Official Series Description


Lab Data Summary

Aggregate lab data for the HOUDEK soil series. This aggregation is based on all pedons with a current taxon name of HOUDEK, 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 HOUDEK 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
55C40A2355S1951SD059003HOUDEK6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6450005,-98.9274979
55C40A2399S1951SD059005Houdek6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.583889,-98.9075012
55C40A2400S1951SD059007Houdek6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.625,-98.8602753

Water Balance

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

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

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Soil series sharing subgroup-level classification with HOUDEK, 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. SD-2010-11-01-17 | Spink County - 2009

    Pattern of soils and underlying materials in the Hand-Ethan-Bonilla and Northville-Farmsworth-Durrstein associations (Soil Survey of Spink County, South Dakota; 2009).

  2. SD-2012-03-15-15 | Davison County - January 1974

    Typical pattern of Houdek and Stickney soils in association 3 and of Houdek, Prosper, and Tetonka in association 4 (Soil Survey of Davison County, SD; 1974).

  3. SD-2012-03-15-16 | Davison County - January 1974

    Typical pattern of soils in associations 5 and 7 near the James River and Firesteel Creek (Soil Survey of Davison County, SD; 1974).

  4. SD-2012-03-15-43 | Hand County - April 1963

    A typical cross section of the northeastern part of Hand County (Soil Survey of Hand County, SD; 1963).

  5. SD-2012-03-15-58 | Jerauld County - September 1994

    Pattern of soils and parent material in the Clarno-Ethan-Prosper association (Soil Survey of Jerauld County, SD; 1994).

  6. SD-2012-03-15-67 | Lake County - December 1973

    Relationship of soils to topography and the underlying materials in the Houdek-Prosper association (Soil Survey of Lake County, SD; 1973).

  7. SD-2012-03-15-78 | Miner County - December 1984

    Pattern of soils and parent material in the Houdek-Dudley-Stickney association (Soil Survey of Miner County, SD; 1984).

  8. SD-2012-03-15-84 | Moody County - April 1989

    Pattern of soils and parent material in the Kranzburg-Houdek association (Soil Survey of Moody County, SD; 1989).

  9. SD-2012-03-15-86 | Moody County - April 1989

    Pattern of soils and parent material in the Dempster-Flandreau-Lamo association (Soil Survey of Moody County, SD; 1989).

