Official Series Description


Lab Data Summary

Aggregate lab data for the TANKSEL soil series. This aggregation is based on all pedons with a current taxon name of TANKSEL, 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 TANKSEL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

Competing Series

Soil series competing with TANKSEL 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 TANKSEL 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 TANKSEL 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 TANKSEL, 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 TANKSEL 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
Belshaw-Tanksel complex, 20 to 50 percent north slopes196E18342620723bvhor6181:24000
Kishwalk-Gwinly-Tanksel complex, 20 to 50 percent slopes4320NO53385401vyl1or62620181:24000
Kishwalk-Gwinly-Tanksel complex, 20 to 50 percent slopes193E100783426046vyl1or6271:24000
Belshaw-Tanksel complex, 20 to 50 percent north slopes196E2358342509023bvhor6271:24000
Kishwalk-Gwinly-Tanksel complex, 15 to 50 percent south slopes178E12834250872dvgpor6271:24000
Kishwalk-Gwinly-Tanksel complex, 15 to 50 percent south slopes178E1477233849892dvgpor6771:24000
Belshaw-Tanksel complex, 20 to 50 percent north slopes196E3892339163223bvhor6771:24000
Tanksel-Lainand-Camaspatch complex, 30 to 70 percent slopes6387380770652l5zwa63720081:24000
Camaspatch-Tanksel-Rubble land complex, 45 to 75 percent slopes8902710772692ldkwa63720081:24000
Tanksel-Patron-Camaspatch complex, 30 to 70 percent slopes6561978770792l6fwa63720081:24000
Tanksel-Rubble land-Rock outcrop complex, 30 to 70 percent slopes8911781772702ldlwa63720081:24000
Tanksel-Wockum complex, 15 to 30 percent slopes6931553771062l79wa63720081:24000
Tanksel-Patron-Camaspatch complex, 15 to 30 percent slopes650774770742l68wa63720081:24000
Camaspatch-Tanksel complex, 30 to 70 percent slopes658341770812l6hwa63720081:24000
Tanksel-Lainand complex, 15 to 30 percent slopes637252770642l5ywa63720081:24000
Tanskel-Patron-Camaspatch complex, 15 to 30 percent slopes1502084708162cpdwa68119941:24000
Camaspatch-Tanksel-Lainand complex, 45 to 60 percent slopes411635708892crrwa68119941:24000
Tanksel-Patron-Camaspatch complex, 30 to 45 percent slopes151927708172cpfwa68119941:24000
Camaspatch-Tanksel complex, 30 to 45 percent slopes40907708882crqwa68119941:24000
Tanksel-Wockum complex, 15 to 30 percent slopes152898708182cpgwa68119941:24000
Tanksel-Wockum complex, 30 to 45 percent slopes153777708192cphwa68119941:24000
Lainand-Tanksel complex, 30 to 45 percent slopes88729712262d3mwa68119941:24000
Tanksel-Wockum complex, 45 to 65 percent slopes154302708202cpjwa68119941:24000

Map of Series Extent

Approximate geographic distribution of the TANKSEL 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 .