Official Series Description


Lab Data Summary

Aggregate lab data for the PLAINBO soil series. This aggregation is based on all pedons with a current taxon name of PLAINBO, 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 PLAINBO 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
10590P0647S1989WI005008Plainbo4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2238884,-91.7549973
10590P0648S1989WI005009Plainbo4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2144432,-91.8847198

Water Balance

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with PLAINBO, 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. WI-2010-11-08-01 | Barron County - 2001

    Typical pattern of soils and parent material in the Arland-Hayriver-Freeon association (Soil Survey of Barron County, Wisconsin; 2001).

Map Units

Map units containing PLAINBO 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
Plainbo-Rock outcrop complex, 12 to 40 percent slopes1070D367396541f9mnmn02519901:15840
Plainbo loamy sand, 6 to 12 percent slopesPdC539431326ggtrwi00519931:20000
Plainbo loamy sand, 2 to 6 percent slopesPdB358431325ggtqwi00519931:20000
Plainbo loamy sand, 12 to 20 percent slopesPdD229431327ggtswi00519931:20000
Plainbo sand, 2 to 6 percent slopes3636B47449256h2h4wi01320041:12000
Plainbo sand, 6 to 12 percent slopes3636C12449257h2h5wi01320041:12000
Plainbo loamy sand, 6 to 12 percent slopesPdC2871421568g4nzwi01719851:15840
Plainbo loamy sand, 12 to 20 percent slopesPdD2801421569g4p0wi01719851:15840
Plainbo loamy sand, 2 to 6 percent slopesPdB1134421567g4nywi01719851:15840
Plainbo sand, sand sheet, 0 to 6 percent slopes573B11612518527h6wxwi03320031:15840
Plainbo sand, sand sheet, 6 to 15 percent slopes573C8282518528h6wywi03320031:15840
Boone-Plainbo complex, 12 to 45 percent slopesBoE7031421751g4vwwi03519741:15840
Plainbo loamy sand, 6 to 12 percent slopes, erodedPdC24129421823g4y6wi03519741:15840
Boone-Plainbo complex, 6 to 12 percent slopesBoC3116421750g4vvwi03519741:15840
Plainbo loamy sand, 2 to 6 percent slopesPdB2966421822g4y5wi03519741:15840
Boone-Plainbo complex, 2 to 6 percent slopesBoB1215421749g4vtwi03519741:15840
Plainbo sand, 2 to 6 percent slopes3636B324276932mh6pwi09519781:15840
Plainbo loamy sand, 2 to 6 percent slopesPbB795426542g9vfwi09719721:20000
Plainbo sand, 2 to 12 percent slopesPbB2629426479g9sdwi14119711:20000
Plainbo sand, 12 to 30 percent slopesPbD204426480g9sfwi14119711:20000

Map of Series Extent

Approximate geographic distribution of the PLAINBO 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 .