Official Series Description


Lab Data Summary

Aggregate lab data for the SYLVAN soil series. This aggregation is based on all pedons with a current taxon name of SYLVAN, 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 SYLVAN 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
115APS73011973IN065001Sylvan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0587972,-87.9513139
115APS73021973IN065002Sylvan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0718333,-87.9320833
115AKX77141977IN083014Sylvan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7015111,-87.4334556
115AGB82111982IN051011Sylvan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4392778,-87.5790722
115C78IL0950011978IL095001Sylvan1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9755376,-90.1355634
115C81IL0130181981IL013018Sylvan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.170422,-90.6237849
115C86IL1490101986IL149010Sylvan2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.612025,-90.823875
n/aKX76101976IN083010Sylvan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPR-0081979-OH127-008Sylvan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SYLVAN 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 SYLVAN 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 SYLVAN 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 SYLVAN 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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Click the image to view it full size.

Competing Series

Soil series competing with SYLVAN 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 SYLVAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SYLVAN 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with SYLVAN, 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. IL-2010-09-01-67 | Schuyler County - 2003

    Typical pattern of soils and underlying material in the Fayette-Sylvan association (Soil Survey of Schuyler County, Illinois; 2003).

  2. IL-2011-06-01-04 | Brown County - 1988

    Typical pattern of soils and parent material in the Fayette-Sylvan association (Soil Survey of Brown County, Illinois; 1988).

  3. IL-2011-06-01-06 | Brown County - 1988

    Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

  4. IL-2011-08-03-03 | Calhoun County - 1989

    Typical pattern of soils and parent material in the Fayette-Sylvan-Rozetta association (Soil Survey of Calhoun County, Illinois; 1989).

  5. IL-2011-08-03-04 | Cass County - 1989

    Typical pattern of soils and parent material in the Sylvan-Rozetta-Bold general soil map unit (Soil Survey of Cass County, Illinois; 1989).

  6. IL-2011-08-04-21 | Henry County - 1984

    Pattern of soils and parent material in the Downs-Sylvan-Fayette association (Soil Survey of Henry County, Illinois; 1984).

  7. IL-2011-08-04-71 | Mercer County - 1991

    Typical pattern of soils and parent material in the Fayette-Hickory association (Soil Survey of Mercer County, Illinois; 1991).

  8. IL-2011-08-04-81 | Peoria County - 1992

    Typical pattern of soils and parent material in the Rozetta-Keomah-Sylvan and Hickory-Strawn-Marseilles associations (Soil Survey of Peoria County, Illinois; 1992).

  9. IN-2012-01-19-18 | Gibson County - June 1989

    Pattern of soils and parent material in the Alford-Sylvan association (Soil Survey of Gibson County, Indiana; 1989).

