Ecological site group R007XG930WA
Loamy Bottom
Last updated: 09/22/2023
Accessed: 11/21/2024
Ecological site group description
Key Characteristics
None specified
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.
Physiography
Hierarchical Classification
Major Land Resource Area (MLRA): 007X – Columbia Basin
LRU – Common Resource Areas (CRA):
7.1 – Sandy Missoula Flood Deposits
7.2 – Silty Missoula Flood Deposits
7.3 – Dry Loess Islands
7.4 – Dry Yakima Folds
7.5 – Yakima Valley – Pleistocene Lake Basins
Site Concept Narrative:
In the upland setting ecological sites are often expansive, and thus, can be delineated and separated on aerial photos. But in the landscape position of bottoms, basins and depressions this is rarely the case as small changes in soil chemistry, the water table and elevation or aspect results in significant changes in plant community composition. In short distances there are often big swings of available water holding capacity, and soils can go from hydric to non-hydric, or from saline-sodic to not. So, in bottoms, riparian areas and depressions, ecological sites and community phases occur as small spots, strips and patches, or as narrow rings around vernal ponds. And generally, in a matter of steps one can walk across several ecological sites. On any given site location, two or more of these ecological sites occur as a patchwork – Loamy Bottom, Alkali Terrace, Sodic Flat, Wetland complex and Riparian complex. These ecological sites may need to be mapped as a complex when doing resource inventory.
Diagnostics:
The first thing that strikes you about the Loamy Bottom ecological site is the vegetation is much taller, and vastly more productive than any upland site. The tall, upright bunchgrasses and shrubs can be taller than six feet. Another striking feature of the Loamy Bottom ecological site is that it provides excellent protection from wind for livestock and wildlife, and provides good habitat (hiding cover, nesting cover, standing winter forage).
Loamy Bottom ecological site is part of the lentic (standing water) ecosystem, but this site is not a wetland, nor or the soils hydric. It occurs on moisture receiving sites such as bottoms, draws, basins and depressions. This site also occurs as a narrow zonal ring around ponds, lakes and vernal pools. The Loamy Bottom ecological site is an important “hinge site” as it connects upland sites with riparian areas, wetlands and saline-sodic sites. The Loamy Bottom ecological site in MLRA 007X is more limited in scope than the similar site in MLRA 008X.
Soils are deep and unrestricted for plant growth. The soils are silt loam or sandy loam texture and are not saline or sodic, and not hydric. In addition, the landscape position of this site could be conducive to soils possibly containing andic soil properties, i.e. volcanic ash. These andic soil properties can be important for productivity in that they retain larger amounts of water compared to other parent materials (higher water-holding capacity (AWC)), have high cation exchange capacity (CEC) and high availability of organically bound plant nutrients.
Across most of the sagebrush steppe region, this site is a basin wildrye-basin or Wyoming big sagebrush site. While tall bunchgrasses and tall, fire-sensitive shrubs dominate the Reference State overstory, mid-sized bunchgrasses and forbs fill the interspaces. The overstory layer is head-high or taller basin wildrye with equally tall basin big or Wyoming big sagebrush. The next layer is bluebunch wheatgrass or Nelson’s needlegrass, and a variety of native wildflowers, while Sandberg bluegrass is the shortest layer.
The natural fire regime maintains a patchy distribution of shrubs. Depending on the time interval since the last fire, the shrub canopy can be as little 0 to 3 percent or as much as 40 percent.
Principle Vegetative Drivers:
The vegetative expression of Loamy Bottom ecological site is driven by two situations. First, this site receives both surface runoff and discharging groundwater from adjacent upland ecological sites. Second, the soils are deep and unrestricted. This makes the Loamy Bottom ecological site far more productive and any upland site.
INFLUENCING WATER FEATURES
A plant’s ability to grow on a site and overall plant production is determined by soil-water-plant relationships:
1. Whether rain and melting snow run off-site or infiltrate into the soil
2. Whether soil condition remain aerobic or become saturated and anaerobic
3. How quickly the soil reaches the wilting point
Loamy Bottom ecological site receives both surface runoff and discharging groundwater from nearby upland sites. The soils are deep, well drained, and unrestricted, and thus, remain saturated for only a short period in late winter to early spring. With adequate cover of live plants and litter, there are no water infiltrating restrictions on the Loamy Bottom ecological site.
