Official Series Description


Lab Data Summary

Aggregate lab data for the GRANILE soil series. This aggregation is based on all pedons with a current taxon name of GRANILE, 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 GRANILE 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
48A91P099591CO069004Granile6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6177788,-105.4869461

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRANILE 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 GRANILE 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 GRANILE 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 GRANILE 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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Competing Series

Soil series competing with GRANILE 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 GRANILE 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 GRANILE 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 hills figure.

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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.

Soil series sharing subgroup-level classification with GRANILE, 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 GRANILE 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
Granile-Peeler complex, 25 to 50 percent slopes1313181498376jqlnco63519791:24000
Granile-Peeler complex, 25 to 50 percent slopes541M904509876k3kmco63620111:24000
Granile-Guffey very gravelly sandy loams, 25 to 50 percent slopes4012369498306jqjdco63719861:24000
Granile very gravelly sandy loam, 25 to 45 percent slopes393508498304jqjbco63719861:24000
Granile very gravelly sandy loam, 4 to 25 percent slopes381658498303jqj9co63719861:24000
Granile very gravelly coarse sandy loam, 30 to 60 percent slopes13402407102k006co64220121:24000
Granile very gravelly coarse sandy loam, 30 to 60 percent slopes132172506453k006co65119991:24000
Granile gravelly sandy loam, 3 to 35 percent slopesGrE4470498061jq8hco65819681:20000
Granile-Tine association27334152071537jwy04319761:24000
Agneston-Granile-Rock outcrop association, 5 to 50 percent slopes8621152135539lwy04319761:24000
Ansel-Granile gravelly sandy loams, 6 to 45 percent slopes1114081501633jtzqwy60119911:24000
Leavitt-Granile complex, 3 to 45 percent slopes1812064501723jv2mwy60119911:24000
Leavitt-Granile complex, 3 to 45 percent slopes19321316697091t1glwy60920061:24000
Ansel-Granile family complex, 10 to 45 percent slopes1687026707841rrklwy6321:24000
Granile-Taglake families, complex, 25 to 40 percent slopes3135979707866rrldwy6321:24000
Rock outcrop-Taglake family-Granile family complex, 40 to 80 percent slopes4631636708036rrrwwy6321:24000
Ansel-Granile family complex, 0 to 10 percent slopes1522998707840rrkkwy6321:24000
Agneston-Granile-Rock outcrop association, 10 to 50 percent slopes1043446361094d3r6wy63319871:24000
Agneston-Granile-Rock outcrop association, 5 to 50 percent slopes1014449715802159fgwy65019821:24000
Tellman-Granile-Agneston association, 2 to 20 percent slopes409545715805159gfwy65019821:24000
Granile-Ansel complex, hilly15310243503018jwfdwy71319861:24000
Agneston-Granile-Rock outcrop association, 5 to 50 percent slopes993941315408961nqfbwy71920131:24000
Tellman-Granile-Agneston association, 2 to 20 percent slopes992772715408951nqf9wy71920131:24000

Map of Series Extent

Approximate geographic distribution of the GRANILE 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 .