Natural Resources
Conservation Service
Ecological site R064XY022NE
Wet Land
Last updated: 7/19/2024
Accessed: 11/13/2024
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.
MLRA notes
Major Land Resource Area (MLRA): 064X–Mixed Sandy and Silty Tableland and Badlands
The Mixed Sandy and Silty Tableland and Badlands (MLRA 64) is shared almost equally between South Dakota (42 percent) and Nebraska (41 percent). A small portion is in Wyoming (17 percent). The MLRA consists of 11,895 square miles. The towns of Kadoka and Pine Ridge, South Dakota; Chadron and Alliance, Nebraska; and Lusk, Wyoming, are all within the boundaries of this MLRA.
The following areas of special interest are in this MLRA: Agate Fossil Beds National Monument, Chadron State Park, Fort Robinson State Park, and the Pine Ridge Indian Reservation; parts of the Oglala and Buffalo Gap National Grasslands, which are in the Nebraska National Forest; and nearly all of Badlands National Park. The Badlands are internationally renowned for their Oligocene vertebrate fossils.
The northern section of the MLRA consists of old plateaus and terraces that have been deeply eroded by wind, water, and time. The southern section consists of nearly level to broad intervalley remnants of smooth fluvial plains. These two sections are separated by the Pine Ridge escarpment. Elevations gradually increase from 2,950 to 5,073 feet from east to west. The main drainageway through Badlands National Park is the White River. The headwaters of both the White and Niobrara Rivers are in MLRA 64. The Pine Ridge escarpment is at the northernmost extent of the Ogallala Aquifer.
Tertiary continental sediments consisting of sandstone, siltstone, and claystone underlie most of the area. Many of the bedrock units in the southern third of the MLRA are covered by loess. Soils range from shallow to very deep and from generally well drained to excessively drained. They are loamy or sandy. The Badlands consist of stream-laid layers of silt, clay, and sand mixed with layers of volcanic ash.
Average annual precipitation for the area ranges from 14 to 20 inches. Most of the rainfall occurs as frontal storms in the spring and early summer. This area supports a mixture of short-, mid-, and tall-statured warm- and cool-season grasses. On the Pine Ridge escarpment, these plants grow in association with ponderosa pine, Rocky Mountain juniper, western snowberry, skunkbush sumac, common chokecherry, and rose. Wyoming big sagebrush grows in minor amounts in the drier, far western portion of the MLRA; however, small remnant stands can be found in the eastern portion of the Oglala National Grassland in Nebraska.
Sixty percent of the MLRA is grassland, 11 percent of which is under Federal management. Twenty-two percent of the area is used as cropland, and 4 percent is forested. Major resource concerns include wind erosion, water erosion, and surface water quality (USDA-NRCS, 2006, Ag Handbook 296).
For development of ecological sites, MLRA 64 is divided into two precipitation zones (PZ): 14 to 17 inches per year and 17 to 20 inches per year. The wetter zone extends from the western end of the Pine Ridge escarpment near Lusk, Wyoming, eastward along the escarpment through Nebraska and into the Big Badlands area of South Dakota. The drier zone extends from Wyoming eastward to Alliance and Oshkosh, Nebraska, south of the Pine Ridge escarpment. MLRA 64 stops at the western edge of the Nebraska Sand Hills (MLRA 65).
A unique geologic area known as the Hartville Uplift is in the far southwest corner of the 14 to 17 inch precipitation zone. The Hartville Uplift is an elongated, north-northwest-oriented, broad domal arch of Laramide age (70-50 million years ago). It extends approximately 45 miles between Guernsey and Lusk, Wyoming, and is 15 miles wide at its widest point. Erosion has exposed a core of granite and Precambrian metasedimentary and metavolcanic rocks (Steele et al., 2018). In addition to the ecological sites in the 14 to 17 inch precipitation zone of MLRA 64, three unique ecological site descriptions were developed to describe the soils and plant community dynamics in the Hartville Uplift.
Classification relationships
USDA Land Resource Region G—Western Great Plains Range and Irrigated Region:
Major Land Resource Area (MLRA) 64—Mixed Sandy and Silty Tableland and Badlands
U.S. Environmental Protection Agency (EPA)
Level IV Ecoregions of the Conterminous United States:
High Plains—25:
Pine Ridge Escarpment—25a.
Flat to Rolling Plains—25d.
Pine Bluffs and Hills—25f.
Sandy and Silty Tablelands—25g.
Northwestern Great Plains—43:
White River Badlands—43h.
Keya Paha Tablelands—43i.
USDA Forest Service
Ecological Subregions: Sections and Subsections of Conterminous United States:
Great Plains and Palouse Dry Steppe Province—331:
Western Great Plains Section—331F:
Subsections:
Shale Scablands—331Fb.
White River Badlands—331Fh.
Pine Ridge Escarpment—331Fj.
High Plains—331Fk.
Hartville Uplift—331Fm.
Western Nebraska Sandy and Silty Tablelands—331Fn.
Keye Paha Tablelands—331Ft.
Powder River Basin Section—331G:
Subsection: Powder River Basin—331Ge.
Ecological site concept
The Wet Land ecological site is found throughout MLRA 64. It is a run-in site on drainageways, oxbows, and flood plains. Slopes range from 0 to 3 percent. The soils are very deep, very poorly drained, and formed in eolian sands and sandy alluvium. The surface layer is loamy fine sand to fine sandy loam and is 5 to 14 inches in depth. A permanent water table fluctuates between the surface and a depth of 1 foot.
Vegetation in Reference State (1.0) consists of grass, sedge, and rush species that are classified as wetland obligate or facultative wetland.
Associated sites
| R064XY024NE |
Subirrigated The Subirrigated ecological site is adjacent to the Wet Land ecological site but has a seasonal high water table within 1 to 3 feet of the surface. |
|---|---|
| R064XY029NE |
Sandy Lowland The Sandy Lowland ecological site is on low terraces above the Wet Land ecological site. |
Similar sites
| R064XY002NE |
Wet Subirrigated The Wet Subirrigated ecological site is found in landscape positions similar to those of the Wet Land site. The Wet Subirrigated plant community has less prairie cordgrass, and fewer obligate grass-like species and forbs than the Wet Land ecological site. |
|---|
Table 1. Dominant plant species
| Tree |
Not specified |
|---|---|
| Shrub |
Not specified |
| Herbaceous |
(1) Spartina pectinata |
Physiographic features
The Wet Land ecological site is found in level or nearly level valleys near springs, seeps, and sloughs. A water table generally occurs at or within 12 inches of the surface.