Physiographic features:
The landscape is part of the Columbia basalt plateau. Loamy Bottom ecological site occurs on non-wetland bottoms, draws, basins, & depressions. The site also occurs as fringes around ponds and lakes at elevations of 300 to 1,500 feet. In bottoms, riparian areas and depressions, as a complex of ecological sites and often is one of the narrow bands around ponds, lakes, vernal pools, springs and seeps.
Physiographic Division: Intermontane Plateau
Physiographic Province: Columbia Plateau
Physiographic Sections: Walla Walla Plateau Section
Landscapes: basin and valleys
Landform: Terraces, floodplains and depressions
Elevation:
Range: 250 to 3,000 feet
Central tendency: 300 to 1,500 feet
Slope: Total range: 0 to 5 percent
Central tendency: 1 to 3 percent
Aspect: Occurs on all aspects
Geology:
This is almost entirely underlain by Miocene basalt flows. Columbia River basalt is covered in most areas with as much as 200 feet of eolian, lacustrine, and alluvial deposits. This basin generally corresponds to the vast temporary lakes created by floodwaters from glacial Lakes Missoula and Columbia. Most of the fluvial and lacustrine sediments were deposited about 16,000 years ago, when an ice dam on the ancient Columbia River burst and when glacial Lake Missoula periodically emptied, creating catastrophic floods.
Climate
The climate is characterized by moderately cold, wet winters, and hot, dry summers, with limited precipitation due to the rain shadow effect of the Cascades. The average annual precipitation for the Loamy Bottom ecological site is mostly between 4 and 9 inches. Seventy to seventy-five percent of the precipitation comes late-October through March as a mixture of rain and snow. Precipitation that comes after March is not as effective for plant growth. June through early-October is mostly dry. Freezing temperatures generally occur from late-October through early-April. Temperature extremes are -10 degrees Fahrenheit in winter and 110 degrees Fahrenheit in summer.
Mean Annual precipitation
Range: 4 - 9 inches (6 - 10 inch zone)
Soil moisture regime is aquic or aridic.
Mean Annual Air Temperature
Range: 48 - 54 F
Central Tendency: 50 – 53 F
Soil temperature regime is mesic.
Frost-free period (days)
Total range: 140 - 200
Central tendency: 150 - 180
The growing season for Loamy Bottom ecological site is March through mid-July.
Soil features
Edaphic:
The soils are deep, well-drained and formed in loess. Loamy Bottom ecological site commonly occurs adjacent to Alkali Terrace, Sodic Flat, Wetland complex and Riparian complex, ecological sites. It also occurs with upland sites such as Loamy and Stony.
REPRESENTATIVE SOIL FEATURES
This ecological site soil components are dominantly Typic, Torrifluventic, Fluvaquentic and Aridic taxonomic subgroups of Haploxerolls, Argixerolls, Endoaquolls great groups of the Mollisols taxonomic orders. Soils are dominantly very deep, but strongly contrasting textural stratification can occur up to 20 inches. Average available water capacity of about 6.0 inches (15.3 cm) in the 0 to 40 inches (0-100 cm) depth range.
Soil parent material is dominantly alluvium derived from mixed sources with possibly minor amounts of ash in the upper part of the soil.
The associated soils are Ashue, Esquatzel, Royal, Toppenish, Weirman, Zillah and similar soils.
Dominate soil surface is silt loam to gravelly loam.
Dominant particle-size class is fine-silty to coarse-loamy.
Fragments on surface horizon > 3 inches (% Volume):
Minimum: 0
Maximum: 2
Average: 0
Fragments within surface horizon > 3 inches (% Volume):
Minimum: 0
Maximum: 5
Average: 0
Fragments within surface horizon ≤ 3 inches (% Volume):
Minimum: 0
Maximum: 10
Average: 3
Subsurface fragments > 3 inches (% Volume)
Minimum: 0
Maximum: 25
Average: 10
Subsurface fragments ≤ 3 inches (% Volume):
Minimum: 0
Maximum: 35
Average: 20
Drainage Class: Somewhat poorly to somewhat excessively drained.
