Official Series Description


Lab Data Summary

Aggregate lab data for the AURA soil series. This aggregation is based on all pedons with a current taxon name of AURA, 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 AURA 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
149A40A0334S1958NJ015002Aura4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5922203,-74.9677811
149A40A0335S1958NJ015003Aura5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6636124,-75.0247192
149A40A0336S1958NJ015005Aura5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6138878,-75.1144409
149A85P0765S1985NJ033005Aura7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5750008,-75.1472244
153D05N0571S2005NJ029001Aura7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8550262,-74.4040298
n/a40A0321S1958NJ015001Aura4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the AURA 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 AURA 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 AURA 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 AURA 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 AURA 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 AURA 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 AURA 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 hills figure.

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.

Soil series sharing subgroup-level classification with AURA, 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. NJ-2010-09-13-01 | Cumberland County -

    Typical relationship of the soils, landform position, and parent material of soils that formed in loamy materials and sandy eolian deposits. The well drained Aura, Sassafras, Fort Mott, and Downer soils are in the higher landform positions. The moderately well drained Hammonton soils are in the lower landform positions in depressions or on flats (Soil Survey of Cumberland County, New Jersey).

  2. NJ-2010-09-13-04 | Gloucester County -

    (Soil Survey of Gloucester County, New Jersey)

  3. NJ-2012-02-14-01 | Cape May County - 2002

    The relationship of soils, landform position, and underlying material in the Downer-Ingleside-Swainton general soil map unit. Evesboro, Fort Mott, and Aura soils are minor components in the map unit (Soil Survey of Cape May County, New Jerser; 2002).