Table 2. Representative physiographic features
| Landforms |
(1)
Drainageway
(2) Oxbow (3) Flood plain |
|---|---|
| Runoff class | Negligible to low |
| Flooding duration | Brief (2 to 7 days) |
| Flooding frequency | Occasional to frequent |
| Ponding duration | Brief (2 to 7 days) to long (7 to 30 days) |
| Ponding frequency | Occasional to frequent |
| Elevation | 2,900 – 5,000 ft |
| Slope | 3% |
| Ponding depth | 12 in |
| Water table depth | 12 in |
| Aspect | Aspect is not a significant factor |
Climatic features
MLRA 64 has a continental climate consisting of cold winters and hot summers, low humidity, light rainfall, and ample sunshine. Extremes in temperature are common in some years. The climate results from MLRA 64 being near the geographic center of North America. There are few natural barriers on the Northern Great Plains. Air masses move freely across the plains and account for rapid changes in temperature.
Average annual precipitation ranges from 14 to 20 inches per year. The normal average annual temperature is about 47 °F. January is the coldest month with average temperatures ranging from about 21 °F (Wood, SD) to about 25 °F (Hemingford, NE). July is the warmest month with average temperatures ranging from about 70 °F (Keeline 3 W, WY: 1953–1986) to about 76 °F (Wood, SD). The range of normal average monthly temperatures between the coldest and warmest months is about 55 °F. This large annual range attests to the continental nature of the climate of this area. Wind speeds average about 11 miles per hour annually, ranging from about 13 miles per hour during the spring to about 10 miles per hour during the summer. Daytime winds are generally stronger than nighttime winds. Occasionally, strong storms bring brief periods of high winds with gusts to more than 50 miles per hour.
Growth of cool-season plants begins in early to mid-March, slowing or ceasing in late June. Warm-season plants begin growth about mid-May and continue to early or mid-September. Cool-season plants may green-up in September and October if adequate soil moisture is present.
Table 3. Representative climatic features
| Frost-free period (characteristic range) | 92-120 days |
|---|---|
| Freeze-free period (characteristic range) | 119-139 days |
| Precipitation total (characteristic range) | 16-19 in |
| Frost-free period (actual range) | 87-122 days |
| Freeze-free period (actual range) | 110-149 days |
| Precipitation total (actual range) | 15-20 in |
| Frost-free period (average) | 107 days |
| Freeze-free period (average) | 130 days |
| Precipitation total (average) | 17 in |
Figure 2. Monthly precipitation range
Figure 3. Monthly minimum temperature range
Figure 4. Monthly maximum temperature range
Figure 5. Monthly average minimum and maximum temperature
Figure 6. Annual precipitation pattern
Figure 7. Annual average temperature pattern
Climate stations used
-
(1) HARRISON 20 SSE [USW00094077], Harrison, NE
-
(2) ALLIANCE 1WNW [USC00250130], Alliance, NE
-
(3) HARRISON [USC00253615], Harrison, NE
-
(4) HEMINGFORD [USC00253755], Hemingford, NE
-
(5) INTERIOR 3 NE [USC00394184], Interior, SD
-
(6) MARTIN [USC00395281], Martin, SD
-
(7) WOOD [USC00399442], Wood, SD
-
(8) LUSK 2 SW [USC00485830], Lusk, WY
-
(9) TORRINGTON 29N [USC00488997], Jay Em, WY
-
(10) GLENDO 6NE [USC00483936], Glendo, WY
-
(11) CHADRON 3NE [USC00251578], Chadron, NE
Influencing water features
The Wet Land ecological site has a combination of physical and hydrological features that: (1) provides season-long ground water within 1 foot of the surface, (2) allows relatively free movement of water and air in the upper part of the soil, and (3) results in occasional or frequent flooding.
Wetland description
Wetland Description: (Cowardin et al., 1979)
System: Lacustrine
Subsystem: Littoral
Class: Unconsolidated Shoreline
Subclass: Permanently, semi-permanently, or seasonally flooded
Wetland Description: (Cowardin et al., 1979)
System: Palustrine
Subsystem: N/A
Class: Persistent Emergent Wetland
Subclass: Permanently, semi-permanently, or seasonally flooded; or saturated
Soil features
Soils are commonly loamy fine sand to fine sandy loam and have slopes of 0 to 3 percent. A number of soils have a surface layer of mucky peat or slightly decomposed plant material. The soils are very poorly drained and formed in eolian sands and sandy alluvium. The surface layer is 5 to 14 inches thick. The subsurface layers range from sand to very fine sandy loam.
Soils Correlated to the Wet Land Site: Bigwinder, Herdcamp, Interior, and Lisco
Also correlated to this site are unnamed Endoaquolls in Niobrara County, Wyoming, and an unnamed Fluvent in Jackson County, South Dakota.
Because of variations in flooding frequencies, the Interior soil can also be correlated to the Badlands Terrace ecological site (R064XY048NE) and the Badlands Overflow ecological site (R064XY049NE).
The Lisco soil can also be correlated to the Saline Subirrigated (R064XY025NE) ecological site.
Rills and gullies are not typically present. Water flow patterns are barely distinguishable if present. Litter typically falls in place, and signs of movement are not common. Chemical and physical crusts are rare to nonexistent.
More information regarding the soil is available in soil survey reports. Contact the local USDA Service Center for details specific to your area of interest, or go online to access USDA’s Web Soil Survey.
