Official Series Description


Lab Data Summary

Aggregate lab data for the PALSGROVE soil series. This aggregation is based on all pedons with a current taxon name of PALSGROVE, 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 PALSGROVE 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
10493P0165S1992WI093004Palsgrove6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5927773,-92.3944473
10494P0166S1993WI091021Palsgrove6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5125008,-92.0961075
105X191182-11-2S1960IA191001Palsgrove1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4728227,-91.7581729
105UMN1808S1974MN1091808Palsgrove3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8988876,-92.3094406
105UMN3648S1982MN1693648Palsgrove2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1570129,-92.067482

Water Balance

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

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

Competing Series

Soil series competing with PALSGROVE 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 PALSGROVE 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 PALSGROVE 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with PALSGROVE, 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-2010-09-01-30 | Jo Daviess County - 1996

    Typical pattern of soils and parent material in the Fayette-Palsgrove-Rozetta association (Soil Survey of Jo Daviess County, Illinois; 1996).

  2. IL-2011-08-04-32 | Jo Daviess County - 1996

    Typical pattern of soils and parent material in the Fayette-Palsgrove-Rozetta association (Soil Survey of Jo Daviess County, Illinois; 1996).

Map Units

Map units containing PALSGROVE 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
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C225359959952t7ycil01520051:12000
Newglarus-Palsgrove silt loams, silurian landscape, 10 to 18 percent slopes, moderately eroded928D2243510149162t7z4il01520051:12000
Newglarus-Palsgrove silt loams, silurian landscape, 5 to 10 percent slopes, moderately eroded928C260810149172t7z5il01520051:12000
Newglarus-Palsgrove silt loams, silurian landscape, 10 to 18 percent slopes, moderately eroded928D21087719496932t7z4il08519901:12000
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C2973119495712t7ycil08519901:12000
Palsgrove silt loam, 10 to 18 percent slopes, moderately eroded429D2831919496632t7ybil08519901:12000
Palsgrove silt loam, 18 to 25 percent slopes, moderately eroded429E2171719496652t7ylil08519901:12000
Palsgrove silt loam, 2 to 6 percent slopes, moderately eroded429B2148323938832t7y6il08519901:12000
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C1959213722t7ycil10320041:12000
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C224142086292t7ycil14120051:12000
Palsgrove silt loam, 2 to 6 percent slopes, moderately eroded429B219502086282t7y6il14120051:12000
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C2456715920482t7ycil17720061:12000
Palsgrove silt loam, 10 to 18 percent slopes, moderately eroded429D2243616514702t7ybil17720061:12000
Palsgrove silt loam, 2 to 6 percent slopes, moderately eroded429B262515920462t7y6il17720061:12000
Newglarus-Palsgrove silt loams, silurian landscape, 10 to 18 percent slopes, moderately eroded928D255416759982t7z4il17720061:12000
Palsgrove silt loam, 5 to 10 percent slopes, moderately eroded429C221861740972t7ycil20119971:12000
Palsgrove silt loam, 2 to 6 percent slopes, moderately eroded429B214841740962t7y6il20119971:12000
Palsgrove silt loam, 6 to 12 percent slopes587C3441429080gdh9mn16919871:20000
Palsgrove silt loam, 12 to 20 percent slopes587D3389429081gdhbmn16919871:20000
Palsgrove silt loam, 2 to 6 percent slopes587B1032429079gdh8mn16919871:20000
Palsgrove silt loam, 6 to 12 percent slopes, moderately eroded175C2373734241882t7y7wi04319591:20000
Palsgrove silt loam, 12 to 20 percent slopes, moderately eroded175D23619129138762t7y8wi04319591:20000
Palsgrove silt loam, 2 to 6 percent slopes, moderately eroded175B270334241862t7y6wi04319591:20000
Palsgrove silt loam, 6 to 12 percent slopes, moderately erodedPgC265134253462t7y7wi04519691:12000
Palsgrove silt loam, 2 to 6 percent slopes, moderately erodedPgB228334253452t7y6wi04519691:12000
Palsgrove silt loam, 12 to 20 percent slopes, moderately erodedPgD223404253472t7y8wi04519691:12000
Palsgrove silt loam, 6 to 12 percent slopes, moderately erodedDtC2226774245712t7y7wi04919601:20000
Palsgrove silt loam, 12 to 20 percent slopes, moderately erodedDtD2124374245732t7y8wi04919601:20000
Palsgrove silt loam, 2 to 6 percent slopes, moderately erodedDtB2112324245692t7y6wi04919601:20000
Palsgrove silt loam, 6 to 12 percent slopes, moderately erodedPaC2326074248792t7y7wi06519641:15840
Palsgrove silt loam, 2 to 6 percent slopes, moderately erodedPaB2148134248772t7y6wi06519641:15840
Palsgrove silt loam, 12 to 20 percent slopes, moderately erodedPaD293354248822t7y8wi06519641:15840

Map of Series Extent

Approximate geographic distribution of the PALSGROVE 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 .