Official Series Description


Lab Data Summary

Aggregate lab data for the JORGE soil series. This aggregation is based on all pedons with a current taxon name of JORGE, 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 JORGE 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
22A40A3419S1975NV031005JORGE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2121201,-119.8801727
22A79P0478S1979NV031023Jorge6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4655571,-119.9494476
22A00P0044S99CA061001Jorge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2315722,-120.1177778
22A00P0046S99CA061004Jorge7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2270194,-120.1251639

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JORGE 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 JORGE 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 JORGE 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 JORGE 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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Competing Series

Soil series competing with JORGE 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 JORGE 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 JORGE 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 flats position figure.

Soil series sharing subgroup-level classification with JORGE, 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 JORGE 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
Tahoma-Jorge complex, 2 to 15 percent slopes7222490516520921sg49ca69320061:24000
Jorge-Tahoma complex, 15 to 30 percent slopes7156438616520931sg4bca69320061:24000
Jorge very cobbly fine sandy loam, 15 to 30 percent slopes, rubbly7152383516522081sg81ca69320061:24000
Jorge very cobbly fine sandy loam, 30 to 50 percent slopes, rubbly7153273516522101sg83ca69320061:24000
Jorge very cobbly fine sandy loam, 5 to 15 percent slopes, rubbly7151157516521771sg71ca69320061:24000
Jorge-Tahoma complex, 30 to 50 percent slopes7157154316520941sg4cca69320061:24000
Jorge very cobbly loam, 15 to 50 percent slopes, extremely stony715527216520911sg48ca69320061:24000
Jorge very cobbly loam, 2 to 15 percent slopes, extremely stony715417916520901sg47ca69320061:24000
Jorge-Tahoma complex, 2 to 30 percent slopesJTE12905464703hlkfca71919821:24000
Jorge very stony sandy loam, 30 to 50 percent slopesJTF11268464704hlkgca71919821:24000
Rubble land-Jorge complex, 30 to 75 percent slopesSTG2812464803hlnnca71919821:24000
Aldi variant-Kyburz-Jorge variant complex, 2 to 30 percent slopesCRE2601464628hlh0ca71919821:24000
Jorge variant-Kyburz complex, 2 to 30 percent slopesXXE2390464844hlpzca71919821:24000
Jorge-Rubble land complex, 30 to 75 percent slopesJUG2179464706hlkjca71919821:24000
Jorge-Waca-Tahoma complex, 30 to 50 percent slopesJWF1638464708hlklca71919821:24000
Jorge-Cryumbrepts, wet-Tahoma complex, 2 to 30 percent slopesJSE1570464701hlkcca71919821:24000
Kyburz-Aldi variant-Jorge variant complex, 2 to 30 percent slopesXCE1540464840hlpvca71919821:24000
Jorge-Waca-Cryumbrepts, wet complex, 2 to 30 percent slopesJXE1319464709hlkmca71919821:24000
Jorge-Rubble land complex, 2 to 30 percent slopesJUE1111464705hlkhca71919821:24000
Rubble land-Jorge complex, 2 to 30 percent slopesSTE1065464802hlnmca71919821:24000
Kyburz-Aldi variant-Jorge variant complex, 30 to 50 percent slopesXCF946464841hlpwca71919821:24000
Jorge variant-Kyburz complex, 30 to 50 percent slopesXXF865464845hlq0ca71919821:24000
Jorge-Waca-Tahoma complex, 2 to 30 percent slopesJWE764464707hlkkca71919821:24000
Aldi variant-Kyburz-Jorge variant complex, 30 to 50 percent slopesCRF537464629hlh1ca71919821:24000
Jorge-Waca-Cryumbrepts, wet complex, 30 to 50 percent slopesJXF485464710hlknca71919821:24000
Fugawee-Jorge-Rubble land complex, 30 to 75 percent slopes, erodedFJG2366464651hlhrca71919821:24000
Jorge-Cryumbrepts, wet complex, 30 to 75 percent slopesJSG316464702hlkdca71919821:24000
Jorge-Tahoma complex, cool, 30 to 50 percent slopesJwFltb2515881461q9ljca71919821:24000
Jorge-Tahoma complex, cool, 15 to 30 percent slopesJwEltb1315881441q9lgca71919821:24000
Jorge-Tahoma cobbly, 2 to 15 percent slopesJtDltb115957861qkjzca71919821:24000
Jorge-Boomtown-Fugawee association146011204474210hxg3nv62819801:24000

Map of Series Extent

Approximate geographic distribution of the JORGE 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 .