Official Series Description


Lab Data Summary

Aggregate lab data for the DEERTON soil series. This aggregation is based on all pedons with a current taxon name of DEERTON, 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 DEERTON 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
9295P0443S1991WI007004DEERTON6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.959446,-90.8511124
93B01P0155S2000MI083003Deerton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3584442,-87.9640274

Water Balance

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

There are insufficient data to create the 3D terrace figure.

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Competing Series

Soil series competing with DEERTON 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 DEERTON 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 DEERTON 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with DEERTON, 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 DEERTON 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
Deerton-Tokiahok-Trout Bay complex, 15 to 70 percent slopes, dissected72F532014552971kvc2mi00320071:24000
Jeske-Gongeau-Deerton complex, bedrock terrace, 1 to 20 percent slopes65D229414552891kvbtmi00320071:24000
Deerton-Tokiahok-Trout Bay complex, 8 to 35 percent slopes, dissected72E189714552961kvc1mi00320071:24000
Deerton-Tokiahok-Jeske complex, 1 to 12 percent slopes, dissected306C158014554451kvhvmi00320071:24000
Deerton-Au Train complex, 1 to 15 percent slopes47C88814552731kvb9mi00320071:24000
Kalkaska-Deerton sands, 0 to 6 percent slopes321B74515078611mm1pmi00320071:24000
Jeske-Gongeau-Deerton complex, bedrock terrace, 1 to 45 percent slopes65F59314552901kvbvmi00320071:24000
Kalkaska-Deerton sands, 6 to 15 percent slopes321D44415271911n857mi00320071:24000
Deerton-Au Train complex, 6 to 35 percent slopes47E36914552741kvbbmi00320071:24000
Deerton and Abbaye soils, dissected, 1 to 8 percent slopes93B576415042fxwgmi01319841:20000
Deerton and Abbaye soils, dissected, 8 to 35 percent slopes93D414415043fxwhmi01319841:20000
Deerton sand, 1 to 8 percent slopes94B282415044fxwjmi01319841:20000
Deerton sand, 1 to 8 percent slopes24B1215416111fyzymi06119891:20000
Deerton variant gravelly loamy sand, 0 to 4 percent slopes15B194918677168bwmi06319781:20000
Deerton loamy sand, 0 to 6 percent slopes206B1194631390p60fmi09520041:24000
Deerton-Brownstone complex, 0 to 6 percent slopes, very stony3608B153517026061v4pswi00320061:12000
Deerton-Brownstone complex, 6 to 15 percent slopes, very stony3608C50217026071v4ptwi00320061:12000
Deerton-Brownstone complex, 0 to 6 percent slopes, very stony3608B83413836581hft4wi00720051:12000
Deerton-Brownstone complex, 6 to 15 percent slopes, very stony3608C45713836601hft6wi00720051:12000

Map of Series Extent

Approximate geographic distribution of the DEERTON 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 .