Official Series Description


Lab Data Summary

Aggregate lab data for the ZAAR soil series. This aggregation is based on all pedons with a current taxon name of ZAAR, 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 ZAAR 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
11269KS0370151969KS037015Zaar2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5281448,-94.8477859
112M95217011995MO217001Zaar4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0425,-94.4597222
11240A182973KS037002Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5288887,-94.8472214
11206N0123S2005KS205002Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5534706,-95.8258896
11213N0426S2012KS021002Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3043694,-94.9396167
11213N0432S2012KS099002Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2818722,-95.0866472
11213N0438S2012MO217002Zaar6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0427778,-94.4741111
11217N0563S2016KS001001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8757,-95.2615117
11217N0567S2016KS125001Zaar6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3569417,-95.74967
11217N0568S2016KS133001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6304833,-95.1556267
11217N0569S2016KS205001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6899317,-95.599845
11217N0570S2017KS011001Zaar8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.790035,-94.9961433
11217N0571S2017KS037001Zaar8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5434817,-94.8375583
7617N0564S2016KS017001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2397267,-96.3802883
7617N0565S2016KS073001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.91735,-96.399185
7617N0566S2016KS111001Zaar7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3299964,-96.3187082

Water Balance

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

Competing Series

Soil series competing with ZAAR 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 ZAAR series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ZAAR 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.

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 ZAAR, 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-2012-01-20-13 | Chase County - June 1974

    Pattern of soils in the Clime-Sogn association (Soil Survey of Chase County, Kansas; 1974).

  2. KS-2012-01-20-41 | Crawford County - December 1973

    Typical cross section of the major soils that formed in material weathered from clayey shale or limestone that is calcareous or is neutral in reaction. These soils are in associations 5, 6, and 7 (Soil Survey of Crawford County, Kansas; 1973).

  3. KS-2012-01-23-47 | Labette County - July 1990

    Typical pattern of soils and parent material in the Parsons-Kenoma-Dennis association (Soil Survey of Labette County, Kansas; 1990).

  4. KS-2012-01-23-49 | Labette County - July 1990

    Typical pattern of soils and parent material in the Catoosa-Apperson-Zaar association (Soil Survey of Labette County, Kansas; 1990).

Map Units

Map units containing ZAAR 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
Zaar silty clay, 1 to 3 percent slopes89912904214271432ydssks00119751:24000
Zaar silty clay, 3 to 8 percent slopes8992504014271442ydstks00119751:24000
Zaar silty clay, 0 to 1 percent slopes899024614271422ydsrks00119751:24000
Zaar silty clay, 1 to 3 percent slopes89912870014270792ydssks01119791:24000
Zaar silty clay, 3 to 8 percent slopes89922712714270802ydstks01119791:24000
Zaar silty clay, 0 to 1 percent slopes8990137214270782ydsrks01119791:24000
Zaar-Dwight complex, 1 to 3 percent slopes8993506913828461hdyyks01719671:24000
Zaar silty clay, 3 to 8 percent slopes8992254013828452ydstks01719671:24000
Zaar silty clay, 1 to 3 percent slopes8991489131019412ydssks02119831:24000
Zaar silty clay, 0 to 1 percent slopes899050014268992ydsrks02119831:24000
Zaar silty clay, 1 to 3 percent slopes89914559813870212ydssks03719691:24000
Zaar silty clay, 0 to 1 percent slopes899018613870202ydsrks03719691:24000
Zaar silty clay, 3 to 8 percent slopes899210313870222ydstks03719691:24000
Zaar silty clay, 0 to 1 percent slopes8990184014536882ydsrks07319811:24000
Zaar silty clay, 1 to 3 percent slopes899111414536892ydssks07319811:24000
Zaar silty clay, 1 to 3 percent slopes89912970931019422ydssks09919871:24000
Zaar silty clay, 0 to 1 percent slopes8990498914268702ydsrks09919871:24000
Zaar silty clay, 3 to 8 percent slopes8992316114537552ydstks11119771:24000
Zaar silty clay, 1 to 3 percent slopes89911884714269512ydssks12519781:24000
Zaar silty clay, 0 to 1 percent slopes8990267614269502ydsrks12519781:24000
Zaar silty clay, 1 to 3 percent slopes89912427914270342ydssks13319801:20000
Zaar silty clay, 0 to 1 percent slopes8990653214270332ydsrks13319801:20000
Zaar silty clay, 1 to 3 percent slopes89911916514269992ydssks20519851:20000
Zaar silty clay, 0 to 1 percent slopes8990388914269982ydsrks20519851:20000
Zaar silty clay, 1 to 3 percent slopes899185314272102ydssks20719731:20000
Zaar silty clay, 3 to 8 percent slopes89923014272112ydstks20719731:20000
Zaar silty clay, 1 to 3 percent slopes400954331019432ydssmo01119691:24000
Zaar silty clay, 1 to 3 percent slopes4009548148867802ydssmo21719741:24000
Zaar silty clay, 3 to 8 percent slopes4009635938867812ydstmo21719741:24000

Map of Series Extent

Approximate geographic distribution of the ZAAR 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 .