Official Series Description


Lab Data Summary

Aggregate lab data for the CAREY soil series. This aggregation is based on all pedons with a current taxon name of CAREY, 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 CAREY 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
78B79-OK-29-379-OK057-29-3Carey4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.8993528,-99.9455361
78C40A469459OK039001Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6847229,-98.9652786
78C40A469559OK039002Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6238899,-99.1805573
78C87P042987OK059002Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8244438,-99.6033325
78C87P043087OK059002ACarey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8244438,-99.6033325
78C87P043187OK059002BCarey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8244438,-99.6033325
78C93P068893OK059003Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8138885,-99.538887
78C94P040194OK059005Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8830566,-99.418335
78C94P040294OK059006Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8811111,-99.4205551
78C94P040394OK059007Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8830566,-99.4205551
78C94P040494OK059008Carey7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8822212,-99.4219437
78C82P0609MLRA78-Tillman-TX207-002Carey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.206665,-99.6897202
78C82P0610MLRA78-Tillman-TX207-003Carey8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.2063904,-99.6894455

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CAREY 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 CAREY 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 CAREY 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 CAREY 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with CAREY 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 CAREY 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 CAREY 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with CAREY, 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. KS-2012-01-20-24 | Clark County - December 1982

    Typical pattern of soils in the Carey-Woodward-Quinlan association (Soil Survey of Clark County, Kansas; 1982).

  2. KS-2012-01-20-37 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Quinlan-Woodward-Carey association (Soil Survey of Comanche County, Kansas; 1989).

  3. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

  4. OK-2012-02-16-24 | Dewey County - December 1963

    Typical pattern of the soils in associations 1 and 2 (Soil Survey of Dewey County, Oklahoma; December 1963).

  5. OK-2012-02-16-28 | Ellis County - April 1966

    Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

  6. OK-2012-02-16-36 | Greer County - March 1967

    Major soils in soil association 2, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

  7. OK-2012-02-16-39 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Woodward-Quinlan map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  8. OK-2012-02-16-40 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Madge-Abilene-Shrewder map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  9. OK-2012-02-16-45 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed over Permian redbeds. The typical slope range is given for each soil. Alternating layers of sandstone and shale underlie these soils (Soil Survey of Harper County, Oklahoma; June 1960).

  10. OK-2012-02-17-10 | Major County - October 1968

    Soil associations in the western part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  11. OK-2012-02-17-42 | Roger Mills County - August 1963

    Typical pattern of soils in association 8. Woodward silt loam is a variation, which is described in the section "Descriptions of Soils" (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  12. OK-2012-02-17-58 | Woodward County - November 1963

    Typical pattern of soils of the St. Paul-Carey-Woodward association (Soil Survey of Woodward County, Oklahoma; November 1963).

  13. TX-2012-03-20-17 | Childress County - July 1963

    Soils developed in sandstone material (Soil Survey of Childress County, TX; 1963).

