Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with BLUESPRIN 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 BLUESPRIN 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 BLUESPRIN 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 BLUESPRIN, 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 BLUESPRIN 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
Bluesprin family-Lithic Mollic Haploxeralfs association, 30 to 70 percent slopes.10612770470327hsdvca70219841:24000
Lithic Mollic Haploxeralfs-Bluesprin family association, 30 to 90 percent slopes.1541872470375hsgdca70219841:24000
Bluesprin-Keuterville complex, 35 to 65 percent slopes6822324872512ph5xid05720131:24000
Bluesprin-Flybow complex, 35 to 65 percent slopes5735424872502ph5wid05720131:24000
Klickson-Bluesprin complex, 35 to 65 percent slopes22638324872672ph6fid05720131:24000
Klickson-Bluesprin association68380026862575595id60019891:24000
Rock outcrop-Bluesprin complex941859268626755b3id60019891:24000
Bluesprin-Klickson association516082686232558jid60019891:24000
Ferdinand-Bluesprin very cobbly loam complex4414662686236558bid60019891:24000
Bluesprin-Rock outcrop complex7133126862335597id60019891:24000
Lawyer-Bluesprin association745862686259559did60019891:24000
Bluesprin-Keuterville association458226862315585id60019891:24000
Bluesprin-Lawyer association, 40 to 75 percent slopes64673253819558wid60019891:24000
Keuterville-Bluesprin complex6339926862525590id60019891:24000
Keuterville-Bluesprin association642126862535591id60019891:24000
Bluesprin-Rock outcrop complex771726863165597id60919891:24000
Ferdinand-Bluesprin very cobbly loam complex442222686330558bid60919891:24000
Bluesprin-Klickson association51182686315558jid60919891:24000
Klickson-Bluesprin association684826863375595id60919891:24000
Southwick-Bluesprin complex, 10 to 35 percent slopes1192256795842nt7id61119941:24000
Klickson-Bluesprin complex, 35 to 65 percent slopes22j12027431012ph6fid61119941:24000
Ferdinand-Bluesprin very cobbly loam complex4444615154018558bid61719761:24000
Bluesprin-Rock outcrop complex7318981540465597id61719761:24000
Bluesprin-Klickson association528325154024558jid61719761:24000
Klickson-Bluesprin complex, 30 to 75 percent slopes68273191540442y6tcid61719761:24000
Rock outcrop-Bluesprin complex, 25 to 70 percent slopes94198181540732y6v3id61719761:24000
Lawyer-Bluesprin association7410133154051559did61719761:24000
Bluesprin-Lawyer association, 40 to 75 percent slopes63914154035558wid61719761:24000
Keuterville-Bluesprin complex, 40 to 90 percent slopes6435671540402y6v4id61719761:24000
Bluesprin-Keuterville association416931540135585id61719761:24000
Keuterville-Bluesprin complex6310961540395590id61719761:24000
Klickson-Bluesprin complex, 30 to 75 percent slopes2y6tc625930989002y6tcid61819651:24000
Keuterville-Bluesprin complex, 40 to 90 percent slopes2y6v434430989092y6v4id61819651:24000
Rock outcrop-Bluesprin complex, 25 to 70 percent slopes2y6v35530989082y6v3id61819651:24000
Bluesprin family, 30 to 60 percent slopes22641812142qhtid65619921:24000
Bluesprin family, 30 to 60 percent slopes65602268633323652qhtid7001:24000

Map of Series Extent

Approximate geographic distribution of the BLUESPRIN 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 .