Official Series Description


Lab Data Summary

Aggregate lab data for the GOSPORT soil series. This aggregation is based on all pedons with a current taxon name of GOSPORT, 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 GOSPORT 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
10606N0844S2006KS103108Gosport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2999992,-95.0884705
108B77IL0730161977IL073016Gosport1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1561693,-89.9773584
109M88041321988MO041032Gosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6970778,-92.6536917
109M88041331988MO041033Gosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7001667,-92.8780833
109M89175061989MO175006Gosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9162472,-93.9829222
109M90117171990MO117017mGosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6325,-93.6163889
10995P0835S1995IA179001GOSPORT8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0255737,-92.6001816
11384IL1210751984IL121075Gosport2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5167583,-88.7338111
11385IL1210041985IL121004Gosport2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4821028,-88.7677167
115BM88121171988MO121017Gosport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88121271988MO121027Gosport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88121291988MO121029Gosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM03115022003MO115002Gosport4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115C81IL0090171981IL009017Gosport2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0791132,-90.8636471
n/a77IL0950861977IL095086Gosport2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a78IL1190411978IL119041Gosport1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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 GOSPORT 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 GOSPORT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the GOSPORT 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 GOSPORT, 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-2010-09-09-23 | Webster County - 2008

    Typical pattern of soils and parent material in the Lester-Coland-Wadena association (Soil Survey of Webster County, Iowa; 2008).

  2. IA-2011-06-01-16 | Lucas County - 1999

    Relationship of the major soils in Lucas County to parent material and to position on the landscape (Soil Survey of Lucas County, Iowa; 1999).

  3. IL-2010-09-01-68 | Schuyler County - 2003

    Typical pattern of soils and underlying material in the Hickory-Rozetta-Gosport association (Soil Survey of Schuyler County, Illinois; 2003).

  4. IL-2011-06-01-05 | Brown County - 1988

    Typical pattern of soils and parent material in the Hickory-Rozetta-Gosport association (Soil Survey of Brown County, Illinois; 1988).

  5. IL-2011-06-01-06 | Brown County - 1988

    Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

  6. KS-2012-01-20-04 | Atchison County - February 1984

    Typical pattern of soils in the Knox-Armster-Gosport association (Soil Survey of Atchison County, Kansas; 1984).

  7. MO-2012-02-06-14 | Buchanan County - September 1989

    Pattern of soils and parent material in the Knox association (Soil Survey of Buchanan County, Missouri; September 1989).

