Official Series Description


Lab Data Summary

Aggregate lab data for the CRESBARD soil series. This aggregation is based on all pedons with a current taxon name of CRESBARD, 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 CRESBARD 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
53A40A002858ND101003Cresbard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6697222,-102.1594444
53A40A002958ND101004Cresbard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6502778,-102.1363889
55A89P028288ND013055Cresbard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8230247497559,-102.06111907959
55A89P029688ND013063Cresbard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8166351318359,-102.07056427002
55A89P028888ND013064Cresbard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8371925354004,-102.039726257324
55A40A0027S1949ND075007Cresbard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7055556,-101.8388889
55A76ND009001S1976ND009001Cresbard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7405556,-100.2902778
55A97P0369S1996ND005001Cresbard8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3055267,-99.5361099
55B09N0932S2009ND039004Cresbard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6148056,-98.2387778
55C40A2366S1950SD059004Cresbard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7435875,-98.8459625
55C40A2367S1951SD059001Cresbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.602478,-98.9281921
55C40A2368S1951SD059004Cresbard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6446991,-98.9281921

Water Balance

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

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

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Competing Series

Soil series competing with CRESBARD 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 CRESBARD 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 CRESBARD 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 hills figure.

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 CRESBARD, 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. ND-2010-09-27-04 | Burke County - 2003

    Typical pattern of soils and parent material in the Barnes-Cresbard association (Soil Survey of Burke County, North Dakota; 2003).

  2. ND-2012-02-07-20 | Cavalier County - May 1990

    Typical pattern of soils and parent material in the Svea-Hamerly-Cresbard association (Soil Survey of Cavalier County, North Dakota; May 1990).

  3. ND-2012-02-07-22 | Dickey County - May 1993

    Typical pattern of soils and parent material in the Barnes-Svea-Hamerly association (Soil Survey of Dickey County, North Dakota; May 1993).

  4. ND-2012-02-08-38 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Hamerly-Svea-Tonka association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  5. ND-2012-02-08-39 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Svea-Buse-Parnell association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  6. ND-2012-02-08-40 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Cresbard-Svea association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  7. ND-2012-02-08-45 | Ramsey County - August 1986

    Typical pattern of soils and underlying material in the Hamerly-Cresbard-Svea association (Soil Survey of Ramsey County, North Dakota; August 1986).

  8. SD-2010-11-01-14 | Spink County - 2009

    Pattern of soils and underlying materials in the Nahon-Aberdeen-Exline and Max-Arnegard-Zahl associations (Soil Survey of Spink County, South Dakota; 2009).

  9. SD-2010-11-01-15 | Spink County - 2009

    Pattern of soils and underlying materials in the Forman-Cresbard-Cavour association (Soil Survey of Spink County, South Dakota; 2009).

  10. SD-2012-03-14-10 | Brown County - April 1993

    Typical pattern of soils and parent material in the Barnes-Svea association (Soil Survey of Brown County, SD; 1993).

  11. 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).

