Official Series Description


Lab Data Summary

Aggregate lab data for the SUSQUEHANNA soil series. This aggregation is based on all pedons with a current taxon name of SUSQUEHANNA, 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 SUSQUEHANNA 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
133A06N0855S06MS039001Susquehanna7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9269447,-88.672142
133A81P0559S1981MS039001Susquehanna7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9424992,-88.6844406
13840A5101S1960FL121035SUSQUEHANNA6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1602345,-82.9623795

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SUSQUEHANNA 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 SUSQUEHANNA 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 SUSQUEHANNA 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 SUSQUEHANNA 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 SUSQUEHANNA 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 SUSQUEHANNA 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 SUSQUEHANNA 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.

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

Soil series sharing subgroup-level classification with SUSQUEHANNA, 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. FL-2011-05-31-16 | Suwannee County - 1965

    Marine terraces in Suwannee County, and the position of some of the soils (Soil Survye of Suwannee County, Florida; 1965).

  2. FL-2012-04-25-01 | Gadsden County - January 1961

    Main geologic formations and other topographic features in a segment of Gadsden County, and the positions of soils in some soil series (Soil Survey of Gadsden County, Florida; January 1961).

  3. FL-2012-04-25-03 | Gadsden County - January 1961

    Geologic formations and some principal soils in relative positions (Soil Survey of Gadsden County, Florida; January 1961).

