Official Series Description


Lab Data Summary

Aggregate lab data for the FREEON soil series. This aggregation is based on all pedons with a current taxon name of FREEON, 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 FREEON 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
90A85P092885WI119002Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2711105,-90.6650009
90A89P029288WI119002Freeon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1236115,-90.703331
90A89P060588WI119006Freeon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3419456,-90.8036118
90A91P049090WI119004Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0458336,-90.8833313
90A91P049290WI119009Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0455551,-90.8191681
90A91P103591WI069283Freeon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3252792,-89.816391
90A97P0260S1996MN065028Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1088905,-93.1633301
90A97P0273S1996MN065030Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1144447,-93.1586075
90A97P0263S1996MN065034Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9505539,-93.492775
90B40A2020S1947WI005012Freeon4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4172211,-91.644165
90BUMN1722S1973MN1631722Freeon2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9651718,-92.9216995
90BUMN1724S1973MN1631724Freeon3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9745483,-92.9429626
90B40A1759S1974MN163004Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9741592,-92.9399261
90B88P0199S1987WI005001Freeon1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4841652,-91.7672195
90B88P0200S1987WI005002Freeon1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4855537,-91.7672195
90B88P0315S1987WI005007Freeon5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4838905,-91.769722
90B88P0316S1987WI005008Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.4049988,-91.5713882
90B90P0442S1989WI019042Freeon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0155563,-90.7600021
90B91P0146S1990WI005007Freeon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3416672,-91.859726

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FREEON 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 FREEON 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 FREEON 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 FREEON 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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Click the image to view it full size.

Competing Series

Soil series competing with FREEON 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 FREEON 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 FREEON 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 .

Click the image to view it full size.

Click the image to view it full size.

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 FREEON, 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).

  2. WI-2012-03-22-01 | Bayfield County - April 1961

    General soil areas: (1) Red clays and pink sands (Ontonagon, Superior, Orienta, Bibon); (2) Rolling and hilly pink stony sandy loams (Gogebic, Cloquet); (3) Rolling and hilly pink sands (Vilas, Omega, Hiawatha); (4) Nearly level pink sands (Omega, Vilas); (5) Undulating and rolling pink stony silt loams, loams, and sandy loams (Freeon, Gogebic, Cloquet); (6) Undulating pink fine sandy loams (Pence); and (7) Wet soils (Peat) (Soil Survey of Bayfield County, WI; 1961).

Map Units

Map units containing FREEON 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
Freeon silt loam, 2 to 6 percent slopes26410616772222tnymmn12319781:15840
Freeon silt loam, 2 to 6 percent slopes264304416770872tnymmn16319781:15840
Freeon silt loam, 2 to 6 percent slopesFnB720284312982tnymwi00519931:20000
Freeon silt loam, 6 to 12 percent slopesFnC285914312992tnynwi00519931:20000
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes157B34134481982v8dxwi01320041:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes157C17654481992v8dywi01320041:12000
Freeon silt loam, 2 to 6 percent slopesFnB258274215262tnymwi01719851:15840
Freeon silt loam, 6 to 12 percent slopesFnC246494215272tnynwi01719851:15840
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopesFnB31634318692v8dxwi01919941:20000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopesFnC3124318702v8dywi01919941:20000
Freeon silt loam, 2 to 6 percent slopesFoB27754210512tnymwi06719831:20000
Freeon silt loam, 2 to 6 percent slopesFoB192114316172tnymwi06919931:20000
Freeon-Sconsin silt loams, 2 to 6 percent slopesFsB7530431619gh46wi06919931:20000
Freeon silt loam, 6 to 12 percent slopesFoC71894316182tnynwi06919931:20000
Freeon silt loam, 2 to 6 percent slopesFnB327394313682tnymwi07319981:20000
Freeon silt loam, 6 to 12 percent slopesFnC39554313692tnynwi07319981:20000
Freeon silt loam, 2 to 6 percent slopesFnB107394211882tnymwi09519781:15840
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes157B6124870312v8dxwi09519781:15840
Magnor-Freeon complex, 0 to 6 percent slopes, very stony757B303526275702v8dvwi09920061:12000
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes457B200286275112v8dxwi09920061:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes457C63866275122v8dywi09920061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B4026627366p1tmwi09920061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C2743627543p20bwi09920061:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes863B556627581p21kwi09920061:12000
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C43914827561lrxvwi09920061:12000
Freeon, very stony-Cathro complex, 0 to 15 percent slopes441C317639560pghzwi09920061:12000
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes457B444396250662v8dxwi10720061:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes457C124196250672v8dywi10720061:12000
Freeon silt loam, bedrock-controlled ground moraine, 2 to 6 percent slopes, very stony1957B895514803211lpd9wi10720061:12000
Magnor-Freeon complex, 0 to 6 percent slopes, very stony757B87846251022v8dvwi10720061:12000
Freeon silt loam, bedrock-controlled ground moraine, 6 to 15 percent slopes, very stony1957C755014801961lp88wi10720061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B1946625174nzjxwi10720061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C1554625082nzfywi10720061:12000
Freeon-Ribhill complex, 6 to 15 percent slopes, very stony478C1400848607xh1fwi10720061:12000
Freeon silt loam, 2 to 6 percent slopesFnB233494221402tnymwi10919751:15840
Freeon silt loam, heavy substratum, 2 to 6 percent slopesFoB8080422141g58gwi10919751:15840
Freeon silt loam, heavy substratum, 6 to 12 percent slopes, erodedFoC22453422142g58hwi10919751:15840
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes457B314296258202v8dxwi11320061:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes457C243586258212v8dywi11320061:12000
Magnor-Freeon complex, 0 to 6 percent slopes, very stony757B74606267762v8dvwi11320061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B5869625844p07jwi11320061:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C3046625839p07cwi11320061:12000
Freeon, very stony-Cathro complex, 0 to 15 percent slopes441C2479625813p06jwi11320061:12000
Magnor-Freeon complex, 0 to 6 percent slopes, very stony757B378104351372v8dvwi11920021:12000
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes457B242584351342v8dxwi11920021:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes457C129134351352v8dywi11920021:12000
Freeon, very stony-Magnor, very stony-Ossmer complex, 0 to 5 percent slopes9078A4807580404mgyqwi11920021:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes863B4204581189mhs1wi11920021:12000
Crystal Lake-Freeon, very stony-Newot, very stony complex, 10 to 20 percent slopes9087C3337435127glscwi11920021:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B2890435139glsrwi11920021:12000
Crystal Lake-Freeon, very stony-Antigo complex, 6 to 15 percent slopes3863C2388579853mgcywi11920021:12000
Freeon, very stony-Antigo complex, 6 to 15 percent slopes545C2216435136glsnwi11920021:12000
Freeon, very stony and Freeon silt loams, 2 to 6 percent slopes157B75834335622v8dxwi12920021:12000
Freeon, very stony and Freeon silt loams, 6 to 15 percent slopes157C63614353382v8dywi12920021:12000
Freeon, very stony-Cathro complex, 0 to 15 percent slopes441C2320448545h1r6wi12920021:12000

Map of Series Extent

Approximate geographic distribution of the FREEON 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 .