Official Series Description


Lab Data Summary

Aggregate lab data for the ENSLEY soil series. This aggregation is based on all pedons with a current taxon name of ENSLEY, 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 ENSLEY 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
94B40A1941S1967MI041002Ensley5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0449982,-87.1925049

Water Balance

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

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

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Soil series sharing subgroup-level classification with ENSLEY, 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. MI-2012-02-06-39 | Menominee County - September 1989

    Typical pattern of soils and parent material in the Onaway-Lupton map unit (Soil Survey of Menominee County, Michigan; September 1989).

  2. WI-2012-03-23-16 | Marinette County - February 1991

    Pattern of soils and parent material in the Emmet-Charlevoix association (Soil Survey of Marinette County, WI; 1991).

Map Units

Map units containing ENSLEY 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
Ensley mucky sandy loam4619901903376d1xmi00119931:20000
Shoepac-Ensley complex, 0 to 6 percent slopes148B2090314553221kvcwmi00320071:24000
Charlevoix-Ensley complex, 0 to 3 percent slopes200A870014553531kvdwmi00320071:24000
Munising, calcareous substratum-Ensley complex, 0 to 6 percent slopes135B93214553181kvcrmi00320071:24000
Ensley muck, 0 to 2 percent slopes3351114552622xwm8mi00320071:24000
Ensley mucky sandy loam463931912966f1vmi00719981:12000
Ensley-Cathro mucks, 0 to 2 percent slopesEnycaA823531559112ytk3mi00919761:15840
Tawas-Ensley complexTe3711241514839smi00919761:15840
Angelica-Ensley loamsAn24141903956d3smi02919701:15840
Ensley-Cathro mucks, 0 to 2 percent slopesEnycaA26631870562ytk3mi02919701:15840
Ensley muck, 0 to 2 percent slopesEs4702515880532xwm8mi04119691:24000
Ensley muck, 0 to 2 percent slopes71158774152472xwm8mi04319851:20000
Ensley sandy loamEy5361893396c0qmi04719681:20000
Ensley loamEn205518795069kxmi06719651:15840
Ensley muck, 0 to 2 percent slopes761964160172xwm8mi07119921:20000
Ensley-Parkhill complexEp4850187641697ymi09919671:20000
Shoepac-Ensley complex, 0 to 6 percent slopes148B10044395083f83mmi10319991:24000
Charlevoix-Ensley complex, bedrock substratum, 0 to 3 percent slopes200A8534395157f860mi10319991:24000
Ensley-Solona complex, 0 to 3 percent slopes92A4646395303f8bqmi10319991:24000
Cathro-Ensley mucks8829143385785f8bhmi10319991:24000
Ensley muck, 0 to 2 percent slopes3323023951902xwm8mi10319991:24000
Cathro-Ensley complex1748322415455fy9smi10919851:20000
Ensley muck, 0 to 2 percent slopes1697344154542xwm8mi10919851:20000
Ensley loam and Edmore loamy fine sand, 0 to 2 percent slopesEb894018727968w8mi11719561:20000
Ensley-Parkhill complex13822508694697ymi12519801:15840
Ensley and Tonkey loamsEs7681900246cqtmi13319661:15840
Ensley and Tonkey loams, overwashEt1281900256cqvmi13319661:15840
Edmore and Ensley sandy loams, 0 to 2 percent slopesEcA0510418825369wpmi15119551:15840
Edmore and Ensley sandy loams, 2 to 6 percent slopes, slightly erodedEcB13918825469wqmi15119551:15840
Charlevoix-Ensley complex, 0 to 3 percent slopes120A937514569871kx3lmi15320071:24000
Ensley muck, 0 to 2 percent slopes43363614569182xwm8mi15320071:24000
Pinckney-Ensley silt loams, undulatingPkB63332918999sr3ny04519811:15840
Ensley very stony silt loamEn49402918169snfny04519811:15840
Ensley silt loamEm40382918159sndny04519811:15840
Ensley muck, 0 to 2 percent slopesEy117024223942xwm8wi07519871:20000
Ensley muck, 0 to 2 percent slopesEs118474224622xwm8wi08319851:15840

Map of Series Extent

Approximate geographic distribution of the ENSLEY 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 .