Ecological site group R007XG143WA
Sandy Loam
Last updated: 09/22/2023
Accessed: 12/22/2024
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
7.5 – Yakima Valley – Pleistocene Lake Basins
Site Concept Narrative:
Diagnostics:
Carey balsamroot is a marker for MLRA 007X.
Sandy Loam is a shrub steppe upland site occurring on moderately deep to deep sandy loam textured soils. Depth to carbonates is 18 inches or deeper below the surface.
In the reference state this site is dominated by Wyoming sage, bluebunch wheatgrass and needle and thread. Carey balsamroot, lupine, fleabane and hawksbeard are also common.
The Sandy site, on the other hand, has the same soil texture as Sandy Loam, but is a grassland community because the carbonates are at or near the surface.
The line between Sandy Loam and Sandy is often sharp. It is possible to stand with one foot on Sandy Loam and the other on Sandy.
Principle Vegetative Drivers:
The shrub steppe vegetative expression for Sandy Loam is driven by the sandy loam soil texture and no carbonates until a depth of 18 inches or deeper.
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 runs off-site or infiltrates into the soil
2. Whether soil condition remain aerobic or become saturated and become anaerobic
3. Water drainage and how quickly the soil reaches wilting point
Sandy Loam ecological sites have more available moisture than Sandy sites since the carbonates are not reached until a depth of 18 inches or deeper. Soils are well drained and dry down quicker than adjacent Loamy ecological sites.
Physiographic features:
The landscape is part of the Columbia basalt plateau. Sandy loam is commonly found on terraces, terrace escarpments, benches and plateaus.
Physiographic Division: Intermontane Plateau
Physiographic Province: Columbia Plateau
Physiographic Sections: Walla Walla Plateau Section
Landscapes: Basin, hills and plateaus
Landform: Hillslopes, ridges, terraces, terraces escarpments and alluvial flats
Elevation:
Range: 300 to 3,500 feet
Central tendency: 300 to 1,200 feet
Slope:
Total range: 0 to 60 percent
Central tendency: 10 to 55 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 across MLRA 007X 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 Sandy Loam is mostly between 4 and 10 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 can be 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. Winter fog is variable and often quite localized, as the fog settles on some areas but not others.
Mean Annual precipitation
Range: 4 - 10 inches
Soil moisture regime is aridic.
Mean Annual Air Temperature
Range: 48 to 54 F
Central Tendency: 50 – 52 F
Soil temperature regime is mesic.
Frost-free period (days)
Total range: 130 to 200
Central tendency: 150 to 180
The growing season for Sandy Loam is March through June.
Soil features
Edaphic:
The Sandy Loam ecological site occurs with Sands, Sandy, and Shallow Stony Sand ecological sites.
REPRESENTATIVE SOIL FEATURES
This ecological site components are dominantly Xeric taxonomic subgroup of Haplocalcids and Haplocambids great groups of the Aridisols taxonomic orders. Soils are dominantly very deep, but strongly contrasting textural stratification can occur up to 20 inches. Average available water capacity of about 5.0 inches (12.7 cm) in the 0 to 40 inches (0 to 100 cm) depth range.
Soil parent material is dominantly alluvium derived from mixed sources.
The associated soils are Adkins, Ephrata, Finley, Prosser, Royal, Taunton, Wiehl and similar soils.
Dominate soil surface is very fine sandy loam to cobbly fine sandy loam.
Dominant particle-size class is coarse-silty to loamy-skeletal.
Fragments on surface horizon > 3 inches (% Volume):
Minimum: 0
Maximum: 2
Average: 0
Fragments within surface horizon > 3 inches (% Volume):
Minimum: 0
Maximum: 25
Average: 2
Fragments within surface horizon ≤ 3 inches (% Volume):
Minimum: 0
Maximum: 30
Average: 10
Subsurface fragments > 3 inches (% Volume)
Minimum: 0
Maximum: 30
Average: 10
Subsurface fragments ≤ 3 inches (% Volume):
Minimum: 0
Maximum: 40
Average: 25
Drainage Class: Dominantly well drained.
Water table depth: Dominantly greater than 60 inches
Flooding:
Frequency: None
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: 10
Maximum: 30
Soil Reaction (pH) (1:1 Water):
0 - 10 inches: 6.1 to 9.0
10 - 40 inches: 6.1 to 9.0
Available Water Capacity (inches, 0 – 40 inches depth)
Minimum: 1.8
Maximum: 7.9
Average: 5.0
Vegetation dynamics
Vegetation Dynamics:
Sandy Loam ecological site produces about 500 to 850 pounds per acre of biomass annually.
Sandy Loam ecological site is a shrub steppe site with Wyoming sagebrush, needle and thread and bluebunch wheatgrass dominant in the reference state.