Map Units

Map units containing CRESBARD 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
Svea-Cresbard loams, 0 to 3 percent slopesG122A1925735922q3vrnd00319881:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A524725877352q4gfnd0051:12000
Hamerly-Cresbard loams, 0 to 3 percent slopesF135A339725877082q4gmnd0051:12000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B282425877532q4ggnd0051:12000
Balaton-Cresbard loams, 3 to 6 percent slopesF135B203425877512q4gnnd0051:12000
Svea-Cresbard loams, 0 to 3 percent slopesG122A33425736892q3vrnd0051:12000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A17025737402pwzdnd0051:12000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B3925736952pwzbnd0051:12000
Svea-Cresbard loams, 0 to 3 percent slopesF122A2174825860352q4gfnd00919811:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B426125860522q4ggnd00919811:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A499825858542q4gfnd01319911:24000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A31425751652pwzfnd01719831:20000
Hamerly-Cresbard loams, 0 to 3 percent slopesF135A5205925875242q4gmnd01919871:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A4504625875202q4gfnd01919871:20000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A3005925875222q4ghnd01919871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B1945025875212q4ggnd01919871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1800725752562pwzbnd02119891:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A1047125752802q3vrnd02119891:20000
Cresbard-Cavour loams, 3 to 6 percent slopesG124B4125752852q4nsnd02119891:20000
Aastad-Cresbard loams, 0 to 3 percent slopesG137A1925060122pwz9nd02119891:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A1025752572pwzdnd02119891:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A20525754202q3vrnd0271:12000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A6325753972pwzdnd0271:12000
Svea-Cresbard loams, 0 to 3 percent slopesG122A75025763912q3vrnd03119901:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A34125763742pwzfnd03119901:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B10625763732pwzbnd03119901:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A1808725765072pwzdnd03519801:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1156125764872pwzbnd03519801:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A1027225764862q3vrnd03519801:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A11725765472pwzfnd03519801:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B10525874862q4ggnd03519801:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A525874812q4gfnd03519801:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A661025765822q3vrnd03919911:24000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A400025765602pwzfnd03919911:24000
Svea-Cresbard loams, 0 to 3 percent slopesG122A2108625770442q3vrnd04519661:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1561825770182pwzbnd04519661:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A177825770192pwzdnd04519661:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A103725770202pwzfnd04519661:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A2534425713422q3vrnd04919871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1864025713242pwzbnd04919871:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A803225713262pwzfnd04919871:20000
Forman-Cresbard loams, west, 0 to 3 percent slopesG662A275925714012q5w0nd04919871:20000
Forman-Cresbard loams, west, 3 to 6 percent slopesG662B138225714022q5w1nd04919871:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A23825857522q4gfnd04919871:20000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A15225855902q4ghnd04919871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B11625857712q4ggnd04919871:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A725713252pwzdnd04919871:20000
Forman-Cresbard loams, west, 0 to 3 percent slopesG662A50925771722q5w0nd05519741:20000
Forman-Cresbard loams, west, 3 to 6 percent slopesG662B5225772012q5w1nd05519741:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A1238425772662q3vrnd0631:12000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B846325772412pwzbnd0631:12000
Svea-Cresbard loams, 0 to 3 percent slopesF122A343025873642q4gfnd0631:12000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A312825772432pwzfnd0631:12000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B275725873762q4ggnd0631:12000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A77225873142q4ghnd0631:12000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A48725772422pwzdnd0631:12000
Svea-Cresbard loams, 0 to 3 percent slopesF122A378025872712q4gfnd06919751:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A12425822642q3vrnd06919751:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1625822492pwzbnd06919751:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B325872822q4ggnd06919751:20000
Hamerly-Cresbard loams, 0 to 3 percent slopesF135A7527825870942q4gmnd07119841:12000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B873925870932q4ggnd07119841:12000
Svea-Cresbard loams, 0 to 3 percent slopesF122A736225870922q4gfnd07119841:12000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A5225811142pwzdnd07319921:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B125811132pwzbnd07319921:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A174525854452q4gfnd07519721:20000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A25425853382q4ghnd07519721:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A673625881792q4gfnd07919901:24000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B184625881952q4ggnd07919901:24000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A179525880122q4ghnd07919901:24000