Table 4. Representative soil features
| Parent material |
(1)
Eolian sands
–
sandstone and siltstone
(2) Alluvium – sandstone and siltstone |
|---|---|
| Surface texture |
(1) Fine sandy loam (2) Very fine sandy loam (3) Loamy fine sand |
| Family particle size |
(1) Sandy |
| Drainage class | Very poorly drained |
| Permeability class | Moderate to rapid |
| Soil depth | 80 in |
| Surface fragment cover <=3" | Not specified |
| Surface fragment cover >3" | Not specified |
| Available water capacity (0-40in) |
4 – 6 in |
| Calcium carbonate equivalent (0-40in) |
40% |
| Electrical conductivity (0-40in) |
16 mmhos/cm |
| Sodium adsorption ratio (0-40in) |
50 |
| Soil reaction (1:1 water) (0-40in) |
5.6 – 9.6 |
| Subsurface fragment volume <=3" (Depth not specified) |
5% |
| Subsurface fragment volume >3" (Depth not specified) |
Not specified |
Ecological dynamics
The Wet Land ecological site developed under Northern Great Plains climatic conditions; light to severe grazing by bison and other large herbivores; sporadic, natural or human-caused wildfire (often of light intensities); and other biotic and abiotic factors that typically influence soil and site development. Changes occur in the plant communities due to short-term weather variations, effects of native and exotic plant and animal species, and management actions. Although the following plant community descriptions are typical of the transitions between communities, severe disturbances, such as periods of well below average precipitation and the introduction of non-native cool-season grasses, can cause significant shifts in plant communities and species composition.
Continuous season-long grazing (during the typical growing season of May through October), or repeated seasonal grazing (e.g., every spring, every summer), without adequate recovery periods following each grazing occurrence causes this site to depart from the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1). Species such as spike sedge and Baltic rush increase in abundance. Grasses and grass-like species such as Nebraska sedge, bluejoint reedgrass, and northern reedgrass decrease in frequency and production.
Interpretations are primarily based on the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1). The community was determined by study of rangeland relic areas, areas protected from excessive disturbance, and areas under long-term rotational grazing regimes. Also studied were trends in plant community dynamics ranging from heavily grazed to lightly grazed areas, seasonal use pastures, and historical accounts. Plant communities, states, transitional pathways, and thresholds were determined through similar studies and experience.
The following state-and-transition diagram illustrates the common plant communities on the site and the transition pathways between communities. The ecological processes are discussed in more detail in the plant community descriptions following the diagram.
State and transition model
More interactive model formats are also available.
View Interactive Models
Click on state and transition labels to scroll to the respective text
Ecosystem states
State 2 submodel, plant communities
State 1
Reference State
The Reference State (1.0) represents the best estimate of the natural range of variability that dominated the dynamics of the Wet Land ecological site prior to European settlement. This site, in the Reference State (1.0), is dominated by grasses, grass-like species, and forbs. Variations in annual precipitation and in length of time the site is ponded greatly influence the species composition from year to year. During wet years, the plant community responds to higher surface water levels. Grass-like species and forbs increase in abundance. During drier years, the plant community is dominated by grasses and obligate sedges and rushes. Grazing pressure on this site and surrounding sites also influence the plant community dynamics. Hoof action during wet periods can cause soil compaction and reduce rooting depth and soil saturation levels. Heavy animal concentrations or cropping on the surrounding landscapes can increase runoff and sedimentation. In pre-European settlement times, the primary disturbances included grazing by large ungulates, occasional fire, and drought. Favorable growing conditions occurred during the spring and the warm months of June through August. Today, a similar state can be found in areas where proper livestock management occurs.
Community 1.1
Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass
Interpretations are based primarily on the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1). This is also considered to be the reference plant community. Potential vegetation is about 60 percent grasses, 25 percent sedges and rushes,10 percent forbs, and 5 percent trees. The major grasses and grass-like species include prairie cordgrass, Nebraska sedge, bluejoint reedgrass, and northern reedgrass. Grasses and grass-like species of lesser importance are Baltic rush and low-growing, unpalatable sedges. The plant community is well adapted to the Northern Great Plains climatic conditions. It is a critical plant community providing water and habitat for the surrounding area. The diversity in plant species provides a variety of habitats for wildlife. It is resistant to drought due to a dependable water supply. This is a sustainable plant community in terms of soil stability, watershed function, and biologic integrity.
Figure 8. 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 | 4280 | 4537 | 4700 |
| Forb | 220 | 688 | 1200 |
| Shrub/Vine | 0 | 275 | 600 |
| Total | 4500 | 5500 | 6500 |
Figure 9. Plant community growth curve (percent production by month). NE6408, Pine Ridge/Badlands, lowland cool-season/warm-season co-dominant. Cool-season, warm-season co-dominant, lowland.
| Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
|---|---|---|---|---|---|---|---|---|---|---|---|
| J | F | M | A | M | J | J | A | S | O | N | D |
| 5 | 12 | 20 | 25 | 19 | 11 | 5 | 3 |
Community 1.2
Sedge/Smartweed/Spikerush-Baltic Rush-Bulrush
This plant community develops during a wetter cycle of precipitation and hydrology in conjunction with either continuous grazing without adequate recovery periods between grazing events or excessive haying. This plant community is approximately 30 percent grasses, 40 percent grass-like species, 25 percent forbs, and 5 percent shrubs. The plant community becomes dominated by grass-like species such as Nebraska sedge, various obligate and facultative wet sedges, spikerush, and Baltic rush. Forbs include Pennsylvania smartweed, swamp smartweed, and cattail. When compared to the Prairie Cordgrass-Bluejoint Reedgrass/Nebraska Sedge Plant Community (1.1), the abundance of prairie cordgrass, northern reedgrass, bluejoint reedgrass, and Nebraska sedge is decreased in Plant Community 1.2. Low growing unpalatable sedges, Baltic rush, and cattails have increased in abundance. The abundant production and proximity to water make Plant Community 1.2 important for livestock and wildlife such as birds, mule deer, and antelope. The plant community is stable and protected from excessive erosion. The biotic integrity of this plant community is intact. The watershed is usually functioning. Although plant diversity has been reduced, the soil is still stable. The water cycle, nutrient cycle, and energy flow are slightly reduced but continue to function adequately.
