Official Series Description


Lab Data Summary

Aggregate lab data for the CATLIN soil series. This aggregation is based on all pedons with a current taxon name of CATLIN, 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 CATLIN 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
108A85P03151984IL039011Catlin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2166672,-88.9000015
108A84IL0390141984IL039014Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.205325,-88.8536917
108A84IL0390351984IL039035Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0795833,-88.9083778
108A84IL0390361984IL039036Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0790333,-88.9072806
108A84IL0390461984IL039046Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2587583,-88.9003611
108A86IL1130021986IL113002Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2851861,-88.9551861
108A86IL1130051986IL113005Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.285175,-88.943025
108A87P02151986IL113053Catlin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4729028,-89.0764111
108A90IL2030261990IL203026Catlin1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8525667,-89.2727972
108A91P02321991IL113010Catlin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5243778,-89.0178056
108A03N0300S2002IL099020Catlin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1998214,-89.0798813
108A13N0529S2012IL115001Catlin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0269611,-89.0199556
11086IL11302086IL-113-020Catlin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6863361,-88.6116972

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CATLIN 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 CATLIN 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 CATLIN 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 CATLIN 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 CATLIN 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 CATLIN 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 CATLIN 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 CATLIN, 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. IL-2010-09-01-41 | Marshall County - 2002

    Typical pattern of soils and parent material in the Flanagan-Graymont-Elpaso association (Soil Survey of Marshall County, Illinois; 2002).

  2. IL-2010-09-01-42 | Marshall County - 2002

    Typical pattern of soils and parent material in the Catlin-Saybrook-Osco association (Soil Survey of Marshall County, Illinois; 2002).

  3. IL-2010-09-01-56 | McLean County - 1998

    Typical pattern of soils and parent material in the Catlin-Ipava-Sable association (Soil Survey of McLean County, Illinois; 1998).

  4. IL-2010-09-01-73 | Stark County - 1996

    Typical pattern of soils and parent material in the Elburn-Plano and Catlin-Flanagan associations (Soil Survey of Stark County, Illinois; 1996).

  5. IL-2010-09-01-82 | Woodford County - 1999

    Typical pattern of soils and parent material in the Saybrook-Catlin-Tama association (Soil Survey of Woodford County, Illinois; 1999).

  6. IL-2011-08-04-06 | De Witt County - 1991

    Typical pattern of soils and parent material in the Catlin-Dana association (Soil Survey of De Witt County, Illinois; 1991).

  7. IL-2011-08-04-07 | De Witt County - 1991

    Typical pattern of soils and parent material in the Sable-Ipava-Catlin association (Soil Survey of De Witt County, Illinois; 1991).

  8. IL-2011-08-04-49 | Lee County - 1985

    Pattern of soils and underlying material in the Tama-Muscatine-Sable association (Soil Survey of Lee County, Illinois; 1985).

  9. IL-2011-08-04-56 | Macon County - 1990

    Typical landscape pattern of soils and parent materials in the Catlin-Dana-Parr association (Soil Survey of Macon County, Illinois; 1990).

  10. IL-2011-08-04-57 | Macon County - 1990

    Typical landscape pattern of soils and parent materials in the Flanagan-Drummer association (Soil Survey of Macon County, Illinois; 1990).

  11. IL-2011-08-04-91 | Putman County - 1992

    Typical pattern of soils and parent material in the Catlin-Flanagan association (Soil Survey of Putnam County, Illinois; 1992).

