Official Series Description


Lab Data Summary

Aggregate lab data for the BILLETT soil series. This aggregation is based on all pedons with a current taxon name of BILLETT, 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 BILLETT 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
104UMN1966S1975MN1091966Billett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8444519,-92.5836334
105X61775S1978IA061003Billett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4457875,-90.9241157
105X49-775-1S1988IA097003Billett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0807317,-90.3651795
108B79IL1030111979IL103011Billett1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6876983,-89.3780419
111DBE80601980IN007060Billett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6500167,-87.3641056
111DBE81251981IN007025Billett2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.651425,-87.39325
115A69IL1010011969IL101001Billett5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6490503,-87.6484609

Water Balance

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BILLETT, 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-2012-03-23-11 | Juneau County - January 1991

    Typical pattern of soils and parent material in the Ettrick-Curran-Jackson association (Soil Survey of Juneau County, WI; 1991).

  2. WI-2012-03-23-24 | Monroe County - June 1984

    Relationship of soils and parent material in the Billett-Impact map unit (Soil Survey of Monroe County, WI; 1984).

Map Units

Map units containing BILLETT 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
Billett sandy loam, 2 to 5 percent slopes775B709413381fw4wia01320011:12000
Billett sandy loam, 2 to 5 percent slopes775B81615860151q7csia01720081:12000
Billett sandy loam, 0 to 2 percent slopes77546415861721q7jvia01720081:12000
Billett sandy loam, 5 to 9 percent slopes775C40615861711q7jtia01720081:12000
Billett sandy loam, 2 to 5 percent slopes775B352404065fkgcia03719891:15840
Billett sandy loam, 5 to 9 percent slopes775C239404066fkgdia03719891:15840
Billett sandy loam, 5 to 9 percent slopes, moderately eroded775C2353407560fp33ia09719881:15840
Billett sandy loam, 2 to 5 percent slopes775B351407559fp32ia09719881:15840
Billett sandy loam, 5 to 14 percent slopes775D658408205fprxia10519881:15840
Billett sandy loam, 2 to 5 percent slopes775B280408204fprwia10519881:15840
Billett sandy loam, 14 to 20 percent slopes775E118408206fpryia10519881:15840
Billett, loamy substratum-Ladoga, sandy substratum complex, 9 to 14 percent slopes294D841447085h073ia10719981:12000
Billett, loamy substratum-Ladoga, sandy substratum complex, 5 to 9 percent slopes294C691447083h071ia10719981:12000
Ladoga-Billett complex, 5 to 9 percent slopes, moderately eroded294C2479412042ftrpia18319831:15840
Ladoga-Billett complex, 9 to 14 percent slopes, moderately eroded294D2242412043ftrqia18319831:15840
Billett fine sandy loam, 2 to 5 percent slopes775B198816575wdq4ia18720061:12000
Billett fine sandy loam, 5 to 9 percent slopes775C173816574wdq3ia18720061:12000
Billett sandy loam, 2 to 5 percent slopes775B616766666tqs5ia19120051:12000
Billett sandy loam, 5 to 9 percent slopes775C282766667tqs6ia19120051:12000
Billett sandy loam, 9 to 14 percent slopes775D126766668tqs7ia19120051:12000
Billett sandy loam, 2 to 5 percent slopes332B36714071731j78pil00720061:12000
Billett sandy loam, 0 to 2 percent slopes332A881998176pxqil00720061:12000
Billett sandy loam, 0 to 2 percent slopes332A5611767265xwvil10119521:42240
Billett sandy loam, 2 to 4 percent slopes332B2591767275xwwil10119521:42240
Billett fine sandy loam, 2 to 5 percent slopes332B1600926992103lzil10320041:12000
Billett fine sandy loam, 5 to 10 percent slopes, eroded332C2622926993103m0il10320041:12000
Billett fine sandy loam, 0 to 2 percent slopes332A552921351zxr0il10320041:12000