Map Units

Map units containing SUSQUEHANNA 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
Susquehanna claySe839329295c1nfal05119481:20000
Susquehanna fine sandy loam, 8 to 15 percent slopesSuD21829950662x5r5al09720181:24000
Susquehanna fine sandy loam, 2 to 5 percent slopesSuB20129950092w9wyal09720181:24000
Susquehanna fine sandy loam, 5 to 8 percent slopesSuC9329950102w8ypal09720181:24000
Susquehanna fine sandy loam, eroded, 5 to 12 percent slopesSoD21660330988c3f1al10119581:20000
Susquehanna fine sandy loam, eroded, nearly level phaseSoB21616330986c3dzal10119581:20000
Susquehanna fine sandy loam, eroded, very gently sloping phaseSoC2442330987c3f0al10119581:20000
Susquehanna fine sandy loam, 2 to 5 percent slopesSuB160626421352w9wyal12920131:24000
Susquehanna fine sandy loam, 5 to 8 percent slopesSuC41926421362w8ypal12920131:24000
Lorman-Freest-Susquehanna complex, 5 to 15 percent slopesLqD27926420992x597al12920131:24000
Lorman-Freest-Susquehanna complex, 15 to 35 percent slopesLqF7826421002rjs8al12920131:24000
Susquehanna very fine sandy loam, 3 to 8 percent slopes erodedSvC25118565330lz8gar02519651:15840
Susquehanna very fine sandy loam 1 to 3 percent slopes, erodedSvB22075565329lz8far02519651:15840
Susquehanna very fine sandy loam, 8 to 25 percent slopesSvE1007565331lz8har02519651:15840
Susquehanna silty clay, 0 to 1 percent slopesSuA432565326lz8bar02519651:15840
Susquehanna very fine sandy loam 0 to 1 percent slopesSvA396565328lz8dar02519651:15840
Susquehanna silty clay, 1 to 3 percent slopesSuB208565327lz8car02519651:15840
Susquehanna loamy sand, 2 to 8 percent slopesSpC95324559bwqnga03119651:20000
Sawyer-Susquehanna cobbly loamy sands, 2 to 8 percent slopes, erodedSSC2615324660bwtxga09519651:20000
Sawyer-Susquehanna loamy sands, 2 to 5 percent slopes, erodedSUB2610324661bwtyga09519651:20000
Sawyer-Susquehanna cobbly loamy sands, 0 to 5 percent slopesSSB595324659bwtwga09519651:20000
Susquehanna sandy loam, 2 to 8 percent slopesSuC6170324781bwytga10719931:20000
Susquehanna loamy sand, 2 to 5 percent slopes, erodedSpB22345324826bx08ga16519661:20000
Susquehanna loamy sand, 5 to 8 percent slopes, erodedSpC21245324827bx09ga16519661:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB56012484845xcga21519801:15840
Susquehanna sandy loam, 5 to 8 percent slopesSuC49012484945xdga21519801:15840
Susquehanna sandy loam, 2 to 5 percent slopesSuB119324951bx49ga27719791:20000
Susquehanna sandy loam, 2 to 5 percent slopesSiB620324993bx5nga28319621:20000
Susquehanna sandy loam, 5 to 8 percent slopes, erodedSiC2530324996bx5rga28319621:20000
Susquehanna sandy loam, 5 to 8 percent slopesSiC335324995bx5qga28319621:20000
Susquehanna sandy loam, 2 to 5 percent slopes, erodedSiB280324994bx5pga28319621:20000
Susquehanna sandy loam, 2 to 8 percent slopes, erodedSiC26155325079bx8fga28919601:20000
Susquehanna sandy loam, 8 to 17 percent slopes, erodedSiE23295325080bx8gga28919601:20000
Oktibbeha-Eutaw-Susquehanna complex, 5 to 12 percent slopes, erodedOfD21005325068bx82ga28919601:20000
Oktibbeha-Eutaw-Susquehanna complex, 2 to 5 percent slopes, erodedOfB2630325067bx81ga28919601:20000
Susquehanna sandy clay loam, 8 to 12 percent slopes, severely erodedSjD3575325082bx8jga28919601:20000
Susquehanna sandy clay loam, 2 to 8 percent slopes, severely erodedSjC3225325081bx8hga28919601:20000
Susquehanna (telfair) loamy sand, shallow, 2 to 8 percent slopesSoC80125107465qga30519621:20000
Esto-Susquehanna loamy sands, 5 to 12 percent slopesEsD8905325111bx9gga32119851:20000
Esto-Susquehanna loamy sands, 2 to 5 percent slopesEsB6670325110bx9fga32119851:20000
Esto-Susquehanna sandy loams, 2 to 5 percent slopesEsB7285325147bxbmga60319811:20000
Esto-Susquehanna sandy loams, 5 to 8 percent slopesEsC2020325148bxbnga60319811:20000
Susquehanna fine sandy loam, 5 to 15 percent slopesSiD3125125232469rga60419721:20000
Susquehanna sandy loam, 5 to 8 percent slopes, erodedSiC21905325219bxdyga60819651:20000
Susquehanna sandy loam, 2 to 5 percent slopesSiB1591325218bxdxga60819651:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuC2925325403bxlwga61019921:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB2530325402bxlvga61019921:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuD2157325615bxtqga63119781:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB1006325614bxtpga63119781:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB3280325802by0rga63419801:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuC2230325803by0sga63419801:20000
Boswell-Susquehanna-Oktibbeha complex, 5 to 12 percent slopes, erodedBrD26470325882by3bga64019651:15840
Boswell-Susquehanna-Oktibbeha complex, 2 to 5 percent slopes, erodedBrB24145325881by39ga64019651:15840
Boswell-Susquehanna-Oktibbeha complex, 5 to 12 percent slopes, severely erodedBrD3950325883by3cga64019651:15840
Susquehanna sandy loam, 2 to 5 percent slopesSuB7440325976by6cga64119861:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuC4580325977by6dga64119861:20000
Nankin-Cowarts-Susquehanna complex, 8 to 15 percent slopesNsD4840326220byg7ga65019941:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuC3650326233bygnga65019941:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB3175326232bygmga65019941:20000
