200–300
	western wheatgrass	PASM	Pascopyrum smithii	200–300	–
2	Cool-season Grasses			50–100
	Nuttall's alkaligrass	PUNU2	Puccinellia nuttalliana	50–100	–
3	Warm-season Grasses			55–175
	alkali sacaton	SPAI	Sporobolus airoides	50–100	–
	saltgrass	DISP	Distichlis spicata	5–75	–
4	Miscellaneous Grasses			5–50
	prairie Junegrass	KOMA	Koeleria macrantha	5–25	–
	Grass, native	2GN	Grass, native	5–25	–
	blue grama	BOGR2	Bouteloua gracilis	5–25	–
	sand dropseed	SPCR	Sporobolus cryptandrus	5–25	–
	plains reedgrass	CAMO	Calamagrostis montanensis	5–25	–
	threadleaf sedge	CAFI	Carex filifolia	5–25	–
	Sandberg bluegrass	POSE	Poa secunda	5–25	–
Forb
5	Forbs			20–30
	scarlet globemallow	SPCO	Sphaeralcea coccinea	5–25	–
	aster	ASTER	Aster	5–25	–
	povertyweed	IVAX	Iva axillaris	5–25	–
	bastard toadflax	COUM	Comandra umbellata	5–25	–
	milkvetch	ASTRA	Astragalus	5–25	–
	spiny phlox	PHHO	Phlox hoodii	5–25	–
	Forb, native	2FN	Forb, native	5–25	–
Shrub/Vine
6	Dominant Shrubs			75–150
	Nuttall's saltbush	ATNU2	Atriplex nuttallii	75–125	–
	greasewood	SAVE4	Sarcobatus vermiculatus	75–125	–
7	Miscellaneous Shrubs			0–125
	silver sagebrush	ARCA13	Artemisia cana	5–25	–
	prairie sagewort	ARFR4	Artemisia frigida	5–25	–
	Shrub (>.5m)	2SHRUB	Shrub (>.5m)	0–25	–
	broom snakeweed	GUSA2	Gutierrezia sarothrae	0–1	–
	plains pricklypear	OPPO	Opuntia polyacantha	0–1	–

Interpretations

Animal community

Livestock Management
The Saline Upland 10-14” p.z. ecological site is suited for livestock grazing. However, prescribed grazing management is needed. Forage production is limited by soil chemistry. Species composition is susceptible to heavy stocking and season long grazing. The cool season medium height grasses are generally selectively grazed giving the short grasses a competitive advantage. Grazing during early spring may also result in soil compaction. Any additional factor reducing infiltration and increasing runoff on this site is a management concern. Shorter grazing periods developed in conjunction with adequate periods of deferment to facilitate regrowth, replenish carbohydrate pools, and accumulate litter on the soil surface are recommended.
The Saline Upland 10-14” p.z. ecological site has a short grass component, as do most other sites in the northern mixed prairie. The short grasses usually increase with grazing and decrease with protection or prescribed grazing. However, succession is not guaranteed in the Northern Great Plains.
Sampling four-year old ungrazed exclosures and grazed areas with 35% utilization, Vogel and Van Dyne (1966) found essentially the same basal cover of grasses, sedges, forbs, litter and bare soil on protected and grazed sites. They concluded that four years was too short of a time for cover to change significantly. Hofmann and Ries (1989) observed similar results following a four-year study in North Dakota. Even after 41 years of exclosure, changes in species composition can be relatively small when the site is in the dry, low production portion of northern mixed prairie (Brand and Goetz, 1986). They concluded that site characteristics limited the development of potential vegetation with the exclusion of grazing, but the potential impacts of prescribed grazing on succession were not discussed. This ecological site is not as productive as the sites evaluated by Vogel and Van Dyne, Hofmann and Ries, or by Brand and Goetz. Therefore, range managers should recognize the environmental limitations of this site. While a prescribed grazing system is always a good recommendation, it may not guarantee significant succession. Seeding and/or mechanical treatment are not recommended.
This ecological site is suited for prescribed grazing by livestock. Because of the terrain and propensity of shrubs, this site may be more compatible for sheep, rather than cattle grazing. Although poisonous plants are not normally a problem, greasewood can cause some livestock losses. Most of the problems develop when livestock are moved onto this site in late summer or early fall. If the livestock are moved into this site from upland sites where forage is mature and limiting, grazing animals often ingest a high quantity of greasewood leaves. This can be dangerous because plants are high in oxalates and can cause bloat or poisoning. However, greasewood and some of the associated species are nutritious, and growing livestock can make good weight gains.

