Official Series Description


Lab Data Summary

Aggregate lab data for the COTACO soil series. This aggregation is based on all pedons with a current taxon name of COTACO, 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 COTACO 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
12578KY-121-00378KY-121-003Cotaco4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8558617,-83.7910309
130B01P004300TN009001Cotaco7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5934347,-83.839065

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COTACO 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 COTACO 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 COTACO 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 COTACO 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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Competing Series

Soil series competing with COTACO 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 COTACO 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 COTACO 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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Soil series sharing subgroup-level classification with COTACO, 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. KY-2010-09-03-17 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topography in the Udorthents-Nelse-Allegheny and Shelocta-Hazleton-Blairton general soil map units. The Udorthents-Nelse-Allegheny general soil map unit is along the Tug and Lavista Forks of the Big Sandy River and their major tributaries, and the Shelocta-Hazleton-Blairton general soil map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  2. KY-2010-09-03-19 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topograhy in the Upshur-Vandalia-Rarden general soil map unit. This map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  3. KY-2012-01-27-58 | Elliott County - 1965

    Diagram of Muskingum-Montevallo-Ramsey association, showing relationship of soil series to topography and parent material (Soil Survey of Elliott County, Kentucky; 1965).

  4. KY-2012-01-31-30 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Allegheny-Huntington-Newark map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  5. KY-2012-01-31-31 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Allegheny-Cotaco-Huntington map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  6. KY-2012-02-01-16 | McCreary-Whitley Area - 1970

    General location of the Atkins, Pope, and Tate soils on flood plains and stream terraces in association 1 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  7. KY-2012-02-01-42 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Westbend general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  8. KY-2012-02-01-43 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Grigsby-Allegheny-Knowlton general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  9. VA-2010-11-05-06 | Buchanan County -

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia).

  10. VA-2010-11-05-15 | Dickenson County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Dickenson County, Virginia; 2009).

  11. VA-2012-05-10-03 | Buchanan County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia; 2009).

  12. VA-2012-05-11-01 | Dickenson County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Dickenson County, Virginia; 2009).