Figure 10. Annual production by plant type (representative values) or group (midpoint values)
Table 6. Annual production by plant type
| Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
|---|---|---|---|
| Grass/Grasslike | 980 | 1170 | 1455 |
| Forb | 220 | 585 | 950 |
| Shrub/Vine | 0 | 45 | 95 |
| Total | 1200 | 1800 | 2500 |
Figure 11. Plant community growth curve (percent production by month). NE6408, Pine Ridge/Badlands, lowland cool-season/warm-season co-dominant. Cool-season, warm-season co-dominant, lowland.
| Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
|---|---|---|---|---|---|---|---|---|---|---|---|
| J | F | M | A | M | J | J | A | S | O | N | D |
| 5 | 12 | 20 | 25 | 19 | 11 | 5 | 3 |
Community 1.3
Prairie Cordgrass/Excessive Litter
This plant community develops after an extended period of non-use and in areas where fire has been eliminated. Excessive litter shades-out plants. This shading inhibits photosynthesis, reduces soil temperatures, and delays green-up in the spring. Plants become decadent and exhibit low vigor. Bunch grasses commonly develop dead centers. Organic matter oxidizes into the air rather than being incorporated into the soil. The dominant plants tend to be somewhat similar to those found in the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1); however, in advanced stages, frequency and production can be lower. Compared to the reference community, litter amounts have increased, causing plants to become decadent. Much of the plant nutrients are tied up in excessive litter. Organic matter oxidizes into the air rather than being incorporated into the soil due to the absence of animal impact. Typically, bunchgrasses develop dead centers and rhizomatous grasses form small colonies because of a lack of tiller stimulation. Weedy species, cool-season grasses, and sedges can potentially increase in abundance. Prairie cordgrass is decreased in abundance. American licorice tends to invade. Noxious weeds such as Canada thistle may invade if a seed source is present. Plant diversity is moderate to high. This plant community is not resistant to change. Prescribed grazing or prescribed fire can easily move Plant Community 1.3 toward the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1). Soil erosion is not a concern due to increased litter levels and landscape position. The plant community is at-risk due to invasive plants.
Figure 12. Annual production by plant type (representative values) or group (midpoint values)
Table 7. Annual production by plant type
| Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
|---|---|---|---|
| Grass/Grasslike | 3550 | 3625 | 3700 |
| Forb | 450 | 1125 | 1750 |
| Shrub/Vine | 0 | 250 | 550 |
| Total | 4000 | 5000 | 6000 |
Figure 13. Plant community growth curve (percent production by month). NE6408, Pine Ridge/Badlands, lowland cool-season/warm-season co-dominant. Cool-season, warm-season co-dominant, lowland.
| Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
|---|---|---|---|---|---|---|---|---|---|---|---|
| J | F | M | A | M | J | J | A | S | O | N | D |
| 5 | 12 | 20 | 25 | 19 | 11 | 5 | 3 |
Pathway 1.1B
Community 1.1 to 1.2
Plant Community 1.1 is shifted to the Sedge/Smartweed/Spikerush-Baltic Rush-Bulrush Plant Community (1.2) by a wetter hydrologic cycle that has a higher stable water level; continuous grazing without adequate recovery periods; or excessive haying.
Pathway 1.1A
Community 1.1 to 1.3
Long-term non-use and no fire convert this plant community (1.1) to the Prairie Cordgrass/Excessive Litter Plant Community (1.3). Initially, excess litter begins to build-up. Eventually, native plants can show signs of mortality and decadence.
Pathway 1.2A
Community 1.2 to 1.1
Prescribed grazing that provides change in season of use and allows adequate recovery time, in conjunction with a return to a normal or slightly drier cycle of precipitation and hydrology, shift Plant Community 1.2 to the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1).
Conservation practices
| Prescribed Grazing |
|---|
Pathway 1.3A
Community 1.3 to 1.1
Prescribed grazing that includes proper stocking rates, change in season of use, and adequate time for plant recovery; or, possibly, prescribed burning in combination with prescribed grazing shift Plant Community 1.3 to the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1).
Conservation practices
| Prescribed Burning | |
|---|---|
| Prescribed Grazing |
Pathway 1.3B
Community 1.3 to 1.2
Change to a wetter hydrologic cycle that has a higher stable water level; or prescribed burning followed by prescribed grazing convert Plant Community 1.3 to the Sedge/Smartweed/Spikerush-Baltic Rush-Bulrush Plant Community (1.2).
Conservation practices
| Prescribed Burning | |
|---|---|
| Prescribed Grazing |
State 2
Native/Invaded State
The Native/Invaded State (2.0) is dominated by native and non-native cool-season grasses and grass-like species. The non-native cool-season grasses, primarily Kentucky bluegrass, make up 10 to 15 percent of the total annual production. This state is the result of heavy grazing; excessive haying; or heavy disturbance that can create soil compaction and sedimentation. Cattails and possibly reed canarygrass increase in abundance and replace the reference plant community. The Native/Invaded State (2.0) is very resilient and resistant to change.
Community 2.1
Cattail/Reed Canarygrass
This plant community develops due to further heavy grazing; excessive haying; or heavy disturbance and sedimentation. Cattails and possibly reed canarygrass invade the site and displace the more palatable grasses and grass-like species. The drier areas of the plant community are likely to be dominated by Kentucky bluegrass. Compared to the Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass Plant Community (1.1), the abundance of prairie cordgrass, bluejoint reedgrass, and Nebraska sedge has decreased. Low growing unpalatable sedges, Baltic rush, and cattails have increased in abundance. The plant community is stable and protected from excessive erosion. The biotic integrity of this plant community is usually intact. The watershed is usually functioning.
Figure 14. Annual production by plant type (representative values) or group (midpoint values)
Table 8. Annual production by plant type
| Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
|---|---|---|---|
| Grass/Grasslike | 1780 | 2175 | 2575 |
| Forb | 220 | 675 | 1100 |
| Shrub/Vine | 0 | 150 | 325 |
| Total | 2000 | 3000 | 4000 |
Figure 15. Plant community growth curve (percent production by month). NE6408, Pine Ridge/Badlands, lowland cool-season/warm-season co-dominant. Cool-season, warm-season co-dominant, lowland.
| Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
|---|---|---|---|---|---|---|---|---|---|---|---|
| J | F | M | A | M | J | J | A | S | O | N | D |
| 5 | 12 | 20 | 25 | 19 | 11 | 5 | 3 |
Transition T1A
State 1 to 2
Heavy grazing, excessive haying with no recovery opportunity, or heavy disturbance that results in sedimentation transition State 1.0 to the Native/Invaded State (2.0).
