Official Series Description


Lab Data Summary

Aggregate lab data for the JUDELL soil series. This aggregation is based on all pedons with a current taxon name of JUDELL, 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 JUDELL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

Soil series sharing subgroup-level classification with JUDELL, 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 JUDELL 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
Fairfield-Judell clay loams, 2 to 8 percent slopes965062342601chhnmt02719791:24000
Judith-Judell clay loams, 2 to 4 percent slopes1294134342356ch7rmt02719791:24000
Judith-Judell clay loams, 0 to 2 percent slopes1284059342355ch7qmt02719791:24000
Fairfield-Judell clay loams, 0 to 2 percent slopes951745342600chhmmt02719791:24000
Gallatin, Judell and Lamoure soils, 0 to 4 percent slopesGr231401473634ybnmt60219631:20000
Judell and Judith soils, 8 to 15 percent slopesJs14271473814yc7mt60219631:20000
Windham-Judell families, complex, 4 to 25 percent slopes1020E6630396732qbzmmt60219631:20000
Judell gravelly loam, 1 to 4 percent slopes, very stony662B581476244ym2mt60919711:24000
Judell loam, 2 to 4 percent slopes61B1831445314vd9mt62119971:24000
Windham-Judell complex, 8 to 15 percent slopes202D119215080251xlmt62719981:24000
Windham-Judell complex, 15 to 35 percent slopes202E86515080351xmmt62719981:24000
Windham-Judell gravelly loams, 8 to 25 percent slopes, stony208D59515084151yvmt62719981:24000
Judell loam, 2 to 8 percent slopes65C31815125252d3mt62719981:24000
Windham-Judell gravelly loams, 8 to 25 percent slopes, stony, warm2088D29315083851yrmt62719981:24000
Judell gravelly loam, 2 to 8 percent slopes651C26115124752cymt62719981:24000
Judell-Lap, very stony, complex, 4 to 15 percent slopes1921D23615076351wbmt62719981:24000
Windham-Judell complex, 8 to 15 percent slopes, warm2082D20015082951ygmt62719981:24000
Windham-Judell very cobbly loams, 4 to 15 percent slopes, bouldery1343D18415059351pvmt62719981:24000
Judell gravelly loam, 2 to 8 percent slopes, warm655C13015125052d1mt62719981:24000
Judell gravelly loam, 1 to 4 percent slopes, very stony662B7215125352d4mt62719981:24000
Judell-Lap, very stony, complex, 15 to 35 percent slopes1921E6215076451wcmt62719981:24000
Judell cobbly loam, 2 to 8 percent slopes652C3915124952d0mt62719981:24000
Windham-Judell families, complex, 4 to 25 percent slopes1020E26526322562qbzmmt6321:24000
Judell and Judith soils, 8 to 15 percent slopesJs12529682454yc7mt6321:24000
Gallatin, Judell and Lamoure soils, 0 to 4 percent slopesGr1029682464ybnmt6321:24000

Map of Series Extent

Approximate geographic distribution of the JUDELL 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 .