Official Series Description


Lab Data Summary

Aggregate lab data for the ENTERPRISE soil series. This aggregation is based on all pedons with a current taxon name of ENTERPRISE, 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 ENTERPRISE 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
78C68-OK-22-5168-OK043-22-51Enterprise3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9555111,-99.0428694
78C94P071894OK059011Enterprise7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.689167,-99.4872208

Water Balance

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

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 ENTERPRISE, 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. OK-2012-02-16-21 | Cotton County - December 1963

    Typical pattern of Pratt, Tivoli, and associated soils (Soil Survey of Cotton County, Oklahoma; December 1963).

  2. OK-2012-02-16-25 | Dewey County - December 1963

    Typical pattern of the dominant soils in association 3 (Soil Survey of Dewey County, Oklahoma; December 1963).

  3. OK-2012-02-16-26 | Dewey County - December 1963

    Typical pattern of the soils in association 4 (Soil Survey of Dewey County, Oklahoma; December 1963).

  4. OK-2012-02-16-27 | Dewey County - December 1963

    Typical pattern of most of the soils in association 5 (Soil Survey of Dewey County, Oklahoma; December 1963).

  5. OK-2012-02-16-28 | Ellis County - April 1966

    Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

  6. OK-2012-02-16-37 | Greer County - March 1967

    Major soils in soil associations 3, 7, and 9, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

  7. OK-2012-02-16-52 | Jackson County - June 1961

    Typical pattern of Miles, Enterprise, Tivoli, and associated soil (Soil Survey of Jackson County, Oklahoma; June 1961).

  8. OK-2012-02-17-40 | Roger Mills County - August 1963

    Typical pattern of soils in associations 3, 4, and 5 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  9. TX-2010-11-05-04 | Young County - 2009

    Pattern of soils and underlying material in the Grandfield-Gowen and Lincoln-Westola-Padgett general soil map units (Soil Survey of Young County, Texas; 2009).

  10. TX-2012-03-20-20 | Childress County - July 1963

    Soils developed in eolian materials (Soil Survey of Childress County, TX; 1963).

  11. TX-2012-03-22-09 | Wilbarger County - September 1962

    Block diagram showing the geographical association of the soils on the low terraces along the Pease River. Sandy alluvial land and Yahola very fine sandy loam, which formed in recent alluvium, are in soil association 6. Miles fine sandy loam, which is in soil association 3; Enterprise very fine sandy loam; and Tipton silt loam formed in sandy outwash that has been reworked by wind in some places (Soil Survey of Wilbarger County, TX; 1962).

Map Units

Map units containing ENTERPRISE 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
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB72563823692t6qtok04319611:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA45953823682t6qsok04319611:24000
Enterprise very fine sandy loam, 8 to 20 percent slopesEnE61393824312t6qxok04519631:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB49503824282t6qtok04519631:24000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC48343824292t6qvok04519631:24000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD19773824302t6qwok04519631:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB24623847352t6qtok12919611:24000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD23663847372t6qwok12919611:24000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC13633847362t6qvok12919611:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA13483847342t6qsok12919611:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB94773627062t6qttx02319711:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA49113627052t6qstx02319711:24000
Enterprise loam, 3 to 8 percent slopesEnD12061363277d60mtx04519721:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEmB29773638172wrvqtx07519611:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEmC18613638182wrvstx07519611:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEmA13083638162t6qztx07519611:20000
Enterprise very fine sandy loam, 5 to 8 percent slopesEmD480363819d6l3tx07519611:20000
Enterprise very fine sandy loam, 1 to 3 percent slopes1925203638702t6qttx07719771:24000
Enterprise very fine sandy loam, 8 to 20 percent slopes2217703638742t6qxtx07719771:24000
Enterprise very fine sandy loam, 0 to 1 percent slopes1815053638692t6qstx07719771:24000
Enterprise very fine sandy loam, 5 to 8 percent slopes219173638732t6qwtx07719771:24000
Enterprise very fine sandy loam, 3 to 5 percent slopes206033638722t6qvtx07719771:24000
Yahola frequently flooded and Enterprise soils, 0 to 20 percent slopesYCD2204364052d6tmtx08319681:24000
Enterprise very fine sandy loam, 5 to 12 percent slopesEnD25873641022wrvttx08719651:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB7803641002wrvqtx08719651:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC3973641012wrvstx08719651:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB18443645872wrvqtx10119691:20000
Enterprise very fine sandy loam, 5 to 12 percent slopesEnD12053645892wrvttx10119691:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC9273645882wrvstx10119691:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA5443645862t6qztx10119691:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC4163651182wrvstx12519651:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB3943651172wrvqtx12519651:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC14313657892wrvstx15119641:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB11933657882wrvqtx15119641:24000
Enterprise very fine sandy loam, 5 to 12 percent slopesEnD9213657902wrvttx15119641:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA1773657872t6qztx15119641:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA98631561412t6qstx15520211:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB75431561432t6qttx15520211:24000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC19631561452t6qvtx15520211:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEmB113253669362wrvqtx19119651:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEmA62063669352t6qztx19119651:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEmC57773669372wrvstx19119651:20000
Enterprise very fine sandy loam, 5 to 12 percent slopesEmD37773669382wrvttx19119651:20000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD4968367563dbgwtx21119671:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC2627367562dbgvtx21119671:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA1902367560dbgstx21119671:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB1286367561dbgttx21119671:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB6523684802wrvqtx26319681:31680
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB59133685832wrvqtx26919991:31680
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC11143685842wrvstx26919991:31680
Enterprise very fine sandy loam, 0 to 1 percent slopes1184123687112t6qstx27519751:24000
Enterprise very fine sandy loam, 1 to 3 percent slopes1228743687122t6qttx27519751:24000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD4824370815dfvstx34119681:24000
Aspermont-Enterprise association, undulatingAPD57053124204dgcytx37519741:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB27063722712wrvqtx43319701:24000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC23223722722wrvstx43319701:24000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA22523722702t6qztx43319701:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB21053726852t6qttx44719911:24000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB102993733492t6qttx48519721:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA67953733482t6qstx48519721:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC22493733502t6qvtx48519721:20000
Enterprise very fine sandy loam, 8 to 20 percent slopesEnE18253733522t6qxtx48519721:20000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD7813733512t6qwtx48519721:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB87873734172t6qttx48719601:20000
Enterprise very fine sandy loam, 0 to 1 percent slopesEnA74013734162t6qstx48719601:20000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC16063734182t6qvtx48719601:20000
Enterprise very fine sandy loam, 5 to 8 percent slopesEnD7753734192t6qwtx48719601:20000
Enterprise very fine sandy loam, 1 to 3 percent slopesEnB36473737482t6qttx50320031:24000
Enterprise very fine sandy loam, 3 to 5 percent slopesEnC33243737492t6qvtx50320031:24000

Map of Series Extent

Approximate geographic distribution of the ENTERPRISE 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 .