Official Series Description


Lab Data Summary

Aggregate lab data for the NORMANGEE soil series. This aggregation is based on all pedons with a current taxon name of NORMANGEE, 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 NORMANGEE 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 NORMANGEE 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 NORMANGEE 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 NORMANGEE 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 NORMANGEE 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with NORMANGEE 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 NORMANGEE 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 NORMANGEE 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.

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 NORMANGEE, 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. TX-2010-11-02-18 | Burleson County - 2005

    Typical pattern of soils in the Benchley-Crockett general soil map unit (Soil Survey of Burleson County, Texas; 2005).

  2. TX-2010-11-03-53 | Lee County - 2007

    Landscape and parent material of the Luling-Benchley-Crockett general soil map unit (Soil Survey of Lee County, Texas; 2007).

Map Units

Map units containing NORMANGEE 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
Normangee loam, 3 to 5 percent slopes, eroded3124713382015dtj2ok01919771:24000
Normangee loam, 3 to 5 percent slopes304059382014dtj1ok01919771:24000
Normangee clay loam, 3 to 5 percent slopes, severely eroded322035382016dtj3ok01919771:24000
Normangee clay loam, 3 to 8 percent slopesNoD1452575161m9hltx00119701:20000
Normangee clay loam, 1 to 3 percent slopesNoB6685751602vtgttx00119701:20000
Normangee clay loam, 3 to 5 percent slopesNoC54173634582vthgtx05119941:24000
Normangee clay loam, 1 to 5 percent slopes, eroded5713087364508d79btx09719731:24000
Normangee clay loam, 1 to 3 percent slopes567140364507d799tx09719731:24000
Normangee and Crockett soils, 3 to 8 percent slopes, severely eroded581749364509d79ctx09719731:24000
Normangee clay loam, 1 to 3 percent slopes5316263648372vtgstx11319751:20000
Normangee clay loam, 0 to 2 percent slopesPcA21283653222vv4wtx13919621:20000
Normangee and Silawa soils, 1 to 3 percent slopesPnB1929365323d84mtx13919621:20000
Normangee clay loam, 2 to 5 percent slopes, moderately eroded4243243654622vv4xtx14519751:20000
Normangee clay loam, 1 to 3 percent slopes4124033654612vtgstx14519751:20000
Normangee clay loam, 0 to 2 percent slopes404153654602vv4wtx14519751:20000
Normangee clay loam, 1 to 3 percent slopesNoB169123655382vtgttx14719891:24000
Normangee clay loam, 2 to 5 percent slopes, erodedNoC278023655392vthftx14719891:24000
Normangee clay loam, 3 to 5 percent slopesNmC42463657382vthgtx14919911:24000
Normangee sandy clay loam, 1 to 3 percent slopesNmB5019366538d9dttx17719971:24000
Normangee sandy clay loam, 3 to 5 percent slopesNmC4205366539d9dvtx17719971:24000
Normangee clay loam, 1 to 3 percent slopes52474903666902vtgstx18119771:20000
Normangee soils, 3 to 8 percent slopes, severely eroded554640366693d9kttx18119771:20000
Normangee clay loam, 4 to 8 percent slopes534532366691d9krtx18119771:20000
Normangee-Urban land complex, 1 to 4 percent slopes543166366692d9kstx18119771:20000
Normangee clay loam, 2 to 5 percent slopes, eroded2816263676182vthftx21319781:20000
Normangee clay loam, 3 to 5 percent slopes62163093677782vthjtx21719751:20000
Normangee clay loam, 1 to 3 percent slopes61119373677772vtgstx21719751:20000
Normangee clay loam, 0 to 2 percent slopes6026333677762vv4wtx21719751:20000
Normangee clay loam, 3 to 5 percent slopesNoC31417480652vthgtx28720021:24000
Normangee clay loam, 1 to 3 percent slopesNoB98873694112vtgstx29319911:24000
Normangee gravelly clay loam, 3 to 8 percent slopes, erodedNrD23879369412dddjtx29319911:24000
Normangee clay loam, 1 to 3 percent slopesNoB26823706842vtgstx33119881:24000
Normangee clay loam, 1 to 3 percent slopesKpB27155755942sshgtx33919671:20000
Normangee soils, 0 to 1 percent slopesKnA427575593m9yjtx33919671:20000
Normangee clay loam, 3 to 8 percent slopes, severely erodedNoC21669373059dj65tx46719941:24000
Normangee gravelly clay loam, 3 to 8 percent slopes, erodedNoD237455761162vthhtx60319841:24000
Normangee clay loam, 2 to 8 percent slopes, erodedNoC24058374491dkpctx61219731:20000
Normangee clay loam, 1 to 3 percent slopes36250733933662vtgttx61419751:20000
Normangee clay loam, 2 to 5 percent slopes, eroded37244243933672vthftx61419751:20000

Map of Series Extent

Approximate geographic distribution of the NORMANGEE 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 .