Official Series Description


Lab Data Summary

Aggregate lab data for the BAYARD soil series. This aggregation is based on all pedons with a current taxon name of BAYARD, 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 BAYARD 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
67A40A2057S1961NE157004Bayard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7221985,-103.871666
n/a40A2056S1961NE157003Bayard6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BAYARD 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 BAYARD 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 BAYARD 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 BAYARD 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 BAYARD 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 BAYARD 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 BAYARD 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 BAYARD, 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. KS-2012-01-23-13 | Grant County - December 1969

    Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).

  2. KS-2012-01-23-16 | Grant County - December 1969

    Relationships of soils in association 5 (Soil Survey of Grant County, Kansas; 1969).

  3. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

  4. KS-2012-01-25-34 | Scott County - December 1965

    An approximate geologic profile extending in an east-west direction across Scott County near Shallow Water (Soil Survey of Scott County, Kansas; 1965).

  5. KS-2012-01-26-30 | Wichita County - November 1965

    Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).

  6. NE-2010-09-09-04 | Garden County - 1999

    Typical pattern of the soils and underlying material in the Gothenburg, Lewellen-Jankosh, and Bayard-Scoville-Rushcreek associations (Soil Survey of Garden County, Nebraska; 1999).

  7. NE-2012-02-08-02 | Banner County - October 1994

    Typical pattern of soils and parent material in the Tassel-Busher-Rock outcrop association (Soil Survey of Banner County, Nebraska; October 1994).

  8. NE-2012-02-08-03 | Banner County - October 1994

    Typical pattern of soils and parent material in the Otero-Bayard-Sarben association (Soil Survey of Banner County, Nebraska; October 1994).

  9. NE-2012-02-08-04 | Banner County - October 1994

    Typical pattern of soils and parent material in the Tripp-Alice association (Soil Survey of Banner County, Nebraska; October 1994).

  10. NE-2012-02-10-29 | Dundy County - February 1963

    The Bridgeport-Havre soil association, on the right, merges with the Sandy alluvial land-Las association (Soil Survey of Dundy County, Nebraska; February 1963).

  11. NE-2012-02-13-44 | Keith County - November 1995

    Typical pattern of soils and parent material in the Bayard-Duroc-Bridget association (Soil Survey of Keith County, Nebraska; November 1995).