Map Units

Map units containing COTACO 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
Cotaco-Barbourville loamsCl3000329137c1hbal04919531:20000
Barbourville-Cotaco fine sandy loamsBC2711522820kk15al07119431:24000
Cotaco silt loamCt2670330100c2hdal07919501:20000
Cotaco loamCu2983331051c3h2al10319491:15840
Cotaco loam, 2 to 6 percent slopesCoB337817274891vzlgky01120061:12000
Cotaco loam, 6 to 12 percent slopesCoC160017274901vzlhky01120061:12000
Allegheny-Cotaco loams, 6 to 12 percent slopesAgC98717274731vzkyky01120061:12000
Allegheny-Cotaco loams, 2 to 6 percent slopesAgB80017274721vzkxky01120061:12000
Cotaco loamCo4684550240lgkpky04319801:20000
Cotaco loam, rarely floodedCa711552515ljy2ky05119941:24000
Gilpin-Ezel-Cotaco complex, 0 to 6 percent slopesGeB177218846652184nky06320071:12000
Cotaco fine sandy loam, 2 to 6 percent slopes, rarely floodedCtB75118846602184hky06320071:12000
Cotaco loam, 2 to 6 percent slopes, occasionally floodedCoB14918846592184gky06320071:12000
Cotaco loamCo4446550389lgqhky60519751:20000
Cotaco loam, 2 to 8 percent slopesCoB642557756lqd4ky61620041:24000
Allegheny-Cotaco complex, 2 to 6 percent slopesuAnoB192124369302mstnky62719841:20000
Cotaco loam, rarely floodedCo1854552214ljmcky62719841:20000
Cotaco loamCo1563552260ljnvky62819731:20000
Cotaco silt loam28206515418561nrf9ky63019661:15840
Allegheny-Cotaco complex, 2 to 6 percent slopesuAnoB102024551652mstnky63019661:15840
Cotaco silt loam, 2 to 6 percent slopesCoB995550825lh5kky63419891:20000
Allegheny-Cotaco complex, 2 to 6 percent slopesAoB535550819lh5cky63419891:20000
Cotaco silt loam, 0 to 2 percent slopesCoA223550824lh5jky63419891:20000
Cotaco loam, rarely floodedCo534550859lh6nky63919911:24000
Cotaco silt loam, 4 to 12 percent slopes, rarely floodedCoC649550897lh7wky64019961:24000
Cotaco silt loam, 0 to 4 percent slopes, occasionally floodedCtB455550898lh7xky64019961:24000
Cotaco silt loam, 0 to 4 percent slopes, rarely floodedCoB168550896lh7vky64019961:24000
Cotaco silt loam, 4 to 12 percent slopesCmC152550895lh7tky64019961:24000
Cotaco silt loam, 0 to 4 percent slopesCmB49550894lh7sky64019961:24000
Cotaco loam, 1 to 4 percent slopesCoB404550930lh8yky64119941:24000
Cotaco fine sandy loam, neutral variant, 2 to 6 percent slopesCoB25014787571lmrvky64519711:20000
Cotaco silt loam, 0 to 3 percent slopes, rarely floodedCtA90524201722m7d2pa00520121:24000
Cotaco silt loam, 0 to 3 percent slopes, rarely floodedCtA98224201702m7d0pa06320121:24000
Cotaco silt loam, 0 to 3 percent slopes, rarely floodedCtA55524201712m7d1pa06520121:12000
Allegheny-Cotaco complex, occasionally floodedAc322188735521byftn00119781:15840
Cotaco silt loamCo6316526870kp7ttn01119511:20000
Cotaco loamCn1128526869kp7stn01119511:20000
Cotaco fine sandy loamCc794527158kpk3tn05119501:20000
Cotaco and Atkins silt loams (Bonair)Ck3641526244knlmtn11519511:20000
Allegheny-Cotaco complex, occasionally floodedAc451728877sgg5tn14320031:24000
Cotaco loamCo334528404kqv9tn17119801:24000
Allegheny-Cotaco complex, occasionally floodedAc13571530679kt6ptn60720031:24000
Allegheny-Cotaco complex, occasionally floodedAc909224390862mw26tn62920031:24000
Cotaco silty clay loam, 2 to 8 percent slopesCoB221557309lpxqtn64020071:24000
Allegheny-Cotaco fine sandy loams, 1 to 7 percent slopes3B6663517760kcryva01519781:15840
Allegheny-Cotaco cobbly fine sandy loams, 1 to 7 percent slopes4B3928517850kcvvva01519781:15840
Allegheny-Cotaco cobbly fine sandy loams, 7 to 15 percent slopes4C1878517852kcvxva01519781:15840
Allegheny-Cotaco fine sandy loams, 7 to 15 percent slopes3C1341517761kcrzva01519781:15840
Cotaco variant silt loam26876517619kcmdva01519781:15840
Cotaco loam, 8 to 15 percent slopes6C20616708231t2mjva02720061:24000
Cotaco loam, 8 to 15 percent slopes4C37523998562lk7qva05120081:24000
Cotaco loam, 2 to 7 percent slopes10B595516644kblyva07119811:15840
Cotaco loam, 7 to 15 percent slopes10C374516645kblzva07119811:15840
Cotaco loam, 2 to 7 percent slopes11B1898517139kc3xva13919951:20000
Cotaco loam, 2 to 7 percent slopes7B1374521299khg3va15519811:15840
Cotaco loam, 7 to 15 percent slopes7C739521300khg4va15519811:15840
Cotaco loam, 0 to 2 percent slopes7A655521298khg2va15519811:15840
Cotaco loam, 2 to 7 percent slopes9B416520430kgk2va16119901:24000
Cotaco loam, 7 to 15 percent slopes9C63520431kgk3va16119901:24000
Cotaco fine sandy loam, 0 to 7 percent slopes18B2239518365kddgva16519801:20000
Cotaco cobbly fine sandy loam, 0 to 7 percent slopes19B2222518366kddhva16519801:20000
Cotaco variant cobbly loam, 1 to 7 percent slopes20B1658518368kddkva16519801:20000
Ezel-Cotaco, deep fine sandy loams, 3 to 8 percent slopes23B45225085432q7prva19520101:24000
Cotaco loam, 8 to 15 percent slopes19C30625074632q2xzva19520101:24000
Allegheny-Cotaco cobbly fine sandy loams-Urban land complex, 1 to 7 percent slopes504B36930258132xd6mva8201:12000
Allegheny-Cotaco-Urban land complex, 1 to 7 percent slopes503B25130258102xd6kva8201:12000
Allegheny-Cotaco cobbly fine sandy loams, 7 to 15 percent slopes4C10830258142xd5yva8201:12000
Allegheny-Cotaco fine sandy loams, 7 to 15 percent slopes3C5230258112xd5mva8201:12000
Allegheny-Cotaco-Urban land complex, 7 to 15 percent slopes503C3330258092xd6lva8201:12000
Allegheny-Cotaco cobbly fine sandy loams, 1 to 7 percent slopes4B2730257632xd5xva8201:12000
Allegheny-Cotaco fine sandy loams, 1 to 7 percent slopes3B830258122xd5lva8201:12000
Cotaco silt loam, 3 to 8 percent slopesCtB550513644k7h5wv01119841:20000
Cotaco silt loamCo470532301kvx0wv01720011:24000
Cotaco loamCt1077512835k6n2wv03919761:20000
Cotaco loam, 3 to 8 percent slopesCoB285553360lktbwv04320051:24000
Cotaco loam, 0 to 3 percent slopesCoA83553361lktcwv04320051:24000
Cotaco-Urban land complex, 3 to 8 percent slopesCuB54553359lkt9wv04320051:24000
Cotaco-Urban land complex, 8 to 15 percent slopesCuC36553358lkt8wv04320051:24000
Cotaco silt loam, 0 to 3 percent slopes, rarely floodedCkA26117206181vrftwv05120071:12000
Urban land-Cotaco complex, 0 to 3 percent slopesUpA13017206251vrg1wv05120071:12000
Cotaco silt loam, 0 to 3 percent slopesChA4417206241vrg0wv05120071:12000
Cotaco loam, 3 to 8 percent slopesCtB1450515006k8x3wv09919931:24000
Urban land-Kanawha-Cotaco complex, 0 to 8 percent slopesUvB1150515038k8y4wv09919931:24000
Cotaco loam, 0 to 3 percent slopesCtA520515005k8x2wv09919931:24000
Cotaco silt loam, 3 to 8 percent slopesCtB991515112k90jwv10119921:24000
Cotaco silt loam, 3 to 10 percent slopesCoB994514585k8gjwv60119661:15840
Cotaco silt loam, 0 to 3 percent slopesCoA482514584k8ghwv60119661:15840
Cotaco silt loam, 10 to 20 percent slopesCoC253514586k8gkwv60119661:15840
Urban land-Kanawha-Cotaco complex, 0 to 8 percent slopesUtB10115556817sgdwv62020051:24000
Cotaco loam, 3 to 8 percent slopesCtB14924271002mglkwv62220101:12000
Cotaco loam, 3 to 8 percent slopesCtB466424532062nbrpwv70520091:24000
Cotaco silt loam, 3 to 8 percent slopesCtB140825934432qdq9wv76720111:20000

Map of Series Extent

Approximate geographic distribution of the COTACO 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 .