Official Series Description


Lab Data Summary

Aggregate lab data for the GRANATH soil series. This aggregation is based on all pedons with a current taxon name of GRANATH, 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 GRANATH 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
3686P085586CO033002Granath7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6755562,-108.6938858

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRANATH 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 GRANATH 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 GRANATH 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 GRANATH 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 GRANATH 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 GRANATH 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 GRANATH 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 mountains figure.

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

Soil series sharing subgroup-level classification with GRANATH, 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 GRANATH 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
Granath loam, 3 to 6 percent slopes4413484576482wr83co67119971:24000
Ormiston-Granath complex, 1 to 12 percent slopes827085577142wqynco67119971:24000
Ilex-Granath complex, 2 to 6 percent slopes584136576811y0pco67119971:24000
Ilex-Granath complex, 6 to 12 percent slopes593291576821y0qco67119971:24000
Granath loam, 6 to 12 percent slopes453107576491xznco67119971:24000
Nortez-Granath complex, 0 to 6 percent slopes782886577051y1gco67119971:24000
Ilex-Pramiss-Granath complex, 2 to 9 percent slopes612227576861y0vco67119971:24000
Pramiss-Granath complex, 3 to 9 percent slopes90813577261y24co67119971:24000
Granath-Fughes complex, 0 to 15 percent slopes46334576501xzpco67119971:24000
Granath-Ormiston-Fivepine complex, 0 to 15 percent slopes48285576532wqygco67119971:24000
Fardraw-Granath complex, 3 to 12 percent slopes35117576331xz4co67119971:24000
Granath-Nortez complex, 0 to 15 percent slopes4720576521xzrco67119971:24000
Granath-Fughes complex, 0 to 15 percent slopes51120710507191k0s0co67220031:24000
Granath-Nortez complex, 0 to 15 percent slopes8607941507278k0vtco67220031:24000
Granath-Dolores-Fivepine complex, 0 to 15 percent slopes8623228507331k0xjco67220031:24000
Granath-Ormiston-Fivepine complex, 0 to 15 percent slopes86321447381002wqygco67220031:24000
Nortez-Granath complex, 1 to 12 percent slopes9681602507313k0wyco67220031:24000
Ormiston-Granath complex, 1 to 12 percent slopes9565175073072wqynco67220031:24000
Granath loam, 3 to 6 percent slopes9592945073092wr83co67220031:24000
Granath-Zoltay-Nortez complex, 0 to 15 percent slopes901186507283k0vzco67220031:24000

Map of Series Extent

Approximate geographic distribution of the GRANATH 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 .