Official Series Description


Lab Data Summary

Aggregate lab data for the GEM soil series. This aggregation is based on all pedons with a current taxon name of GEM, 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 GEM 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
1079P043379ID087001Gem7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2586098,-116.706665
1040A1094S1957ID045041GEM6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9601517,-116.4359741
1040A1093S1957ID045042GEM6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0432053,-116.4870911

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GEM 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 GEM 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 GEM 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 GEM 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 GEM 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 GEM 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 GEM 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 terrace figure.

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

Soil series sharing subgroup-level classification with GEM, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. AZ-2011-05-27-04 | Beaver Creek Area - 1967

    Typical section of soils, upper part of Beaver Creek Area. Elevations range from 3,800 feet to 8,500 feet (Soil Survey of Beaver Creek Area, Arizona; 1967).

  2. AZ-2011-05-27-24 | Long Valley Area - 1974

    Typical pattern of soils in area north of East Clear Creek (Soil Survey of Long Valley Area, Arizona; 1974).

  3. ID-2010-08-30-01 | Adams-Washington Area - 2001

    Typical pattern of soils and underlying material in general soil map units 5, 10, 16, and 17 (Soil Survey of Adams-Washington Area, Idaho; 2001).

  4. NM-2012-02-15-06 | Zuni Mountain Area - July 1967

    Typical section of soils in the southern part of the Zuni Mountains, between Zuni Canyon and the Ice Cave area (Soil Survey of Zuni Mountain Area, New Mexico; July 1967).

Map Units

Map units containing GEM 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
Gem clay loamGm462615452971nw09az64119651:31680
Gem-Springerville complexGn53715452981nw0baz64119651:31680
Gem cobbly clay loam, 0 to 20 percent slopesGcD3547615274441n8fdaz64319671:31680
Springerville-Gem complex, 0 to 20 percent sloepsSsD2710315275201n8hvaz64319671:31680
Gem-Rock outcrop complex, 5 to 40 percent slopes6432125190322qbnid00120121:24000
Gem silty clay loam, 2 to 15 percent slopes6320925190312qbmid00120121:24000
Gem-Reywat complex, 2 to 30 percent slopes7361448812702qkmid65619921:24000
Gem-Reywat complex, 30 to 65 percent slopes7449983812712qknid65619921:24000
Gem-Bakeoven complex, 2 to 30 percent slopes7131587812682qkkid65619921:24000
Gem stony clay loam, 2 to 30 percent slopes6815728812642qkfid65619921:24000
Gem-Bakeoven complex, 30 to 60 percent slopes7214644812692qklid65619921:24000
Gem stony clay loam, 30 to 60 percent slopes691798812652qkgid65619921:24000
Gem extremely stony clay loam, 2 to 30 percent slopes, stony701579812672qkjid65619921:24000
Gem-Bakeoven complex 30 to 65 percent slopesGBF2814813202qm7id65919711:20000
Gem-Bakeoven complex, 2 to 30 percent slopesGBE2796813192qm6id65919711:20000
Gem and Bakeoven soils, 30 to 60 percent slopes, extremely stonyGnF12103805472pt9id66019621:15840
Gem and Bakeoven soils, 0 to 30 percent slopes, extremely stonyGnE8675805462pt8id66019621:15840
Gem very stony clay loam, 0 to 30 percent slopesGmE7613805452pt7id66019621:15840
Gem stony clay loam, 30 to 60 percent slopesGhF2105805442pt6id66019621:15840
Gem clay loam, 12 to 30 percent slopesGcE1689805422pt4id66019621:15840
Gem stony clay loam, 12 to 30 percent slopesGhE1079805432pt5id66019621:15840
Gem clay loam, 3 to 7 percent slopesGcC369805402pt2id66019621:15840
Gem clay loam, 7 to 12 percent slopesGcD334805412pt3id66019621:15840
Gem-Bakeoven complex, 30 to 60 percent slopes65607237633323882qklid7001:24000
Gem-Bakeoven complex, 2 to 30 percent slopes65607111333323872qkkid7001:24000
Gem-Reywat complex, 30 to 65 percent slopes6560741633323892qknid7001:24000
Gem-Reywat complex, 2 to 30 percent slopes656073633324032qkmid7001:24000
Gem stony clay loam, 2 to 30 percent slopes656068333324022qkfid7001:24000
Ridley-Gem complex, 8 to 25 percent slopes7018482824822222p9ypor6451:24000

Map of Series Extent

Approximate geographic distribution of the GEM 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 .