Map Units

Map units containing AURA 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
Aura gravelly sandy loam, 5 to 10 percent slopesAuC90424406802mxqmmd01520091:12000
Aura gravelly sandy loam, 2 to 5 percent slopesAuB77424406792mxqlmd01520091:12000
Aura gravelly sandy loam, 10 to 15 percent slopesAuD70224406812mxqnmd01520091:12000
Aura sandy loam, 2 to 5 percent slopes, Northern Tidewater AreaAugaB1191730503952x8s9nj00119751:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Tidewater AreaAucdB344633185402ztvznj00119751:24000
Aura sandy loam, 0 to 2 percent slopes, Northern Tidewater AreaAugaA91730503872thxynj00119751:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Coastal PlainAugdB8807458272x8s8nj00119751:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Coastal PlainAucaB5067458252ztw1nj00119751:24000
Aura variant loamy sand, 0 to 5 percent slopesAwbB503745828t12znj00119751:24000
Aura sandy loam, 0 to 2 percent slopes, Northern Coastal PlainAugdA2707458262thxxnj00119751:24000
Aura gravelly sandy loam, 2 to 5 percent slopesAuhB32784247vb29nj00119751:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Tidewater AreaAucdB13846979322ztvznj00519671:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Tidewater AreaAugaB260230503972x8s9nj00719641:12000
Aura-Downer loamy sands, 0 to 5 percent slopesAvdB2059710838rvp8nj00719641:12000
Aura loamy sand, 0 to 5 percent slopes, Northern Tidewater AreaAucdB172133185432ztvznj00719641:12000
Aura-Downer sandy loams, 0 to 5 percent slopesAveB1476710839rvp9nj00719641:12000
Aura loamy sand, 0 to 5 percent slopes, Northern Coastal PlainAucaB13307108352ztw1nj00719641:12000
Aura sandy loam, 0 to 2 percent slopes, Northern Tidewater AreaAugaA105930503892thxynj00719641:12000
Downer-Aura complex, 5 to 10 percent slopesDonC842710850rvpnnj00719641:12000
Aura sandy loam, 2 to 5 percent slopes, Northern Coastal PlainAugdB8317108372x8s8nj00719641:12000
Aura sandy loam, 0 to 2 percent slopes, Northern Coastal PlainAugdA6187108362thxxnj00719641:12000
Aura-Urban land complex, 0 to 5 percent slopesAvuB292710840rvpbnj00719641:12000
Aura sandy loam, 0 to 2 percent slopes, Northern Coastal PlainAugA11867455472thxxnj00919971:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Coastal PlainAugB5937455482x8s8nj00919971:24000
Aura gravelly sandy loam, 2 to 5 percent slopesAuhB59521359154kfcnj01120031:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Coastal PlainAugdB54771359142x8s8nj01120031:24000
Aura sandy loam, 0 to 2 percent slopes, Northern Coastal PlainAugdA45231359132thxxnj01120031:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Tidewater AreaAugaB425530503992x8s9nj01120031:24000
Aura sandy loam, 0 to 2 percent slopes, Northern Tidewater AreaAugaA345430503912thxynj01120031:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Coastal PlainAucaB23661359122ztw1nj01120031:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Tidewater AreaAucdB102233185452ztvznj01120031:24000
Aura-Urban land complex, 0 to 5 percent slopesAvuB1871359164kfdnj01120031:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Tidewater AreaAugB1827810893632x8s9nj01520041:24000
Aura-Urban land complex, 0 to 5 percent slopesAvuB5804108937315kl2nj01520041:24000
Aura-Sassafras sandy loams, 2 to 5 percent slopesAvtB4743108936915kkynj01520041:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Coastal PlainAucaB260910893612ztw1nj01520041:24000
Urban land-Aura complex, 0 to 5 percent slopesUSAURB1409108959315kt5nj01520041:24000
Aura-Sassafras loamy sands, 0 to 5 percent slopesAvsB1167108936715kkwnj01520041:24000
Aura-Sassafras sandy loams, 5 to 10 percent slopesAvtC761108937015kkznj01520041:24000
Aura-Sassafras loamy sands, 5 to 10 percent slopesAvsC613108936815kkxnj01520041:24000
Aura-Sassafras sandy loams, 5 to 10 percent slopes, erodedAvtC2390108937115kl0nj01520041:24000
Aura-Urban land complex, 5 to 10 percent slopesAvuC346108937415kl3nj01520041:24000
Aura sandy loam, 0 to 2 percent slopes, Northern Tidewater AreaAugA25510893622thxynj01520041:24000
Aura sandy loam, 5 to 10 percent slopesAugC75108936415kksnj01520041:24000
Aura loam, 2 to 5 percent slopesAupB47108936515kktnj01520041:24000
Aura sandy loam, moderately firm, 2 to 5 percent slopesAugmB5641351154jlknj02119691:24000
Aura sandy loam, moderately firm, 5 to 10 percent slopesAugmC761351164jllnj02119691:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Coastal PlainAugB20076975102x8s8nj02919781:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Tidewater AreaAucdB76976052ztvznj02919781:24000
Aura sandy loam, 2 to 5 percent slopes, Northern Tidewater AreaAugB47551357392x8s9nj03320041:24000
Aura loam, 2 to 5 percent slopesAupB37421356414k4jnj03320041:24000
Aura gravelly sandy loam, 2 to 5 percent slopesAuhB25321357404k7qnj03320041:24000
Aura loam, 0 to 2 percent slopesAupA12711356404k4hnj03320041:24000
Aura sandy loam, 5 to 10 percent slopesAugC2551355794k2jnj03320041:24000
Aura loamy sand, 0 to 5 percent slopes, Northern Coastal PlainAucaB1741357382ztw1nj03320041:24000
Aura gravelly sandy loam, 5 to 10 percent slopesAuhC1341357414k7rnj03320041:24000
Aura-Galestown-Sassafras complex, 15 to 30 percent slopesAwE104824535612nc44va15319851:15840
Aura-Galestown-Sassafras complex, 6 to 15 percent slopesAwD37824535602nc43va15319851:15840
Aura-Galestown-Sassafras complex, 15 to 30 percent slopesAwE520612048241cjva17919701:15840
Aura-Galestown-Sassafras complex, 6 to 15 percent slopesAwD275412048141chva17919701:15840
Aura gravelly fine sandy loam, 2 to 6 percent slopesAvB226512047741ccva17919701:15840
Aura gravelly fine sandy loam, 6 to 10 percent slopes, erodedAvC2156212047841cdva17919701:15840
Aura gravelly fine sandy loam, 18 to 35 percent slopes, erodedAvE2154012048041cgva17919701:15840
Aura gravelly fine sandy loam, 10 to 18 percent slopes, erodedAvD2128512047941cfva17919701:15840

Map of Series Extent

Approximate geographic distribution of the AURA 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 .