Map Units

Map units containing HOUDEK 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
Houdek-Dudley complex, 0 to 2 percent slopesHdA1044233548512wbpwsd00319791:20000
Houdek-Ethan loams, 2 to 6 percent slopesHeB479413548532tlbmsd00319791:20000
Houdek-Prosper loams, 0 to 2 percent slopesHpA374363548582tlbgsd00319791:20000
Houdek-Dudley complex, 2 to 6 percent slopesHdB186973548522wbpxsd00319791:20000
Houdek-Ethan loams, 6 to 9 percent slopesHeC158273548542wkqksd00319791:20000
Houdek-Hoven complex, 0 to 3 percent slopesHhA56483548552yyh4sd00319791:20000
Houdek-Hoven complex, 0 to 6 percent slopesHhB45653548562yyh5sd00319791:20000
Houdek-Plankinton complex, 0 to 6 percent slopesHoB12063548572yyh6sd00319791:20000
Houdek-Prosper loams, 1 to 6 percent slopesHoB1499633545872tlbksd00519761:20000
Houdek-Prosper loams, 0 to 2 percent slopesHoA871243545862tlbgsd00519761:20000
Houdek-Ethan loams, 6 to 9 percent slopesHeC132653545852wkqksd00519761:20000
Houdek-Dudley complex, 2 to 6 percent slopesHdB59723545832wbpxsd00519761:20000
Houdek stony loam, 0 to 9 percent slopesHcB33343545822yyh7sd00519761:20000
Houdek-Ethan loams, 2 to 6 percent slopesHeB11203545842tlbmsd00519761:20000
Houdek loam, 0 to 2 percent slopesHuA11363550392tlb5sd02319801:20000
Houdek loam, 2 to 6 percent slopesHuB9683550402tlb6sd02319801:20000
Houdek-Stickney complex, 0 to 2 percent slopesHsA39204177442wkp9sd02519921:20000
Houdek-Stickney-Tetonka complex, 0 to 2 percent slopesHt33474177462wkpcsd02519921:20000
Houdek-Prosper loams, 0 to 2 percent slopesHpA28614177422tlbgsd02519921:20000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHnB16584177402tlb9sd02519921:20000
Houdek-Prosper loams, 1 to 6 percent slopesHpB14064177432tlbksd02519921:20000
Houdek-Stickney complex, 2 to 6 percent slopesHsB5484177452wkpbsd02519921:20000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHnC594177412tlbbsd02519921:20000
Houdek-Prosper loams, 0 to 2 percent slopesHkA667743529242tlbgsd03519661:20000
Houdek-Stickney complex, 0 to 2 percent slopesHsA339363529262wkp9sd03519661:20000
Houdek-Stickney complex, 0 to 2 percent slopesCsA67273548852wkp9sd04319791:20000
Houdek-Dudley complex, 2 to 6 percent slopesMnB79563551812wbpxsd04919811:20000
Houdek-Dudley complex, 0 to 2 percent slopesWpA40813552052wbpwsd04919811:20000
Houdek-Prosper loams, 0 to 2 percent slopesHkA9633628627492tlbgsd05919591:20000
Houdek-Prosper loams, 1 to 6 percent slopesHkB916953526182tlbksd05919591:20000
Houdek loam, 2 to 6 percent slopesHhB328133526152tlb6sd05919591:20000
Houdek-Dudley complex, 0 to 2 percent slopesHlA297793526192wbpwsd05919591:20000
Houdek-Dudley complex, 2 to 6 percent slopesHlB166883526202wbpxsd05919591:20000
Houdek-Ethan loams, 6 to 9 percent slopesHuD146213526272wkqksd05919591:20000
Ethan-Houdek loams, hillyZhD50193527042yyhjsd05919591:20000
Houdek loam, 0 to 2 percent slopesHhA39933526142tlb5sd05919591:20000
Houdek loam, 6 to 9 percent slopesHhC31603526162tlb7sd05919591:20000
Houdek-Jerauld complex, undulatingHmB11263526222yyh8sd05919591:20000
Ethan-Houdek loams, hillyZaD10433527032yyhhsd05919591:20000
Jerauld-Houdek complex, undulatingMhB9103526492yyhdsd05919591:20000
Houdek-Talmo complex, hillyHsD7503526252yyhcsd05919591:20000
Houdek-Delmont loams, rollingHsC3433526242yyhbsd05919591:20000
Houdek-Delmont loams, undulatingHsB33526232yyh9sd05919591:20000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHwB310433564462tlb9sd07319871:20000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHwC279293564472tlbbsd07319871:20000
Houdek-Dudley complex, 0 to 2 percent slopesHrA104573564442wbpwsd07319871:20000
Houdek-Prosper loams, 0 to 2 percent slopesHyA65443564482tlbgsd07319871:20000
Houdek-Dudley-Jerauld complex, 2 to 6 percent slopesHtB12593564452yyhfsd07319871:20000
Houdek-Stickney complex, 0 to 2 percent slopesHsA415924174892wkp9sd07719921:20000
Houdek-Stickney-Tetonka complex, 0 to 2 percent slopesHt204344174912wkpcsd07719921:20000
Houdek-Stickney complex, 2 to 6 percent slopesHsB78234174902wkpbsd07719921:20000
Houdek-Prosper loams, 1 to 6 percent slopesHpB17354174882tlbksd07719921:20000
Houdek-Prosper loams, 0 to 2 percent slopesHpA1404174872tlbgsd07719921:20000
Houdek-Prosper loams, 0 to 2 percent slopesHpA45574165042tlbgsd07919671:20000
Houdek loam, 2 to 6 percent slopesHkB18234165032tlb6sd07919671:20000
Houdek-Stickney-Tetonka complex, 0 to 2 percent slopesCnA425633553902wkpcsd09719831:20000
Houdek-Dudley-Tetonka complex, 0 to 6 percent slopesHgB312923554042yyhgsd09719831:20000
Houdek-Dudley complex, 0 to 2 percent slopesHdA192993554012wbpwsd09719831:20000
Houdek-Dudley complex, 2 to 6 percent slopesHdB107693554022wbpxsd09719831:20000
Shindler-Houdek clay loams, 15 to 40 percent slopesSdE2736446074gz5hsd09919951:24000
Houdek-Shindler clay loams, 6 to 9 percent slopesHsC2240446050gz4qsd09919951:24000
Houdek clay loam, 2 to 6 percent slopesHoB1060446049gz4psd09919951:24000
Houdek-Talmo complex, 9 to 15 percent slopesHtD947446052gz4ssd09919951:24000
Houdek-Shindler clay loams, 9 to 15 percent slopesHsD831446051gz4rsd09919951:24000
Houdek clay loam, 2 to 6 percent slopesHoB16285418335g19psd10119851:20000
Houdek-Shindler clay loams, 6 to 25 percent slopesHsD4895418337g19rsd10119851:20000
Houdek-Shindler clay loams, 5 to 9 percent slopesHsC4411418336g19qsd10119851:20000
Shindler-Houdek clay loams, 15 to 40 percent slopesShE2156418353g1b8sd10119851:20000
Houdek-Talmo complex, 6 to 40 percent slopesHtD1286418338g19ssd10119851:20000
Houdek clay loam, 0 to 2 percent slopesHoA976418334g19nsd10119851:20000
Houdek-Stickney complex, 0 to 2 percent slopesHfA223993547962wkp9sd11119781:20000
Houdek-Dudley complex, 2 to 6 percent slopesHcB94013547922wbpxsd11119781:20000
Houdek-Prosper loams, 0 to 2 percent slopesHeA68723547942tlbgsd11119781:20000
Houdek-Prosper loams, 1 to 6 percent slopesHeB54963547952tlbksd11119781:20000
Houdek-Ethan loams, 2 to 6 percent slopesHdB49293547932tlbmsd11119781:20000
Houdek-Stickney complex, 0 to 2 percent slopesHwA144933566592wkp9sd11519971:24000
Houdek-Stickney-Tetonka complex, 0 to 2 percent slopesHxA88723566602wkpcsd11519971:24000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHtB52103566552tlb9sd11519971:24000
Houdek-Prosper loams, 0 to 2 percent slopesHuA5223566572tlbgsd11519971:24000
Houdek-Prosper loams, 1 to 6 percent slopesHuB3373566582tlbksd11519971:24000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHtC523566562tlbbsd11519971:24000
Houdek-Stickney complex, 0 to 2 percent slopesCsA44574179482wkp9sd60219751:20000

Map of Series Extent

Approximate geographic distribution of the HOUDEK 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 .