Official Series Description


Lab Data Summary

Aggregate lab data for the JUGHANDLE soil series. This aggregation is based on all pedons with a current taxon name of JUGHANDLE, 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 JUGHANDLE 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
43A75-ID-256675ID049001Jughandle3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3906937,-115.5811386
43B14N0135S2013ID049001Jughandle6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7777528,-116.0724667
43B14N0139S2013ID049005Jughandle6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7543417,-116.0538361
43B14N0140S2013ID049006Jughandle6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8698361,-115.5541306
43B14N0141S2013ID049007Jughandle6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8924083,-115.5683139

Water Balance

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

Competing Series

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the JUGHANDLE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 JUGHANDLE, 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 JUGHANDLE 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
Jughandle-Suttler association59192686250558vid60019891:24000
Jughandle loam, cool, 40 to 90 percent slopes579452686333558sid60919891:24000
Jughandle ashy loam, cool, 7 to 40 percent slopes565072686332558rid60919891:24000
Jughandle-Ericson association582252686334558tid60919891:24000
Jughandle loam, cool, 40 to 90 percent slopes578041154032558sid61719761:24000
Jughandle-Suttler association596685154034558vid61719761:24000
Jughandle ashy loam, cool, 7 to 40 percent slopes566132154031558rid61719761:24000
Jughandle-Ericson association583051154033558tid61719761:24000
Jughandle variant silt loam601003154036558xid61719761:24000
Jughandle sandy loam, 35 to 65 percent slopesJuE2674115410755c6id61819651:24000
Jughandle sandy loam, 12 to 35 percent slopesJuD318015410655c5id61819651:24000
Jughandle-Suttler association, 40 to 90 percent slopes1052096811022qd6id65619921:24000
Jughandle ashy sandy loam, 30 to 60 percent slopes104824811012qd5id65619921:24000
Jughandle-Suttler association6170599273417659558vid7001:24000
Jughandle-Suttler association, 40 to 90 percent slopes65610539833324072qd6id7001:24000
Jughandle ashy loam, cool, 7 to 40 percent slopes6170561433417657558rid7001:24000
Jughandle ashy sandy loam, 30 to 60 percent slopes6561041933324062qd5id7001:24000
Jughandle-Ericson association61705843417658558tid7001:24000
Jughandle-Parkay families complex, 15 to 45 percent slopes422107481251j4s7ut60119851:24000

Map of Series Extent

Approximate geographic distribution of the JUGHANDLE 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 .