Official Series Description


Lab Data Summary

Aggregate lab data for the WITHAM soil series. This aggregation is based on all pedons with a current taxon name of WITHAM, 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 WITHAM 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
206N1055S2006OR071015Witham7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3791122,-123.2373581

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WITHAM 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 WITHAM 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 WITHAM 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 WITHAM 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 flats position figure.

Competing Series

Soil series competing with WITHAM 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 WITHAM 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 WITHAM 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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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.

Soil series sharing subgroup-level classification with WITHAM, 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

No block diagrams are available.

Map Units

Map units containing WITHAM 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
Dixonville-Gellatly-Witham complex, 2 to 12 percent slopes604142852442vptor00320041:24000
Witham silty clay loam, 2 to 12 percent slopes1723069853912vvkor00320041:24000
Witham silty clay loam, 12 to 20 percent slopes173171852382vpmor00320041:24000
Witham silty clay loam, hummocky, 2 to 25 percent slopes2798D5427111521vkrfor05319771:20000
Panther-Witham complex, hummocky, 2 to 25 percent slopes2776D1427111671j8cvor05319771:20000
Witham silty clay loam, 2 to 12 percent slopes2734C514045771j4kyor05319771:20000
Melbourne-Witham complex, hummocky, 2 to 25 percent slopes,2769C3427111111j8cgor06719751:20000
Witham silty clay loam, hummocky, 2 to 25 percent slopes2798D568627113011vkrfor07119671:24000
Panther-Witham complex, hummocky, 2 to 25 percent slopes2776D399327114141j8cvor07119671:24000
Melbourne-Witham complex, hummocky, 2 to 25 percent slopes,2769C313327114101j8cgor07119671:24000
Dixonville-Gellatly-Witham complex, hummocky, 2 to 20 percent slopes2800D68127114262n8qyor07119671:24000
Hazelair-Witham complex, 2 to 12 percent slopes2825C51827112802p8tlor07119671:24000
Melbourne-Witham complex, hummocky, 5 to 25 percent, moist2805E43627112962n8r1or07119671:24000
Witham-Dixonville complex, hummocky, 2 to 25 percent slopes2827E19827113572q3kmor07119671:24000
Goodin-Witham complex, hummocky, 2 to 25 percent slopes2808D17527113352q3kror07119671:24000
Goodin-Witham complex, hummocky, 2 to 25 percent, stony2818E12127314522q3knor07119671:24000
Steiwer-Witham complex, hummocky, 12 to 30 percent slopes2820E11827113722p8v3or07119671:24000
Melbourne-Witham complex, very hummocky, 2 to 40 percent slopes2822E7627113602q3klor07119671:24000
Steiwer-Witham complex, 30 to 60 percent slopes2820F6127113522p8v5or07119671:24000
Steiwer-Witham complex, hummocky, 2 to 20 percent slopes2803D6027114022q3kvor07119671:24000
Hazelair-Witham complex, 12 to 20 percent slopes2825D3127314462p8tnor07119671:24000
Witham silty clay, 2 to 12 percent slopes103C12756425124vmor63919831:20000

Map of Series Extent

Approximate geographic distribution of the WITHAM 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 .