Official Series Description


Lab Data Summary

Aggregate lab data for the COVERT soil series. This aggregation is based on all pedons with a current taxon name of COVERT, 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 COVERT 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
9740A1976S1973MI159002Covert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3280678,-86.2824707
9808N00772007MI139010Covert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.976944,-86.1830826
9807N0380F2006MI121003Covert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.366,-86.1202778
9808N0665F2008MI121012Covert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1404722,-86.0904444
9808N0669F2008MI121016Covert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1546669,-86.0007782
98S79MI-107-6S1979MI107006Covert5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5111111,-85.52975
98S80MI-73-6S1980MI073006Covert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6275556,-84.6858333

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COVERT 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 COVERT 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 COVERT 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 COVERT 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 COVERT 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 COVERT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the COVERT 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

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

Soil series sharing subgroup-level classification with COVERT, 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-2012-02-06-46 | Oceana County - April 1996

    Typical pattern of soils and underlying material in the Benona-Spinks-Grattan association (Soil Survey of Oceana County, Michigan; April 1996).

  2. MI-2012-02-06-47 | Oceana County - April 1996

    Typical pattern of soils and underlying material in the Spinks-Remus-Fern association (Soil Survey of Oceana County, Michigan; April 1996).

  3. MI-2012-02-06-50 | Saginaw County - January 1994

    Pattern of soils and parent material in the Pipestone-Granby-Wixom association (Soil Survey of Saginaw County, Michigan; January 1994).

