Official Series Description


Lab Data Summary

Aggregate lab data for the QUIRK soil series. This aggregation is based on all pedons with a current taxon name of QUIRK, 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 QUIRK 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 QUIRK 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 QUIRK 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 QUIRK 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 QUIRK 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.

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 QUIRK 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 QUIRK 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 QUIRK 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 QUIRK, 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 QUIRK 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
Quirk-Fourbeaver complex, 0 to 15 percent slopes3437AO6431204581r059or60720181:24000
Lamulita-Quirk complex, mass failure, 15 to 30 percent slopes3416BM6331204501r04sor60720181:24000
Volstead-Quirk-Bocker complex, 0 to 15 percent slopes3325AO5831202272msztor60720181:24000
Quirk-Fivebeaver complex, 0 to 15 percent slopes3342AO5631204301r024or60720181:24000
Meaufun-Quirk-Humarel complex, mass failure, 15 to 30 percent slopes3412BM2331204481r04nor60720181:24000
Quirk-Anatone complex, 15 to 30 percent slopes3455BO2331203371qy74or60720181:24000
Quirk-Fourbeaver-Humarel complex, 15 to 30 percent slopes3374BO1231204411r02wor60720181:24000
Quirk-Anatone complex, 15 to 30 percent slopes3455BO225331221681qy74or62620181:24000
Quirk-Fivebeaver complex, 0 to 15 percent slopes3342AO223031222271r024or62620181:24000
Quirk-Fourbeaver-Humarel complex, 15 to 30 percent slopes3374BO194531222391r02wor62620181:24000
Fivebeaver-Grubcreek-Quirk complex, 30 to 60 percent slopes1799CO181431222211qzzjor62620181:24000
Meaufun-Quirk-Humarel complex, 15 to 30 percent slopes3412BO147331222471r04por62620181:24000
Herberger-Quirk complex, 2 to 20 percent slopes4071AO92033853392qcz1or62620181:24000
Lamulita-Quirk complex, mass failure, 15 to 30 percent slopes3416BM69131222501r04sor62620181:24000
Quirk-Fourbeaver complex, 0 to 15 percent slopes3437AO62731222601r059or62620181:24000
Quirk-Volstead complex, 15 to 30 percent slopes3414AO58431224731shrnor62620181:24000
Meaufun-Quirk-Humarel complex, mass failure, 15 to 30 percent slopes3412BM28731222461r04nor62620181:24000
Meaufun-Quirk-Humarel complex, 0 to 15 percent slopes3412AO26631222451r04mor62620181:24000
Alding-Quirk complex, 20 to 50 percent south slopes4075CO1203385474zs2jor62620181:24000
Dupratt-Quirk complex, 2 to 20 percent slopes4079AO7333853422qcykor62620181:24000
Meaufun-Quirk-Humarel complex, mass failure, 0 to 15 percent slopes3412AM3831222441r03wor62620181:24000
Volstead-Quirk-Bocker complex, 0 to 15 percent slopes3325AO195624370902msztor63120181:24000
Quirk-Anatone-Volstead complex, 15 to 30 percent slopes3326BO76424370931qqfjor63120181:24000
Volstead-Quirk-Bocker complex, 15 to 30 percent slopes3325BO024370912mszvor63120181:24000
Volstead-Quirk-Bocker complex, 15 to 30 percent slopes348126847462v5ror67019991:24000
Volstead-Quirk-Bocker complex, 0 to 15 percent slopes34753847452v5qor67019991:24000

Map of Series Extent

Approximate geographic distribution of the QUIRK 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 .