Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with NUMA 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 NUMA 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 NUMA 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.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with NUMA, 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. CO-2011-05-27-10 | Otero County - 1972

    Rocky Ford-Numa-Kornman soil association (Soil Survey of Otero County, Colorado; 1972).

  2. CO-2011-05-27-11 | Otero County - 1972

    Cross section of Otero County showing relief, drainage, and relation of soils to underlying geologic formations (Soil Survey of Otero County, Colorado; 1972).

  3. CO-2011-05-27-19 | Prowers County - 1966

    Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

Map Units

Map units containing NUMA 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
Numa clay loam, 1 to 3 percent slopesNmB6722942672rgr1co01119651:15840
Numa clay loam, 0 to 1 percent slopesNmA3993942662rgr0co01119651:15840
Numa clay loam, sand substratum, 0 to 3 percent slopesNvB1506942692yz4cco01119651:15840
Numa clay loam, wet, 0 to 3 percent slopesNuB1051942682yz4bco01119651:15840
Numa clay loam, 0 to 1 percent slopesNmA5052943832rgr0co02519651:15840
Numa clay loam, 1 to 3 percent slopesNmB4919943842rgr1co02519651:15840
Numa clay loam, 1 to 3 percent slopesNmB902626111512rgr1co08919661:15840
Kornman-Numa clay loams, 0 to 1 percent slopes, very rarely floodedKnA525826111462rgqtco08919661:15840
Numa clay loam, 0 to 1 percent slopesNmA450126111502rgr0co08919661:15840
Kornman-Numa clay loams, 1 to 3 percent slopes, very rarely floodedKnB442126111472rgqvco08919661:15840
Numa clay loam, 3 to 5 percent slopesNmC153926111522rgrpco08919661:15840
Numa-Cascajo complex, 3 to 9 percent slopes, very rarely floodedNvD134326111842rgs3co08919661:15840
Kornman-Numa clay loams, wet, 0 to 3 percent slopes, very rarely floodedKnW55626111482rgr7co08919661:15840
Numa clay loam, 1 to 3 percent slopesNtB2559948602rgr1co09919631:15840
Numa clay loam, moist, 0 to 3 percent slopesNuA240028378512w4p6co09919631:15840
Numa clay loam, 3 to 5 percent slopesNtC600948612rgrpco09919631:15840
Numa clay loam, moist, 3 to 5 percent slopesNuC57129207632w4p7co09919631:15840
Numa clay loam, saline, 0 to 3 percent slopesNuB1789486235q2co09919631:15840
Numa clay loam, wet, 0 to 3 percent slopesNwB1559486335q3co09919631:15840
Numa clay loam, 0 to 1 percent slopesNtA108948592rgr0co09919631:15840
Sweatbee-Numa sandy clay loams, 0 to 3 percent slopes23227751045873htswy03119981:24000

Map of Series Extent

Approximate geographic distribution of the NUMA 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 .