  12. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

Map Units

Map units containing BAYARD 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
Bayard fine sandy loam, 2 to 6 percent slopes10869679837qjco06319961:24000
Bayard-Canyon complex, 1 to 9 percent slopes1532469449435b6co07519741:24000
Bayard-Canyon complex, 3 to 5 percent slopesBcC5159477035m3co09519711:20000
Bayard-Ascalon-Manter sandy loams, 5 to 12 percent slopesBaE91729491935rxco11519691:15840
Bayard-Canyon complex, 5 to 12 percent slopesBcE71149492035ryco11519691:15840
Bayard fine sandy loam, 2 to 6 percent slopes7117539509535ylco12519761:24000
Las-Bayard sandy loams, occasionally flooded12342161115231517p2gks05519621:24000
Bayard fine sandy loam, 0 to 3 percent slopes132786811522992w5f1ks05519621:24000
Bayard fine sandy loam, 0 to 3 percent slopes1327334513806482w5f1ks06719651:24000
Bayard fine sandy loam, 0 to 1 percent slopes1326149311522072w5dyks07519591:24000
Bayard fine sandy loam, 0 to 3 percent slopes13278813806142w5f1ks08119651:24000
Bayard fine sandy loam, 0 to 1 percent slopes132698611522522w5dyks09319611:24000
Bayard fine sandy loam, 0 to 3 percent slopes1327164413826212w5f1ks17519631:24000
Bayard very fine sandy loam, 1 to 3 percent slopes13071538316924582wz97ne00719881:20000
Bayard very fine sandy loam, 3 to 6 percent slopes13081273516924591tt4gne00719881:20000
Bayard-Dix complex, 9 to 20 percent slopes13161080516924631tt4lne00719881:20000
Bayard-Dix complex, 3 to 9 percent slopes1315776316924621tt4kne00719881:20000
Bayard very fine sandy loam, 6 to 9 percent slopes1309413516924601tt4hne00719881:20000
Bayard very fine sandy loam, 9 to 20 percent slopes1310285516924611tt4jne00719881:20000
Bayard fine sandy loam, 0 to 3 percent slopes132711922281382w5dzne00719881:20000
Bayard fine sandy loam, 3 to 6 percent slopes13014222281372dskdne00719881:20000
Canyon-Bayard complex, 6 to 20 percent slopes51553103316986721v0lwne03319891:20000
Bayard fine sandy loam, 0 to 3 percent slopes13271314522196752w5dzne03319891:20000
Bayard fine sandy loam, 3 to 6 percent slopes13011094416986601v0lhne03319891:20000
Bayard fine sandy loam, 0 to 1 percent slopes1326496116986582w5dyne03319891:20000
Bayard fine sandy loam, 6 to 9 percent slopes1302441116986611v0ljne03319891:20000
Bayard fine sandy loam, 9 to 20 percent slopes1303112116986621v0lkne03319891:20000
Chappell-Bayard-Broadwater complex, 0 to 2 percent slopes13728122196772dhrhne03319891:20000
Vetal and Bayard soils, 1 to 6 percent slopes507012294358176d0q2ne04519731:20000
Bayard fine sandy loam, 0 to 3 percent slopes1327479416987252w5dzne06919951:20000
Bayard fine sandy loam, 0 to 1 percent slopes1326264116987242w5dyne06919951:20000
Bayard loam, 0 to 1 percent slopes1305158516987281v0npne06919951:20000
Bayard fine sandy loam, 3 to 6 percent slopes1301148816987261v0nmne06919951:20000
Bayard very fine sandy loam, 1 to 3 percent slopes130726116987272wz96ne06919951:20000
Bayard fine sandy loam, 0 to 3 percent slopes1327106016992872w5dzne08719651:20000
Bayard fine sandy loam, 0 to 1 percent slopes132662816992862w5dyne08719651:20000
Bayard loam, 0 to 1 percent slopes130540516992931v17xne08719651:20000
Bayard very fine sandy loam, 1 to 3 percent slopes13072121816988742wz96ne10119901:20000
Bayard fine sandy loam, 0 to 3 percent slopes13271422195892w5dzne10119901:20000
Bayard fine sandy loam, 0 to 3 percent slopes13272159616925362w5dzne10520041:24000
Chappell-Bayard-Broadwater complex, 0 to 2 percent slopes13721094916925401tt72ne10520041:24000
Bayard fine sandy loam, 3 to 6 percent slopes1301458316925371tt6zne10520041:24000
Bayard very fine sandy loam, 1 to 3 percent slopes13072122279232wz97ne10520041:24000
Bayard fine sandy loam, 0 to 1 percent slopes1326622279302w5dyne10520041:24000
Bayard very fine sandy loam, 1 to 3 percent slopes1307117922197222wz96ne11119711:24000
Bayard fine sandy loam, 0 to 3 percent slopes132720122203552w5dzne12319811:20000
