Official Series Description


Lab Data Summary

Aggregate lab data for the INTERIOR soil series. This aggregation is based on all pedons with a current taxon name of INTERIOR, 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 INTERIOR 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
60A82P042682NE165029Interior6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9308319,-103.6641693
63A82P083582SD071010Interior6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9027786,-101.9861145
6482P082682SD071004Interior8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7069435,-101.961113
6484P026384SD071001INTERIOR7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6974983,-101.9344406
6410N0720S2009SD103004Interior8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8874278,-102.0565167

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the INTERIOR 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 INTERIOR 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 INTERIOR 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 INTERIOR 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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Click the image to view it full size.

Competing Series

Soil series competing with INTERIOR 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 INTERIOR series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the INTERIOR 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with INTERIOR, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NE-2010-09-09-06 | Sioux County - 1998

    Typical pattern of soils and parent material in the Bufton-Orella-Badland association (Soil Survey of Sioux County, Nebraska; 1998).

  2. NE-2012-02-14-01 | Sioux County - 1998

    Typical pattern of soils and parent material in the Bufton-Orella-Badland association (Soil Survey of Sioux County, Nebraska; 1998).

  3. SD-2012-03-15-13 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils, topography, and underlying material in the Cedarpass-Denby-Interior and the Orella-Fairburn-Badland associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

  4. SD-2012-03-15-55 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Weta-Cactusflat and Blackpipe-Wortman associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

Map Units

Map units containing INTERIOR 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
Interior silty clay, channeled, frequently flooded50004015357917d0fqne16519931:20000
Interior silt loam, channeledHc5439353367cvpysd09519711:20000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesIrB1492025809142t34xsd60620111:24000
Interior loam, channeled, 0 to 6 percent slopes, floodedIo1447025809132t34wsd60620111:24000
Cedarpass-Interior-Badland complexCh45952580884cyglsd60620111:24000
Orella-Interior-Badland complex, 0 to 25 percent slopesOeE33242580946cyjlsd60620111:24000
Cedarpass-Interior, frequently flooded-Badland complex, 0 to 6 percent slopesU125B261825828902kqh8sd60620111:24000
Interior loamIn23722580912cyhhsd60620111:24000
Orella-Interior, moderately deep, frequently flooded-Badland complex, 0 to 25 percent slopesU565E151525829142kqrssd60620111:24000
Interior loam, 0 to 3 percent slopes, occasionally floodedU315A60925829092kqhpsd60620111:24000
Interior, moderately deep, occasionally flooded-Cedarpass complex, 0 to 6 percent slopesU340B28225829292qqtrsd60620111:24000
Badland-Denby-Interior complex, 0 to 90 percent slopesBa5783233336462zj55sd61019651:20000
Interior silt loam, 0 to 3 percent slopesLm115702925511cv63sd61019651:20000
Interior loam, channeled, 0 to 6 percent slopes, floodedIo956425810282t34wsd61120111:24000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesIv935825826302t34xsd61120111:24000
Interior-Cedarpass-Badland complex, 0 to 6 percent slopesIsB66522581029cy2vsd61120111:24000
Interior loamIn37452581027cy2ssd61120111:24000
Cedarpass-Interior, frequently flooded-Badland complex, 0 to 6 percent slopesU125B152825828652kqh8sd61120111:24000
Interior loam, 0 to 3 percent slopes, occasionally floodedU315A81125828702kqhpsd61120111:24000
Orella-Interior, moderately deep, frequently flooded-Badland complex, 0 to 25 percent slopesU565E8925828742kqrssd61120111:24000
Interior, moderately deep, occasionally flooded-Cedarpass complex, 0 to 6 percent slopesU340B3825828822qqtrsd61120111:24000
Cedarpass-Interior, frequently flooded-Badland complex, 0 to 6 percent slopesU125B2131023751042kqh8sd61220111:20000
Orella-Interior, moderately deep, frequently flooded-Badland complex, 0 to 25 percent slopesU565E1924023753682kqrssd61220111:20000
Interior loam, channeled, 0 to 6 percent slopes, floodedU325B1002123751182t34wsd61220111:20000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesU335B614623751202t34xsd61220111:20000
Interior, moderately deep, occasionally flooded-Cedarpass complex, 0 to 6 percent slopesU340B465125526302qqtrsd61220111:20000
Interior loam, 0 to 3 percent slopes, occasionally floodedU315A57923751172kqhpsd61220111:20000
Interior-Riverwash complex, 0 to 6 percent slopes, frequently floodedU235B49424852542pf3hsd61220111:20000
Interior, poorly drained-Interior, frequently flooded-Epping, moist complex, 0 to 9 percent slopesU342C7725526312qqtmsd61220111:20000
Badland-Denby-Interior complex, 0 to 90 percent slopesBa4751133336472zj55sd61320111:24000
Interior silt loam, 0 to 3 percent slopesLm244952582716cv3ysd61320111:24000
Interior loam, channeled, 0 to 6 percent slopes, floodedU325B1097225828232t34wsd61320111:24000
Cedarpass-Interior, frequently flooded-Badland complex, 0 to 6 percent slopesU125B150325828122kqh8sd61320111:24000
Interior, moderately deep, occasionally flooded-Cedarpass complex, 0 to 6 percent slopesU340B103925828402qqtrsd61320111:24000
Orella-Interior, moderately deep, frequently flooded-Badland complex, 0 to 25 percent slopesU565E82725828432kqrssd61320111:24000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesU335B26525828242t34xsd61320111:24000
Interior-Riverwash complex, 0 to 6 percent slopes, frequently floodedU235B22725828262pf3hsd61320111:24000
Interior loam, 0 to 3 percent slopes, occasionally floodedU315A6225828222kqhpsd61320111:24000
Interior, poorly drained-Interior, frequently flooded-Epping, moist complex, 0 to 9 percent slopesU342C1925828412qqtmsd61320111:24000

Map of Series Extent

Approximate geographic distribution of the INTERIOR 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 .