Restoration pathway R2A
State 2 to 1
Removal of management-induced disturbance coupled with long-term prescribed grazing; or prescribed burning in combination with prescribed grazing may eventually move the Native/Invaded State (2.0) toward the Reference State (1.0). This transition pathway assumes the availability of an adequate seed and vegetative source. This process may require a long time to accomplish and may be difficult to attain depending on the degree of degradation. Wetland restoration may be an alternative but may be cost prohibitive and may not meet management objectives.
Conservation practices
| Prescribed Burning | |
|---|---|
| Prescribed Grazing |
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 | Tall Warm-Season Grasses | 2200–3025 | ||||
| prairie cordgrass | SPPE | Spartina pectinata | 2200–3025 | – | ||
| 2 | Cool-Season Grasses | 550–1650 | ||||
| bluejoint | CACA4 | Calamagrostis canadensis | 550–1375 | – | ||
| northern reedgrass | CASTI3 | Calamagrostis stricta ssp. inexpansa | 275–825 | – | ||
| 3 | Other Native Grasses | 275–550 | ||||
| foxtail barley | HOJU | Hordeum jubatum | 110–275 | – | ||
| reed canarygrass | PHAR3 | Phalaris arundinacea | 0–275 | – | ||
| slender wheatgrass | ELTR7 | Elymus trachycaulus | 110–275 | – | ||
| Grass, perennial | 2GP | Grass, perennial | 0–275 | – | ||
| American sloughgrass | BESY | Beckmannia syzigachne | 0–55 | – | ||
| 4 | Grass-Likes | 1100–1925 | ||||
| Nebraska sedge | CANE2 | Carex nebrascensis | 550–1375 | – | ||
| bulrush | SCHOE6 | Schoenoplectus | 275–550 | – | ||
| sedge | CAREX | Carex | 275–550 | – | ||
| rush | JUNCU | Juncus | 0–275 | – | ||
| spikerush | ELEOC | Eleocharis | 55–275 | – | ||
| scouringrush horsetail | EQHY | Equisetum hyemale | 0–275 | – | ||
| 5 | Non-Native Cool-Season Grasses | 0 | ||||
|
Forb
|
||||||
| 6 | Forbs | 275–1100 | ||||
| Forb, perennial | 2FP | Forb, perennial | 0–275 | – | ||
| aster | ASTER | Aster | 0–110 | – | ||
| American licorice | GLLE3 | Glycyrrhiza lepidota | 0–110 | – | ||
| broadleaf cattail | TYLA | Typha latifolia | 0–110 | – | ||
| iris | IRIS | Iris | 0–110 | – | ||
| milkvetch | ASTRA | Astragalus | 0–110 | – | ||
| Pennsylvania smartweed | POPE2 | Polygonum pensylvanicum | 0–110 | – | ||
| poison hemlock | COMA2 | Conium maculatum | 0–110 | – | ||
| swamp smartweed | POHY2 | Polygonum hydropiperoides | 0–110 | – | ||
| water hemlock | CICUT | Cicuta | 0–110 | – | ||
| onion | ALLIU | Allium | 0–110 | – | ||
| curly dock | RUCR | Rumex crispus | 0–110 | – | ||
| plantain | PLANT | Plantago | 0–110 | – | ||
| duckweed | LEMNA | Lemna | 0–110 | – | ||
|
Shrub/Vine
|
||||||
| 7 | Shrubs | 0–550 | ||||
| willow | SALIX | Salix | 0–550 | – | ||
Table 10. Community 1.2 plant community composition
| Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/Grasslike
|
||||||
| 1 | Tall Warm-Season Grasses | 0–90 | ||||
| prairie cordgrass | SPPE | Spartina pectinata | 0–90 | – | ||
| 2 | Cool-Season Grasses | 0–90 | ||||
| bluejoint | CACA4 | Calamagrostis canadensis | 0–90 | – | ||
| northern reedgrass | CASTI3 | Calamagrostis stricta ssp. inexpansa | 0–90 | – | ||
| 3 | Other Native Grasses | 90–180 | ||||
| reed canarygrass | PHAR3 | Phalaris arundinacea | 90–180 | – | ||
| Grass, perennial | 2GP | Grass, perennial | 0–90 | – | ||
| foxtail barley | HOJU | Hordeum jubatum | 18–90 | – | ||
| American sloughgrass | BESY | Beckmannia syzigachne | 0–36 | – | ||
| slender wheatgrass | ELTR7 | Elymus trachycaulus | 0–18 | – | ||
| 4 | Grass-Likes | 360–810 | ||||
| bulrush | SCHOE6 | Schoenoplectus | 90–360 | – | ||
| spikerush | ELEOC | Eleocharis | 180–360 | – | ||
| Nebraska sedge | CANE2 | Carex nebrascensis | 90–270 | – | ||
| sedge | CAREX | Carex | 18–180 | – | ||
| rush | JUNCU | Juncus | 18–90 | – | ||
| scouringrush horsetail | EQHY | Equisetum hyemale | 0–90 | – | ||
| 5 | Non-Native Cool-Season Grasses | 0–90 | ||||
| Kentucky bluegrass | POPR | Poa pratensis | 0–90 | – | ||
|
Forb
|
||||||
| 6 | Forbs | 270–900 | ||||
| Pennsylvania smartweed | POPE2 | Polygonum pensylvanicum | 270–540 | – | ||
| broadleaf cattail | TYLA | Typha latifolia | 90–270 | – | ||
| swamp smartweed | POHY2 | Polygonum hydropiperoides | 90–180 | – | ||
| curly dock | RUCR | Rumex crispus | 36–180 | – | ||
| duckweed | LEMNA | Lemna | 0–90 | – | ||
| Forb, perennial | 2FP | Forb, perennial | 0–90 | – | ||
| American licorice | GLLE3 | Glycyrrhiza lepidota | 0–90 | – | ||
| iris | IRIS | Iris | 0–36 | – | ||
| water hemlock | CICUT | Cicuta | 0–36 | – | ||
| poison hemlock | COMA2 | Conium maculatum | 0–36 | – | ||
| plantain | PLANT | Plantago | 0–36 | – | ||
| aster | ASTER | Aster | 0–36 | – | ||
| onion | ALLIU | Allium | 0–18 | – | ||
| milkvetch | ASTRA | Astragalus | 0–18 | – | ||
|
Shrub/Vine
|
||||||
| 7 | Shrubs | 0–90 | ||||
| willow | SALIX | Salix | 0–90 | – | ||
Table 11. Community 1.3 plant community composition
| Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/Grasslike
|
||||||
| 1 | Tall Warm-Season Grasses | 1000–1500 | ||||
| prairie cordgrass | SPPE | Spartina pectinata | 1000–1500 | – | ||
| 2 | Cool-Season Grasses | 500–1000 | ||||
| bluejoint | CACA4 | Calamagrostis canadensis | 250–750 | – | ||
