Official Series Description


Lab Data Summary

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with JUMPE 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 JUMPE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the JUMPE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 JUMPE, 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 JUMPE 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
Baldmountain-Rock outcrop-Jumpe family complex, 30 to 50 percent slopes6136167465219hm32ca76019811:24000
Baldmountain-Rock outcrop-Jumpe family complex, 5 to 30 percent slopes6124393465218hm31ca76019811:24000
Jumpe-Chumstick families-Rock outcrop complex, 30 to 60 percent slopes7133220465271hm4rca76019811:24000
Jumpe very stony silt loam, 25 to 65 percent slopesJnF676733502gb4wa60719691:20000
Jumpe stony silt loam, 0 to 25 percent slopesJmD370733492gb3wa60719691:20000
Jumpe stony ashy loam, 5 to 25 percent slopes1321131766582krvwa63720081:24000
Jumpe stony ashy loam, 25 to 45 percent south slopes4910759769232l1dwa63720081:24000
Jumpe stony ashy loam, 25 to 45 percent north slopes148581766672ks4wa63720081:24000
Jumpe stony ashy loam, 45 to 65 percent north slopes487595769112l10wa63720081:24000
Jumpe-Rock outcrop complex, 30 to 70 percent north slopes514535769462l24wa63720081:24000
Bocker-Jumpe complex, 0 to 15 percent slopes334214768192ky1wa63720081:24000
Jumpe stony ashy loam, 45 to 65 percent south slopes503667769352l1swa63720081:24000
Jumpe ashy loam, 35 to 60 percent slopes, stony6852400863082wt4wa67620141:12000
Jumpe ashy loam, 5 to 20 percent slopes, stony6821310863032wszwa67620141:12000
Jumpe ashy loam, 20 to 35 percent slopes, stony683420863092wt5wa67620141:12000
Jumpe ashy loam, 60 to 90 percent slopes, stony687330863062wt2wa67620141:12000
Jumpe, stony-Sapkin, very stony complex, 35 to 60 percent slopes6807280867962x9wwa67620141:12000
Jumpe stony loam, 25 to 45 percent north slopes62181736903229tvwa67719791:24000
Jumpe stony loam, 25 to 45 percent slopes60144906903029tswa67719791:24000
Jumpe stony loam, 5 to 25 percent slopes59138096902829tqwa67719791:24000
Jumpe stony loam, 45 to 65 percent north slopes6341026903329twwa67719791:24000
Jumpe-Rock outcrop complex, 40 to 80 percent slopes6423686903429txwa67719791:24000
Jumpe stony loam, 45 to 65 percent slopes6116226903129ttwa67719791:24000
Bocker-Jumpe complex, 0 to 15 percent slopes713326904029v3wa67719791:24000
Jumpe stony ashy loam, 45 to 65 percent north slopes46715754992jkgwa68020031:24000
Jumpe stony ashy loam, 25 to 45 percent north slopes45418754972jkdwa68020031:24000
Jumpe stony ashy loam, 25 to 45 percent south slopes44369754902jk5wa68020031:24000
Jumpe stony ashy loam, 5 to 25 percent slopes43217754872jk2wa68020031:24000

Map of Series Extent

Approximate geographic distribution of the JUMPE 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 .