Official Series Description


Lab Data Summary

Aggregate lab data for the COMFREY soil series. This aggregation is based on all pedons with a current taxon name of COMFREY, 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 COMFREY 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
105UMN2522S1977MN0552522Comfrey3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5987015,-91.2662659
110BE80311980IN007031Comfrey3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.679325,-87.4403222
111DBE79051979IN007005Comfrey2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5148972,-87.3412944
115C85IL1490081985IL149008Comfrey3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7429611,-91.2837472

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with COMFREY, 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-2010-08-31-14 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Sabina-Miami-Xenia association (Soil Survey of Cumberland County, Illinois; 2002).

  2. IL-2010-08-31-15 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Starks-Drummer-Camden association (Soil Survey of Cumberland County, Illinois; 2002).

Map Units

Map units containing COMFREY 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
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A318214832221lsdwil00720061:12000
Comfrey loam, 0 to 2 percent slopes, occasionally flooded8776A71014072231j7b9il00720061:12000
Comfrey loams, undrained, 0 to 2 percent slopes, commonly flooded1776A22814834011lslnil00720061:12000
Comfrey clay loam, 0 to 2 percent slopes, frequently flooded, long duration3776L16062628238th5il01720031:12000
Comfrey loams, undrained, 0 to 2 percent slopes, commonly flooded1776A5252628358thkil01720031:12000
Comfrey silt loam overwash, frequently flooded3776+7031748355vxvil03519921:15840
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A34218392365d0il03719981:12000
Comfrey loam, 0 to 2 percent slopes, occasionally flooded8776A153414159851jjfyil06320051:12000
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A20415903561qcwtil06320051:12000
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A32841755985wqgil07519801:15840
Comfrey loam, 0 to 2 percent slopes, occasionally flooded8776A605394215310md1il10320041:12000
Comfrey silt loam, undrained, 0 to 2 percent slopes, frequently flooded1776A228394216510mdfil10320041:12000
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A39111769705y4qil10519911:15840
Comfrey loam, 0 to 2 percent slopes, occasionally flooded8776A6538182792646jil11119971:12000
Comfrey loam, 0 to 2 percent slopes, undrained, occasionally flooded1776A226918244563vbil11119971:12000
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A954913987601hyj9il14120051:12000
Comfrey silt loam, undrained, 0 to 2 percent slopes, frequently flooded1776A55414790061ln0wil14120051:12000
Comfrey loam, 0 to 2 percent slopes, frequently flooded3776A147921742185v8yil20119971:12000
Comfrey loam, undrained, 0 to 2 percent slopes, frequently flooded1776A247124553422ndzlil20119971:12000
Comfrey silty clay loam, sandy substratum, occasionally floodedCk34391645415j6sin00719851:15840
Comfrey silty clay loam, sandy substratum, frequently floodedCm20671645425j6tin00719851:15840
Comfrey loam, frequently flooded, undrainedCo9401635275h52in11119901:15840
Comfrey loam, stratified substratum, frequently flooded, undrainedCs24781631035gqdin17119871:15840
Comfrey loam, stratified substratum, rarely floodedCg8041631025gqcin17119871:15840
Comfrey clay loam185487396146f96xmn01319751:12000
Comfrey clay loam, frequently flooded3533306396179f97zmn01319751:12000
Comfrey silty clay loam, channeled18606922398238fcddmn05519811:15840
Comfrey silt loam, occasionally flooded18602398228fcd2mn05519811:15840
Comfrey clay loam, 0 to 2 percent slopes, occasionally floodedP7A4029630075p4n0mn10520041:12000
Comfrey clay loam, 0 to 2 percent slopes, frequently floodedP49A1869630074p4mzmn10520041:12000
Comfrey clay loam, 0 to 2 percent slopes, occasionally floodedP7A2004432671gj74mn13320021:12000
Comfrey silty clay loamCc1529427945gc9pmn13919881:20000
Comfrey silt loam, channeled18602261428998gddnmn16919871:20000

Map of Series Extent

Approximate geographic distribution of the COMFREY 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 .