Official Series Description


Lab Data Summary

Aggregate lab data for the BISCAY soil series. This aggregation is based on all pedons with a current taxon name of BISCAY, 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 BISCAY 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
103UMN1122S1970MN0471122Biscay3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.542038,-93.5473099
103UMN3303S1980MN015001(3303)Biscay2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1475983,-94.8793869
103UMN3474S1981MN015002 (3474)Biscay3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2413788,-94.6551361
103UMN3460S1981MN1273460Biscay3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4919891,-95.3029327
103UMN4363S1990MN085805 (4363)Biscay2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.936039,-94.4108124
104X45-259-1S1965IA089915Biscay1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.32646,-92.53757
91AUMN1590S1972MN1451590Biscay3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4575577,-95.0402679
91AUMN2038S1975MN1452038Biscay2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7444115,-95.0894547

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BISCAY, 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. IA-2010-09-02-10 | Emmet County - 1997

    Typical pattern of soils and parent material in the Millington-Spillville-Colo association (Soil Survey of Emmet County, Iowa; 1997).

  2. IA-2011-05-31-31 | Greene County - 1985

    Pattern of soils and parent material in the Mayer-Biscay-Coland association (Soil Survey of Greene County, Iowa; 1985).

  3. IA-2011-05-31-32 | Greene County - 1985

    Pattern of soils and parent material in the Clarion-Coland-Storden association (Soil Survey of Greene County, Iowa; 1985).

  4. IA-2011-05-31-39 | Hancock, County - 1989

    Typical pattern of soils and parent material in the Fieldon-Harcot-Ridgeport association (Soil Survey of Hancock County, Iowa; 1989).

  5. IA-2011-05-31-40 | Hancock, County - 1989

    Typical pattern of soils and parent material in the Truman-Estherville-Webster association (Soil Survey of Hancock County, Iowa; 1989).

  6. IA-2011-06-01-29 | Osceola County - 1988

    Typical pattern of soils and parent material in the Wadena-Coland- Cylinder association (Soil Survey of Osceola County, Iowa; 1988).

  7. IA-2011-06-01-33 | Pocahontas County - 1985

    Typical pattern of soils and parent material in the Havelock-Coland-Estherville association (Soil Survey of Pocahontas County, Iowa; 1985).

