Official Series Description


Lab Data Summary

Aggregate lab data for the BUCKS soil series. This aggregation is based on all pedons with a current taxon name of BUCKS, 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 BUCKS 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
14840A0368S1956PA029008Bucks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1733322,-75.6038895

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BUCKS 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 BUCKS 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 BUCKS 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 BUCKS 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 flats position figure.

Competing Series

Soil series competing with BUCKS 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 BUCKS 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 BUCKS 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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Soil series sharing subgroup-level classification with BUCKS, 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 BUCKS 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
Bucks silt loam, 0 to 3 percent slopesBuA142824957682ptj4md01320101:12000
Bucks silt loam, 3 to 8 percent slopesBuB130624957692ptj5md01320101:12000
Bucks silt loam, 3 to 8 percent slopes19B1863533589kx7kmd03119891:15840
Goresville and Bucks soils, 3 to 8 percent slopesGbB12585336672v7hjmd03119891:15840
Goresville and Bucks soils, 8 to 15 percent slopesGbC4735336682v7hkmd03119891:15840
Bucks silt loam, 0 to 3 percent slopes19A311533588kx7jmd03119891:15840
Bucks silt loam, 2 to 6 percent slopesBucB6652548584ldv8nj01919701:24000
Penn-Bucks complex, 2 to 6 percent slopesPepB426314784891lmh6nj01919701:24000
Bucks silt loam, 6 to 12 percent slopes, erodedBucC2116514784201lmdznj01919701:24000
Penn-Bucks complex, 6 to 12 percent slopes, erodedPepC292914784901lmh7nj01919701:24000
Bucks silt loam, 2 to 6 percent slopesBucB1008114453761kj11nj02119691:24000
Bucks silt loam, 6 to 12 percent slopes, erodedBucC2156314823831lrjtnj02119691:24000
Bucks silt loam, 2 to 6 percent slopes, erodedBucB2149114823821lrjsnj02119691:24000
Bucks silt loam, 0 to 2 percent slopesBucA96814453751kj10nj02119691:24000
Bucks silt loam, 6 to 12 percent slopesBucC49914823811lrjrnj02119691:24000
Bucks silt loam, 2 to 6 percent slopesBucB320614049921j50bnj03519721:24000
Bucks silt loam, 6 to 12 percent slopes, erodedBucC263514049931j50cnj03519721:24000
Penn-Bucks complex, 6 to 12 percent slopes, erodedPepC26914050751j530nj03519721:24000
Penn-Bucks complex, 2 to 6 percent slopesPepB614050741j52znj03519721:24000
Bucks silt loam, 3 to 8 percent slopesBuB13816542729l6rdpa07119821:15840
Bucks silt loam, 8 to 15 percent slopesBuC5663542730l6rfpa07119821:15840
Bucks silt loam, 15 to 25 percent slopesBuD918542731l6rgpa07119821:15840
Bucks very stony silt loam, 8 to 25 percent slopesBxC477542732l6rhpa07119821:15840
Bucks silt loam, 0 to 3 percent slopesBuA364542728l6rcpa07119821:15840
Bucks silt loam, 3 to 8 percent slopesByB1807541279l57mpa07519761:20000
Bucks loam, permeable substratum, 2 to 7 percent slopes, erodedBsB376516937kbxdva11319671:15840
Bucks loam, permeable substratum, 7 to 15 percent slopes, erodedBsC2134516938kbxfva11319671:15840
Bucks silt loam, 2 to 7 percent slopes, moderately erodedBsB218881197922z1vyva13719661:15840
Bucks silt loam, conglomerate substratum, 7 to 15 percent slopes, moderately erodedBtC27841197952z1w1va13719661:15840
Bucks silt loam, 7 to 15 percent slopes, moderately erodedBsC27721197932z1vzva13719661:15840
Bucks silt loam, conglomerate substratum, 2 to 7 percent slopes, moderately erodedBtB27401197942z1w0va13719661:15840
Bucks silty clay loam, 7 to 15 percent slopes, severely erodedBuC313611979640ndva13719661:15840

Map of Series Extent

Approximate geographic distribution of the BUCKS 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 .