Official Series Description


Lab Data Summary

Aggregate lab data for the TOLER soil series. This aggregation is based on all pedons with a current taxon name of TOLER, 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 TOLER 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
889P022389WA017020Toler5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6941681,-119.8286133

Water Balance

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

There are insufficient data to create the 2D hillslope position figure.

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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 TOLER 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 TOLER 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 TOLER 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 .

There are insufficient data to create the 2D hillslope position figure.

Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with TOLER, 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 TOLER 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
Toler ashy silt loam, 3 to 8 percent slopes41212234704469rn1twa01719981:12000
Argabak-Horseflat-Toler complex, 0 to 20 percent slopes2612011704317rmwxwa01719981:12000
Toler-Horseflat complex, 3 to 8 percent slopes4207095704475rn20wa01719981:12000
Toler-Horseflat-Ralls complex, 8 to 15 percent slopes4246540704473rn1ywa01719981:12000
Toler ashy fine sandy loam, 0 to 8 percent slopes4086133700695rj42wa01719981:12000
Toler-Horseflat complex, 8 to 15 percent slopes4215098704476rn21wa01719981:12000
Toler ashy silt loam, 0 to 3 percent slopes4113844704468rn1swa01719981:12000
Toler-Horseflat-Benwy complex, 3 to 8 percent slopes4233687704472rn1xwa01719981:12000
Toler ashy silt loam, 8 to 15 percent slopes4133582704470rn1vwa01719981:12000
Toler-Horseflat-Ralls complex, 15 to 30 percent slopes4252660704474rn1zwa01719981:12000
Toler-Corbaley complex, 3 to 8 percent slopes4162328699469rgvjwa01719981:12000
Toler-Corbaley complex, 8 to 15 percent slopes4171583699470rgvkwa01719981:12000
Toler-Horseflat complex, 15 to 30 percent slopes422960699581rgz4wa01719981:12000
Toler-Kester complex, 3 to 8 percent slopes426939699452rgtzwa01719981:12000
Toler ashy fine sandy loam, 8 to 15 percent slopes409784700696rj43wa01719981:12000
Toler-Horseflat complex, 0 to 3 percent slopes419293699568rgyqwa01719981:12000
Toler ashy silt loam, 15 to 30 percent slopes414235704471rn1wwa01719981:12000
Toler-Corbaley complex, 15 to 30 percent slopes418220699471rgvlwa01719981:12000
Toler ashy fine sandy loam, 15 to 30 percent slopes410121700697rj44wa01719981:12000
Toler-Argabak-Horseflat complex, 0 to 20 percent slopes41581700584rj0hwa01719981:12000

Map of Series Extent

Approximate geographic distribution of the TOLER 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 .