Official Series Description


Lab Data Summary

Aggregate lab data for the PARR soil series. This aggregation is based on all pedons with a current taxon name of PARR, 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 PARR 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
108A78IL1030151978IL103015Parr1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6418042,-89.3989564
108A78IL1030191978IL103019Parr1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6551125,-89.3901006
108A83P055483IL011067Parr6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3933334,-89.6600037
11076IL0190241976IL019024Parr1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3272373,-87.9837028
111CJR79221979IN073022Parr2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9689472,-87.1703944
111CJR80281980IN073028Parr3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9689472,-87.16945
111DMY80011980IN107001Parr3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2113389,-86.8787389
111D82P0840S1982IN107003Parr6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.211113,-86.8731003
111D82P0841S1982IN107004Parr6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2109756,-86.8731003
n/aWA-0171958-OH165-017Parr3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0191958-OH165-019Parr3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

Geomorphic description summaries for the PARR 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.

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

Soil series sharing subgroup-level classification with PARR, 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. IL-2010-09-01-58 | McLean County - 1998

    Typical pattern of soils and parent material in the Parr-Lisbon-Drummer association (Soil Survey of McLean County, Illinois; 1998).

  2. IL-2011-08-03-01 | Bureau County - 1992

    Typical pattern of soils and parent material in the Saybrook-Parr-La Rose association (Soil Survey of Bureau County, Illinois; 1992).

  3. IL-2011-08-04-06 | De Witt County - 1991

    Typical pattern of soils and parent material in the Catlin-Dana association (Soil Survey of De Witt County, Illinois; 1991).

  4. IL-2011-08-04-56 | Macon County - 1990

    Typical landscape pattern of soils and parent materials in the Catlin-Dana-Parr association (Soil Survey of Macon County, Illinois; 1990).

  5. IN-2012-01-19-42 | Pulaski County - January 1968

    Prairie soils that formed in loam till and adjoining soils that formed in outwash and lacustrine deposits (Soil Survey of Pulaski County, Indiana; 1968).

Map Units

Map units containing PARR 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
Parr silt loam, 2 to 5 percent slopes221B67341997936pwyil00720061:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C2123913953601htzmil00720061:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C2807318391465cqil03719981:12000
Parr silt loam, 2 to 5 percent slopes, eroded221B2725618391365cpil03719981:12000
Parr clay loam, 5 to 10 percent slopes, severely eroded221C34611983636ndtil05320011:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C21631983796nfbil05320011:12000
Parr silt loam, 2 to 5 percent slopes221B47327146693gzil08920001:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C2258271306939til08920001:12000
Parr silt loam, 2 to 5 percent slopes, eroded221B237271307939vil08920001:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C276114514617fm6il10320041:12000
Parr silt loam, 2 to 5 percent slopes, eroded221B227114514517fm5il10320041:12000
Parr silt loam, 2 to 5 percent slopes221B504718249363wwil11119971:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C2101618249463wxil11119971:12000
Parr silt loam, 5 to 10 percent slopes, eroded221C24079179007608fil17319901:15840
Parr silt loam, 2 to 5 percent slopes, eroded221B22909179006608dil17319901:15840
Parr silt loam, 2 to 5 percent slopes, eroded221B2268416132181r4p9il18320061:12000
Parr clay loam, 5 to 10 percent slopes, severely eroded221C326816127701r46vil18320061:12000
Parr silt loam, 1 to 5 percent slopesPgB7451623485fy1in02319781:20000
Parr fine sandy loam, 2 to 6 percent slopesPaB23451613785dxrin07319851:15840
Parr-Ayr complex, 2 to 6 percent slopesPdB20061613795dxsin07319851:15840
Parr loam, 0 to 2 percent slopesPrA232927262494pbin08719781:20000
Parr silt loam, 2 to 6 percent slopesPfB10841630485gnmin10719841:15840
Parr loam, 0 to 2 percent slopesPdA88027256594mfin11319741:15840
Parr silt loam, 1 to 4 percent slopesPbB2814138141jg5xoh02119661:15840
Parr silt loam, 1 to 4 percent slopesPaB9261711535r32oh09119771:15840

Map of Series Extent

Approximate geographic distribution of the PARR 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 .