Map Units

Map units containing GOSPORT 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
Sogn-Gosport-Clanton complex, 9 to 18 percent slopes, moderately eroded413D21160402683fj0sia00719701:15840
Gosport-Clanton silt loams, 14 to 18 percent slopes, moderately eroded complex313E2744402676fj0kia00719701:15840
Gosport-Clanton silt loams, 9 to 14 percent slopes, moderately eroded complex313D2736402675fj0jia00719701:15840
Gosport-Clanton silt loams, 18 to 24 percent slopes, moderately eroded complex313F2243402677fj0lia00719701:15840
Gosport silt loam, 18 to 30 percent slopes, moderately eroded313F21315406377fmvyia07719681:15840
Gosport silt loam, 9 to 18 percent slopes, moderately eroded313E2310406376fmvxia07719681:15840
Clanton-Gosport silt loams, 18 to 25 percent slopes, moderately eroded322F22429409174fqs5ia12119681:15840
Clanton-Gosport silt loams, 25 to 40 percent slopes, moderately eroded322G21301409175fqs6ia12119681:15840
Clanton-Gosport silt loams, 14 to 18 percent slopes, moderately eroded322E2499409173fqs4ia12119681:15840
Gosport silt loam, 18 to 25 percent slopes313F318409201fqt1ia12119681:15840
Clanton-Gosport silt loams, 9 to 14 percent slopes, moderately eroded322D2220409172fqs3ia12119681:15840
Gosport silt loam, 14 to 18 percent slopes313E218409200fqt0ia12119681:15840
Gosport-Emeline-Ridgeton complex, 25 to 75 percent slopes413G230116123221r3rdia18720061:12000
Hickory-Gosport complex, 15 to 30 percent slopes967F35721738935tygil00519811:12000
Hickory-Gosport complex, 18 to 35 percent slopes967F1623210920028ssqil02519931:12000
Hickory-Gosport complex, 30 to 60 percent slopes967G351748795vz8il03519921:15840
Gosport loam, 35 to 50 percent slopes551G590843571x9szil04519971:12000
Gosport silt loam, 18 to 35 percent slopes551F130843570x9syil04519971:12000
Hickory-Gosport silt loams, 18 to 35 percent slopes967F581615864441q7tmil07920051:12000
Gosport silty clay loam, 4 to 7 percent slopes, eroded551C2371767445xxfil10119521:42240
Gosport silty clay loam, 7 to 12 percent slopes, severely eroded551D3141767455xxgil10119521:42240
Hickory-Gosport silt loams, 18 to 35 percent slopes967F5821989806p1qil11920011:12000
Hickory-Gosport silt loams, 18 to 35 percent slopes967F33752027383261ngil12120081:12000
Gosport silt loam, 10 to 18 percent slopes, eroded551D210622027525261t1il12120081:12000
Gosport silt loam, 18 to 35 percent slopes551F3242027527261t3il12120081:12000
Gosport silt loam, 35 to 60 percent slopes551G1352027526261t2il12120081:12000
Gosport shaly silt loam, 50 to 70 percent slopesGpG6321604385cyfin16519771:20000
Gosport channery silt loam, 25 to 40 percent slopesGoF4721631155gqsin17119871:15840
Gosport silty clay loam, 25 to 45 percent slopes7951638714753921lj89ks00519981:24000
Knox-Gosport complex, 10 to 30 percent slopes7959573914753951lj8dks00519981:24000
Gosport-Sogn complex, 7 to 35 percent slopes72508035186236420hy8ks10319731:24000
Gosport complex, 10 to 30 percent slopes79503971186241420hzwks10319731:24000
Knox-Gosport complex, 10 to 30 percent slopes7959243186242020j02ks10319731:24000
Gosport silty clay loam, 25 to 45 percent slopes795166186241520hzxks10319731:24000
Gosport-Sogn complex, 7 to 35 percent slopes72506487186225220htnks20919731:24000
Gosport complex, 10 to 30 percent slopes795074186230220hw8ks20919731:24000
Gosport silty clay loam, 15 to 45 percent slopes10155488425282522ql0xmo02119841:24000
Gosport-Gasconade complex, 20 to 45 percent slopes101603435913532znlsmo02119841:24000
Gosport silty clay loam, 14 to 30 percent slopes3007316825311702qnqwmo02519671:24000
Gosport silt loam, 14 to 35 percent slopes300729525311672qnqvmo02519671:24000
Gosport silty clay loam, 9 to 14 percent slopes300759225311802qnqymo02519671:24000
Gosport silt loam, 5 to 30 percent slopes50025313885961yqxdmo02719861:24000
Gosport silty clay loam, 9 to 14 percent slopes300751375225311822qnqymo03319881:24000
Gosport silty clay loam, 14 to 30 percent slopes300731028025311712qnqwmo03319881:24000
Gosport silty clay loam, 5 to 9 percent slopes30074228225311762qnqxmo03319881:24000
Gosport silt loam, 14 to 35 percent slopes30072180925311662qnqvmo03319881:24000
Gosport silty clay loam, 14 to 30 percent slopes30073660625311732qnqwmo04119921:24000
Gosport silty clay loam, 9 to 14 percent slopes, eroded30076427525311862qnqzmo04119921:24000
Gosport silty clay loam, 15 to 45 percent slopes101556425282512ql0xmo04919811:24000
Gosport-Gasconade complex, 14 to 30 percent slopes300718825311642qnqtmo06119521:24000
Gosport-Gasconade complex, 14 to 30 percent slopes30071278025311652qnqtmo06319741:24000
Gosport silty clay loam, 5 to 9 percent slopes300742125311772qnqxmo10319731:24000
Gosport silty clay loam, 9 to 35 percent slopes, eroded30077229225311882qnr0mo11519871:24000
Gosport silty clay loam, 14 to 30 percent slopes3007322425311722qnqwmo11519871:24000
Gosport silty clay loam, 9 to 14 percent slopes, eroded300761425311852qnqzmo11519871:24000
Gosport silt loam, 14 to 35 percent slopes30072992825311682qnqvmo11719961:24000
Gosport silty clay loam, 9 to 14 percent slopes3007521425311812qnqymo11719961:24000
Gosport loam, 14 to 20 percent slopes, eroded601113063888558ytm5mo12119911:24000
Gosport silty clay loam, 9 to 35 percent slopes, eroded3007734625311872qnr0mo12119911:24000
Gosport silt loam, 14 to 30 percent slopes, eroded500246125326712qnzbmo12119911:24000
Gosport silty clay loam, 14 to 30 percent slopes300732125311742qnqwmo12119911:24000
Gosport silty clay loam, 9 to 14 percent slopes30075279125311842qnqymo12719821:24000
Gosport silty clay loam, 14 to 20 percent slopes50026176625326742qnzcmo12719821:24000
Gosport silty clay loam, 14 to 20 percent slopes50026245525326752qnzcmo13719731:24000
Gosport silty clay loam, 9 to 14 percent slopes30075192025311832qnqymo13719731:24000
Gosport silty clay loam, 5 to 9 percent slopes30074128325311782qnqxmo13719731:24000
Gosport silt loam, 14 to 30 percent slopes, eroded500246825326702qnzbmo13719731:24000
Gosport silty clay loam, 14 to 20 percent slopes50026215725326732qnzcmo17319821:24000
Gosport silty clay loam, 9 to 14 percent slopes30075159525311792qnqymo17319821:24000
Gosport silt loam, 14 to 30 percent slopes, eroded500242844725326722qnzbmo17519861:24000
Reger-Gosport complex, 14 to 35 percent slopes601977372888604ytnnmo17519861:24000
Gosport silty clay loam, 14 to 30 percent slopes3007328225311692qnqwmo17519861:24000
Gosport silty clay loam, 5 to 9 percent slopes300742225311752qnqxmo20519731:24000
Gosport silty clay loam, 25 to 70 percent slopesGoF44452868169mg4oh08519761:15840

Map of Series Extent

Approximate geographic distribution of the GOSPORT 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 .