Official Series Description


Lab Data Summary

Aggregate lab data for the COZAD soil series. This aggregation is based on all pedons with a current taxon name of COZAD, 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 COZAD 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
7181P0120S1979NE175030COZAD7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.646946,-98.980835
7402N0479S2001KS029003Cozad7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5655403,-97.3811493
7402N0481S2001KS029005Cozad7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5837402,-97.5792084
7402N0482S2001KS029006Cozad7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5839043,-97.5825577

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COZAD 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 COZAD 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 COZAD 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 COZAD 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 COZAD 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 COZAD 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 COZAD 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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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 COZAD, 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. NE-2012-02-10-22 | Custer County - July 1982

    Typical pattern of soils and relationship of soils to topography and parent material in three associations: No. 8—Cozad association; No. 13—Ipage-Valentine association; No. 14—Boel-Barney-Gannett association (Soil Survey of Custer County, Nebraska; July 1982).

  2. NE-2012-02-13-15 | Gosper County - February 1981

    Typical pattern of soils and parent material in the Hobbs-Cozad-Hord association (Soil Survey of Gosper County, Nebraska; February 1981).

  3. NE-2012-02-13-18 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Hord-Cozad and the Boel-Loup-Leshara associations (Soil Survey of Greeley County, Nebraska; April 1993).

  4. NE-2012-02-13-21 | Hamilton County - March 1985

    Typical pattern of soils and relationship to topography and parent material in the Gothenburg-Platte-Alda association (1) and the Thurman-Coly association (4) (Soil Survey of Hamilton County, Nebraska; March 1985).

  5. NE-2012-02-13-99 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Loup-Bolent-Barney and Gibbon-Wann-Saltine associations (Soil Survey of Sherman County, Nebraska; May 1990).

  6. NE-2012-02-14-09 | Valley County - October 1985

    Typical pattern of soils and parent material in the Holdrege-Uly-Cozad association (Soil Survey of Valley County, Nebraska; October 1985).

  7. NE-2012-02-14-11 | Valley County - October 1985

    Typical pattern of soils and parent material in the Cozad-Hord and Boel-Loup-Leshara associations (Soil Survey of Valley County, Nebraska; October 1985).