| northern reedgrass | CASTI3 | Calamagrostis stricta ssp. inexpansa | 250–500 | – | ||
| 3 | Other Native Grasses | 250–1000 | ||||
| foxtail barley | HOJU | Hordeum jubatum | 250–500 | – | ||
| reed canarygrass | PHAR3 | Phalaris arundinacea | 250–500 | – | ||
| Grass, perennial | 2GP | Grass, perennial | 0–250 | – | ||
| American sloughgrass | BESY | Beckmannia syzigachne | 0–100 | – | ||
| slender wheatgrass | ELTR7 | Elymus trachycaulus | 0–100 | – | ||
| 4 | Grass-Likes | 500–1250 | ||||
| sedge | CAREX | Carex | 250–750 | – | ||
| rush | JUNCU | Juncus | 250–500 | – | ||
| Nebraska sedge | CANE2 | Carex nebrascensis | 250–500 | – | ||
| bulrush | SCHOE6 | Schoenoplectus | 250–500 | – | ||
| spikerush | ELEOC | Eleocharis | 50–250 | – | ||
| scouringrush horsetail | EQHY | Equisetum hyemale | 0–250 | – | ||
| 5 | Non-Native Cool-Season Grasses | 100–500 | ||||
| Kentucky bluegrass | POPR | Poa pratensis | 100–500 | – | ||
|
Forb
|
||||||
| 6 | Forbs | 500–1750 | ||||
| American licorice | GLLE3 | Glycyrrhiza lepidota | 250–750 | – | ||
| broadleaf cattail | TYLA | Typha latifolia | 250–750 | – | ||
| Pennsylvania smartweed | POPE2 | Polygonum pensylvanicum | 0–500 | – | ||
| swamp smartweed | POHY2 | Polygonum hydropiperoides | 0–500 | – | ||
| curly dock | RUCR | Rumex crispus | 100–500 | – | ||
| Forb, perennial | 2FP | Forb, perennial | 0–250 | – | ||
| plantain | PLANT | Plantago | 0–100 | – | ||
| water hemlock | CICUT | Cicuta | 0–100 | – | ||
| poison hemlock | COMA2 | Conium maculatum | 0–100 | – | ||
| iris | IRIS | Iris | 0–100 | – | ||
| aster | ASTER | Aster | 0–100 | – | ||
| milkvetch | ASTRA | Astragalus | 0–50 | – | ||
| onion | ALLIU | Allium | 0–50 | – | ||
| duckweed | LEMNA | Lemna | 0–50 | – | ||
|
Shrub/Vine
|
||||||
| 7 | Shrubs | 0–500 | ||||
| willow | SALIX | Salix | 0–500 | – | ||
Table 12. Community 2.1 plant community composition
| Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/Grasslike
|
||||||
| 1 | Tall Warm-Season Grasses | 300–450 | ||||
| prairie cordgrass | SPPE | Spartina pectinata | 300–450 | – | ||
| 2 | Cool-Season Grasses | 150–600 | ||||
| bluejoint | CACA4 | Calamagrostis canadensis | 150–300 | – | ||
| northern reedgrass | CASTI3 | Calamagrostis stricta ssp. inexpansa | 150–300 | – | ||
| 3 | Other Native Grasses | 450–750 | ||||
| reed canarygrass | PHAR3 | Phalaris arundinacea | 300–600 | – | ||
| foxtail barley | HOJU | Hordeum jubatum | 150–300 | – | ||
| Grass, perennial | 2GP | Grass, perennial | 0–150 | – | ||
| American sloughgrass | BESY | Beckmannia syzigachne | 0–60 | – | ||
| slender wheatgrass | ELTR7 | Elymus trachycaulus | 0–60 | – | ||
| 4 | Grass-Likes | 450–750 | ||||
| Nebraska sedge | CANE2 | Carex nebrascensis | 150–450 | – | ||
| bulrush | SCHOE6 | Schoenoplectus | 150–450 | – | ||
| sedge | CAREX | Carex | 150–450 | – | ||
| rush | JUNCU | Juncus | 150–300 | – | ||
| spikerush | ELEOC | Eleocharis | 30–150 | – | ||
| scouringrush horsetail | EQHY | Equisetum hyemale | 0–150 | – | ||
| 5 | Non-Native Cool-Season Grasses | 150–600 | ||||
| Kentucky bluegrass | POPR | Poa pratensis | 150–600 | – | ||
|
Forb
|
||||||
| 6 | Forbs | 300–1050 | ||||
| broadleaf cattail | TYLA | Typha latifolia | 300–750 | – | ||
| Pennsylvania smartweed | POPE2 | Polygonum pensylvanicum | 60–300 | – | ||
| curly dock | RUCR | Rumex crispus | 30–300 | – | ||
| swamp smartweed | POHY2 | Polygonum hydropiperoides | 0–150 | – | ||
| Forb, perennial | 2FP | Forb, perennial | 0–150 | – | ||
| American licorice | GLLE3 | Glycyrrhiza lepidota | 0–150 | – | ||
| aster | ASTER | Aster | 0–60 | – | ||
| water hemlock | CICUT | Cicuta | 0–60 | – | ||
| plantain | PLANT | Plantago | 0–60 | – | ||
| poison hemlock | COMA2 | Conium maculatum | 0–60 | – | ||
| iris | IRIS | Iris | 0–60 | – | ||
| milkvetch | ASTRA | Astragalus | 0–60 | – | ||
| duckweed | LEMNA | Lemna | 0–30 | – | ||
| onion | ALLIU | Allium | 0–30 | – | ||
|
Shrub/Vine
|
||||||
| 7 | Shrubs | 0–300 | ||||
| willow | SALIX | Salix | 0–300 | – | ||
Interpretations
Animal community
Wildlife Interpretations:
MLRA 64 is in the drier areas of a northern mixed-grass prairie ecosystem in which sagebrush steppes to the west yield to grassland steppes to the east. Prior to European settlement, this MLRA supported diverse grassland and shrubland habitats interspersed with varying densities of depressional, instream wetlands and woody riparian corridors. These habitats provided critical life cycle components for many users. Many species of grassland birds, small mammals, reptiles, and amphibians and herds of roaming bison, elk, and pronghorn were among the inhabitants adapted to this semi-arid region. Roaming herbivores, as well as several species of small mammals and insects, were the primary consumers linking the grassland resources to large predators, such as the wolf, mountain lion, and grizzly bear, and to smaller carnivores, such as the coyote, bobcat, fox, and raptors. The prairie dog was once abundant and remains a keystone species within its range. The black-footed ferret, burrowing owl, ferruginous hawk, mountain plover, and swift fox are associated with prairie dog complexes.
