Official Series Description


Lab Data Summary

Aggregate lab data for the ZENDA soil series. This aggregation is based on all pedons with a current taxon name of ZENDA, 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 ZENDA 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
78C84P069784KS033003Zenda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2075005,-99.4372253
78C84P069884KS033004Zenda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2075539,-99.43927
7940A182476KS151002Zenda8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6555557,-98.5824966

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZENDA 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 ZENDA 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 ZENDA 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 ZENDA 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 .

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.

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

Competing Series

Soil series competing with ZENDA 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 ZENDA 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 ZENDA 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 ZENDA, 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-2012-01-20-49 | Edwards County - September 1973

    Pattern of soils in associations 1, 3, and 7. Association 1 is to the left of Big Coon Creek. Association 7 extends from Big Coon Creek to the Arkansas River. Association 3 is to the right of the Arkansas River (Soil Survey of Edwards County, Kansas; 1973).

  2. KS-2012-01-25-15 | Pratt County - September 1968

    Major soils of associations 8 and 9 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

Map Units

Map units containing ZENDA 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
Zenda clay loam, occasionally flooded5690105913825381hdn0ks00719731:24000
Zenda loam, occasionally flooded5692182813817591hctwks02519801:24000
Zenda clay loam, occasionally flooded5690135513813021hcc4ks03319871:24000
Zenda clay loam, occasionally flooded5690970113804022wtxlks04719671:24000
Zenda-Drummond complex, occasionally flooded5693113213804032zt7hks04719671:24000
Zenda fine sandy loam, occasionally flooded5691639313827591hdw4ks07719651:24000
Zenda clay loam, occasionally flooded56903713827582wtxlks07719651:24000
Zenda clay loam, occasionally flooded5690619214447622wtxlks09519771:24000
Zenda-Drummond complex, occasionally flooded56932414447632zt7hks09519771:24000
Zenda loam, occasionally flooded5692572813801591hb58ks14519761:24000
Zenda clay loam, occasionally flooded569032513801582wtxlks14519761:24000
Zenda clay loam, occasionally flooded5690152214451202wtxlks15119651:24000
Zenda-Drummond complex, occasionally flooded569369014451212zt7hks15119651:24000
Zenda-Natrustolls complex, occasionally flooded5694364514436362zt7jks18519751:24000
Zenda-Drummond complex, occasionally flooded56935214436352zt7hks18519751:24000

Map of Series Extent

Approximate geographic distribution of the ZENDA 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 .