Official Series Description


Lab Data Summary

Aggregate lab data for the ALBRIGHTS soil series. This aggregation is based on all pedons with a current taxon name of ALBRIGHTS, 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 ALBRIGHTS 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
14762PA0570121962PA057012Albrights4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0883333,-78.0625
14766PA1070021966PA107002Albrights4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6544444,-76.5216667
14770PA0270441970PA027044Albrights5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8438889,-77.9475

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALBRIGHTS 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 ALBRIGHTS 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 ALBRIGHTS 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 ALBRIGHTS 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ALBRIGHTS 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 ALBRIGHTS 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 ALBRIGHTS 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 ALBRIGHTS, 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. PA-2012-03-12-11 | Bedford County - 1998

    Typical pattern of soils and underlying material in the Calvin-Klinesville-Leck Kill general soil map unit (Soil Survey of Bedford County, PA; 1998).

  2. PA-2012-03-12-17 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Laidig-Hazleton-Buchanan association (Soil Survey of Blair County, PA; 1981).

  3. PA-2012-03-12-19 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Leck Kill-Meckesville-Albrights association (Soil Survey of Blair County, PA; 1981).

  4. PA-2012-03-13-06 | Cameron and Elk Counties - February 1993

    Typical pattern of soils and underlying material in the Leck Kill-Hartleton-Albrights association (Soil Survey of Cameron and Elk Counties, PA; 1993).

  5. PA-2012-03-13-61 | McKean County - August 1987

    Typical landscape pattern of the soils and the underlying material in the Buchanan-Hartleton-Leck Kill general soil map unit (Soil Survey of McKean County, PA; 1987).

  6. PA-2012-03-14-06 | Northumberland County - March 1985

    Typical pattern of soils and underlying material in the Klinesville-Calvin-Leck Kill association (Soil Survey of Northumberland County, PA; 1985).

  7. PA-2012-03-14-15 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Leck Kill-Albrights soils (Soil Survey of Somerset County, PA; 1983).