Wildlife Interpretations
The HCPC associated with this ecological site provides diverse and valuable wildlife habitat. This site often occurs as a mosaic with other ecological sites, thus creating “ecotones” that serve as a magnet to attract many species of wildlife. Antelope and mule deer prefer grazing this site because of the Nuttall saltbush and other shrubs. When this site occurs in the landscape as a mosaic with other sites, thermal and escape cover are provided for many species of wildlife. The lack of species diversity limits the value of the site for some species of wildlife. The bare ground and lack of litter also limits the potential of the site for upland birds and for ground-nesting birds.
This ecological site becomes less valuable for deer and antelope when plant diversity declines with regression. For example, the disappearance of either the alkali sacaton or western wheatgrass, and the reduction of Nuttall saltbush would shorten the length of the “green forage” season. The increase of blue grama, hoods phlox etc. is associated with the loss of palatable forbs. These changes also adversely impact foraging opportunities for deer, antelope, upland birds, etc. Because of insufficient vegetative structural diversity, residual grass carry-over and litter cover, the value of Communities B and C for wildlife habitat are greatly reduced.

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

Water and alkalinity are the main factors limiting vegetative production on this site. Soil components in this ecological site are normally in Hydrologic Group D. These soils have a medium to very high runoff potential, with hydrologic runoff curves of 89 to 80. Field investigations are needed to adjust the runoff curves when plant communities deteriorate from the HCPC. Areas with ground cover less than 50% have the greatest potential for reduced infiltration and higher runoff.

Recreational uses

This site provides hunting opportunities for upland game species. Outdoor enthusiasts may also appreciate the serenity and openness of is site.

Wood products

This site has no significant value for wood products.

Other information

This ecological site is not highly resistant to disturbances. Species diversity is adversely affected by season long continuous grazing and by heavy stocking. Medium height grasses are replaced by short grasses. There is also a shift from predominantly herbaceous plants in State #1 to more woody plants in States #2 and #3. The number of structural/functional groups is reduced with regression from the HCPC. The amount of solar energy that is captured and converted to carbohydrates for plant growth is reduced in States #2 and #3. A reduction in total vegetative growth results in less potential vegetation that can be transformed into litter. Litter reductions result in less infiltration, and more runoff and soil erosion.

Supporting information

Inventory data references

Data Source Number of Records Sample Period State County
SCS-Range-417
ECS-1
Modified Double Sampling
Ross, R. L. and H. E. Hunter. 1976. Climax vegetation of Montana. USDA Soil Conservation Service. Bozeman, MT.
USDA-SCS-MT 1981 Technical Range Site Description

Other references

Brand, M.D. and H. Goetz. 1986. Vegetation of exclosures in Southwestern North Dakota. J. Range Manage. 39:434-437.
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, C. 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 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.
Hofmann, L. and R.E. Ries. 1989. Animal performance and plant production from continuously grazed cool-season reclaimed and native pastures. J. Range Manage. 42:248-251.
U.S. Department of Interior and U.S. Department of Agriculture. 2000. Interpreting indicators of rangeland health. Tech. Ref. 1734-6.
Vogel, W.G. and G.M. Van Dyne. 1966. Vegetation responses to grazing management on a foothill sheep range. J. Range Manage. 19:80-85.

Contributors

Kirt Walstad

Approval

Kirt Walstad, 1/24/2024

Acknowledgments

Site Description Revisions
The 2005 Saline Upland 10-14” p.z. ecological site description replaces earlier dated versions of the Saline Upland 10-14” p.z. description in Rangeland Resource Unit 52XC.
This 2005 revision incorporates the State and Transition Model theory, additional data on site productivity, and an improved understanding of many rangeland health indicators.
Site Description Approval
This ecological site description is approved with the understanding that it is no more than another step in our continual effort to update the NRCS technical guide. In order to facilitate the process, NRCS field personnel are encouraged to forward existing information and/or new data that can be used to improve the utility of this site description. Please forward the information and data to the State Rangeland Management Specialist.
Authors Date Approval Date
Dr. John Lacey 02/28/2005 Loretta J. Metz 03/19/2005
Maxine Rasmussen, Area RMS, Glasgow, MT
Jon Siddoway, Area RMS, Great Falls, MT
Rick Bandy, Area RSS, Great Falls, MT
Greg Snell, Area RSS, Glasgow, MT

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)	Loretta Metz, Maxine Rasmussen, Jon Siddoway
Contact for lead author	Area Rangeland Management Specialist, Glasgow Area Office, MT Reference site used? No
Date	05/04/2005
Approved by	Kirt Walstad
Approval date
Composition (Indicators 10 and 12) based on	Annual Production