Official Series Description


Lab Data Summary

Aggregate lab data for the CONOVER soil series. This aggregation is based on all pedons with a current taxon name of CONOVER, 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 CONOVER 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
111CWH72151972IN181015Conover3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7367028,-87.0460889
111CKO74031974IN085003Conover3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3902389,-85.9963444
111CDK78111978IN033011Conover3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4696972,-85.1425083
111CBE81281981IN007028Conover3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5987889,-87.1347806
111DCT76011976IN023001Conover3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1926778,-86.4502556
9807N0254S2005MI049002Conover1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0305444,-83.8123917

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CONOVER 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 CONOVER 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 CONOVER 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 CONOVER 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 CONOVER 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 CONOVER 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 CONOVER 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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Soil series sharing subgroup-level classification with CONOVER, 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. IN-2012-01-20-20 | White County - February 1982

    Typical pattern of soils, topography, and underlying material in the Wolcott-Conover map unit (Soil Survey of White County, Indiana; 1982).

  2. MI-2012-02-06-14 | Hillsdale County - 1997

    Typical pattern of soils and parent material in the Miami-Williamston-Conover association (Soil Survey of Hillsdale County, Michigan; 1997).

Map Units

Map units containing CONOVER 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
Conover silt loam, 0 to 3 percent slopesCpA20061645445j6win00719851:15840
Conover loam, 0 to 3 percent slopesCrA12951603225ctpin03319801:15840
Conover loam, 0 to 3 percent slopesCrA1151827259794ngin08719781:20000
Conover loam, 0 to 1 percent slopesCpcA51118493066fhin13120011:12000
Conover loam, 0 to 1 percent slopesCnA156991618445fdsin18119791:20000
Conover loam, 0 to 3 percent slopesCvrabA1831173022y14kmi01719781:20000
Conover loam, 0 to 4 percent slopesCvraaB7784231173002yct3mi03719741:15840
Metamora-Conover complex, 0 to 3 percent slopesMetaaA396631172982y14mmi03719741:15840
Conover loam, 0 to 3 percent slopesCvrabA87631172962y14kmi03719741:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB22731172972y14lmi03719741:15840
Conover loam, 0 to 4 percent slopesCvraaB3576631172942yct3mi04519741:15840
Conover loam, 0 to 4 percent slopesCvraaB8009931172902yct3mi04919671:20000
Conover loam, 0 to 3 percent slopesCvrabA1896031172912y14kmi04919671:20000
Celina-Conover loams, 2 to 6 percent slopesClB1470318683668dzmi04919671:20000
Conover-Metamora sandy loams, 0 to 2 percent slopesCwA478018684368f6mi04919671:20000
Conover-Metamora sandy loams, 2 to 6 percent slopesCwB378218684468f7mi04919671:20000
Conover-Williamstown loams, 0 to 6 percent slopesCvracB289731172922y14lmi04919671:20000
Conover loam, 2 to 6 percent slopesCvB28701868422w64cmi04919671:20000
Metamora-Conover complex, 0 to 3 percent slopesMetaaA178631172932y14mmi04919671:20000
Celina-Conover loams, 0 to 2 percent slopesClA138818683568dymi04919671:20000
Conover loam, 0 to 2 percent slopesCvA10501868412w64bmi04919671:20000
Metamora-Conover complex, 0 to 3 percent slopesMetaaA942031172872y14mmi05719751:12000
Conover loam, 0 to 3 percent slopesCvrabA668131172842y14kmi05719751:12000
Conover-Parkhill complex, 0 to 3 percent slopesCvraeA308331172862y14qmi05719751:12000
Conover-Williamstown loams, 0 to 6 percent slopesCvracB28931172852y14lmi05719751:12000
Parkhill-Conover loams, 0 to 3 percent slopesPkhabA831172882y14nmi05719751:12000
Williamstown-Conover complex, 1 to 6 percent slopes12B370411886156b8cmi05919911:15840
Conover loam, 1 to 4 percent slopes13B127611886196b8hmi05919911:15840
Conover loam, 0 to 3 percent slopesCvrabA88031172822y14kmi06319781:20000
Conover-Williamstown loams, 0 to 6 percent slopesCvracB9731172832y14lmi06319781:20000
Conover loam, 0 to 4 percent slopesCvraaB5641331172792yct3mi06519771:15840
Conover loam, 0 to 4 percent slopesCvraaB340731172772yct3mi06719651:15840
Conover extremely stony loam, 2 to 6 percent slopesCuB7718793469kdmi06719651:15840