Map Units

Map units containing BISCAY 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
Biscay clay loam, 0 to 2 percent slopes259111725502522tsjcia01519771:15840
Biscay clay loam, 0 to 2 percent slopes2599024032862tsjcia02119731:15840
Biscay clay loam, 0 to 2 percent slopes2597304034682tsjcia02519791:15840
Biscay clay loam, 0 to 2 percent slopes2594764035242tsjcia02719791:15840
Biscay clay loam, 0 to 2 percent slopes25980203993182tsjcia04120021:12000
Biscay clay loam, depressional, 0 to 1 percent slopes12597943992722tsjbia04120021:12000
Biscay clay loam, 0 to 2 percent slopes25923594045872tsjcia04919801:15840
Biscay clay loam, 0 to 2 percent slopes25978824953222tsjcia05920111:12000
Talcot-Biscay complex, 0 to 2 percent slopes55713024812252p8xjia05920111:12000
Biscay clay loam, 0 to 2 percent slopes2595634055422tsjcia06319891:15840
Biscay clay loam, 0 to 2 percent slopes25923104062142tsjcia07319831:15840
Biscay clay loam, 0 to 2 percent slopes2598344064742tsjcia07919841:15840
Biscay clay loam, 0 to 2 percent slopes25936264065402tsjcia08119871:15840
Biscay clay loam, depressional, 0 to 1 percent slopes125912554065202tsjbia08119871:15840
Biscay clay loam, 0 to 2 percent slopes25914694475332tsjcia09119981:12000
Biscay clay loam, 0 to 2 percent slopes25918984083572tsjcia10919801:15840
Biscay clay loam, deep, 0 to 2 percent slopes259377409083fqp7ia11919731:15840
Biscay clay loam, 32 to 40 inches to sand and gravel, 0 to 2 percent slopes259684410062frptia14119771:15840
Biscay clay loam, 0 to 2 percent slopes259145725065722tsjcia14319851:15840
Talcot-Biscay complex, 0 to 2 percent slopes5579925065652q4mbia14319851:15840
Biscay clay loam, 0 to 2 percent slopes25944804102682tsjcia14719731:15840
Biscay clay loam, 0 to 2 percent slopes25929884103832tsjcia15119821:15840
Biscay clay loam, 0 to 2 percent slopes25927764128822tsjcia15319931:12000
Biscay clay loam, 0 to 2 percent slopes2598164107842tsjcia16119751:15840
Biscay loam, 32 to 40 inches to sand and gravel, 0 to 2 percent259545411201fswkia16719871:15840
Biscay clay loam, 0 to 2 percent slopes25911104113052tsjcia16919811:15840
Biscay clay loam, loamy substratum, 0 to 2 percent slopes27891116513551sfcjia18720061:12000
Biscay clay loam, 0 to 2 percent slopes2596297979412tsjcia18720061:12000
Biscay clay loam, depressional, 0 to 1 percent slopes125912916123012tsjbia18720061:12000
Biscay clay loam, 0 to 2 percent slopes25933974126752tsjcia19719881:15840
Biscay clay loam, 0 to 2 percent slopesBY15263963992tsjcmn01919871:12000
Biscay clay loam, 0 to 2 percent slopesL6A157224216092tsjcmn03320081:12000
Biscay clay loam, loamy substratum, 0 to 2 percent slopesL230A68817206911vrj5mn03320081:12000
Biscay clay loam, depressional, 0 to 1 percent slopesL7A3217276022tsjbmn03320081:12000
Biscay clay loam, 0 to 2 percent slopes3924243971162tsjcmn04319891:20000
Biscay clay loam, 0 to 2 percent slopes39261523978602tsjcmn04719771:15840
Biscay clay loam, 0 to 2 percent slopesL6A4654516242tsjcmn05320011:12000
Medo, Dassel and Biscay soils, ponded, 0 to 1 percent slopesL31A246451580301v5mn05320011:12000
Biscay clay loam, depressional, 0 to 1 percent slopesL7A734516232tsjbmn05320011:12000
Biscay clay loam, 0 to 2 percent slopes39212483985102tsjcmn06319841:20000
Biscay clay loam, depressional, 0 to 1 percent slopes39934523986882tsjbmn06719831:20000
Biscay-Palms complex19081286398678fcvlmn06719831:20000
Biscay loam3921176398687fcvwmn06719831:20000
Biscay clay loam, 0 to 2 percent slopesL6A64128350772tsjcmn06719831:20000
Biscay clay loam, 0 to 2 percent slopes39210723989562tsjcmn07919861:20000
Biscay clay loam, 0 to 2 percent slopes39217803991682tsjcmn08519931:20000
Biscay clay loam, 0 to 2 percent slopes39213994000502tsjcmn09119851:20000
Mayer-Biscay, depressional complex, 0 to 2 percent slopes10974861436177gmw7mn09319961:20000
Medo, Dassel and Biscay soils, ponded, 0 to 1 percent slopes14064386436235301v5mn09319961:20000
Biscay clay loam, 0 to 2 percent slopes109834394361782tsjcmn09319961:20000
Biscay clay loam, depressional, 0 to 1 percent slopes3993514363652tsjbmn09319961:20000
Biscay clay loam, 0 to 2 percent slopes39297018594472tsjcmn10120081:12000
Biscay silty clay loam, 0 to 2 percent slopes, occasionally floodedP3A716526111sgp1mn10120081:12000
Biscay silty clay loam, 0 to 2 percent slopes, occasionally floodedP3A5533630076p4n1mn10520041:12000
Biscay clay loam, 0 to 2 percent slopesL6A3438064552tsjcmn10520041:12000
Biscay clay loam, 0 to 2 percent slopes392167023740352tsjcmn12720081:12000
Biscay clay loam, depressional, 0 to 1 percent slopes399155623740362tsjbmn12720081:12000
Biscay clay loam, 0 to 2 percent slopes39212324360932tsjcmn12919951:20000
Biscay clay loam, 0 to 2 percent slopes39216384296552tsjcmn13119961:12000
Biscay silty clay loam, 0 to 2 percent slopes, occasionally floodedP3A251432702gj84mn13320021:12000
Webster-Biscay complex1093661431514gh0tmn14319911:20000
Biscay loam3924292428132gchqmn14519801:15840
Biscay loam, depressional3991574428133gchrmn14519801:15840
Biscay clay loam, 0 to 2 percent slopesL6A31828350782tsjcmn14519801:15840
Biscay clay loam, 0 to 2 percent slopesBc34754281962tsjcmn14719671:20000
Biscay clay loam, depressional, 0 to 1 percent slopesBd10054281972tsjbmn14719671:20000
Biscay silty clay loamBe1064428316gcpnmn14919661:15840
Biscay silty clay loam, depressionalBf760428317gcppmn14919661:15840
Biscay clay loam, 0 to 2 percent slopes3922944289472tsjcmn16519871:20000
Biscay clay loam, 0 to 2 percent slopes3929424337322tsjcmn17119981:12000
Medo, Dassel and Biscay soils, ponded, 0 to 1 percent slopes1406274435064301v5mn17119981:12000

Map of Series Extent

Approximate geographic distribution of the BISCAY 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 .