Cavour-Cresbard loams, 3 to 6 pecent slopesF125B96525881632q4gjnd07919901:24000
Aastad-Cresbard loams, 0 to 3 percent slopesG137A99225795402pwz9nd08119591:12000
Svea-Cresbard loams, 0 to 3 percent slopesG122A3025794422q3vrnd08119591:12000
Svea-Cresbard loams, 0 to 3 percent slopesG122A112625819462q3vrnd08319901:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A55925819292pwzdnd08319901:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B39925819282pwzbnd08319901:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A18025819302pwzfnd08319901:20000
Cresbard-Cavour loams, 3 to 6 percent slopesG124B14325819632q4nsnd08319901:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A437425797322q3vrnd09119911:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A95325797152pwzfnd09119911:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A3725797142pwzdnd09119911:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A1610125813452q3vrnd09319901:24000
Hamerly-Cresbard loams, 0 to 3 percent slopesG135A1077425813532q4nvnd09319901:24000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B619925813242pwzbnd09319901:24000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A370725813252pwzdnd09319901:24000
Hamerly-Cresbard loams, 0 to 3 percent slopesF135A306525870452q4gmnd09519921:24000
Svea-Cresbard loams, 0 to 3 percent slopesF122A2444325861152q4gfnd09919671:20000
Hamerly-Cresbard loams, 0 to 3 percent slopesF135A251725861172q4gmnd09919671:20000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A16625861162q4ghnd09919671:20000
Svea-Cresbard loams, 0 to 3 percent slopesF122A38825852612q4gfnd10119671:20000
Forman-Cresbard loams, west, 0 to 3 percent slopesG662A35525060012q5w0nd10119671:20000
Cavour-Cresbard loams, 0 to 3 percent slopesF125A23625851202q4ghnd10119671:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A15025734922pwzfnd10119671:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A19425795882pwzdnd10319661:12000
Svea-Cresbard loams, 0 to 3 percent slopesG122A1925796082q3vrnd10319661:12000
Barnes-Cresbard-Tonka complex, 0 to 6 percent slopesG131B2796627977202sd0ssd01319871:20000
Barnes-Cresbard-Tonka complex, 0 to 3 percent slopesG131A2397727977192sd0rsd01319871:20000
Cresbard-Cavour-Forman loams, 0 to 6 percent slopesG141B1669427977262sd13sd01319871:20000
Cresbard-Cavour-Ferney loams, 0 to 3 percent slopesG130A669827977182sd0qsd01319871:20000
Forman-Cresbard loams, 3 to 6 percent slopesG139B346127977252sd10sd01319871:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A279527656272pwzdsd01319871:20000
Cavour-Cresbard loams, 0 to 3 percent slopesG125A261227656282pwzfsd01319871:20000
Forman-Cresbard loams, 0 to 3 percent slopesG139A137927977242sd0zsd01319871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B17827656262pwzbsd01319871:20000
Forman-Cresbard-Tonka complex, 0 to 3 percent slopesG136A11527977232sd0wsd01319871:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A8627976502q3vrsd01319871:20000
Cresbard-Cavour loams, 3 to 6 percent slopesG124B6627976562q4nssd01319871:20000
Cresbard-Cavour-Heil complex, 0 to 3 percent slopesG126A5427977162q5cxsd01319871:20000
Kranzburg-Cresbard silt loams, 0 to 2 percent slopesG796A327978232sd62sd01319871:20000
Forman-Cresbard loams, 0 to 3 percent slopesG139A776327979912sd0zsd02519921:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A412627979592pwzdsd02519921:20000
Forman-Cresbard-Tonka complex, 0 to 3 percent slopesG136A270827979902sd0wsd02519921:20000
Forman-Cresbard loams, 3 to 6 percent slopesG139B181027979922sd10sd02519921:20000
Peever-Cresbard-Tonka complex, 0 to 3 percent slopesG203A166927980072sd1zsd02519921:20000
Forman-Cresbard-Tonka complexFt110417732g0p7sd02519921:20000
Cresbard-Cavour-Heil complex, 0 to 3 percent slopesG126A9227979892q5cxsd02519921:20000
Forman-Cresbard loams, 2 to 6 percent slopesFoB15417731g0p6sd02519921:20000
Kranzburg-Cresbard complex, 0 to 2 percent slopesJ145A122816844491tjt2sd02920061:12000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A125527984372pwzdsd03719921:20000
Kranzburg-Cresbard silt loams, 0 to 2 percent slopesG796A17227985292sd62sd03719921:20000
Cresbard-Cavour loams, 3 to 6 percent slopesG124B467227988002q4nssd08919801:20000
Cresbard-Cavour-Ferney loams, 0 to 3 percent slopesG130A411927988292sd0qsd08919801:20000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A152127987932pwzdsd08919801:20000
Forman-Cresbard loams, 0 to 3 percent slopesG139A100127992312sd0zsd08919801:20000
Svea-Cresbard loams, 0 to 3 percent slopesG122A3027987982q3vrsd08919801:20000
Cresbard-Cavour-Forman loams, 0 to 6 percent slopesG141B1727992322sd13sd08919801:20000
Kranzburg-Cresbard silt loams, 0 to 2 percent slopesG796A241327993822sd62sd09119701:20000
Kranzburg-Cresbard silt loams, 2 to 6 percent slopesG796B43127993832sd63sd09119701:20000
Forman-Cresbard loams, 0 to 3 percent slopesG139A3566727995722sd0zsd11519971:24000
Cresbard-Cavour-Heil complex, 0 to 3 percent slopesG126A1851727995692q5cxsd11519971:24000
Kranzburg-Cresbard silt loams, 0 to 2 percent slopesG796A1429628000392sd62sd11519971:24000
Cresbard-Cavour loams, 0 to 3 percent slopesG124A1186127995322pwzdsd11519971:24000
Forman-Cresbard loams, 3 to 6 percent slopesG139B828827995732sd10sd11519971:24000
Forman-Cresbard-Tonka complex, 0 to 3 percent slopesG136A607927995712sd0wsd11519971:24000
Kranzburg-Cresbard-Tonka silt loams, 0 to 2 percent slopesG797A177228000412sd64sd11519971:24000
Peever-Cresbard-Tonka complex, 0 to 3 percent slopesG203A51727995872sd1zsd11519971:24000
Kranzburg-Cresbard silt loams, 2 to 6 percent slopesG796B3828000402sd63sd11519971:24000

Map of Series Extent

Approximate geographic distribution of the CRESBARD 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 .