Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with SPANPEAK 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 SPANPEAK 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 SPANPEAK 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 .

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

Soil series sharing subgroup-level classification with SPANPEAK, 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 SPANPEAK 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
Catgulch, very stony-Spanpeak, stony-Bavdark complex, 25 to 60 percent slopes787F2304155726571fmt62219971:24000
Spanpeak-Bavdark coarse sandy loams, 25 to 50 percent slopes778F20371557215718mt62219971:24000
Spanpeak coarse sandy loam, 35 to 60 percent slopes278F50715536756nvmt62219971:24000
Duckcreek-Cloud Peak-Spanpeak families, complex, 15 to 50 percent slopes1141F656424850282pdw6mt6321:24000
Spanpeak-Bavdark coarse sandy loams, 25 to 50 percent slopes2001111465674xhzmt63619831:24000
Catgulch, very stony-Spanpeak, stony-Bavdark complex, 25 to 60 percent slopes182751465714xj3mt63619831:24000
Wineglass-Woodhall-Spanpeak complex, 15 to 60 percent slopes5614F764315647957tqmt6691:24000
Spanpeak, stony-Booneville-Surdal, stony complex, 35 to 70 percent slopes8605F36621567695842mt6691:24000
Spanpeak, very stony - Woodhall, stony - Adel complex, 15 to 60 percent slopes8602F1075156766583zmt6691:24000
Boonville, extremely bouldery-Adel-Spanpeak, bouldery complex, 8 to 45 percent slopes3502F85415663757ztmt6691:24000
Elve, extremely bouldery- Spanpeak, very stony -Beehive,extremely stony complex ,4 to 60 percent slopes3519F809697277rdktmt6691:24000
Spanpeak, very bouldery-Beaveridge-Currycreek complex, 20 to 60 percent slopes750631368982ypq2wy6291:24000
Leavitt-McCort-Spanpeak families, complex, 15 to 40 percent slopes2513302919596dwy6291:24000
Leavitt-McCort-Spanpeak families, complex, 15 to 40 percent slopes1662772157740594dwy6471:24000
Spanpeak, very bouldery-Beaveridge-Currycreek complex, 20 to 60 percent slopes750632533372ypq2wy65620081:24000
McCort-Spanpeak-Amsden families, complex, 15 to 40 percent slopes415113161578895996wy65620081:24000
Leavitt-McCort-Spanpeak families, complex, 15 to 40 percent slopes25110579157802596dwy65620081:24000
Ustic Calcicryolls-Spanpeak family, complex, 20 to 30 percent slopes2443925157801596cwy65620081:24000

Map of Series Extent

Approximate geographic distribution of the SPANPEAK 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 .