Official Series Description


Lab Data Summary

Aggregate lab data for the STEIGER soil series. This aggregation is based on all pedons with a current taxon name of STEIGER, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to STEIGER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
2172C0049S1972OR035003Steiger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7125015,-121.9649963
604N039103OR035017Steiger6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2262192,-121.8061218
687P051987OR035001Steiger6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5333328,-121.4583359
672C0050S1972OR035004Steiger7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.771389,-122.0347214

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STEIGER soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the STEIGER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the STEIGER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the STEIGER series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with STEIGER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the STEIGER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the STEIGER series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D hills figure.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with STEIGER, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing STEIGER as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Steiger loamy coarse sand, 0 to 15 percent slopes129C2124863442240jor62019921:24000
Steiger loamy coarse sand, low, 0 to 3 percent slopes131A1917163450240sor62019921:24000
Steiger loamy coarse sand, high elevation, 3 to 15 percent slopes130C608763446240nor62019921:24000
Steiger loamy coarse sand, high elevation, 15 to 30 percent slopes130D241963447240por62019921:24000
Steiger loamy coarse sand, high elevation, 30 to 50 percent slopes130E105463448240qor62019921:24000
Steiger ashy loamy coarse sand, cool, 0 to 3 percent slopes6081100316901081tqpmor63520061:24000
Steiger ashy loamy coarse sand, low landscape position, 0 to 3 percent slopes694569116901931tqscor63520061:24000
Steiger ashy loamy coarse sand, 0 to 3 percent slopes607409616901071tqplor63520061:24000
Steiger ashy loamy coarse sand, 3 to 15 percent slopes609306916901091tqpnor63520061:24000
Steiger ashy loamy coarse sand, high elevation, 15 to 30 percent slopes69339716901921tqsbor63520061:24000
Steiger ashy loamy coarse sand, 0 to 15 percent slopes69232716901911tqs9or63520061:24000
Steiger-Rock outcrop complex, 30 to 65 percent south slopes61126916901111tqpqor63520061:24000
Steiger-Rock outcrop complex, 30 to 65 percent north slopes61012216901101tqppor63520061:24000
Steiger loamy coarse sand, 1 to 15 percent slopes73B9469488822jdngor64019771:20000
Lapine-Steiger-Wuksi complex, high elevation, 2 to 25 percent slopes311700627822p29bor68220011:24000

Map of Series Extent

Approximate geographic distribution of the STEIGER soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .