Official Series Description


Lab Data Summary

Aggregate lab data for the RARITAN soil series. This aggregation is based on all pedons with a current taxon name of RARITAN, 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 RARITAN 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
14779PA0990181979PA099018Raritan5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3544444,-77.3730556
14779PA0990191979PA099019Raritan5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.34,-77.3369444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RARITAN 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 RARITAN 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 RARITAN 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 RARITAN 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 RARITAN 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 RARITAN 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 RARITAN 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 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 RARITAN, 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 RARITAN 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
Raritan silt loam, 0 to 3 percent slopesRaA48424960342ptnkmd01320101:12000
Raritan silt loam, 0 to 3 percent slopes, rarely floodedRarAr142014277861jxqmnj01919701:24000
Raritan silt loam, 3 to 8 percent slopesRarB136914277871jxqnnj01919701:24000
Raritan silt loam, 0 to 3 percent slopes, rarely floodedRarAr4451548521lds7nj03519721:24000
Raritan-Urban land-Passaic complex, 0 to 3 percent slopes, rarely floodedRasAr1444298722b0v6nj03919891:24000
Raritan silt loam, 0 to 3 percent slopes, rarely floodedRarAr17414440621kgnnnj03919891:24000
Raritan silt loam, 0 to 3 percent slopesRaA219545637l9s6pa00119911:24000
Raritan silt loam, 3 to 8 percent slopesRaB52545638l9s7pa00119911:24000
Raritan silt loam, 3 to 8 percent slopesRaB1173543068l73bpa01119971:24000
Raritan silt loam, 3 to 8 percent slopesRaB70543710l7s1pa01719971:24000
Raritan silt loam, 0 to 3 percent slopesRaA46543709l7s0pa01719971:24000
Raritan silt loam, 8 to 15 percent slopesRaC12543711l7s2pa01719971:24000
Raritan silt loam, 3 to 8 percent slopesRaB12641370pjdcpa02920081:24000
Raritan silt loam, 2 to 10 percent slopesRaB630542038l613pa06119741:20000
Raritan silt loam, 0 to 3 percent slopesRaA656541245l56jpa09120081:12000
Raritan silt loam, 3 to 8 percent slopesRaB45922326242dy74pa09120081:12000
Raritan silt loam, 0 to 5 percent slopesRaA853694016r95mpa09919801:15840
Raritan silt loam, 3 to 8 percent slopesRaB1053542945l6zcpa13319901:24000
Raritan silt loam, 0 to 3 percent slopesRaA516542944l6zbpa13319901:24000

Map of Series Extent

Approximate geographic distribution of the RARITAN 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 .