Map Units

Map units containing CATLIN 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
Catlin silt loam, 2 to 5 percent slopes, eroded171B22546018627032t6zmil01120071:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C2424618627042xcldil01120071:12000
Catlin silt loam, 2 to 5 percent slopes171B12418627022t6zlil01120071:12000
Catlin silt loam, 2 to 5 percent slopes171B174002429662t6zlil01919991:12000
Catlin silt loam, 2 to 5 percent slopes171B358911838862t6zlil03719981:12000
Catlin silt loam, 0 to 2 percent slopes171A78551839212xclcil03719981:12000
Catlin silt loam, 2 to 5 percent slopes, eroded171B2436008693122t6zmil03920051:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C213408693132xcldil03920051:12000
Catlin silt loam, 2 to 5 percent slopes171B96715988772t6zlil03920051:12000
Catlin silt loam, 2 to 5 percent slopes171B24652001922t6zlil04120041:12000
Catlin silt loam, 2 to 5 percent slopes171B5658435532t6zlil04519971:12000
Catlin silt loam, 0 to 2 percent slopes171A15721988072xclcil08920001:12000
Catlin silt loam, 2 to 5 percent slopes171B14671988082t6zlil08920001:12000
Catlin silt loam, 0 to 2 percent slopes171A77617156302xclcil09320071:12000
Catlin silt loam, 2 to 5 percent slopes171B33317156292t6zlil09320071:12000
Flanagan-Catlin silt loams, 0 to 3 percent slopes818A3502914160561jjj7il09920061:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C21408610299272xcldil09920061:12000
Catlin silt loam, 2 to 5 percent slopes171B1027810299262t6zlil09920061:12000
Catlin silt loam, 2 to 5 percent slopes, eroded171B2401013862102t6zmil09920061:12000
Catlin silty clay loam, 5 to 10 percent slopes, severely eroded171C3111914160632xclgil09920061:12000
Catlin silt loam, 0 to 2 percent slopes171A18510299252xclcil09920061:12000
Catlin silt loam, Illinois till plain, 2 to 5 percent slopes171iB311609239472ww9sil10320041:12000
Catlin silt loam, Illinois till plain, 5 to 10 percent slopes, eroded171iC219469213202ww9til10320041:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C2437215960092xcldil10720061:12000
Catlin silt loam, 2 to 5 percent slopes171B124115957412t6zlil10720061:12000
Catlin silt loam, 10 to 18 percent slopes, eroded171D240215960151qkscil10720061:12000
Catlin silt loam, 2 to 5 percent slopes, eroded171B2494581990812t6zmil11320001:12000
Catlin silt loam, 2 to 5 percent slopes171B165081990802t6zlil11320001:12000
Catlin-Saybrook silt loams, 2 to 5 percent slopes893B50461957636kpyil11320001:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C232511990822xcldil11320001:12000
Catlin silt loam, 2 to 5 percent slopes171B2443919139402t6zlil11520071:12000
Catlin silt loam, 2 to 5 percent slopes171B73381820922t6zlil12319971:15840
Catlin silt loam, 2 to 5 percent slopes, eroded171B238381820932t6zmil12319971:15840
Catlin silt loam, 5 to 10 percent slopes, eroded171C233271820942xcldil12319971:15840
Catlin silt loam, 2 to 5 percent slopes, eroded171B213742089642t6zmil14319861:15840
Catlin silt loam, 5 to 10 percent slopes, eroded171C25162089652xcldil14319861:15840
Catlin silt loam, 2 to 5 percent slopes, eroded171B2632319129652t6zmil14720091:12000
Catlin silt loam, 2 to 5 percent slopes171B447019108982t6zlil14720091:12000
Catlin silt loam, 2 to 5 percent slopes171B64121726472t6zlil15519871:15840
Catlin silt loam, 5 to 10 percent slopes, eroded171C217471726502xcldil15519871:15840
Catlin silt loam, 2 to 5 percent slopes171B17221790012t6zlil17319901:15840
Catlin silt loam, 2 to 5 percent slopes171B57451790642t6zlil17519921:15840
Catlin silt loam, 2 to 5 percent slopes, eroded171B2240925423332t6zmil17519921:15840
Catlin silt loam, 5 to 10 percent slopes, eroded171C211611790662xcldil17519921:15840
Catlin silt loam, 5 to 10 percent slopes, eroded171C257231793632xcldil17919911:15840
Catlin silt loam, 2 to 5 percent slopes171B360516010372t6zlil18320061:12000
Catlin silt loam, 2 to 5 percent slopes171B92808691742t6zlil20320081:12000
Catlin silt loam, 5 to 10 percent slopes, eroded171C220038691762xcldil20320081:12000
Catlin silt loam, 2 to 5 percent slopes, eroded171B2548691752t6zmil20320081:12000

Map of Series Extent

Approximate geographic distribution of the CATLIN 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 .