Susquehanna sandy loam, 5 to 12 percent slopesSuD7805326374bym6ga65419791:20000
Susquehanna sandy loam, 2 to 5 percent slopesSuB3435326373bym5ga65419791:20000
Memphis-Susquehanna association, hillyMSE6333567415m1fqms00119661:15840
Susquehanna-Smithdale association, hillySSE18243567455m1h0ms00519711:20000
Susquehanna soils, 2 to 5 percent slopesSuB2296332194c4nyms03119621:15840
Susqehanna soils, 5 to 8 percent slopesSuC1493332195c4nzms03119621:15840
Susquehanna soils, 8 to 17 percent slopesSuD1480332196c4p0ms03119621:15840
Petal-Susquehanna-Benndale association, rollingPEC17596332229c4q2ms03519761:20000
Susquehanna silt loam, 5 to 12 percent slopesSuD6572332239c4qdms03519761:20000
Falkner-Susquehanna-Urban land complex, 2 to 5 percent slopesFsB2846332214c4plms03519761:20000
Susquehanna silt loam, 1 to 5 percent slopesSuB17243322382w8yrms03519761:20000
Susquehanna-Benndale complex, 12 to 17 percent slopesSxE17752332284c4rvms03919671:20000
Susquehanna complex, 5 to 12 percent slopesSuD8061332282c4rsms03919671:20000
Susquehanna complex, 2 to 5 percent slopesSuB4391332281c4rrms03919671:20000
Susquehanna complex, 12 to 17 percent slopesSuE4204332283c4rtms03919671:20000
Susquehanna fine sandy loam, 2 to 5 percent slopesSnB10293322782w9wyms03919671:20000
Susquehanna fine sandy loam, 5 to 8 percent slopesSnC7683322792w8ypms03919671:20000
Susquehanna fine sandy loam, 8 to 12 percent slopesSnD373332280c4rqms03919671:20000
Lorman-Freest-Susquehanna complex, 5 to 15 percent slopesLqD3371626422042x597ms04120121:24000
Susquehanna fine sandy loam, 2 to 5 percent slopesSuB950526422462w9wyms04120121:24000
Susquehanna fine sandy loam, 5 to 8 percent slopesSuC590326422472w8ypms04120121:24000
Susquehanna-Freest complex, 2 to 8 percent slopesSvC561326422482rs3sms04120121:24000
Lorman-Freest-Susquehanna complex, 15 to 35 percent slopesLqF41326422052rrz3ms04120121:24000
Saucier-Susquehanna complex, 5 to 12 percent slopesScD5676332416c4x3ms04519791:20000
Saucier-Susquehanna complex, 2 to 5 percent slopesScB8743324152w8y1ms04519791:20000
Saucier, Smithton, and Susquehanna soils, rollingShC20513332452c4y8ms04719711:20000
Saucier-Susquehanna complex, 2 to 5 percent slopesSnB77083324532w8y1ms04719711:20000
Susquehanna-Freest complex, 1 to 5 percent slopes787107332600c531ms05919971:24000
Susquehanna-Freest complex, 5 to 8 percent slopes797075332601c532ms05919971:24000
Susquehanna silt loam, 8 to 12 percent slopes801400332603c534ms05919971:24000
Susquehanna fine sandy loam, 5 to 8 percent slopes, erodedSnC24951332660c54zms06119741:20000
Susquehanna fine sandy loam, 2 to 5 percent slopesSnB18813326592w9wyms06119741:20000
Susquehanna-Petal association, rolling809677332738c57hms06719841:20000
Susquehanna fine sandy loam, 5 to 12 percent slopes83D8469332743c57nms06719841:20000
Susquehanna fine sandy loam, undulating8527856332746c57rms06719841:20000
Susquehanna fine sandy loam, 2 to 5 percent slopes83B20743327422w9wyms06719841:20000
Susquehanna fine sandy loam, rolling652664332736c57fms06719841:20000
Freestone-McLaurin-Susquehanna association, rolling (freest-mclaurin-susquehanna)FMC43159332851c5c4ms07319691:20000
Freestone, Susquehanna, and Prentiss soils, 5 to 12 percent slopes (freest, susquehanna and prentiss)FsD34438332853c5c6ms07319691:20000
Susquehanna silt loam, 1 to 5 percent slopesSuB27583328662w8yrms07319691:20000
Susquehanna silt loam, 5 to 12 percent slopesSuC2508332867c5cnms07319691:20000
Petal-Susquehanna association, rollingPS13676333131c5n5ms09119831:20000
Luverne-Susquehanna association, hilly (sweatman, susquehanna)LSF9550568278m2bkms09319681:20000
Luverne and Susquehanna soils, 12 to 30 percent slopes, severely eroded (sweatman, susquehanna)LvE32366568286m2btms09319681:20000
Malbis-Susquehanna-Saucier association slopingME55625333544c62hms10919801:20000
Susquehanna loam, 5 to 10 percent slopesSuD9484333567c637ms10919801:20000
Susquehanna loam, 2 to 5 percent slopesSuB7414333566c636ms10919801:20000
Lorman-Freest-Susquehanna complex, 5 to 15 percent slopesLsD386293336092x597ms11119971:20000
Susquehanna and Freest soils, 2 to 5 percent slopesST8219333620c64yms11119971:20000
Susquehanna fine sandy loam, 2 to 5 percent slopesSsB39483336242w9wyms11119971:20000
Susquehanna silt loam, 5 to 15 percent slopes3816937334132c6pgms13119971:24000
Susquehanna silt loam, undulating399935334133c6phms13119971:24000
Saucier-Susquehanna association, 2 to 8 percent slopes323582334122c6p4ms13119971:24000
Susquehanna silt loam, 1 to 5 percent slopes3711883341312w8yrms13119971:24000
Susquehanna fine sandy loam, 2 to 5 percent slopesSuB1024224034752w9wyms15320081:24000
Susquehanna clay, 5 to 12 percent slopes, severely erodedSuC3788327252bzjjtn02319891:24000
Susquehanna clay, 2 to 5 percent slopes, severely erodedSuB393327251bzjhtn02319891:24000
SUSQUEHANNA VERY FINE SANDY LOAMSs328327370bznbtn03920081:24000
Cuthbert and Susquehanna soils, 5 to 12 percent slopes (Luverne Smithdale)CsD488327542bztwtn07119611:15840
Susquehanna soils, 2 to 10 percent slopesSuC20424535812nc4sva15319851:15840
Susquehanna soils, 2 to 10 percent slopesSuC15312056441g5va17919701:15840

Map of Series Extent

Approximate geographic distribution of the SUSQUEHANNA 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 .