Conover loam, 0 to 3 percent slopesCvrabA1818331172732y14kmi07319831:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB10731172742y14lmi07319831:15840
Metamora-Conover complex, 0 to 3 percent slopesMetaaA6331172752y14mmi07319831:15840
Conover loam, 2 to 6 percent slopesCvB133841920136fszmi08719661:15840
Conover loam, 0 to 2 percent slopesCvA115111920126fsymi08719661:15840
Conover loam, 0 to 3 percent slopesCvrabA66031172702y14kmi08719661:15840
Conover loam, 0 to 4 percent slopesCvraaB34231172682yct3mi08719661:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB24331172692y14lmi08719661:15840
Celina-Conover loams, 2 to 6 percent slopesClB13424095632lwbvmi08719661:15840
Conover-Metamora sandy loams, 2 to 6 percent slopesCwB124200332m77lmi08719661:15840
Conover loam, 0 to 3 percent slopesCgA35811884576b38mi09119571:20000
Conover loam, 3 to 7 percent slopesCgB15801884586b39mi09119571:20000
Conover loam, 3 to 7 percent slopes, moderately erodedCgB2331884596b3bmi09119571:20000
Conover loam, 0 to 4 percent slopesCvraaB1673531172662yct3mi09319681:20000
Miami-Conover loams, 2 to 6 percent slopesMrB65831875896968mi09319681:20000
Conover-Miami loams, 0 to 2 percent slopesCxA22351875536953mi09319681:20000
Conover loam, 0 to 2 percent slopesCvA16551875512w64bmi09319681:20000
Conover loam, 2 to 6 percent slopesCvB2801875522w64cmi09319681:20000
Celina-Conover loams, 0 to 2 percent slopesClA824393152mw9lmi09319681:20000
Conover loam, 0 to 2 percent slopesCvA23911187631697mmi09919671:20000
Conover loam, 2 to 6 percent slopesCvB2143187632697nmi09919671:20000
Conover loam, 0 to 3 percent slopesCvrabA648131172602y14kmi11119761:15840
Parkhill-Conover loams, 0 to 3 percent slopesPkhabA15831172632y14nmi11119761:15840
Metamora-Conover complex, 0 to 3 percent slopesMetaaA10831172622y14mmi11119761:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB1131172612y14lmi11119761:15840
Conover loam, 0 to 3 percent slopes60A238618726568vtmi11519801:15840
Conover loam, 0 to 4 percent slopesCvraaB10431172562yct3mi12519801:15840
Celina-Conover loams, 2 to 6 percent slopes105B6124206892m7xrmi12519801:15840
Conover loam, 0 to 2 percent slopes109A4624207062w64bmi12519801:15840
Conover loam, 2 to 6 percent slopes109B3224200472w64cmi12519801:15840
Conover-Metamora sandy loams, 2 to 6 percent slopes110B924382292mv5kmi12519801:15840
Conover loam, 2 to 6 percent slopesCnB7451926552w64cmi13919671:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvrabA2925731172522y14lmi14519911:15840
Parkhill-Conover loams, 0 to 3 percent slopesPkhabA694231172552y14nmi14519911:15840
Conover gravelly sandy loam, 0 to 3 percent slopesCvradA278731172532y14pmi14519911:15840
Conover loam, 0 to 3 percent slopesCvracB46231172512y14kmi14519911:15840
Metamora-Conover complex, 0 to 3 percent slopesMetaaA2431172542y14mmi14519911:15840
Conover loam, 0 to 3 percent slopesCvrabA2398131172492y14kmi14719691:20000
Conover-Parkhill loams, 0 to 2 percent slopesCwA12497187409690gmi14719691:20000
Conover loam, 0 to 2 percent slopesCvA10394187407690dmi14719691:20000
Conover-Williamstown loams, 0 to 6 percent slopesCvracB242131172502y14lmi14719691:20000
Conover loam, 2 to 6 percent slopesCvB1030187408690fmi14719691:20000
Conover loam, 0 to 3 percent slopesCvrabA7701331172472y14kmi15119551:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB198831172482y14lmi15119551:15840
Conover loam, 0 to 4 percent slopesCvraaB7972831172402yct3mi15519671:12000
Conover loam, 0 to 3 percent slopesCvrabA899531172442y14kmi15519671:12000
Conover-Williamstown loams, 0 to 6 percent slopesCvracB53631172452y14lmi15519671:12000
Metamora-Conover complex, 0 to 3 percent slopesMetaaA26331172462y14mmi15519671:12000
Celina-Conover loams, 2 to 6 percent slopesClB11523992492ljm4mi15519671:12000
Miami-Conover loams, 2 to 6 percent slopesMxB1224395562mwkcmi15519671:12000
Conover-Metamora sandy loams, 0 to 2 percent slopesCwA723992382ljlsmi15519671:12000
Conover loam, 0 to 3 percent slopesCvrabA1658031172412y14kmi15719841:15840
Conover-Williamstown loams, 0 to 6 percent slopesCvracB217931172422y14lmi15719841:15840
Metamora-Conover complex, 0 to 3 percent slopesMetaaA29831172432y14mmi15719841:15840
Conover loam, 0 to 4 percent slopesCoB151891916166fd5mi16119741:20000
Conover-Brookston loams, 0 to 2 percent slopesCpA42861916176fd6mi16119741:20000
Conover silt loam, 1 to 3 percent slopesCyA1910425608g8w9wi12719671:15840
Conover silt loam, 1 to 3 percent slopesCyA527424021g773wi60119671:15840

Map of Series Extent

Approximate geographic distribution of the CONOVER 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 .