Official Series Description


Lab Data Summary

Aggregate lab data for the SCOBEY soil series. This aggregation is based on all pedons with a current taxon name of SCOBEY, 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 SCOBEY 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
43B07N0156S06MT073001Scobey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3045349,-111.9236298
5283P064182MT073001Scobey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3094444,-111.9238892
5288P045188MT051003Scobey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.1336098,-110.8477783
5207N0155S06MT051001Scobey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4357834,-111.1842346
5240A3339S1962MT005015Scobey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7132645,-108.5135727
5240A3671S1968MT013006Scobey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6829643,-111.2014236

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SCOBEY 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 SCOBEY 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 SCOBEY 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 SCOBEY 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 SCOBEY 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 SCOBEY series and competing. 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 SCOBEY 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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Soil series sharing subgroup-level classification with SCOBEY, 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 SCOBEY 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
Scobey-Kevin clay loams, 0 to 4 percent slopes561B2438233439862t3kbmt04119941:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes561C63563439872t3k4mt04119941:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes561B926893442272t3kbmt05119921:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes561C25763442282t3k4mt05119921:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes561B894793452172t3kbmt10119921:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes561C56013452182t3k4mt10119921:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes571306113455752t3k4mt10519761:24000
Scobey-Kevin loams, undulatingSk332201469344xwtmt60019691:24000
Scobey-Zahl complex, hillySO138151469194xwbmt60019691:24000
Scobey clay loam, 0 to 4 percent slopesSg105521469322t3k3mt60019691:24000
Scobey-Kevin clay loams, 2 to 8 percent slopesSh44991469332t3k4mt60019691:24000
Scobey-Kevin clay loams, 0 to 4 percent slopesKc17171468362t3kbmt60019691:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes110935713462552t3k4mt60819761:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes109189343462532t3kbmt60819761:24000
Hillon-Scobey clay loams, 4 to 20 percent slopes6911284346519cml1mt60819761:24000
Scobey clay loam, 0 to 4 percent slopes10892653462522t3k3mt60819761:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes17471223418392t3kbmt61319751:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes11321253417722t3k4mt61319751:24000
Scobey clay loam, 0 to 4 percent slopes17314253418382t3k3mt61319751:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes561B1779843468322t3kbmt61519921:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes561C675243468332t3k4mt61519921:24000
Scobey-Linnet complex, 0 to 4 percent slopes562B16448346834cmx6mt61519921:24000
Scobey clay loam, 0 to 4 percent slopes56A147183468382t3k3mt61519921:24000
Fortbenton-Scobey fine sandy loams, 0 to 3 percent slopes563A9363346835cmx7mt61519921:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes563C1838753477532t3k4mt64119941:24000
Kevin-Scobey-Phillips association, 2 to 15 percent slopes1441D132313347603cnq0mt64119941:24000
Scobey-Phillips complex, 0 to 4 percent slopes561B86567347750cnvrmt64119941:24000
Scobey clay loam, 0 to 4 percent slopes56B347733477582t3k3mt64119941:24000
Kevin-Scobey-Nishon association, 0 to 25 percent slopes1443E32569347604cnq1mt64119941:24000
Scobey-Elloam-Absher gravelly clay loams, 2 to 8 percent slopes567C12232347757cnvzmt64119941:24000
Scobey-Kevin clay loams, 0 to 4 percent slopes164B2054833483802t3kbmt65719901:24000
Scobey-Kevin clay loams, 2 to 8 percent slopes263C1477563485062t3k4mt65719901:24000
Scobey-Acel complex, 0 to 4 percent slopes264B2621348507cpn5mt65719901:24000

Map of Series Extent

Approximate geographic distribution of the SCOBEY 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 .