Map Units

Map units containing COVERT 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
Covert sand, 0 to 4 percent slopes57A64662124767432mi00519841:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB3626894342rfgwmi00519841:15840
Covert sand, 1 to 6 percent slopes109B302507996687ymi01719781:20000
Covert sand, 0 to 3 percent slopes131A1526735712qz4dmi01719781:20000
Covert sand, 0 to 3 percent slopesCmA126735112qz4dmi03519771:15840
Covert sand, 0 to 6 percent slopesCxB212026736632qz69mi04919671:20000
Covert-Urban land-Pipestone complex, 0 to 6 percent slopesCovaaB18190542321yr8mi04919671:20000
Covert sand, 1 to 6 percent slopesCzB823995502ljxvmi04919671:20000
Covert sand, 0 to 3 percent slopesCmA658126734812qz4dmi05119661:15840
Grayling-Covert-Pipestone associationGW402626734922qz5ymi05119661:15840
Covert-Pipestone-Roscommon associationCZ347426734902qz5wmi05119661:15840
Covert-Pipestone associationCX313626734882qz5tmi05119661:15840
Grattan-Covert association, undulatingGNB229326734962qz62mi05119661:15840
Covert-Pipestone-Kinross associationCY159426734892qz5vmi05119661:15840
Covert sand, 0 to 6 percent slopesCtB1572673460686gmi05119661:15840
Gladwin-Epoufette-Covert association, undulatingGFB13926734992qz6dmi05119661:15840
Covert stony sand, 0 to 6 percent slopesCsB7426734802qz5kmi05119661:15840
Covert sand, loamy substratum, 0 to 6 percent slopesCvB482673461686hmi05119661:15840
Covert sand, 1 to 6 percent slopesCvB32673582687ymi05719751:12000
Covert-Tobico complex, 0 to 6 percent slopes28B946918678068c5mi06319781:20000
Plainfield-Covert sands, 2 to 12 percent slopes32C500818678468c9mi06319781:20000
Covert sand, 0 to 2 percent slopes20A423118677468bzmi06319781:20000
Covert sand, loamy substratum, 0 to 2 percent slopes11A352718676768brmi06319781:20000
Covert sand, 0 to 6 percent slopes117B972508174693gmi06319781:20000
Covert sand, 0 to 4 percent slopes18B2654186607685lmi07319831:15840
Covert sand, 0 to 4 percent slopes3B114418714368qwmi08119841:15840
Covert-Lamson complex, 0 to 6 percent slopesCyB2626737362qz4cmi09919671:20000
Covert sand, 0 to 6 percent slopes58B137671925796gd7mi10519921:15840
Covert sand, loamy substratum, 0 to 6 percent slopes43B25851925606gcmmi10519921:15840
Covert sand, 0 to 3 percent slopes14A1004618771469b9mi10719821:15840
Covert loamy sand, gravelly substratum, 0 to 3 percent slopes49A338918775869cqmi10719821:15840
Covert sand, 0 to 6 percent slopesCoB23049186634686gmi11119761:15840
Covert sand, loamy substratum, 0 to 6 percent slopesCsB3491186635686hmi11119761:15840
Covert sand, 0 to 4 percent slopesCmB4462673541685lmi11119761:15840
Grattan-Covert association, undulatingGNB826735602qz62mi11119761:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA2968226894382rfgvmi12119661:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB2649426894372rfgwmi12119661:15840
Covert sand, 0 to 4 percent slopes19B19007186450680jmi12319901:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA8326894632rfgvmi12319901:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB4626894622rfgwmi12319901:15840
Covert sand, 0 to 6 percent slopes111B2526737052qz69mi12519801:15840
Covert sand, 0 to 6 percent slopes50B128671890536bqhmi12719921:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA1426894712rfgvmi12719921:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB526894702rfgwmi12719921:15840
Covert-Pipestone sands, 0 to 6 percent slopesCovabB1521126894782rfgwmi13919671:15840
Pipestone-Covert-Saugatuck sands, 0 to 3 percent slopesPpsaaA1487226894792rfgvmi13919671:15840
Covert sand, 1 to 6 percent slopes58B8847186680687ymi14519911:15840
Covert sand, loamy substratum, 0 to 6 percent slopes136B32673601686hmi14519911:15840
Covert sand, 0 to 6 percent slopes135B22673600686gmi14519911:15840
Chelsea-Covert sands, 0 to 6 percent slopesCcB866526736882qz6bmi14719691:20000
Covert-Lamson complex, 0 to 6 percent slopesCyB65126736872qz4cmi14719691:20000
Iosco sandy loam and Covert loamy sand, 0 to 2 percent slopesIcA0655626736412qz3nmi15119551:15840
Iosco sandy loam and Covert loamy sand, 2 to 7 percent slopes, slightly erodedIcB196926736422qz3pmi15119551:15840
Covert loamy sand, 0 to 2 percent slopes, slightly erodedCgA159126736392qz3lmi15119551:15840
Covert loamy sand, 2 to 7 percent slopes, slightly erodedCgB156326736402qz3mmi15119551:15840
Iosco sandy loam and Covert loamy sand, 7 to 14 percent slopes, slightly erodedIcC117626736432qz3qmi15119551:15840
Covert sand, 0 to 6 percent slopesCnB132508259693gmi15119551:15840
Covert sand, loamy substratum, 0 to 2 percent slopesCoA13250826068brmi15119551:15840
Iosco sandy loam and Covert loamy sand, 14+ percent slopes, slightly erodedIcD11226736442qz3rmi15119551:15840
Covert sand, 1 to 6 percent slopesCyA124230942mbfbmi15519671:12000
Covert sand, 0 to 6 percent slopes4B6579187502693gmi15719841:15840
Covert sand, 0 to 4 percent slopes45B354518632567whmi15919841:15840
Covert sand, 0 to 6 percent slopes58B76731932706h3jmi61420051:12000
Covert-Dair complex, 0 to 6 percent slopes106B5251899733z67nmi61420051:12000
Covert-Pipestone sands, 0 to 6 percent slopes104B4198899731z67lmi61420051:12000
Covert loamy sandCs17092901389qx9ny01919951:24000
Covert loamy sand, 0 to 3 percent slopes81A35382934979vdnny06519931:24000
Covert loamy sand, 3 to 8 percent slopes81B21252934989vdpny06519931:24000

Map of Series Extent

Approximate geographic distribution of the COVERT 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 .