Official Series Description


Lab Data Summary

Aggregate lab data for the NAMELA soil series. This aggregation is based on all pedons with a current taxon name of NAMELA, 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 NAMELA 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
48A90P098790CO077007Namela7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1022224,-107.8744431

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NAMELA 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 NAMELA 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 NAMELA 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 NAMELA 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 NAMELA 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 NAMELA 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 NAMELA 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 NAMELA, 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 NAMELA 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
Namela-Rogert, very flaggy-Rock outcrop complex, 35 to 75 percent slopes388115509336k306co6471:24000
Namela cobbly loam, 25 to 75 percent slopes, extremely bouldery161508507034k0lyco6481:24000
Irson-Namela-Doughspon, well drained complex, 0 to 10 percent slopes, extremely stony1645775509526k36bco66019941:24000
Namela, moist-Bullbasin-Doughspon complex, 0 to 10 percent slopes1684602509530k36gco66019941:24000
Irson-Namela complex, 25 to 65 percent slopes1632186509525k369co66019941:24000
Namela-Cheadle channery loams, 5 to 50 percent slopes805930496926jp2wco68419841:24000
Adel-Namela-Splitro complex, 5 to 25 percent slopes35567496870jp12co68419841:24000
Gothic-Rhone-Namela complex, 5 to 25 percent slopes493267496891jp1rco68419841:24000
Adel-Namela-Splitro complex, 25 to 65 percent slopes42715496881jp1fco68419841:24000
Gothic-Rhone-Namela complex, 25 to 65 percent slopes50904496893jp1tco68419841:24000
Namela-Adel-Hapgood complex, 5 to 25 percent slopes79787496924jp2tco68419841:24000
Quietus family-Mikesell-Namela family, very stony surface, complex, 5 to 30 percent slopes1051538429808412x003id7131:24000
Hourglass family, extremely stony surface-Stringam-Namela family, extremely stony surface, complex, 10 to 60 percent slopes809430127334352slr0id7131:24000
Quietus-Starley, very stony surface-Namela, very stony surface, families, complex, 8 to 30 percent slopes1072b429329808572x00mid7131:24000
Namela, extremely stony surface-Bickmore families, complex, 40 to 75 percent slopes842158627334522slrpid7131:24000
Ericson, high effective precipitation-Ericson-Namela families, complex, 5 to 55 percent slopes978109229638842wv3cid7131:24000
Namela, extremely stony surface-Bickmore families, complex, 40 to 75 percent slopes84231228586482slrpid75819981:24000
Hourglass family, extremely stony surface-Stringam-Namela family, extremely stony surface, complex, 10 to 60 percent slopes80912928586402slr0id75819981:24000

Map of Series Extent

Approximate geographic distribution of the NAMELA 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 .