Official Series Description


Lab Data Summary

Aggregate lab data for the BIRDSBORO soil series. This aggregation is based on all pedons with a current taxon name of BIRDSBORO, 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 BIRDSBORO 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
14769PA0090061969PA009006Birdsboro5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1602778,-78.5266667

Water Balance

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

Soil series sharing subgroup-level classification with BIRDSBORO, 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 BIRDSBORO 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
Birdsboro silt loam, 3 to 8 percent slopesBfB142024939572pqs6md01320101:12000
Birdsboro silt loam, 0 to 3 percent slopesBfA39724939562pqs5md01320101:12000
Birdsboro silt loam, 8 to 15 percent slopesBfC15824957612pthxmd01320101:12000
Birdsboro silt loam, 3 to 8 percent slopesBgB258534771kygpmd02120011:12000
Birdsboro silt loam, 0 to 3 percent slopesBgA246534770kygnmd02120011:12000
Birdsboro silt loam, 2 to 6 percent slopesBhnB1635548581ldv5nj01919701:24000
Birdsboro silt loam, 0 to 2 percent slopesBhnA412548580ldv4nj01919701:24000
Birdsboro silt loam, 6 to 12 percent slopes, erodedBhnC2411548582ldv6nj01919701:24000
Birdsboro sandy subsoil variant soils, 2 to 6 percent slopesBHRSB7681351234jltnj02119691:24000
Birdsboro gravelly solum variant soils, 0 to 6 percent slopesBHSGB75014453681kj0snj02119691:24000
Birdsboro silt loam, 2 to 6 percent slopesBhnB38314453621kj0lnj02119691:24000
Birdsboro sandy subsoil variant soils, 6 to 12 percent slopesBHRSC30414453661kj0qnj02119691:24000
Birdsboro loam, 2 to 6 percent slopesBhmB19514453591kj0hnj02119691:24000
Birdsboro loam, 6 to 12 percent slopes, erodedBhmC218014822141lrccnj02119691:24000
Birdsboro loam, 2 to 6 percent slopes, erodedBhmB216514453601kj0jnj02119691:24000
Birdsboro silt loam, 0 to 2 percent slopesBhnA15314453611kj0knj02119691:24000
Birdsboro sandy subsoil variant soils, 0 to 2 percent slopesBHRSA12814453631kj0mnj02119691:24000
Birdsboro silt loam, 2 to 6 percent slopesBhnB16414453511kj07nj02319851:24000
Birdsboro, rarely flooded-Urban land complex, 0 to 8 percent slopesBhpBr10714551531kv6fnj02319851:24000
Birdsboro silt loam, 6 to 12 percent slopesBhnC314453521kj08nj02319851:24000
Birdsboro silt loam, 2 to 6 percent slopesBhnB2914829571ls4bnj02719741:24000
Birdsboro silt loam, 2 to 6 percent slopesBhnB515114050171j514nj03519721:24000
Birdsboro silt loam, 0 to 2 percent slopesBhnA46414050011j50mnj03519721:24000
Birdsboro silt loam, 6 to 12 percent slopesBhnC43814050181j515nj03519721:24000
Birdsboro silt loam, 2 to 6 percent slopes, rarely floodedBhnBr27414730831lfvtnj03519721:24000
Birdsboro-Urban land complex, 0 to 6 percent slopes, rarely floodedBhpBr242014526631krm3nj03919891:24000
Birdsboro silt loam, 2 to 6 percent slopes, rarely floodedBhnBr35914440471kgn5nj03919891:24000
Birdsboro silt loam, 3 to 8 percent slopesBgB1974545557l9pmpa00119911:24000
Birdsboro silt loam, 0 to 3 percent slopesBgA292545556l9plpa00119911:24000
Birdsboro silt loam, 8 to 15 percent slopesBgC226545558l9pnpa00119911:24000
Basher-Birdsboro complex, 0 to 8 percent slopesBbB6383541759l5r3pa00919891:24000
Birdsboro silt loam, rarely floodedBm2872541769l5rfpa00919891:24000
Birdsboro silt loam, 3 to 8 percent slopesBmB2870542982l70kpa01119971:24000
Birdsboro silt loam, 0 to 3 percent slopesBmA89542981l70jpa01119971:24000
Birdsboro silt loam, 0 to 5 percent slopesBoA179693689r8v2pa04119801:15840
Birdsboro gravelly loam, 2 to 10 percent slopesBnB1127541964l5yqpa06119741:20000
Birdsboro silt loam, 3 to 8 percent slopesBmB360543117l74xpa07719971:24000
Birdsboro silt loam, 0 to 3 percent slopesBmA27543116l74wpa07719971:24000
Birdsboro silt loam, 0 to 3 percent slopesBnA292541148l53dpa09120081:12000
Birdsboro silt loam, 3 to 8 percent slopesBnB18423791162kvnppa09120081:12000
Birdsboro silt loam, 0 to 5 percent slopesBoA1753693914r92bpa09919801:15840
Birdsboro silt loam, rarely floodedBm66542129l641pa11119771:20000
Basher-Birdsboro complex, 0 to 8 percent slopesBbB15542128l640pa11119771:20000
Birdsboro silt loam, 3 to 8 percent slopesBgB997542811l6v1pa13319901:24000
Birdsboro silt loam, 0 to 3 percent slopesBgA156542810l6v0pa13319901:24000
Birdsboro silt loam, 8 to 15 percent slopesBgC32542812l6v2pa13319901:24000
Birdsboro loam, 2 to 7 percent slopes9B32922502612fjl2va05920071:12000
Chantilly-Birdsboro complex, 2 to 7 percent slopes16B6822502762fjlkva05920071:12000
Birdsboro loam2508521081kh72va06919831:15840
Birdsboro loam, 7 to 15 percent slopes72C1072642107pk54va10720061:12000

Map of Series Extent

Approximate geographic distribution of the BIRDSBORO 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 .