Official Series Description


Lab Data Summary

Aggregate lab data for the CATAULA soil series. This aggregation is based on all pedons with a current taxon name of CATAULA, 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 CATAULA 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
13609N1023S2009SC045001Cataula7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.6552124,-82.2559967

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CATAULA 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 CATAULA 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 CATAULA 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 CATAULA 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 CATAULA 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 CATAULA 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 CATAULA 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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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 CATAULA, 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

No block diagrams are available.

Map Units

Map units containing CATAULA 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
Cataula gravelly sandy loam, rolling phaseCd17243329240c1lnal05119481:20000
Cataula gravelly sandy loam, 0 to 6 percent slopesCb6767329238c1llal05119481:20000
Cataula gravelly sandy loam, hilly phaseCc2733329239c1lmal05119481:20000
Cataula sandy loam, 2 to 6 percent slopesCaB21401018574135x7ga03520031:24000
Cataula-Cecil complex, 6 to 15 percent slopes, moderately erodedCcD21849025804702wq9jga13320111:24000
Cecil-Cataula complex, 10 to 25 percent slopes, severely erodedCfE3540525804732qfkxga13320111:24000
Pacolet-Cataula complex, 6 to 15 percent slopes, moderately erodedPfD2530025804972qflpga13320111:24000
Cataula coarse sandy loam, 6 to 15 percent slopes, very boulderyCaD11725804692qfksga13320111:24000
Cataula sandy loam, 2 to 6 percent slopesCaB307522005252cvtpga20720071:24000
Cataula-Cecil complex, 6 to 15 percent slopes, moderately erodedCcD24456026390392wq9jga63920121:24000
Cataula-Cecil complex, 2 to 6 percent slopes, moderately erodedCcB23067526391052rj2mga63920121:24000
Cataula-Shoulderbone complex, 6 to 15 percent slopes, stonyCdD1226026390402rj2pga63920121:24000
Shoulderbone-Cataula complex, 15 to 25 percent slopes, moderately erodedShE2366026390912rj4kga63920121:24000
Cataula coarse sandy loam, 6 to 15 percent slopes, very boulderyCaD364526390382rj2lga63920121:24000
Cataula coarse sandy loam, 2 to 6 percent slopes, very boulderyCaB231026390372rj2kga63920121:24000
Pacolet-Cataula complex, 6 to 15 percent slopes, moderately erodedPdD2177526390852rj49ga63920121:24000
Cecil-Cataula complex, 10 to 25 percent slopes, severely erodedCfE342526391282rq87ga63920121:24000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCcD2008111549932zzyysc00119761:20000
Cataula sandy loam, 2 to 6 percent slopesCaB1880911549882th01sc00119761:20000
Cataula sandy loam, 6 to 10 percent slopesCaC11899115498917rvqsc00119761:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCbC22563115499017rvrsc00119761:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCdD278081317952zzyysc00719751:20000
Cataula sandy loam, 2 to 6 percent slopesCbB107251317902th01sc00719751:20000
Cataula sandy loam, 6 to 10 percent slopesCbC49811317914f4bsc00719751:20000
Cataula clay loam, 6 to 10 percent slopes, erodedCcC26551317924f4csc00719751:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCdD9511320752zzyysc02119601:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCcC284801321824fjysc02319771:20000
Cataula sandy loam, 2 to 6 percent slopesCaB48801321802th01sc02319771:20000
Cataula sandy loam, 6 to 10 percent slopesCaC2301321814fjxsc02319771:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCcD97321298372zzyysc03719781:20000
Cataula sandy loam, 2 to 6 percent slopesCaB93731298332th01sc03719781:20000
Cataula sandy loam, 6 to 10 percent slopesCaC88871298344c36sc03719781:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCcC2185351299034c5fsc03919771:20000
Cataula sandy loam, 2 to 6 percent slopesCaB30051299012th01sc03919771:20000
Cataula sandy loam, 6 to 10 percent slopesCaC21201299024c5dsc03919771:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCeD321691324712zzyysc04519721:20000
Cataula sandy loam, 2 to 6 percent slopes, moderately erodedCdB229541324672th03sc04519721:20000
Cataula sandy loam, 6 to 10 percent slopes, erodedCdC220811324684fv5sc04519721:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCdD84661300342zzyysc04719731:20000
Cataula sandy loam, 2 to 6 percent slopesCbB29531300282th01sc04719731:20000
Cataula sandy loam, 6 to 10 percent slopesCbC26111300294c9hsc04719731:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCcC225641300314c9ksc04719731:20000
Cataula sandy clay loam, 2 to 6 percent slopes, erodedCcB29161300304c9jsc04719731:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedClD200351303592zzyysc05919701:20000
Cataula sandy loam, 6 to 10 percent slopes, erodedCdC2129941303544cmzsc05919701:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCeC2118621303564cn1sc05919701:20000
Cataula sandy loam, 2 to 6 percent slopes, moderately erodedCdB2111021303532th03sc05919701:20000
Cataula sandy clay loam, 2 to 6 percent slopes, erodedCeB236161303554cn0sc05919701:20000
Cataula sandy loam, 2 to 6 percent slopesCbB103371306812th01sc06519731:20000
Cataula sandy loam, 6 to 10 percent slopesCbC102291306824czksc06519731:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCdD31671306872zzyysc06519731:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCcC217421306844czmsc06519731:20000
Cataula sandy clay loam, 2 to 6 percent slopes, erodedCcB214501306834czlsc06519731:20000
Cataula sandy loam, 2 to 6 percent slopes, moderately erodedCdB23456392222th03sc07120051:24000
Cataula sandy loam, 6 to 10 percent slopes, moderately erodedCdC2299639223pg53sc07120051:24000
Cataula sandy clay loam, 2 to 7 percent slopes, moderately eroded8B29914592671kzh4sc07120051:24000
Cataula sandy clay loam, 7 to 15 percent slopes, moderately eroded8C27314592761kzhfsc07120051:24000
Cataula sandy loam, 2 to 7 percent slopes7B3714592681kzh5sc07120051:24000
Cataula sandy loam, 2 to 6 percent slopes, moderately erodedCdB27051310182th03sc07719671:20000
Cataula sandy loam, 6 to 10 percent slopes, erodedCdC295741314614dspsc08719701:20000
Cataula sandy clay loam, 6 to 10 percent slopes, erodedCeC257251314634dsrsc08719701:20000
Cataula sandy loam, 2 to 6 percent slopes, moderately erodedCdB248041314602th03sc08719701:20000
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedClD42171314662zzyysc08719701:20000
Cataula sandy clay loam, 2 to 6 percent slopes, erodedCeB218871314624dsqsc08719701:20000
Cataula sandy clay loam, 6 to 10 percent slopes, moderately erodedCaC222325138312lpzxsc09120131:15840
Cecil-Cataula complex, 10 to 15 percent slopes, moderately erodedCdD19051309312zzyysc60219601:20000

Map of Series Extent

Approximate geographic distribution of the CATAULA 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 .