Historically, the northern mixed-grass prairie was a disturbance-driven ecosystem in which fire, herbivory, and climate functioned as the primary disturbance factors, either singly or in combination. Following European settlement, livestock grazing, cropland conversion, elimination of fire, energy development, and other anthropogenic factors influenced species composition and abundance. Introduced and invasive species further affected plant and animal communities. The bison was a historical keystone species but has been extirpated in this area as a free-ranging herbivore. The loss of the bison and the reduction of prairie dog populations and fire as ecological drivers greatly influenced the character of the remaining native plant communities and altered wildlife habitats. Human development reduced habitat quality for area-sensitive species.
Within MLRA 64, the Wet Land ecological site provides wetland obligate or facultative wet plant communities. This site is typically part of an expansive grassland landscape that included combinations of Thin Breaks, Clayey, Claypan, Dense Clay, Loamy, Saline, Sandy, Shallow, Overflow, and Terrace ecological sites.
The Wet Land ecological site has remained relatively intact but may be subject to haying under drier conditions. This site receives surface and subsurface water from adjacent upland sites during precipitation events. The site provides ponded water that is important habitat for water fowl and shore birds. Other birds that frequent this site include red-wing blackbirds, sandhill cranes, Wilson snipe, Virginia rail, sora, American bittern, and upland sandpipers. The diverse plant communities are beneficial to small rodents, bats, mammalian predators, reptiles, amphibians, and insects. These sites may provide forage sites for sharp-tailed grouse broods.
Grazing Interpretations:
The following list suggests annual, initial stocking rates for average growing conditions. These estimates are conservative and should be used only as guidelines in the initial stages of conservation planning. Commonly, the current plant composition does not entirely match any particular plant community (as described in this ecological site description). Therefore, a resource inventory is necessary to document plant composition and production. More accurate estimates of carrying capacity should eventually be calculated using the following stocking rate information along with animal preference data and actual stocking records, particularly when grazers other than cattle are involved. In consultation with the land manager, a more intensive grazing management program that results in improved harvest efficiencies and increased carrying capacity may be developed.
The following suggested initial stocking rates are based on 912 lb/acre (air-dry weight) per animal-unit-month (AUM) with a 25 percent harvest efficiency of preferred and desirable forage species (refer to USDA-NRCS National Range and Pasture Handbook). An AUM is defined as the equivalent amount of forage required by a 1,000-pound cow, with or without calf, for one month.
Plant Community: Prairie Cordgrass/Nebraska Sedge/Bluejoint Reedgrass (1.1)
Average Production (lb/acre, air-dry): 5,500
Stocking Rate (AUM/acre): 1.51
*Plant Community: Sedge/Smartweed/Spikerush-Baltic Rush-Bulrush (1.2)
Average Production (lb/acre, air-dry): 1,800
Stocking Rate (AUM/acre): Variable
Plant Community: Prairie Cordgrass/Excessive Litter (1.3)
Average Production (lb/acre, air-dry): 5,000
Stocking Rate (AUM/acre): 1.37
*Plant Community: Cattails/Reed Canarygrass (2.1)
Average Production (lb/acre, air-dry): Variable
Stocking Rate (AUM/acre): Variable
* Total annual production and stocking rates are highly variable and require onsite sampling.
Plant Community: All other plant communities identified in this document have variable annual production values and require onsite sampling to determine initial stocking rates.
Total onsite annual production may contain vegetation deemed undesirable or untargeted by the grazing animal. Therefore, AUM values may have been reduced to reflect only preferred or desirable forage species.
Grazing by domestic livestock is one of the major income-producing industries in the area. Rangeland in this area may provide yearlong forage for livestock. During the dormant period, the forage for livestock likely has insufficient protein to meet livestock requirements. Added protein allows ruminants to better utilize the energy stored in grazed plant materials. A forage quality test (either directly or through fecal sampling) should be used to determine the level of supplementation needed.
Hydrological functions
Excessive water is the principal factor limiting forage production on this site. Soils on this site are in Hydrologic Soil Groups C and D due to high water tables. Although the soils are permeable, the high water tables limit infiltration. Surrounding upland areas tend to have very permeable soils that cause surface inflow peaks to these sites to be muted. Generally, outflows occur only as a result of very intense storms or seepage inflows during very wet years. Many areas of the Wet Land ecological site are frequently to continuously flooded. Refer to the USDA-NRCS National Engineering Handbook, Part 630, for hydrologic soil groups, runoff quantities, and hydrologic curves.
Recreational uses
This site provides opportunities for bird watching and for hunting upland game species and water fowl. The wide variety of plants that bloom from spring until fall have aesthetic value that appeals to visitors.
Wood products
No appreciable wood products are present on the site.
Other products
Harvesting the seeds of native plants can provide additional income on this site.
Other information
Revision Notes: “Previously Approved” Provisional
This provisional ecological site description (ESD) has passed quality control (QC) and quality assurance (QA) to ensure the it meets the 2014 NESH standards for a provisional ecological site description.
