Official Series Description


Lab Data Summary

Aggregate lab data for the JEDEDIAH soil series. This aggregation is based on all pedons with a current taxon name of JEDEDIAH, 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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 JEDEDIAH 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.

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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 JEDEDIAH, 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 JEDEDIAH 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
Jedediah-Liza complex, 10 to 20 percent slopes13742342124304172ml1kid65020111:24000
Jedediah-Liza complex, 1 to 10 percent slopes13541209824259662mfdzid65020111:24000
Ezbin-Jedediah complex, 12 to 30 percent slopes43B753124524813232p90pid65020111:24000
Jedediah-Kucera complex, 4 to 24 percent slopes1354753624314402mm3kid65020111:24000
Jedediah-Middlehill families, complex, 25 to 60 percent slopes2083431636202rfztid70919761:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 13749331636262mnb6id70919761:24000
Jedediah-Middlehill families, complex, 25 to 60 percent slopes20844431732402rfztid71119831:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 1374910425584322mnb6id71119831:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 133091531732452q7wgid71119831:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 43B749433131733182x01zid71220081:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 13749883424326072mnb6id7131:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 13309399625086322q7wgid7131:24000
Jedediah-Middlehill families, complex, 25 to 60 percent slopes208380526198582rfztid7131:24000
Woolsted-Jedediah families, complex, 1 to 8 percent slopes928162727335122slt8id7131:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 43B7494337629809062x01zid7131:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 43B309434429809052x01yid7131:24000
Woolsted-Jedediah families, complex, 1 to 8 percent slopes92860931634752slt8id7161:24000
Sparky-Jedediah family, complex, 10 to 60 percent slopes, MLRA 1374923631634282mnb6id7161:24000
Jedediah-Middlehill families, complex, 25 to 60 percent slopes208131634232rfztid7161:24000
Jedediah-Liza complex, 10 to 20 percent slopes1374279225152572qf56id75819981:24000
Jedediah-Liza complex, 1 to 10 percent slopes135415225152512qf50id75819981:24000
Ezbin-Jedediah complex, 12 to 30 percent slopes43B7533325185832qj1rid75819981:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 13309428586342q7wgid75819981:24000
Ezbin-Jedediah complex, 12 to 30 percent slopes43B75310225152432qf4rid76619781:24000
Jedediah family-Robin complex, 10 to 40 percent slopes, MLRA 1330915628586572q7wgwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the JEDEDIAH 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 .