Official Series Description


Lab Data Summary

Aggregate lab data for the BENSON soil series. This aggregation is based on all pedons with a current taxon name of BENSON, 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 BENSON 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/a40A5415S1956VT013002Benson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BENSON 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 BENSON 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 BENSON 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 BENSON 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 BENSON 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 BENSON 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 BENSON 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 BENSON, 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. NY-2012-02-15-19 | Genesee County - March 1969

    A typical cross section of the Cazenovia-Ovid association, the Benson-Honeoye, moderately deep, association, and the Onondaga limestone escarpment (Soil Survey of Genesee County, New York; March 1969).

Map Units

Map units containing BENSON 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
Benson silt loam, 0 to 8 percent slopesBeB343301808b41rme60719601:20000
Benson silt loam, 8 to 15 percent slopesBeC324301809b41sme60719601:20000
Benson silt loam, 15 to 25 percent slopesBeD173301810b41tme60719601:20000
Aurora, Farmington, and Benson very rocky soils, 20 to 70 percent slopesAzF31632893669q3dny01119681:15840
Benson loam, 1 to 8 percent slopesBeB8092893689q3gny01119681:15840
Benson very rocky loam, 2 to 20 percent slopesBkD3222893709q3jny01119681:15840
Benson loam, 8 to 14 percent slopesBeC2132893699q3hny01119681:15840
Gardenisle-Benson complex, strongly sloping, rockyGfC19342901599qxzny01919951:24000
Benson loam, strongly sloping, very rockyBhC11602901129qwgny01919951:24000
Benson loam, steep, very rockyBhE1772901139qwhny01919951:24000
Benson very channery loam, 0 to 3 percent slopesBfA18282907499rk0ny02919791:15840
Benson very channery loam, 3 to 8 percent slopesBfB5052907509rk1ny02919791:15840
Benson-Rock outcrop complex, 3 to 8 percent slopesBhB3522907529rk3ny02919791:15840
Urban land-Benson complex, 3 to 6 percent slopesUeB2102909109rq6ny02919791:15840
Benson very channery loam, very rocky, 8 to 15 percent slopesBgC2002907519rk2ny02919791:15840
Benson soils, 0 to 8 percent slopesBeB4750301673b3xdny03720041:24000
Benson soils, 8 to 25 percent slopesBeD722301674b3xfny03720041:24000
Benson soils, 25 to 40 percent slopesBeE366301675b3xgny03720041:24000
Benson-Galoo complex, very rocky, 0 to 8 percent slopesBgB311922917709slyny04519811:15840
Benson channery silt loam, very rocky, 25 to 50 percent slopesBfF40182917699slxny04519811:15840
Benson loam, 0 to 8 percent slopes, very rocky210B297631057702ywkvny05120191:24000
Benson channery loam, 0 to 8 percent slopesBcB20482926699tjyny05519671:15840
Benson silt loam, undulatingBeB40832935339vftny06719731:20000
Benson-Wassaic-Rock outcrop association, slopingBNC31262935309vfqny06719731:20000
Benson-Wassaic-Rock outcrop association, very steepBNF14162935319vfrny06719731:20000
Benson silt loam, rollingBeC3572935349vfvny06719731:20000
Wassaic-Benson silt loams, moderately steepWDD2892936659vl2ny06719731:20000
Benson-Rock outcrop complex, 8 to 25 percent slopesBeC60002962789y9cpa08919751:20000
Benson-Rock outcrop complex, 25 to 70 percent slopesBeF56802962799y9dpa08919751:20000
Benson-Rock outcrop complex, 0 to 8 percent slopesBeB17722962779y9bpa08919751:20000
Benson rocky silt loam, over shaly limestone, 3 to 8 percent slopesBeB52652792349ckkvt01319561:20000
Benson rocky silt loam, over shaly limestone, 8 to 15 percent slopesBeC29042792359cklvt01319561:20000
Benson very rocky loam, over massive limestone, 3 to 8 percent slopesBdB13972792299ckdvt01319561:20000
Benson rocky silt loam, over shaly limestone, 15 to 25 percent slopesBeD10012792369ckmvt01319561:20000
Benson very rocky loam, over massive limestone, 8 to 15 percent slopesBdC5992792309ckfvt01319561:20000
Benson rocky loam, over massive limestone, 3 to 8 percent slopesBcB5302792269ck9vt01319561:20000
Benson rocky silt loam, over shaly limestone, 0 to 3 percent slopesBeA1662792339ckjvt01319561:20000
Benson very rocky loam, over massive limestone, 15 to 25 percent slopesBdD1302792319ckgvt01319561:20000
Benson rocky loam, over massive limestone, 8 to 15 percent slopesBcC1012792279ckbvt01319561:20000
Benson rocky silt loam, over shaly limestone, 25 to 35 percent slopesBeE872792379cknvt01319561:20000
Benson very rocky silt loam, over shaly limestone, 8 to 15 percent slopesBfC832792409ckrvt01319561:20000
Benson rocky silt loam, over shaly limestone, 35 to 50 percent slopesBeF802792389ckpvt01319561:20000
Benson very rocky loam, over massive limestone, 25 to 35 percent slopesBdE652792329ckhvt01319561:20000
Benson very rocky silt loam, over shaly limestone, 3 to 8 percent slopesBfB292792399ckqvt01319561:20000
Benson very rocky silt loam, over shaly limestone, 15 to 25 percent slopesBfD272792419cksvt01319561:20000
Benson rocky loam, over massive limestone, 0 to 3 percent slopesBcA262792259ck8vt01319561:20000
Benson very rocky loam, over massive limestone, 0 to 3 percent slopesBdA222792289ckcvt01319561:20000
Benson very rocky silt loam, over shaly limestone, 25 to 50 percent slopesBfE152792429cktvt01319561:20000
Benson very channery loam, 15 to 25 percent slopes140D4872821819gmmvt02119851:20000
Benson very channery loam, 25 to 50 percent slopes140E3302821829gmnvt02119851:20000
Benson very channery loam, 3 to 15 percent slopes140C2592821809gmlvt02119851:20000

Map of Series Extent

Approximate geographic distribution of the BENSON 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 .