Map Units

Map units containing COZAD 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
Cozad silt loam, 2 to 5 percent slopes, rarely flooded23162517115075417mg3ks13719731:24000
Cozad silt loam, 0 to 2 percent slopes, rarely flooded23151944115075317mg2ks13719731:24000
Cozad silt loam, rarely flooded3715641913821592ywssks16919891:24000
Cozad silt loam, 0 to 1 percent slopes8815151116918892tml6ne00119701:20000
Cozad loam, sand substratum, 0 to 3 percent slopes881245422160852dd0mne00119701:20000
Cozad silt loam, 0 to 1 percent slopes88153747426939gb87ne00319751:20000
Cozad silt loam, 0 to 1 percent slopes8815839417000392tml6ne01919671:20000
Cozad silt loam, 6 to 11 percent slopes, eroded8819166517000422tmkwne01919671:20000
Cozad silt loam, 1 to 3 percent slopes88161655170004030rstne01919671:20000
Cozad silt loam, 3 to 6 percent slopes, eroded88181444170004130rsvne01919671:20000
Cozad fine sandy loam, calcareous variant, 0 to 1 percent slopes8824473170002130rswne01919671:20000
Cozad loam, 0 to 1 percent slopes881115822282112dsmsne01919671:20000
Cozad silt loam, 1 to 3 percent slopes8816236016912721trx5ne02319791:20000
Cozad silt loam, 0 to 1 percent slopes88153322190282tml6ne02319791:20000
Cozad silt loam, 0 to 1 percent slopes88153804316995802tml6ne04119801:20000
Cozad silt loam, 1 to 3 percent slopes881620717169958330rstne04119801:20000
Cozad silt loam, 3 to 6 percent slopes88171039316995812wtjnne04119801:20000
Cozad silt loam, 0 to 1 percent slopes88158133716996662tml6ne04719751:20000
Cozad silt loam, 1 to 3 percent slopes881615120169966730rstne04719751:20000
Cozad fine sandy loam, 0 to 1 percent slopes88101161016996651v1mxne04719751:20000
Cozad silt loam, saline-alkali, 0 to 1 percent slopes8820849516996701v1n2ne04719751:20000
Cozad silt loam, 3 to 6 percent slopes8817749916996682wtjnne04719751:20000
Cozad silty clay loam, 0 to 1 percent slopes8821434116996732tmkxne04719751:20000
Cozad silt loam, 6 to 11 percent slopes, eroded8819267516996692tmkwne04719751:20000
Cozad silt loam, wet substratum, 1 to 3 percent slopes882869416996721v1n4ne04719751:20000
Cozad silt loam, wet substratum, 0 to 1 percent slopes88272116996711v1n3ne04719751:20000
Cozad silt loam, 1 to 3 percent slopes88161683169941630rstne06319731:20000
Cozad silt loam, rarely flooded3715422193562dhf4ne06319731:20000
Cozad silt loam, 0 to 1 percent slopes88151073716997361v1q6ne06519751:20000
Cozad silt loam, 1 to 3 percent slopes88163102169973730rstne06519751:20000
Cozad silt loam, 3 to 6 percent slopes8817123516997382wtjnne06519751:20000
Cozad silt loam, 0 to 1 percent slopes8815323416997722tml6ne07119841:20000
Cozad silt loam, 1 to 3 percent slopes8816496169977330rstne07119841:20000
Cozad silt loam, rarely flooded3715205716922021tsw5ne07319781:20000
Cozad silt loam, 1 to 3 percent slopes88161041169220330rstne07319781:20000
Cozad silt loam, 3 to 6 percent slopes881742916922042wtjnne07319781:20000
Cozad fine sandy loam, 0 to 1 percent slopes881024322194972dhkpne07319781:20000
Cozad silt loam, 0 to 1 percent slopes88151322194952tml6ne07319781:20000
Cozad silt loam, 0 to 1 percent slopes8815224816999332tml6ne07719871:20000
Cozad silt loam, 1 to 3 percent slopes88161002169993430rstne07719871:20000
Cozad silt loam, 3 to 6 percent slopes88173022288812wtjnne07719871:20000
Cozad loam, sand substratum, 0 to 3 percent slopes8812520617001131v23cne07920031:12000
Cozad loam, 0 to 1 percent slopes8811267217001121v23bne07920031:12000
Cozad, sand substratum-Hobbs, occasionally flooded, silt loams, 0 to 3 percent slopes844768517001141v23dne07920031:12000
Cozad silt loam, rarely flooded3715103216921441tst9ne08119821:20000
Cozad silt loam, wet substratum, rarely flooded844637116921461tstcne08119821:20000
Cozad silt loam, 1 to 3 percent slopes881625816921451tstbne08119821:20000
Cozad silt loam, 0 to 1 percent slopes8815128016922361tsx8ne08319671:20000
Cozad silt loam, 1 to 3 percent slopes8816148169223730rstne08319671:20000
Cozad silt loam, 3 to 6 percent slopes88176716922382wtjnne08319671:20000
Kenesaw-Cozad complex90721808997212wtjmne09319681:12000
Cozad silt loam, 1 to 3 percent slopes881634222889730rstne09319681:12000
Cozad loam, sand substratum, 0 to 3 percent slopes88121922289112dtccne09319681:12000
Cozad silt loam, 0 to 1 percent slopes8815942516991522tml6ne11119711:24000
Cozad silt loam, 1 to 3 percent slopes88164144169915330rstne11119711:24000
Cozad silt loam, saline-alkali, 0 to 1 percent slopes8820370216991551v13gne11119711:24000
Cozad silt loam, 3 to 6 percent slopes8817149816991542wtjnne11119711:24000
Cozad loam, sandy subsoil variant881395416991581v13kne11119711:24000
Cozad silt loam, wet882681516991561v13hne11119711:24000
Cozad silty clay loam, 0 to 1 percent slopes882156316991572tmkxne11119711:24000
Cozad silt loam, 1 to 3 percent slopes88161821169952430rstne11519861:20000
Cozad silt loam, 0 to 1 percent slopes8815180716995232tml6ne11519861:20000
Cozad silt loam, 3 to 6 percent slopes88171022198182wtjnne11519861:20000
Cozad loam, wet substratum, 0 to 1 percent slopes8814633517096291vd0bne12119781:20000
Cozad loam, sand substratum, 0 to 3 percent slopes881220922282652dspjne12119781:20000
Kenesaw-Cozad complex90721422282862wtjmne12119781:20000
Cozad silt loam, 0 to 1 percent slopes8815185716920491tsq7ne12919741:20000
Cozad silt loam, 0 to 1 percent slopes8815112616917332tml6ne13719671:20000
Cozad silt loam, rarely flooded371521622194722dhjwne13719671:20000
Cozad silt loam, 0 to 1 percent slopes8815212016922682tml6ne14319671:20000
Cozad-variant complex882586616922861tsywne14319671:20000
Cozad silt loam, 1 to 3 percent slopes881686516922691tsybne14319671:20000
Cozad silt loam, 3 to 6 percent slopes881741716922702wtjnne14319671:20000
Cozad silt loam, 1 to 3 percent slopes88166334169944630rstne14519651:20000
Cozad silt loam, 0 to 1 percent slopes8815491116994451v1dtne14519651:20000
Cozad silt loam, 3 to 6 percent slopes8817158016994472wtjnne14519651:20000
Cozad silt loam, 0 to 1 percent slopes8815372516999852tml6ne16319871:20000
Cozad silt loam, 1 to 3 percent slopes88163573169998630rstne16319871:20000
Cozad silt loam, 0 to 1 percent slopes88151183016998782tml6ne17519831:20000
Cozad silt loam, 1 to 3 percent slopes88169970169987930rstne17519831:20000
Cozad silt loam, 3 to 6 percent slopes8817261616998802wtjnne17519831:20000

Map of Series Extent

Approximate geographic distribution of the COZAD 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 .