Official Series Description


Lab Data Summary

Aggregate lab data for the CYLINDER soil series. This aggregation is based on all pedons with a current taxon name of CYLINDER, 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 CYLINDER 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
103UMN1113S1970MN0471113Cylinder3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5464211,-93.5431442
91AUMN2039S1975MN1452039Cylinder2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.7236023,-95.0980453

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CYLINDER 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 CYLINDER 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 CYLINDER 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 CYLINDER 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 CYLINDER 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 CYLINDER 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 CYLINDER 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 hills figure.

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 CYLINDER, 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. IA-2010-09-02-14 | Humboldt County - 2005

    Typical pattern of soils and parent material in the Lester-Spillville-Coland association (Soil Survey of Humboldt County, Iowa; 2005).

  2. IA-2010-09-09-23 | Webster County - 2008

    Typical pattern of soils and parent material in the Lester-Coland-Wadena association (Soil Survey of Webster County, Iowa; 2008).

  3. IA-2011-05-31-32 | Greene County - 1985

    Pattern of soils and parent material in the Clarion-Coland-Storden association (Soil Survey of Greene County, Iowa; 1985).

  4. IA-2011-06-01-29 | Osceola County - 1988

    Typical pattern of soils and parent material in the Wadena-Coland- Cylinder association (Soil Survey of Osceola County, Iowa; 1988).

  5. IA-2011-06-01-33 | Pocahontas County - 1985

    Typical pattern of soils and parent material in the Havelock-Coland-Estherville association (Soil Survey of Pocahontas County, Iowa; 1985).

Map Units

Map units containing CYLINDER 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
Cylinder loam, 0 to 2 percent slopes203110625502462wd84ia01519771:15840
Cylinder loam, 0 to 2 percent slopes20324424032812wd84ia02119731:15840
Cylinder loam, 0 to 2 percent slopes20318594034662wd84ia02519791:15840
Cylinder loam, 0 to 2 percent slopes20316534035212wd84ia02719791:15840
Cylinder loam, 0 to 2 percent slopes203105153993062wd84ia04120021:12000
Cylinder loam, 0 to 2 percent slopes20320084045832wd84ia04919801:15840
Cylinder complex, 0 to 2 percent slopes2002067186904920qwxia05920111:12000
Cylinder-Nicollet complex, 0 to 3 percent slopes19925724812232p8xgia05920111:12000
Cylinder loam, 0 to 2 percent slopes20323544061992wd84ia07319831:15840
Cylinder loam, 0 to 2 percent slopes2037824063552wd84ia07719681:15840
Cylinder loam, 0 to 2 percent slopes20311614064692wd84ia07919841:15840
Cylinder loam, 0 to 2 percent slopes20310824475092wd84ia09119981:12000
Cylinder loam, 0 to 2 percent slopes20317924083512wd84ia10919801:15840
Cylinder silty clay loam, deep, 0 to 2 percent slopes2031276409082fqp6ia11919731:15840
Cylinder silty clay loam, 32 to 40 inches to sand and gravel, 0 to 2 percent slopes203389410061frpsia14119771:15840
Cylinder clay loam, 24 to 32 inches to sand and gravel, 0 to 2 percent slopes202254410060frpria14119771:15840
Cylinder loam, 0 to 2 percent slopes20330284101182wd84ia14319851:15840
Cylinder complex, 0 to 2 percent slopes20059324992322q4lwia14319851:15840
Cylinder-Nicollet complex, 0 to 3 percent slopes19913625065642q4m9ia14319851:15840
Cylinder loam, 0 to 2 percent slopes20340934102642wd84ia14719731:15840
Cylinder loam, 0 to 2 percent slopes20323324103812wd84ia15119821:15840
Cylinder loam, 0 to 2 percent slopes20318924128682wd84ia15319931:12000
Cylinder-Urban land complex, 0 to 2 percent slopes4203247412930fvpbia15319931:12000
Cylinder loam, 0 to 2 percent slopes20321004107772wd84ia16119751:15840
Cylinder loam, 32 to 40 inches to sand and gravel, 0 to 2 percent slopes203502411200fswjia16719871:15840
Cylinder loam, 0 to 2 percent slopes2038434112952wd84ia16919811:15840
Cylinder loam, 0 to 2 percent slopes20312357979302wd84ia18720061:12000
Cylinder loam, loamy substratum, 0 to 2 percent slopes22890616513541sfchia18720061:12000
Cylinder loam, 0 to 2 percent slopes20316904126702wd84ia19719881:15840
Cylinder loam, 0 to 2 percent slopes12981583967782wd84mn03719801:15840
Cylinder loam, 0 to 2 percent slopes12922983978062wd84mn04719771:15840
Shandep-Cylinder complex, 0 to 2 percent slopesN577A108015275401n8jhmn04920071:12000
Cylinder loam, 1 to 4 percent slopes129496398930fd3qmn07919861:20000
Cylinder loam, 0 to 2 percent slopes12912804362212wd84mn09319961:20000
Cylinder loam1292374400419ffnrmn09919861:15840
Cylinder loam, 0 to 2 percent slopes, occasionally floodedP8A215326471nfv7mn10120081:12000
Cylinder loam, 0 to 2 percent slopesL137A1897848192wd84mn10520041:12000
Cylinder loam, 0 to 2 percent slopes, occasionally floodedP8A250725503sbybmn11720051:12000
Cylinder loam, 0 to 2 percent slopes, occasionally floodedP8A1223432685gj7lmn13320021:12000
Cylinder loam1291222428076gcfxmn14519801:15840

Map of Series Extent

Approximate geographic distribution of the CYLINDER 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 .