Map Units

Map units containing SYLVAN 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
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D323091729495sz0il00919841:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C39461729485syzil00919841:12000
Sylvan silt loam, 18 to 35 percent slopes, severely eroded19F36601729505sz1il00919841:12000
Sylvan silt loam, 35 to 60 percent slopes19G2196186265620j7pil01120071:12000
Sylvan silt loam, 10 to 18 percent slopes19D741186265420j7mil01120071:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3635186265520j7nil01120071:12000
Sylvan silty clay loam, 18 to 35 percent slopes, severely eroded19F317501755025wmcil01319861:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D316311755015wmbil01319861:15840
Sylvan silt loam, 10 to 18 percent slopes, eroded19D212081755005wm9il01319861:15840
Sylvan silty clay loam, terrace, 10 to 18 percent slopes, severely eroded9019D310325423752qzksil01319861:15840
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D385402628278th9il01720031:12000
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E268392628288thbil01720031:12000
Sylvan-Bold Complex, 5 to 10 percent slopes, severely eroded962C340062628268th8il01720031:12000
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D22546780783v6gkil01720031:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes962F577758469tg7ril01720031:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D36331615624nnlvil05719971:12000
Sylvan-Bold silt loams, 35 to 60 percent slopes962G466921179373d1il06119681:15840
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E2149521179273d0il06119681:15840
Sylvan-Bold silt loams, 18 to 35 percent slopes962F117121179173czil06119681:15840
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D2105121179073cyil06119681:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D31689324462486k3il07320011:12000
Sylvan silt loam, 10 to 18 percent slopes, eroded19D2650724462386k2il07320011:12000
Sylvan silt loam, 18 to 35 percent slopes19F337724462586k4il07320011:12000
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D3308424478386q7il07320011:12000
Sylvan-Bold silt loams, 35 to 60 percent slopes962G3651728443sg05il08320021:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes962F1916728442sg04il08320021:12000
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E21605728445sg07il08320021:12000
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D2914728439sg01il08320021:12000
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D3217728441sg03il08320021:12000
Sylvan-Bold complex, terrace, 10 to 18 percent slopes, severely eroded9962D3147728475sg16il08320021:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C32196680859qvh6il09520021:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3688680860qvh7il09520021:12000
Hickory-Sylvan complex, 18 to 35 percent slopes, eroded898F290315960691qkv3il10720061:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes, eroded962F241301989236nzwil11920011:12000
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D219551989226nzvil11920011:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C317918210763hfil12319971:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D32318210863hgil12319971:15840
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D2392814061161j65lil12920051:12000
Hickory-Sylvan complex, 18 to 35 percent slopes, eroded898F2354814867341lx25il12920051:12000
Sylvan-Bold silt loams, 5 to 10 percent slopes, eroded962C2307114869671lx9pil12920051:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes, eroded962F2285914867441lx2hil12920051:12000
Sylvan-Bold complex, 5 to 10 percent slopes, severely eroded962C3277114060541j63lil12920051:12000
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D3161014061231j65til12920051:12000
Hickory-Sylvan complex, 10 to 18 percent slopes, eroded898D2119214066321j6q7il12920051:12000
Hickory-Sylvan complex, 18 to 35 percent slopes, severely eroded898F371914867381lx29il12920051:12000
Hickory-Sylvan silt loams, 35 to 60 percent slopes898G68214070341j746il12920051:12000
Hickory-Sylvan complex, 10 to 18 percent slopes, severely eroded898D364814066331j6q8il12920051:12000
Sylvan-Bold silt loams, 35 to 60 percent slopes962G39514060441j638il12920051:12000
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E229614884791lywgil12920051:12000
Hickory-Sylvan silt loams, 35 to 60 percent slopes898G1044024501186ylil13120001:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3976324494486wfil13120001:12000
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D3335024501986yvil13120001:12000
Sylvan silt loam, 10 to 18 percent slopes, eroded19D2140524494386wdil13120001:12000
Hickory-Sylvan-Fayette silt loams, 18 to 35 percent slopes960F4024501886ytil13120001:12000
Hickory-Sylvan complex, 18 to 35 percent slopes, severely eroded898F31624501086ykil13120001:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C3577116721201t3zcil13719841:15840
Sylvan-Bold complex, 18 to 25 percent slopes, severely eroded962E3301216721881t41kil13719841:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3226016721221t3zfil13719841:15840