This ESD is an updated “Previously Approved” ESD that represented a first-generation tier of documentation that, prior to the release of the 2014 National Ecological Site Handbook (NESH), met all requirements as an “Approved” ESD as laid out in the 1997 National Range and Pasture Handbook (NRPH). The document fully described the reference state and community phase in the state-and-transition model. All other alternative states are at least described in narrative form. The “Previously Approved” ESD has been field-tested for a minimum of 5 years and is a proven functional document for conservation planning. The “Previously Approved” ESD may not contain all tabular and narrative entries as required in the current “Approved” level of documentation, but continued refinement toward an “Approved” status is expected.
Site Development and Testing Plan
Future work, as described in an official project plan, is necessary to validate the information in this provisional ecological site description. The plan will include field activities for low-, medium-, and high-intensity sampling, soil correlations, and analysis of the data. Annual field reviews should be done by soil scientists and vegetation specialists. Final field review, peer review, quality control, and quality assurance reviews are required to produce the final document.
Supporting information
Inventory data references
Information presented here has been derived from NRCS clipping data and other inventory data. Field observations from range-trained personnel were also used. Those involved in developing this site include: Stan Boltz, range management specialist (RMS), NRCS; Jill Epley, RMS, NRCS; Rick Peterson, RMS, NRCS; David Steffen, RMS, NRCS; Jeff Vander Wilt; RMS, NRCS; Phil Young, soil scientist, NRCS; and George Gamblin, RMS, NRCS.
Other references
Cleland, D.T., J.A. Freeouf, J.E. Keys, G.J. Nowacki, C.A. Carpenter, and W.H McNab. 2007. Ecological subregions: Sections and subsections of the conterminous United States. USDA Forest Service, General Technical Report WO-76D. https://www.fs.fed.us/research/publications/misc/73326-wo-gtr-76d-cleland2007.pdf (accessed 31 January 2019).
U.S. Environmental Protection Agency. 2018. EPA level III and level IV ecoregions of the conterminous United States. https://www.epa.gov/eco-research/level-iii-and-iv-ecoregions- conterminous-united-states (accessed 26 April 2018).
High Plains Regional Climate Center, University of Nebraska. 2018. http://www.hprcc.unl.edu/ (accessed 6 April 2018).
Steele, Ken, M.P. Fisher, and D.D. Steele. 2018. Fort Laramie and the Hartville Uplift. In: Geology of Wyoming. https://www.geowyo.com/fort-laramie--hartville-uplift.html (accessed 14 November 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2018. Electronic field office technical guide. https://efotg.sc.egov.usda.gov (accessed 12 April 2018).
Soil Survey Staff. 2018. Official soil series descriptions. USDA Natural Resources Conservation Service. https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/home/?cid=nrcs142p2_053587 (accessed 12 April 2018).
Soil Survey Staff. 2018. Web Soil Survey. USDA Natural Resources Conservation Service. https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx (accessed 12 April 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2006. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. Agriculture Handbook 296. https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_050898.pdf (accessed 17 January 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2014. National ecological site handbook, 1st Ed. https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ref/?cid=nrcseprd1291232 (accessed 27 January 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2012. National engineering handbook, part 630. Hydrology chapters from e-Directives. https://directives.sc.egov.usda.gov/viewerFS.aspx?hid=21422 (accessed 17 January 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2018. Climate data. National Water and Climate Center. http://www.wcc.nrcs.usda.gov/ (accessed 12 April 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 1997. National range and pasture handbook, rev. 1, 2003. https://www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb1043055.pdf (accessed 7 November 2018).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2018. National Soil Information System, Information Technology Center. http://nasis.nrcs.usda.gov (accessed 7 November 2017).
U.S. Department of Agriculture, Natural Resources Conservation Service. 2018. PLANTS database. National Plant Data Team, Greensboro, NC. http://plants.usda.gov (accessed 12 April 2018).
Contributors
Rick L. Peterson
Stan C. Boltz
Approval
Suzanne Mayne-Kinney, 7/19/2024
Acknowledgments
This ecological site was reviewed and approved at the Provisional Level by David Kraft, Regional ESS, Salina, KS on 2/15/2019.
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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) | Stan Boltz |
|---|---|
| Contact for lead author | Stan Boltz, stanley.boltz@sd.usda.gov, 605-352-1236 |
| Date | 03/31/2004 |
| Approved by | Suzanne Mayne-Kinney |
| Approval date | |
| Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
None. -
Presence of water flow patterns:
None. -
Number and height of erosional pedestals or terracettes:
None. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is typically less than 5 percent. During periods of above average precipitation and run-on, this site may be ponded for longer than normal durations, and typical vegetation may be temporarily reduced, creating areas of bare ground for relatively short periods of time. -
Number of gullies and erosion associated with gullies:
None. -
Extent of wind scoured, blowouts and/or depositional areas:
None. -
Amount of litter movement (describe size and distance expected to travel):
Litter falls in place. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil aggregate stability ratings should typically be 5 to 6, normally 6. This site typically has an O-horizon (roots and partly decomposed stems and leaves of plants) that is 0-3 inches thick. Surface organic matter adheres to the soil surface. Soil surface fragments will typically retain structure indefinitely when dipped in distilled water. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
A-horizon should be 12 to 24 inches thick with dark gray or gray colors when moist. Structure typically is medium to fine angular blocky in the A-horizon. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Deep rooted species (tall rhizomatous cool- and warm-season grasses and grass-likes) with fine and coarse roots positively influences infiltration. Infiltration is somewhat limited naturally due to poor drainage and relatively low permeability. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
None – when dry, B horizons can be hard and appear to be compacted, but no platy structure will be present. -
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 rhizomatous grasses > grass-likes species >Sub-dominant:
Mid and tall, cool-season rhizomatous grasses = forbs >Other:
Trees > mid and short, cool-season grassesAdditional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Little evidence of decadence or mortality. -
Average percent litter cover (%) and depth ( in):
Litter cover is typically 80 to 90 percent, and depth of litter ranges from 0.5 to 1.5 inches. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Total annual production ranges from 4,500 to 6,500 pounds/acre, with the reference values being 5,500 pounds/acre (air-dry basis). -
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:
State and local noxious weeds; Kentucky bluegrass may be prevalent during dry cycles, but will typically not dominate the site. Most invasive species will occupy the perimeter of this site. -
Perennial plant reproductive capability:
Perennial grasses and grass-likes should have vigorous rhizomes or tillers.
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