Water table depth: 20 to greater than 60 inches
Flooding:
Frequency: None to occasional
Ponding:
Frequency: None
Saturated Hydraulic Conductivity Class:
0 to 10 inches: Moderately high and high
10 to 40 inches: Moderately high and high
Depth to root-restricting feature (inches):
Minimum: Dominantly greater than 60 inches
Maximum: Greater than 60
Electrical Conductivity (dS/m)
Minimum: 0
Maximum: 10
Sodium Absorption Ratio
Minimum: 0
Maximum: 10
Calcium Carbonate Equivalent (percent):
Minimum: 0
Maximum: 10
Soil Reaction (pH) (1:1 Water):
0 - 10 inches: 6.1 to 9.4
10 - 40 inches: 6.6 to 9.4
Available Water Capacity (inches, 0 – 40 inches depth)
Minimum: 1.6
Maximum: 9.1
Average: 6.0
Vegetation dynamics
ECOLOGICAL DYNAMICS:
Vegetation Dynamics:
Loamy Bottom ecological site produces about 3000 pounds per acre of biomass annually.
Regarding saline-alkali soils Daubenmire (page 50) wrote, “It seems impossible to find areas where one can be confident that the vegetation has not been somewhat altered by domesticated animals.” The same is also true of loamy bottoms, riparian areas and wetlands. Some areas were also manipulated by tillage or other farming practices.
Basin wildrye, also called Great Basin wildrye, is at the core of the Loamy Bottom ecological site and warrants a degree of understanding. Basin wildrye is a cool season bunchgrass but is considered weakly rhizomatous. It has coarse, robust stems and leaves, grows to 5 to 7 feet tall and sometimes exceeds three feet in diameter, and thus, is one of the highest producing species. Basin wildrye is commonly found on loamy bottoms, mildly to moderately saline-sodic soils and on the tops of loamy mounds. It tolerates alkaline soils and seasonal flooding but not anaerobic conditions. On a good Loamy Bottom ecological site, basin wildrye, given good plant vigor, can take ownership even with invasive species in the community.
Basin big sagebrush and Wyoming big sagebrush overlap in range and elevation. Basin big sagebrush plants are taller (up to 13 feet) and typically have a single main trunk. Wyoming big sagebrush is considerably shorter (3 to 5 feet), and plants have multiple main stems branching from the ground. Big sagebrush in a long-lived, multi-branched, evergreen shrub. Sagebrush has a significant rooting system, composed of a two-part rooting structure with a primary deep taproot, and a shallow extensive network of finer roots that spread laterally. This rooting system allows big sagebrush to survive in the hottest and driest portions of the sagebrush range by tapping into groundwater sources deep into the soil profile itself. This also allows sagebrush to be more competitive with bunchgrasses when the landscape positions and soils are less ideal for grass species to maintain the competitive advantage.
The stability and resiliency of the reference communities on Loamy Bottom ecological sites is directly linked to the health and vigor of basin wildrye. Given the opportunity (good vigor and favorable moisture), basin wildrye can establish ownership and expand across the Loamy Bottom ecological site. Basin wildrye expands via two processes: (1) Tillering from basal buds for new shoots, and (2) new seedlings from germinating seed.
The natural fire regime maintains a patchy distribution of shrubs. Depending on the time interval since the last fire, the shrub canopy can be as little 0 to 3 percent or as much as 40 percent.
The natural disturbance regime for sagebrush-bunchgrass communities is periodic lightning-caused fires. The fire return intervals (FRI) listed in research for sagebrush steppe communities is quite variable. Ponderosa pine communities have the shortest FRI of about 10 to 20 years (Miller). The FRI increases as one moves to wetter forested sites or to drier shrub steppe communities. Given the uncertainties and opinions of reviewers, a mean of 75 years and a range of 50 to 100 was chosen for Wyoming big sagebrush communities (Rapid Assessment Model). The FRI for Loamy Bottom ecological site is the same as upland sites.
Some fires are spotty or do not burn hot enough to fully remove the sagebrush. Fires with light severity will remove less sagebrush and open smaller patches for grass and forb recovery, whereas the more severe fires will remove almost all the sagebrush and leave vast areas open to return to bunchgrass dominance. This is how the patchy distribution occurs. Rabbitbrush is a sprouting shrub and may also increase following fire.
Because basin wildrye produces a large amount of biomass, fire can burn and smolder in the crown of the plant for considerable time. This leaves basin wildrye plants much diminished. It can take a few years for basin wildrye to fully recover from the effects of fire.
Grazing is another common disturbance that occurs to this ecological site. Grazing pressure can be defined as heavy grazing intensity, or frequent grazing during reproductive growth, or season-long grazing. As grazing pressure increases the plant community unravels in stages:
1. More preferred grasses decline first and then basin wildrye plants produce fewer shoots and tillers and crowns become smaller.
