Official Series Description


Lab Data Summary

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

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
131AM06181022006MO181002Eutrudepts4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5136389,-90.64
13498UTK05300198TN053UTK001eutrudepts4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9372222,-88.71
13498UTK05300698TN053UTK006eutrudepts4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9105556,-88.7433333
n/a90UTK05700190TN057UTK001eutrudepts2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a90UTK05700790TN057UTK007eutrudepts3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a93UTK04700493TN047UTK004eutrudepts3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EUTRUDEPTS 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.

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the EUTRUDEPTS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the EUTRUDEPTS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the EUTRUDEPTS 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

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

Competing Series

Soil series competing with EUTRUDEPTS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the EUTRUDEPTS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the EUTRUDEPTS 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

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

Soil series sharing subgroup-level classification with EUTRUDEPTS, 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 .

This figure is not available.

Block Diagrams

No block diagrams are available.

Map Units

Map units containing EUTRUDEPTS 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
Prim-Eutrudepts complex, 35 to 60 percent slopes, very stonyPrG5600600048n4ddal02520041:24000
Eutrudepts-Graycalm-Rollins complex, pitted, 10 to 20 percent slopesD83D2511427326452dfljmn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, pitted, 10 to 20 percent slopes6-5D2270527327672smgdmn03520091:24000
Eutrudepts-Graycalm-Rollins complex, 10 to 20 percent slopesD84D1567027326592ndrjmn03520091:24000
Eutrudepts-Graycalm-Rollins complex, pitted, 2 to 10 percent slopesD83C1376227326542ndr3mn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, pitted, 2 to 10 percent slopes6-5B1336427327662smgcmn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, pitted, 20 to 40 percent slopes6-5F1248827327682smgfmn03520091:24000
Eutrudepts-Graycalm-Rollins complex, pitted, 20 to 45 percent slopesD83F934627326462dflkmn03520091:24000
Eutrudepts-Graycalm-Rollins complex, 2 to 10 percent slopesD84C886227326582ndrhmn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, 10 to 20 percent slopes6-13D591827327712smgjmn03520091:24000
Eutrudepts-Graycalm-Rollins complex, 20 to 45 percent slopesD84F591727326932slnqmn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, 20 to 40 percent slopes6-13F389528404492v44smn03520091:24000
Gerrish-Hapludalfs-Hegberg-Eutrudepts complex, 2 to 10 percent slopes6-13B313427327702smghmn03520091:24000
Eutrudepts, occasionally flooded-Greaney, frequently flooded, complex, 0 to 4 percent slopesB84B10662493992wmh3mn61320161:24000
Udalfs-Eutrudepts complex, 25 to 70 percent slopesF155G234014260631jvy1mn61520071:24000
Udalfs-Eutrudepts complex, 0 to 8 percent slopesF155B100414247371jtk8mn61520071:24000
Cuttre-Eutrudepts, complex, 0 to 8 percent slopesE4B499626071p0gvmn61520071:24000
Eutrudepts complex, 1 to 8 percent slopesF153B478114900417kmnmn61520071:24000
Fluvaqents-Eutrudepts-Udifluvents complex, 0 to 35 percent slopes, floodedB268E695024256812mf3smn61920091:24000
Fluvaquents-Eutrudepts-Udifluvents complex, 0 to 18 percent slopes, floodedB268D398824256802mf3rmn61920091:24000
Eutrudepts-Fluvaquents complex, 0 to 8 percent slopes, floodedB268B281324256702mf3fmn61920091:24000
Eutrudepts-Itasca-Endoaqualfs, depressional, complex, 0 to 8 percent slopesA45B33524233812mbqlmn61920091:24000
Eutrudepts, occasionally flooded-Greaney, frequently flooded, complex, 0 to 4 percent slopesB84B1195823084wmh3mn62120061:24000
Rough broken landRo1678125183959sz2ny04320181:24000
Aquolls-Eutrudepts complex, frequently floodedAx86926331452rg7xpa03919731:20000
Aquolls-Eutrudepts complex, frequently floodedAx973726330842rg7xpa04920121:12000

Map of Series Extent

Approximate geographic distribution of the EUTRUDEPTS 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 .