Official Series Description


Lab Data Summary

Aggregate lab data for the STEESE soil series. This aggregation is based on all pedons with a current taxon name of STEESE, 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 STEESE 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
23104N0969S2004AK090002Steese7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties64.7925797,-148.1788635

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STEESE 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.

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the STEESE 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 STEESE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the STEESE 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 mountains figure.

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

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

Competing Series

Soil series competing with STEESE 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 STEESE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the STEESE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

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

Soil series sharing subgroup-level classification with STEESE, 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 STEESE 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
Steese silt loam, 20 to 30 percent slopes1738286692884r803ak61020031:25000
Steese silt loam, 12 to 20 percent slopes1724721692883r802ak61020031:25000
Gilmore-Steese complex, 3 to 15 percent slopes1321620692924r81dak61020031:25000
Steese-Gilmore complex, 20 to 30 percent slopes1771471692920r818ak61020031:25000
Steese silt loam, 30 to 45 percent slopes1741391692885r804ak61020031:25000
Steese-Gilmore complex, 12 to 20 percent slopes1761301692919r817ak61020031:25000
Steese silt loam, 7 to 12 percent slopes1711124692882r801ak61020031:25000
Fairbanks-Steese complex, 20 to 30 percent slopes123695692918r816ak61020031:25000
Steese-Gilmore complex, 30 to 45 percent slopes178404692921r819ak61020031:25000
Fairbanks-Steese complex, 12 to 20 percent slopes122178692917r815ak61020031:25000
Steese silt loam, 3 to 7 percent slopes170130692881r800ak61020031:25000
Steese-Gilmore complex, 45 to 70 percent slopes179122692922r81bak61020031:25000
Steese silt loam, 45 to 70 percent slopes17513692886r805ak61020031:25000
Steese-Ester association, 12 to 45 percent slopes32410224494491ng4ak64019861:24000
Ester-Steese association, 7 to 12 percent slopes3023499494271nffak64019861:24000
Steese-Gilmore complex, 10 to 45 percent slopes13679786517721qw2ak64219901:24000
Gilmore-Steese complex, 3 to 15 percent slopes11421995517501qvcak64219901:24000
Steese silt loam, 12 to 45 percent slopes135773517711qw1ak64219901:24000
Steese silt loam, 7 to 12 percent slopes134116517701qw0ak64219901:24000
Gilmore and Steese silt loams, 15 to 45 percent slopes82X70502520021r3hak65020061:24000
Steese-Gilmore complex, 30 to 45 percent slopes441F6288519911r34ak65020061:24000
Steese silt loam, 20 to 30 percent slopes44E3417510691q4dak65020061:24000
Steese silt loam, 12 to 20 percent slopes44D3273510681q4cak65020061:24000
Gilmore and Steese silt loams, 3 to 15 percent slopes82V3018520031r3jak65020061:24000
Steese-Gilmore complex, 20 to 30 percent slopes441E2938519921r35ak65020061:24000
Gilmore-Steese complex, 3 to 15 percent slopes4522137510981q5bak65020061:24000
Steese silt loam, 30 to 45 percent slopes44F1551511251q66ak65020061:24000
Steese silt loam, 7 to 12 percent slopes44C898510671q4bak65020061:24000
Steese-Gilmore complex, 12 to 20 percent slopes441D770511231q64ak65020061:24000
Fairbanks-Steese complex, 12 to 20 percent slopes421D629511151q5wak65020061:24000
Fairbanks and Steese silt loams, 15 to 45 percent slopes89X514520101r3rak65020061:24000
Steese silt loam, 3 to 7 percent slopes44B97510661q49ak65020061:24000
Steese-Gilmore complex, 45 to 70 percent slopes441G92511241q65ak65020061:24000
Steese silt loam, 20 to 30 percent slopes31ST0421139202560825zt6ak65520071:25000
Steese silt loam, 30 to 45 percent slopes31ST058024202560925zt7ak65520071:25000
Fairbanks-Steese complex, 20 to 30 percent slopes31FA112741202557525zs4ak65520071:25000
Fairbanks-Steese complex, 12 to 20 percent slopes31FA102020202557425zs3ak65520071:25000
Steese silt loam, 7 to 12 percent slopes31ST021721202560625zt4ak65520071:25000
Fairbanks-Steese complex, 30 to 45 percent slopes31FA12811202557625zs5ak65520071:25000
Fairbanks-Steese complex, 7 to 12 percent slopes31FA09676202557325zs2ak65520071:25000
Steese-Gilmore complex, 7 to 12 percent slopes31ST07608202561125zt9ak65520071:25000
Fairbanks-Steese complex, 3 to 7 percent slopes31FA08393202557225zs1ak65520071:25000
Steese silt loam, 3 to 7 percent slopes31ST01285202560525zt3ak65520071:25000

Map of Series Extent

Approximate geographic distribution of the STEESE 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 .