Map Units

Map units containing ALBRIGHTS 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
Albrights silt loam, 3 to 8 percent slopesAbB51605328832stxmmd02319701:20000
Albrights gravelly silt loam, 0 to 15 percent slopes, very stonyAgC49705328852sgrbmd02319701:20000
Albrights silt loam, 8 to 15 percent slopesAbC211605328842sgr2md02319701:20000
Albrights silt loam, 8 to 15 percent slopesAlC25582931349v0yny08319801:15840
Albrights very stony silt loam, 15 to 40 percent slopesAmD24932931379v11ny08319801:15840
Albrights very stony silt loam, 3 to 15 percent slopesAmC17612931369v10ny08319801:15840
Albrights silt loam, 3 to 8 percent slopesAlB15582931339v0xny08319801:15840
Albrights silt loam, 15 to 25 percent slopesAlD9102931359v0zny08319801:15840
Albrights silt loam, 8 to 15 percent slopesAbC5334541749l5qspa00919891:24000
Albrights silt loam, 3 to 8 percent slopesAbB2690541748l5qrpa00919891:24000
Albrights very stony silt loam, 8 to 25 percent slopesAcD1528542314l6b0pa01319781:20000
Albrights gravelly silt loam, 3 to 8 percent slopesAbB1063542311l69xpa01319781:20000
Albrights very stony silt loam, 3 to 8 percent slopesAcB853542313l69zpa01319781:20000
Albrights gravelly silt loam, 8 to 15 percent slopesAbC502542312l69ypa01319781:20000
Albrights silt loam, 3 to 8 percent slopesAbB6695418852stxmpa02119781:20000
Albrights silt loam, 8 to 15 percent slopesAbC3705418862sgr2pa02119781:20000
Albrights very stony loam, 0 to 8 percent slopesAcB6643539282l356pa02519601:20000
Albrights silt loam, 3 to 8 percent slopes moderately erodedAbB21909539281l355pa02519601:20000
Albrights silt loam, 0 to 3 percent slopesAbA727539280l354pa02519601:20000
Albrights very stony loam, 8 to 25 percent slopesAcD205539283l357pa02519601:20000
Albrights channery loam, 3 to 8 percent slopes moderately erodedAaB256539279l353pa02519601:20000
Albrights channery loam, 0 to 3 percent slopesAaA33539278l352pa02519601:20000
Albrights silt loam, 8 to 15 percent slopes, extremely stonyAcC17065382342sgrfpa02719751:20000
Albrights silt loam, 3 to 8 percent slopesAbB16715382312stxmpa02719751:20000
Albrights silt loam, 8 to 15 percent slopesAbC14465382322sgr2pa02719751:20000
Albrights silt loam, 0 to 8 percent slopes, extremely stonyAcB7875382332vb8mpa02719751:20000
Albrights gravelly silt loam, 3 to 8 percent slopes, moderately erodedAaB23526539436l3b5pa03719651:20000
Albrights gravelly silt loam, 8 to 15 percent slopesAaC551539437l3b6pa03719651:20000
Albrights gravelly silt loam, 0 to 3 percent slopesAaA259539435l3b4pa03719651:20000
Albrights silt loam, 3 to 10 percent slopes, moderately erodedAbB21719540690l4mmpa04319671:15840
Albrights silt loam, 0 to 3 percent slopesAbA638540689l4mlpa04319671:15840
Albrights silt loam, 3 to 8 percent slopesAbgB164737593srjbpa04319671:15840
Albrights silt loam, 8 to 25 percent slopes, very stonyAeD223215911352sgrdpa05120051:24000
Albrights silt loam, 8 to 15 percent slopesAbC207415910522sgr2pa05120051:24000
Albrights silt loam, 3 to 8 percent slopesAbB167415910512stxmpa05120051:24000
Albrights silt loam, 0 to 8 percent slopes, very stonyAeB105015911342sgrcpa05120051:24000
Albrights very stony silt loam, 8 to 25 percent slopesAcD3265541950l5y8pa06119741:20000
Albrights silt loam, 3 to 8 percent slopesAbB2516541947l5y5pa06119741:20000
Albrights silt loam, 8 to 15 percent slopesAbC809541948l5y6pa06119741:20000
Albrights very stony silt loam, 0 to 8 percent slopesAcB421541949l5y7pa06119741:20000
Albrights silt loam, 3 to 8 percent slopesAbB29955390432stxmpa08119811:20000
Albrights silt loam, 8 to 15 percent slopesAbC19385390442sgr2pa08119811:20000
Albrights silt loam, 8 to 15 percent slopesAbC239575398802sgr2pa08319841:20000
Albrights silt loam, 3 to 8 percent slopesAbB86225398792stxmpa08319841:20000
Albrights silt loam, 8 to 15 percent slopes, extremely stonyAdC13365398812sgrfpa08319841:20000
Albrights silt loam, 3 to 8 percent slopesAbB133538955l2tnpa09319801:20000
Albrights silt loam, 3 to 8 percent slopesAbB1989539587l3h1pa09719801:20000
Albrights silt loam, 3 to 8 percent slopesAbB6933693894r91ppa09919801:15840
Albrights silt loam, 8 to 15 percent slopesAbC1889693895r91qpa09919801:15840
Albrights silt loam, 3 to 8 percent slopesAbB626540778l4qgpa10919801:20000
Albrights silt loam, 3 to 8 percent slopesAbB25425420492stxmpa11119771:20000
Albrights silt loam, 0 to 8 percent slopes, very stonyAgB12715420512sgrcpa11119771:20000
Albrights silt loam, 8 to 15 percent slopesAbC11245420502sgr2pa11119771:20000
Albrights silt loam, 8 to 25 percent slopes, very stonyAgD10545420522sgrdpa11119771:20000
Albrights silt loam, 3 to 8 percent slopesAbB2001540873l4tjpa11919801:20000
Albrights silt loam, 8 to 25 percent slopes, very stonyAlD11815573602sgrdpa12920031:24000
Albrights silt loam, 0 to 8 percent slopes, very stonyAlB3595573612sgrcpa12920031:24000
Albrights silt loam, 8 to 15 percent slopesAbC34275391492sgr2pa60719861:20000
Albrights silt loam, 15 to 25 percent slopesAbD1391539150l30ypa60719861:20000
Albrights silt loam, 3 to 8 percent slopesAbB12505391482stxmpa60719861:20000
Albrights silt loam, 3 to 8 percent slopesAbB150817113822stxmwv07719551:24000
Albrights silt loam, 8 to 15 percent slopesAbC69318842692sgr2wv07719551:24000
Albrights gravelly silt loam, 0 to 15 percent slopes, very stonyAgC1018686752sgrbwv07719551:24000
Albrights silt loam, moist, 3 to 8 percent slopesAbB9385139532stxnwv60219651:20000
Albrights silt loam, moist, 8 to 15 percent slopesAbC1305139542sgr3wv60219651:20000
Albrights silt loam, 3 to 8 percent slopesAbB824555853lndrwv60819731:20000
Albrights silt loam, 8 to 15 percent slopesAbC500555854lndswv60819731:20000

Map of Series Extent

Approximate geographic distribution of the ALBRIGHTS 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 .