Official Series Description


Lab Data Summary

Aggregate lab data for the MAYHEW soil series. This aggregation is based on all pedons with a current taxon name of MAYHEW, 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 MAYHEW 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
135AS92AL-023-392AL023003-pgmMayhew3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3022222,-88.035
135A40A5034S1958AL091003MAYHEW5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2555542,-87.8444443

Water Balance

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

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Soil series sharing subgroup-level classification with MAYHEW, 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. MS-2012-04-27-11 | Newton County - February 1960

    Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

Map Units

Map units containing MAYHEW 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
Mayhew silty clay loam, 0 to 2 percent slopesMaA2503285732sht8al02319981:24000
Mayhew silty clay loam, 0 to 2 percent slopesMaA262703314832sht8al11919861:24000
Mayhew silty clay loam, 0 to 2 percent slopes4145343179375lyn4ar01919831:20000
Mayhew silty clay loam, 0 to 2 percent slopes216595565646lzlnar05719761:20000
Mayhew silty clay loam, 0 to 2 percent slopes41683179265lyn4ar05919831:20000
Mayhew silty clay loamMe234115274681n8g5la04319821:24000
Mayhew loam, 1 to 5 percent slopesMhC805190317421wdqla06919831:24000
Kisatchie-Mayhew-Rayburn association, 5 to 20 percent slopesKSF18761190303521w87la08519911:24000
Mayhew loam, 1 to 5 percent slopesMhC6203190304321w8hla08519911:24000
Mayhew silt loam, 1 to 5 percent slopesMhC2180917255631vxlbla11519921:24000
Mayhew silty clay loamMa647331852c49xms01319631:15840
Mayhew silt loamMw8634331894c4c8ms01719691:20000
Mayhew silt loam, 0 to 2 percent slopesMhA67413320932sht7ms02519741:20000
Mayhew silt loam, 0 to 2 percent slopesMeA41093327682sht7ms06919911:20000
Mayhew silty clay loam, very gently sloping phase (2 to 5 percent slopes)McB997333330c5vlms10119571:20000
Mayhew silty clay loam, nearly level phase (0 to 2 percent slopes)McA672333329c5vkms10119571:20000
Mayhew silty clay loam, 0 to 2 percent slopesMsA8399333708c67sms11519691:20000
Mayhew silty clay loam, 2 to 5 percent slopesMsB5962333709c67tms11519691:20000
Mayhew silty clay loam, 5 to 12 percent slopesMsD3489333710c67vms11519691:20000
Mayhew silty clay loam, 8 to 12 percent slopes, erodedMsD21206333711c67wms11519691:20000

Map of Series Extent

Approximate geographic distribution of the MAYHEW 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 .