Official Series Description


Lab Data Summary

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

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with GRANO, 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 GRANO 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
Grano clay, 0 to 1 percent slopesI92A58279883521bxsmn06920071:12000
Grano loam, 0 to 1 percent slopesI744A827988892qtw1mn06920071:12000
Grano clay, 0 to 1 percent slopesI92A7617279985121bxsmn13519991:24000
Grano loam, map 18-22, 0 to 2 percent slopes14494593394901f7xrmn13519991:24000
Grano clay, map 18-22, 0 to 2 percent slopes14483479394900f7xqmn13519991:24000
Grano loam, 0 to 1 percent slopesI744A209927998852qtw1mn13519991:24000
Grano silty clay, saline, 0 to 1 percent slopesF449A219525877112q55hnd0051:12000
Grano silty clay, 0 to 1 percent slopesF47A156125877302q3w6nd0051:12000
Grano-Hegne silty clays, 0 to 1 percent slopesI649A726426082pgdpnd03519801:20000
Grano silty clay, 0 to 1 percent slopesI232A126425391nystnd03519801:20000
Grano silty clay, 0 to 1 percent slopesC15A2625966432q0rtnd04319851:20000
Grano silty clay, 0 to 1 percent slopesC15A11325664332q0rtnd04519661:20000
Grano silty clay, dry, 0 to 1 percent slopesE4723A16222699363d336nd05320031:24000
Grano silty clay, 0 to 1 percent slopesC15A7125666322q0rtnd05519741:20000
Grano silty clay, plane, 0 to 1 percent slopesI644A2764826430342pgc6nd06719721:20000
Grano silty clay, moderately saline, 0 to 1 percent slopesI645A93126430522qkvvnd06719721:20000
Grano silty clay, 0 to 1 percent slopesF47A275425870852q3w6nd07119841:12000
Grano silty clay, saline, moderately deep over sandy substratum, 0 to 1 percent slopesI563A6132479042yw6pnd07319921:20000
Grano silty clay, sandy substratum, 0 to 1 percent slopesI510A926413541vh7lnd07319921:20000
Grano silty clay, 0 to 1 percent slopesI232A45226410791nystnd07720051:12000
Grano silty clay, saline, moderately deep over sandy substratum, 0 to 1 percent slopesI563A15832479102yw6pnd08119591:12000
Grano silty clay, 0 to 1 percent slopesI232A6826412011nystnd08119591:12000
Grano silty clay, sandy substratum, 0 to 1 percent slopesI510A1026412631vh7lnd08119591:12000
Grano silty clay, 0 to 1 percent slopesI232A27026415851nystnd09719741:20000
Grano-Hegne silty clays, 0 to 1 percent slopesI649A338526429292pgdpnd09919671:20000
Grano silty clay, plane, 0 to 1 percent slopesI644A190826429282pgc6nd09919671:20000
Grano silty clay, 0 to 1 percent slopesI232A31626428321nystnd09919671:20000
Grano silty clay, 0 to 1 percent slopesC15A84425669492q0rtnd10319661:12000

Map of Series Extent

Approximate geographic distribution of the GRANO 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 .