2. As some basin wildrye plants die and other plants are weaker yet, native species such as sagebrush expands
3. As the decline continues invasive species such as knapweed, perennial pepperweed and cheatgrass colonize the site
4. With further decline the site can become a sagebrush-invasive weed community
Managing sagebrush steppe to improve the vigor and health of native bunchgrasses begins with an understanding of grass physiology. New growth for existing bunchgrasses begins each year from basal buds. Basin wildrye plants can expand via tillering, or new plants through natural reseeding. Regrowth from spring grazing comes mostly from photosynthesis.
In the spring each year it is important to monitor and maintain an adequate top growth: (1) to optimize regrowth following spring grazing, (2) so plants have enough energy to replace basal buds annually, and (3) to protect the elevated growing points of basin wildrye.
During seed formation, the growing points of basin wildrye become elevated 4 to 6 inches and are vulnerable to damage or removal. Repeated grazing during late spring is especially damaging. Over several years each native bunchgrass pasture should be rested during the critical period two out of every three years (approximately April 15through July 15). And each pasture should be rested the entire growing-season every third year (approximately
March 1 through July 15).
Basin wildrye and bluebunch wheatgrass remain competitive if:
(1) Basal buds are replaced annually,
(2) Enough top-growth is maintained for growth and protection of growing points, and
(3) The timing of grazing and non-grazing is managed over a several-year period. Careful management of late spring grazing is especially critical
In Washington, basin wildrye-sagebrush communities provide habitat for a variety of upland wildlife species.
Supporting Information
Associated Sites:
Loamy Bottom ecological site is associated with other ecological sites in bottoms and basin areas of MLRA 007X, including Alkali Terrace, Sodic Flat, Wetland Complex and Riparian Complex. Loamy Bottom ecological site is also associated with upland ecological sites such as Loamy and Stony.
Similar sites:
MLRA 007X Columbia Basin & MLRA 009X Palouse Prairie have a similar Loamy Bottom ecological site.
Inventory Data References (narrative)
Data to populate Reference Community came from several sources: (1) NRCS ecological sites from 2004, (2) Soil Conservation Service range sites from 1980s and 1990s, (3) Daubenmire’s habitat types, and (4) ecological systems from Natural Heritage Program
State Correlation:
References: Washington
Boling M., Frazier B., Busacca, A., General Soil Map of Washington, Washington State University, 1998
Daubenmire, R., Steppe Vegetation of Washington, EB1446, March 1968
Davies, Kirk, Medusahead Dispersal and Establishment in Sagebrush Steppe Plant Communities, Rangeland Ecology & Management, 2008
Environmental Protection Agency, map of Level III and IV Ecoregions of Washington, June 2010
Miller, Baisan, Rose and Pacioretty, “Pre and Post Settlement Fire regimes in mountain Sagebrush communities: The Northern Intermountain Region
Natural Resources Conservation Service, map of Common Resource Areas of Washington, 2003
Rapid Assessment Reference Condition Model for Wyoming sagebrush, LANDFIRE project, 2008
Rocchio, Joseph & Crawford, Rex C., Ecological Systems of Washington State. A Guide to Identification. Washington State Department of Natural Resources, October 2015. Pages 156-161 Inter-Mountain Basin Big Sagebrush.
Rouse, Gerald, MLRA 8 Ecological Sites as referenced from Natural Resources Conservation Service-Washington FOTG, 2004
Soil Conservation Service, Range Sites for MLRA 8 from 1980s and 1990s
Tart, D., Kelley, P., and Schlafly, P., Rangeland Vegetation of the Yakima Indian reservation, August 1987, YIN Soil and Vegetation Survey
Site Development and Testing Plan
Future work, as described in a Project Plan, to validate the information in this Provisional Ecological Site Description is needed. This will include field activities to collect low, medium and high intensity sampling, soil correlations, and analysis of that data. Annual field reviews should be done by soil scientists and vegetation specialists. A final field review, peer review, quality control, and quality assurance reviews of the ESD will be needed to produce the final document.
Annual reviews of the Project Plan are to be conducted by the Ecological Site Technical Team.
Major Land Resource Area
MLRA 007X
Columbia Basin
Subclasses
Stage
Provisional
Contributors
Provisional Site Author: Kevin Guinn
Technical Team: R. Fleenor, W. Keller, K. Bomberger, K. Paup-Lefferts
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