Official Series Description


Lab Data Summary

Aggregate lab data for the PEEVER soil series. This aggregation is based on all pedons with a current taxon name of PEEVER, 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 PEEVER 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
102AUMN3634S1982MN155039 (3634)Peever3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.615612,-96.7538834
102AUMN3633S1982MN1553633Peever3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.614557,-96.760117
102A93P0768S1993MN111006Peever7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1724434,-95.9368896

Water Balance

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

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

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Competing Series

Soil series competing with PEEVER 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 PEEVER 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 PEEVER 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 PEEVER, 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. MN-2010-09-08-22 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Forman-Buse-Peever association (Soil Survey of Otter Tail County, Minnesota; 2001).

  2. MN-2010-09-27-03 | Lac qui Parle County -

    Typical pattern of soils and underlying material in the Forman-Mehurin-Parnell association (Soil Survey of Lac qui Parle County, Minnesota).

Map Units

Map units containing PEEVER 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
Peever clay loam, 6 to 12 percent slopes646C4433435882gmkqmn11119961:20000
Peever-Mehurin complex, 2 to 6 percent slopes779B3469435949gmmwmn11119961:20000
Peever clay loam, 12 to 18 percent slopes646D1737435883gmkrmn11119961:20000
Peever-Buse complex, 2 to 6 percent slopes822B2115357382czwgmn15519861:20000
Peever clay loam, 2 to 6 percent slopes646B2953573752w8f7mn15519861:20000
Gwinner-Peever-Parnell complex, 0 to 3 percent slopesG205A1043125811372pwzznd07319921:20000
Peever-Gwinner complex, 3 to 6 percent slopesG206B174525811382px01nd07319921:20000
Gwinner-Peever complex, 0 to 3 percent slopesG206A16625060142px00nd07319921:20000
Gwinner-Peever complex, 0 to 3 percent slopesG206A313525774102px00nd07720051:12000
Peever-Forman complex, 0 to 3 percent slopesG207A98925773932px02nd07720051:12000
Forman-Peever complex, 3 to 6 percent slopesJ211B96315449421nvmvnd07720051:12000
Peever-Gwinner complex, 3 to 6 percent slopesG206B81425774182px01nd07720051:12000
Gwinner-Peever complex, 0 to 3 percent slopesJ213A9515449441nvmxnd07720051:12000
Gwinner-Peever complex, 0 to 3 percent slopesG206A1367125794862px00nd08119591:12000
Gwinner-Peever-Parnell complex, 0 to 3 percent slopesG205A964725794582pwzznd08119591:12000
Peever-Gwinner complex, 3 to 6 percent slopesG206B10525795132px01nd08119591:12000
Peever-Buse clay loams, 1 to 6 percent slopesG208B139127977452sd22sd01319871:20000
Peever clay loam, 0 to 3 percent slopesG204A66927977442sd20sd01319871:20000
Peever-Cavour complex, 0 to 3 percent slopesG202A5827977432sd1ysd01319871:20000
Peever clay loam, 0 to 3 percent slopesG204A209127980082sd20sd02519921:20000
Peever-Cavour complex, 0 to 3 percent slopesG202A195627980062sd1ysd02519921:20000
Peever-Cresbard-Tonka complex, 0 to 3 percent slopesG203A166927980072sd1zsd02519921:20000
Peever clay loam, 3 to 6 percent slopesG204B56927980092sd21sd02519921:20000
Peever clay loam, 0 to 2 percent slopesPcA215829473692w8f6sd03919921:20000
Peever clay loam, coteau, 2 to 6 percent slopesPeB1238416887fzszsd03919921:20000
Peever clay loam, 2 to 6 percent slopesPcB110629473672w8f7sd03919921:20000
Peever-Cavour clay loamsPg352416888fzt0sd03919921:20000
Peever clay loam, coteau, 0 to 2 percent slopesPeA127416886fzsysd03919921:20000
Peever clay loam, 0 to 2 percent slopesPeA2498429473702w8f6sd05119771:20000
Peever clay loam, 2 to 6 percent slopesPeB2165229473682w8f7sd05119771:20000
Peever-Cavour complexPd17790418174g14hsd05119771:20000
Peever clay loam, coteau, 2 to 6 percent slopesPcB6107418172g14fsd05119771:20000
Peever clay loam, 6 to 9 percent slopesPcC4691418173g14gsd05119771:20000
Peever-Tonka complexPe1130418175g14jsd05119771:20000
Peever clay loam, coteau, 0 to 2 percent slopesPcA602418171g14dsd05119771:20000
Peever clay loam, 2 to 6 percent slopesPeB62814165912w8f7sd09119701:20000
Peever clay loam, 0 to 2 percent slopesPeA38904165902w8f6sd09119701:20000
Peever-Hamerly complex, 0 to 2 percent slopesPhA3260416593fzhhsd09119701:20000
Peever clay loam, 6 to 9 percent slopesPeC490416592fzhgsd09119701:20000
Gwinner-Peever complex, 0 to 3 percent slopesG206A11727992762px00sd09119701:20000
Peever-Gwinner complex, 3 to 6 percent slopesG206B1127992772px01sd09119701:20000
Peever clay loam, 2 to 6 percent slopesPeB500654178542w8f7sd10919771:20000
Peever clay loam, 0 to 2 percent slopesPeA335874178532w8f6sd10919771:20000
Peever-Tonka complexPk17824417857g0t8sd10919771:20000
Peever clay loam, 6 to 9 percent slopesPeC4382417855g0t6sd10919771:20000
Peever-Cavour complex, 0 to 3 percent slopesPhA1655417856g0t7sd10919771:20000
Peever-Buse clay loams, 1 to 6 percent slopesG208B100927995892sd22sd11519971:24000
Peever-Cavour complex, 0 to 3 percent slopesG202A74027995862sd1ysd11519971:24000
Peever-Cresbard-Tonka complex, 0 to 3 percent slopesG203A51727995872sd1zsd11519971:24000
Peever clay loam, 0 to 3 percent slopesG204A20127995882sd20sd11519971:24000

Map of Series Extent

Approximate geographic distribution of the PEEVER 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 .