Official Series Description


Lab Data Summary

Aggregate lab data for the HAYES soil series. This aggregation is based on all pedons with a current taxon name of HAYES, 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 HAYES 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
7993KS155005R93KS155005RHayes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0293884,-98.3670273
7993KS15511093KS155110Hayes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0055542,-98.3987198
7993KS15523293KS155232Hayes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8754158,-98.449585

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HAYES 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 HAYES 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 HAYES 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 HAYES 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 HAYES 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 HAYES 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 HAYES 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 HAYES, 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-2010-09-03-01 | Reno County - 2002

    Typical pattern of soils and parent material in the Tivin-Hayes-Pratt association (Soil Survey of Reno County, Kansas; 2002).

Map Units

Map units containing HAYES 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
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes590510527682322xlj4ks00719731:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes5905978427682352xlj4ks00919791:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59059627682492xlj4ks04719671:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59051013527682552xlj4ks07719651:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes5905136627682572xlj4ks07919701:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes5905398527682632xlj4ks09519771:24000
Hayes fine sandy loam, 1 to 5 percent slopes59028813805152tt51ks09719831:24000
Hayes loamy fine sand, 5 to 10 percent slopes59045226057622tt52ks09719831:24000
Hayes fine sandy loam, 1 to 5 percent slopes59027914292452tt51ks11319801:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59051527682712xlj4ks11319801:24000
Hayes fine sandy loam, 1 to 5 percent slopes59024194914451412tt51ks15119651:24000
Hayes loamy fine sand, 5 to 10 percent slopes59041192726057632tt52ks15119651:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59051008014451432xlj4ks15119651:24000
Hayes-Turon complex, 0 to 5 percent slopes5906356927682762r8yxks15119651:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59053176714438332xlj4ks15519991:24000
Hayes-Turon complex, 0 to 5 percent slopes5906859427682842r8yxks15519991:24000
Hayes fine sandy loam, 1 to 5 percent slopes5902450214438322tt51ks15519991:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes5905867827682952xlj4ks15919711:24000
Hayes fine sandy loam, 1 to 5 percent slopes590223814332872tt51ks15919711:24000
Hayes-Turon complex, 0 to 5 percent slopes590614827682912r8yxks15919711:24000
Hayes-Solvay loamy fine sands, 0 to 5 percent slopes59055907814436592xlj4ks18519751:24000
Hayes-Turon complex, 0 to 5 percent slopes59063153327683032r8yxks18519751:24000
Hayes fine sandy loam, 1 to 5 percent slopes5902140514436572tt51ks18519751:24000
Hayes loamy fine sand, 5 to 10 percent slopes590446726057642tt52ks18519751:24000

Map of Series Extent

Approximate geographic distribution of the HAYES 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 .