Official Series Description


Lab Data Summary

Aggregate lab data for the LUMBEE soil series. This aggregation is based on all pedons with a current taxon name of LUMBEE, 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 LUMBEE 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
n/a40A5175S1955NC049002Lumbee4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LUMBEE 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 LUMBEE 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 LUMBEE 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 LUMBEE 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 LUMBEE 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 LUMBEE 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 LUMBEE 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 LUMBEE, 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 LUMBEE 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
Lumbee fine sandy loamLum581512492545zvga22919651:20000
Lumbee fine sandy loamLu34971155453w78nc01919831:24000
Lumbee fine sandy loamLu35701156523wbqnc04719861:24000
Lumbee sandy loam, 0 to 1 percent slopes, rarely floodedLuA19860186597920mpwnc06119551:24000
Lumbee fine sandy loamLu43691015566132s6nc06519761:20000
Lumbee sandy loamLu60741128083scznc07919781:24000
Lumbee sandy loamLu62911160103wq8nc10719731:20000
Lumbee fine sandy loam, occasionally floodedLu42751161773wwnnc14119861:24000
Lumbee sandy loamLu195021147733vfcnc15519721:20000
Lumbee sandy loamLm78621150573vqjnc16319821:24000
Lumbee sandy loam, 0 to 2 percent slopes, rarely floodedLuA171214123641jdp4nc16520061:12000
Lumbee sandy loamLv60681162503wz0nc19119681:20000
Lumbee loam, 0 to 2 percent slopes, frequently floodedLuA7361381184mqfsc00919971:24000
Lumbee sandy loam, 0 to 2 percent slopesLmA1638619153ns8psc03119981:24000
Lumbee sandy loamLm17101297584c0rsc03319761:20000
Lumbee fine sandy loam, occasionally floodedLm45001298124c2hsc03519851:20000
Lumbee sandy loam, 0 to 2 percent slopes, rarely floodedLuA49016065871qxsdsc06120051:24000
Lumbee sandy loamLw20731305264ctjsc06319721:20000
Lumbee sandy loamLm19951305734cw1sc06719751:20000
Lumbee loamy sand, frequently floodedLu215411308944d6dsc07519851:20000
Lumbee loamy sandLm17441308934d6csc07519851:20000
Lumbee-Johns complex, 0 to 2 percent slopes, rarely floodedLbA108124859282pft7sc08519691:20000
Lumbee-Rutlege complex, 0 to 2 percent slopesLeA79624859312pftbsc08519691:20000
Meggett-Lumbee complex, 0 to 2 percent slopes, rarely floodedMeA17424859602pfv8sc08519691:20000
Lumbee loamy sandLu2493115149117n6wsc66519731:24000
Lumbee sandy loam1681161189483zs1va07319781:15840
Lumbee variant sandy loam1718831189493zs2va07319781:15840
Lumbee silt loam1226911963140h2va11919821:15840
Lumbee loam96791203794186va15919801:20000
Lumbee loam10885312059041h0va19319801:20000

Map of Series Extent

Approximate geographic distribution of the LUMBEE 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 .