Wyoming sagebrush in a long-lived, multi-branched, evergreen shrub. Size varies from three to five feet depending on soil and site conditions. Wyoming big 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 Wyoming 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 Wyoming big sagebrush to be more competitive with bunchgrasses when the landscape positions and/or soils are less ideal for grass species to maintain the competitive advantage.
Needle and thread is a very drought tolerant perennial bunchgrass. It prefers excessively drained sandy and coarse textured gravelly loam soils. Needle and thread produces erect, unbranched stems about three feet in height. The seeds have a 4 to 5-inch long twisted awn. With wetting and drying the seed drills itself into the ground. Thus, needle and thread is one of the best seeders in the reference community. With grazing pressure needle and thread initially increases.
Bluebunch wheatgrass is a long-lived, mid-sized bunchgrass with an awned or awnless seed head arranged is a spike. Bluebunch provides a crucial and extensive network of roots to the upper portions (up to 48 inch deep in soils with no root-restrictive horizons) of the soil profile. These roots create a massive underground source to stabilize the soils, provide organic matter and nutrients inputs, and help maintain soil pore space for water infiltration and water retention in the soil profile. The extensive rooting system of mid-sized bunchgrasses leave very little soil niche space available for invasion by other species. This drought resistant root can compete with, and suppress, the spread of exotic weeds.
The stability and resiliency of the reference communities is directly linked to the health and vigor of bluebunch wheatgrass and needle and thread Research has found that the community remains resistant to medusahead if the site maintains at least 0.8 plants per square foot of mid-sized bunchgrass (K. Davies, 2008). These two grasses help hold the system together. If we lose either grass the ecosystem begins to unravel.
The natural disturbance regime for grassland 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 dries shrub steppe
communities. Given the uncertainties and opinions or reviewers, a mean of 75 years was chosen for Wyoming sagebrush communities (Rapid Assessment Model). This would place the historic FRI for grassland steppe around 30 to 50 years.
The effect of fire on the community depends upon the severity of the burn. With a light to moderate fire there can be a mosaic of burned and unburned patches. Bunchgrasses thrive as the fire does not get into the crown. With adequate soil moisture the bunchgrasses can make tremendous growth the year after the fire. Largely, the community is not affected by lower intensity fire. Needle and thread is a native species that can increase via new seedlings following a fire.
A severe fire puts stress on the entire community. Spots and areas that were completely sterilized are especially vulnerable to exotic invasive species. Sterilized spots must be seeded to prevent invasive species (annual grasses, tumble mustard) from totally occupying the site. Bluebunch wheatgrass may have weak vigor for a few years but generally survive. Needle and thread is largely unaffected by fire.
Grazing is another common disturbance that occurs in this ecological site. Grazing pressure can be defined as heavy grazing intensity, or frequent grazing during reproductive growth, or season-long grazing (the same plants grazed more than once). As grazing pressure increases the plant community unravels in stages:
1. Bluebunch wheatgrass declines while needle and thread increases
2. Both bluebunch wheatgrass and needle and thread decline. Invasive species such as cheatgrass colonize the site
3. With further decline the site can become a cheatgrass dominated community
Managing grasslands to improve the vigor and health of bluebunch wheatgrass and needle and thread begins with an understanding their needs. New growth each year begins from basal buds. B wheatgrass plants rely principally on tillering while needle and thread establishes new plants through natural seeding. During seed formation, the growing points of bluebunch wheatgrass becomes elevated and are vulnerable to damage or removal.
Repeated critical period grazing (boot stage through seed formation) is especially damaging to bluebunch. Over several years each native bunchgrass pasture should be rested during the critical period two out of every three years (approximately April 1 throughJune 30). And each pasture should be rested the entire growing-season every third year (approximately March 1 through June 30).
In the spring each year it is important to monitor and maintain an adequate topgrowth: (1) so plants have enough energy to replace basal buds annually, (2) to optimize regrowth following spring grazing, and (3) to protect the elevated growing points of bluebunch wheatgrass.
Bluebunch wheatgrass and needle and thread remain competitive if:
(1) Basal buds are replaced annually,
(2) Viable seed is produced by needle and thread in most years
(3) Enough top-growth is maintained for growth and protection of growing points, and
(4) The timing of grazing and non-grazing is managed over a several-year period. Careful management of late spring grazing is especially critical
For more grazing management information refer to Range Technical Notes found in Section I Reference Lists of NRCS Field Office Technical Guide for Washington State.
In Washington, Wyoming sagebrush – bluebunch wheatgrass – needle and thread communities provide habitat for a variety of upland wildlife species.
Supporting Information:
Associated Sites:
Sandy Loam ecological site is associated with Sandy, Sands, Loamy, Stony, Shallow Stony Sand and Very Shallow ecological sites.
Similar sites:
Sandy Loam ecological site is a Wyoming sage – bluebunch wheatgrass – needle-and-thread ecological site. Non-sandy shrub steppe sites do not have the needle and thread but are similar otherwise.
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: Washington
References:
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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