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E2201416721871t41jil13719841:15840
Sylvan silt loam, 10 to 18 percent slopes, eroded19D2201016721211t3zdil13719841:15840
Sylvan silt loam, 18 to 25 percent slopes, eroded19E2126516721231t3zgil13719841:15840
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D3106216721861t41hil13719841:15840
Sylvan silty clay loam, 18 to 25 percent slopes, severely eroded19E399716721241t3zhil13719841:15840
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D27325421632qvjqil13719841:15840
Sylvan-Bold complex, 5 to 10 percent slopes, severely eroded962C35125421622qvjpil13719841:15840
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C31660620902670hsil14319861:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3316320902770htil14319861:15840
Sylvan silty clay loam, 18 to 25 percent slopes, severely eroded19E3126820902870hvil14319861:15840
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D314242010946r7xil14920011:12000
Hickory-Sylvan-Fayette silt loams, 18 to 30 percent slopes960F116811987696ntxil16120021:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D386171986756nqwil16120021:12000
Hickory-Sylvan silt loams, 35 to 60 percent slopes898G81321987586ntkil16120021:12000
Hickory-Sylvan-Fayette silt loams, 10 to 18 percent slopes, eroded960D251021987676ntvil16120021:12000
Sylvan silt loam, 18 to 35 percent slopes19F45521986766nqxil16120021:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C3245327143093ftil16120021:12000
Sylvan silty clay loam, 18 to 35 percent slopes, severely eroded19F317051986776nqyil16120021:12000
Hickory-Sylvan-Fayette complex, 10 to 18 percent slopes, severely eroded960D315751987686ntwil16120021:12000
Sylvan silt loam, 10 to 18 percent slopes19D14611986746nqvil16120021:12000
Hickory-Sylvan complex, 18 to 35 percent slopes, severely eroded898F313181987576ntjil16120021:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes962F13121987646ntril16120021:12000
Sylvan-Bold silt loams, 18 to 35 percent slopes, eroded962F2482518319864mmil16319971:12000
Sylvan-Bold silt loams, 35 to 60 percent slopes962G194118320064mpil16319971:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D312752021766sctil16920001:12000
Sylvan-Bold silt loams, 18 to 25 percent slopes, eroded962E2339525420832qrcmil17119841:12000
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C3221216058131qwzfil17119841:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3190625420482qrb8il17119841:12000
Sylvan-Bold complex, 18 to 25 percent slopes, severely eroded962E3124325420842qrcnil17119841:12000
Sylvan silty clay loam, 18 to 25 percent slopes, severely eroded19E381625420512qrbcil17119841:12000
Sylvan-Bold complex, 10 to 18 percent slopes, severely eroded962D380025420822qrclil17119841:12000
Sylvan silt loam, 10 to 18 percent slopes, eroded19D259825420492qrb9il17119841:12000
Sylvan silt loam, 18 to 25 percent slopes, eroded19E252225420502qrbbil17119841:12000
Sylvan-Bold silt loams, 10 to 18 percent slopes, eroded962D2925420812qrckil17119841:12000
Sylvan silty clay loam, 10 to 18 percent slopes, severely eroded19D3246417907360bkil17519921:15840
Sylvan silty clay loam, 5 to 10 percent slopes, severely eroded19C3111217907260bjil17519921:15840
Sylvan silt loam, 18 to 35 percent slopes19F81317907460blil17519921:15840
Sylvan silt loam, 10 to 18 percent slopes, eroded19D2163017936860n2il17919911:15840
Sylvan silt loam, 5 to 10 percent slopes, eroded19C252517936760n1il17919911:15840
Sylvan-Hickory silt loams, 35 to 70 percent slopes898G199615439291ntl5il19320061:12000
Sylvan silt loam, 18 to 35 percent slopes19F69515438631ntj1il19320061:12000
Sylvan silt loam, 6 to 12 percent slopes, severely erodedSyC338331601615cnhin05119861:15840
Sylvan silt loam, 18 to 50 percent slopesSyF34241601635cnkin05119861:15840
Sylvan silt loam, 2 to 6 percent slopes, erodedSyB218481601605cngin05119861:15840
Udorthents-Sylvan complex, 12 to 18 percent slopes, severely erodedUmD311921601675cnpin05119861:15840
Sylvan silt loam, 12 to 18 percent slopesSyD3211601625cnjin05119861:15840
Sylvan silt loam, 2 to 6 percent slopes, erodedSyB2191101645055j5min08319791:15840
Sylvan silt loam, 25 to 40 percent slopesSyF37101645085j5qin08319791:15840
Sylvan silt loam, 6 to 12 percent slopes, severely erodedSyC330041645065j5nin08319791:15840
Sylvan silt loam, 12 to 18 percent slopes, severely erodedSyD314381645075j5pin08319791:15840
Sylvan silt loam, 2 to 6 percent slopes, erodedSyB210721619395fhvin12519831:15840
Sylvan silt loam, 6 to 12 percent slopes, severely erodedSyC36201619405fhwin12519831:15840
Sylvan silt loam, 25 to 50 percent slopesSyF2041619415fhxin12519831:15840
Sylvan silt loam, 6 to 12 percent slopes, severely erodedSyC369441599165cdlin12919781:15840
Sylvan silt loam, 18 to 40 percent slopesSyF55001599185cdnin12919781:15840
Sylvan silt loam, 12 to 18 percent slopes, severely erodedSyD344321599175cdmin12919781:15840
Sylvan silt loam, 2 to 6 percent slopes, severely erodedSyB33971599155cdkin12919781:15840

Map of Series Extent

Approximate geographic distribution of the SYLVAN 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 .