Billett sandy loam, 2 to 5 percent slopes332B219314731941lfzdil20119971:12000
Billett sandy loam, 0 to 2 percent slopes332A5521740415v37il20119971:12000
Billett sandy loam, 2 to 6 percent slopes, erodedBdB213841645325j6hin00719851:15840
Billett loam, 6 to 12 percent slopes, erodedBeC22681645335j6jin00719851:15840
Billett loam, gravelly substratum, 0 to 2 percent slopesBnA34941638655hhzin15719901:15840
Billett fine sandy loam, gravelly substratum, 0 to 2 percent slopesBlA10021638555hhnin15719901:15840
Billett loam, gravelly substratum, 2 to 6 percent slopes, erodedBnB26491638665hj0in15719901:15840
Urban land-Billett, gravelly substratum, complex, 2 to 8 percent slopesUbB4861643395j08in15719901:15840
Oakville-Billett moderately wet, complex, 2 to 6 percent slopes, erodedOaB22671641635htlin15719901:15840
Billett fine sandy loam, moderately wet, 0 to 2 percent slopesBmA1981638585hhrin15719901:15840
Billett fine sandy loam, gravelly substratum, 2 to 6 percent slopes, erodedBlB21781638565hhpin15719901:15840
Billett sandy loam, 1 to 4 percent slopes, erodedBmB28431630905gpzin17119871:15840
Billett sandy loam, 6 to 12 percent slopes, erodedBnC21061630915gq0in17119871:15840
Billett sandy loam, 2 to 6 percent slopesN604B47216701781t1yqmn04920071:12000
Billett fine sandy loam, 0 to 4 percent slopesN627A42016904611tr20mn04920071:12000
Lilah-Billett complex, 12 to 18 percent slopes, moderately erodedN603D228716701771t1ypmn04920071:12000
Billett sandy loam, 6 to 12 percent slopes, moderately erodedN604C227716701791t1yrmn04920071:12000
Lilah-Billett complex, 6 to 12 percent slopes, moderately erodedN603C213016701761t1ynmn04920071:12000
Billett sandy loam, 1 to 6 percent slopes79B341398320fch1mn05519811:15840
Billett sandy loam, 6 to 12 percent slopes79C275398321fch2mn05519811:15840
Billett fine sandy loam, 2 to 6 percent slopes79B2237400484ffqvmn09919861:15840
Billett fine sandy loam, 1 to 6 percent slopes79B868429088gdhkmn16919871:20000
Billett sandy loam, 0 to 3 percent slopesBlA6410422921g62mwi00119781:20000
Billett sandy loam, 2 to 6 percent slopesBlB13434421496g4lnwi01719851:15840
Billett sandy loam, 0 to 2 percent slopesBlA2870421495g4lmwi01719851:15840
Billett sandy loam, moderately well drained, 0 to 3 percent slopesBmA2713421498g4lqwi01719851:15840
Billett sandy loam, 6 to 12 percent slopes, erodedBlC21212421497g4lpwi01719851:15840
Billett sandy loam, 1 to 6 percent slopesBlB9648421745g4vpwi03519741:12000
Billett sandy loam, 6 to 12 percent slopes, erodedBlC23624421746g4vqwi03519741:12000
Billett sandy loam, 12 to 20 percent slopes, erodedBlD21323421747g4vrwi03519741:12000
Billett sandy loam, moderately well drained, 0 to 3 percent slopesBmA1000421748g4vswi03519741:12000
Billett sandy loam, 2 to 6 percent slopes, moderately erodedBlB2877425204g8g8wi04519691:12000
Billett sandy loam, 0 to 2 percent slopesBlA837425203g8g7wi04519691:12000
Billett sandy loam, 6 to 12 percent slopes, moderately erodedBlC2237425205g8g9wi04519691:12000
Billett sandy loam, 0 to 2 percent slopesBt25093426507g9t9wi09719721:20000
Billett sandy loam, 2 to 6 percent slopesBlB1360426275g9ktwi10519701:20000
Billett sandy loam, 0 to 2 percent slopesBlA679426274g9kswi10519701:20000
Billett sandy loam, mottled subsoil variant, 0 to 3 percent slopesBmA555426276g9kvwi10519701:20000
Billett sandy loam, 1 to 6 percent slopesBlB7410423125g696wi11119771:15840
Billett sandy loam, 6 to 12 percent slopes, erodedBlC22009423126g697wi11119771:15840
Billett fine sandy loam, moderately well drained, 0 to 3 percent slopesBmA1945423128g699wi11119771:15840
Billett sandy loam, 12 to 20 percent slopes, erodedBlD2425423127g698wi11119771:15840
Billett sandy loam, 0 to 2 percent slopesBt9252423949g74swi13719861:20000

Map of Series Extent

Approximate geographic distribution of the BILLETT 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 .