Bayard-Dix complex, 9 to 20 percent slopes13168622203782djh3ne12319811:20000
Bayard very fine sandy loam, 6 to 9 percent slopes13091922203772djh2ne12319811:20000
Otero-Bayard fine sandy loams, 0 to 3 percent slopes17121674916537731shwjne15719651:20000
Bayard fine sandy loam, 3 to 6 percent slopes1301634716537191shtsne15719651:20000
Bayard fine sandy loam, 6 to 9 percent slopes1302497716537201shttne15719651:20000
Otero-Bayard fine sandy loams, 3 to 6 percent slopes1713436916537741shwkne15719651:20000
Dix-Bayard complex, 6 to 20 percent slopes1575342816537331shv7ne15719651:20000
Bayard fine sandy loam, 9 to 20 percent slopes1303308516537211shtvne15719651:20000
Otero-Bayard fine sandy loams, 6 to 9 percent slopes1714253516537751shwlne15719651:20000
Bayard very fine sandy loam, 6 to 9 percent slopes1309158522276382ds19ne15719651:20000
Bayard very fine sandy loam, 3 to 6 percent slopes1308123922276372ds18ne15719651:20000
Bayard fine sandy loam, 0 to 3 percent slopes132777516537182w5dzne15719651:20000
Blueridge-Bayard complex, 6 to 20 percent slopes592844622276742ds2gne15719651:20000
Bayard very fine sandy loam, 1 to 3 percent slopes130734322276362wz97ne15719651:20000
Bayard very fine sandy loam, 9 to 20 percent slopes13108222276392ds1bne15719651:20000
Bayard-Dix complex, 3 to 9 percent slopes13151022276402ds1cne15719651:20000
Blueridge-Bayard complex, 6 to 20 percent slopes592812421357877d0dfne16519931:20000
Bayard fine sandy loam, 0 to 3 percent slopes132754923578612w5dzne16519931:20000
Bayard fine sandy loam, 3 to 6 percent slopes13014094357862d0cyne16519931:20000
Bayard fine sandy loam, 0 to 1 percent slopes13261373578602w5dyne16519931:20000
Bayard fine sandy loam, 0 to 3 percent slopes10817583495292w5dzwy02719931:24000
Alice-Bayard fine sandy loams, 0 to 6 percent slopes103220291044453hp6wy03119981:24000
Graystone-Greenhope-Bayard fine sandy loams, 0 to 10 percent slopes164146991045193hrlwy03119981:24000
Bayard-Phiferson-Treon, thin solum complex, 3 to 45 percent slopes109133191044583hpmwy03119981:24000
Bayard-Phiferson-Treon, thin solum complex, 0 to 6 percent slopes10888391044563hpkwy03119981:24000
Cedak-Bayard-Treon, thin solum, complex, 0 to 6 percent slopes12420721044813hqcwy03119981:24000
Bayard fine sandy loam, 0 to 3 percent slopes10615831044532w5dzwy03119981:24000
Featherlegs-Bayard fine sandy loams, 0 to 6 percent slopes15014101045053hr4wy03119981:24000
Bayard fine sandy loam, 0 to 15 percent slopes107411044233hnhwy03119981:24000
Bayard fine sandy loam, 0 to 7 percent slopesBgB56191046673hxcwy61519651:20000
Bayard and Otero fine sandy loams, 0 to 3 percent slopesBoA30481046683hxdwy61519651:20000
Bayard and Otero fine sandy loams, 3 to 6 percent slopesBoB6791046693hxfwy61519651:20000
Bayard fine sandy loam, 0 to 3 percent slopes11180341047992w5dzwy62119801:24000
Bayard fine sandy loam, 3 to 6 percent slopes1280261048003j1nwy62119801:24000
Bayard variant fine sandy loam, 0 to 3 percent slopes1438791048023j1qwy62119801:24000
Bayard fine sandy loam, 6 to 10 percent slopes1322801048013j1pwy62119801:24000
Bayard fine sandy loam, wet, 0 to 3 percent slopes55821047653j0jwy62119801:24000
Bayard fine sandy loam, 0 to 15 percent slopes59631047703j0pwy62119801:24000
Featherlegs-Bayard fine sandy loams, 0 to 6 percent slopes434914148131jh74wy71519741:20000
Blueridge-Bayard complex, 6 to 20 percent slopes952514153811jhtgwy71519741:20000
Bayard-Paoli fine sandy loams, 0 to 10 percent slopes10770641049083j54wy72119941:24000
Bayard fine sandy loam, 0 to 15 percent slopes10532661049063j52wy72119941:24000
Treon, dry-Bayard association, 3 to 30 percent slopes17518591049763j7bwy72119941:24000
Bayard fine sandy loam, wet, 0 to 3 percent slopes1067831049073j53wy72119941:24000
Urban land-Bayard complex, 0 to 15 percent slopes1851131049863j7nwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the BAYARD 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 .