Official Series Description


Lab Data Summary

Aggregate lab data for the TOKUL soil series. This aggregation is based on all pedons with a current taxon name of TOKUL, 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 TOKUL 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
298P0260S1997WA061001TOKUL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9330559,-121.9561081
298P0397S1998WA061001TOKUL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5044441,-121.8763885
298P0398S1998WA061002TOKUL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7513885,-121.8719406
298P0399S1998WA061003TOKUL6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5044441,-121.8763885

Water Balance

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

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Competing Series

Soil series competing with TOKUL 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 TOKUL series and competing. 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 TOKUL 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.

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

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 TOKUL, 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 TOKUL 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
Tokul gravelly medial loam, 8 to 15 percent slopes25534425740662t61lwa63419861:24000
Tokul gravelly medial loam, 15 to 30 percent slopes25615908740672t61mwa63419861:24000
Tokul gravelly medial loam, 0 to 8 percent slopes2549272740652t61kwa63419861:24000
Tokul gravelly medial loam, 30 to 65 percent slopes2576034740682t61nwa63419861:24000
Tokul-Pastik complex, 45 to 90 percent slopes2585811740692h2bwa63419861:24000
Tokul-Pastik complex, windswept, 45 to 90 percent slopes259317740702h2cwa63419861:24000
Tokul gravelly medial loam, 8 to 15 percent slopes1477400747792t61lwa65719811:24000
Tokul gravelly medial loam, 0 to 8 percent slopes1464410747782t61kwa65719811:24000
Tokul gravelly medial loam, 15 to 30 percent slopes1484350747802t61mwa65719811:24000
Tokul gravelly medial loam, 30 to 65 percent slopes1491400747812t61nwa65719811:24000
Tokul gravelly medial loam, 0 to 8 percent slopes7261376749612t61kwa66119791:24000
Tokul gravelly medial loam, 8 to 15 percent slopes7343515749622t61lwa66119791:24000
Tokul-Winston gravelly loams, 25 to 65 percent slopes7720393749662j08wa66119791:24000
Tokul-Ogarty-Rock outcrop complex, 25 to 65 percent slopes7618697749652j07wa66119791:24000
Tokul gravelly medial loam, 15 to 30 percent slopes7415217749632t61mwa66119791:24000
Tokul-Ogarty-Rock outcrop complex, 0 to 25 percent slopes759527749642j06wa66119791:24000
Ogarty-Tokul-Rock outcrop complex, 65 to 90 percent slopes411521749272hz0wa66119791:24000
Tokul silt loam, 2 to 8 percent slopes70930749592j01wa66119791:24000
Tokul silt loam, 8 to 15 percent slopes71495749602j02wa66119791:24000

Map of Series Extent

Approximate geographic distribution of the TOKUL 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 .