Map Units

Map units containing CAREY 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
Carey silt loam, 1 to 3 percent slopes54121597713817042t6pdks02519801:24000
Carey silt loam, 0 to 1 percent slopes54111590613817032t6pbks02519801:24000
Carey silt loam, 3 to 5 percent slopes5413759213817052t6pfks02519801:24000
Carey silt loam, 3 to 5 percent slopes54131600013812452t6pfks03319871:24000
Carey silt loam, 0 to 1 percent slopes5411658813812432t6pbks03319871:24000
Carey silt loam, 1 to 3 percent slopes541232113812442t6pdks03319871:24000
Carey loam, 1 to 3 percent slopes7123633817072t6plok00919781:24000
Carey and Woodward soils, 3 to 5 percent slopesCaC45869382310dttlok03919731:24000
Carey silt loam, 1 to 3 percent slopesCaB444563823092t6pdok03919731:24000
St. Paul and Carey soils, 3 to 5 percent slopesStC27036382344dtvpok03919731:24000
Carey and Woodward soils, 3 to 5 percent slopes, severely erodedCbC31135382311dttmok03919731:24000
Carey silt loam, 3 to 5 percent slopesCeC313513823582t6pfok04319611:24000
Carey silt loam, 1 to 3 percent slopesCeB168563823572t6pdok04319611:24000
Woodward-Carey complex, 3 to 5 percent slopes, erodedWcC28661382410dtxtok04319611:24000
Carey silt loam, 5 to 8 percent slopesCeD78703823592t6pgok04319611:24000
Woodward-Carey complex, 5 to 8 percent slopes, erodedWcD22908382411dtxvok04319611:24000
Woodward-Carey complex, 1 to 3 percent slopesWcB2026382409dtxsok04319611:24000
Carey silt loam, 1 to 3 percent slopesCaB27793824232t6pdok04519631:24000
Carey loam, 1 to 3 percent slopesCarB3556366402t6plok05520051:24000
Carey loam, 1 to 3 percent slopes1114379754422t6plok05719821:24000
Carey silt loam, 3 to 5 percent slopes, erodedCaC29742383439dw00ok07519731:24000
Carey silt loam, 3 to 5 percent slopesCaC78353834382t6pfok07519731:24000
Carey-Hinkle complex, 1 to 5 percent slopesCbD5342383440dw01ok07519731:24000
Carey silt loam, 1 to 3 percent slopesCaB43913834372t6pdok07519731:24000
Carey silt loam, 2 to 8 percent slopes, severely erodedCeD31760383441dw02ok07519731:24000
Carey silt loam, 3 to 5 percent slopesCrC37833838172t6pfok09319651:24000
Carey silt loam, 5 to 8 percent slopes, erodedCrD225763838182t6pkok09319651:24000
Carey silt loam, 1 to 3 percent slopesCrB24833838162t6pdok09319651:24000
Carey silt loam, 1 to 3 percent slopesCaB33553847272t6pdok12919611:24000
Carey silt loam, 3 to 5 percent slopesCaC7473847282t6pfok12919611:24000
Carey silt loam, 3 to 5 percent slopes8373463850462t6pfok14919761:24000
Carey silt loam, 1 to 3 percent slopes7357383850452t6pdok14919761:24000
Carey silt loam, 1 to 3 percent slopesCaB219813852632t6pdok15319611:24000
Carey silt loam, 3 to 5 percent slopesCaC187643852642t6pfok15319611:24000
Carey silt loam, 5 to 8 percent slopes, erodedCaD243623852662t6pkok15319611:24000
Carey silt loam, 5 to 8 percent slopesCaD10303852652t6pgok15319611:24000
Carey loam, 1 to 3 percent slopesCaB425603638112t6pltx07519611:20000
Carey loam, 1 to 3 percent slopesCaB179873640962t6pltx08719651:20000
Carey loam, 0 to 1 percent slopesCaA49333640952t6pjtx08719651:20000
Carey loam, 3 to 5 percent slopesCaC20583640972t6pmtx08719651:20000
Carey loam, 1 to 3 percent slopesCaB137903645792t6pltx10119691:20000
Carey loam, 0 to 1 percent slopesCaA9723645782wt7ctx10119691:20000
Carey loam, 1 to 3 percent slopesCaB28733651132t6pltx12519651:20000
Carey loam, 3 to 5 percent slopesCaC22453651142t6pmtx12519651:20000
Carey loam, 1 to 3 percent slopesCaB22133651672t6pltx12919751:24000
Carey loam, 0 to 1 percent slopesCaA2113651662t6pjtx12919751:24000
Carey loam, 1 to 3 percent slopesCaB218093669292t6pltx19119651:20000
Carey loam, 3 to 5 percent slopesCaC66223669302t6pmtx19119651:20000
Carey loam, 1 to 3 percent slopesCaB314433686022t6pltx26919991:31680
Carey loam, 0 to 1 percent slopesCaA113683685752wt7ctx26919991:31680
Carey silt loam, 1 to 3 percent slopesCaB105033732842t6pdtx48319701:24000
Carey silt loam, 0 to 1 percent slopesCaA5793732832t6pbtx48319701:24000

Map of Series Extent

Approximate geographic distribution of the CAREY 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 .