Official Series Description


Lab Data Summary

Aggregate lab data for the PEAWICK soil series. This aggregation is based on all pedons with a current taxon name of PEAWICK, 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 PEAWICK 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
133AVPI0266V1984-VA081-266Peawick1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5950241,-77.4343262
133AVPI0267V1984-VA081-267Peawick3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5636063,-77.5356445
133AVPI0268V1984-VA081-268Peawick3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5839157,-77.4567566

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PEAWICK 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 PEAWICK 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 PEAWICK 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 PEAWICK 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 PEAWICK 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 PEAWICK 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 PEAWICK 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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Click the image to view it full size.

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 PEAWICK, 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

No block diagrams are available.

Map Units

Map units containing PEAWICK 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
Peawick fine sandy loam, 2 to 8 percent slopesPeB342014856621lvylnc03720051:24000
Peawick fine sandy loam, 0 to 2 percent slopesPeA157714856581lvygnc03720051:24000
Peawick fine sandy loam, 0 to 2 percent slopes, rarely floodedPcA116914856601lvyjnc03720051:24000
Mattaponi-Peawick complex, 8 to 15 percent slopesMcC35714856061lvwsnc03720051:24000
Peawick loam, 0 to 3 percent slopesPkA253022335992dz7lnc12320071:24000
Peawick fine sandy loam, 2 to 6 percent slopesPeB64401147293vcync15319961:24000
Peawick fine sandy loam, 0 to 2 percent slopesPeA23761147283vcxnc15319961:24000
Peawick silt loam, 0 to 3 percent slopes, rarely floodedPfA3601147303vcznc15319961:24000
Peawick silt loam, 2 to 6 percent slopes39B36331178913ynyva03619931:24000
Peawick silt loam, 0 to 2 percent slopes39A34861178903ynxva03619931:24000
Peawick loam, 0 to 3 percent slopes27A6842695363rbl2va08119861:15840
Peawick clay loam, 6 to 12 percent slopes, severely eroded28C31202695365rbl4va08119861:15840
Peawick clay loam, 2 to 6 percent slopes, severely eroded28B3920695364rbl3va08119861:15840
Peawick silt loam, 0 to 2 percent slopes12A5440119306404lva09319821:15840
Uchee-Peawick complex, 2 to 6 percent slopes20B35351193214052va09319821:15840
Peawick-Slagle complex, 2 to 6 percent slopes14B3340119310404qva09319821:15840
Peawick silt loam, 2 to 6 percent slopes12B2080119307404mva09319821:15840
Uchee-Peawick complex, 6 to 10 percent slopes20C7201193224053va09319821:15840
Peawick clay loam, 2 to 6 percent slopes, severely eroded13B3290119309404pva09319821:15840
Peawick silt loam, 6 to 10 percent slopes12C280119308404nva09319821:15840
Peawick silt loam, 0 to 2 percent slopes23A6070120326416hva14919801:15840
Peawick silt loam, 2 to 6 percent slopes23B3361120327416jva14919801:15840
Peawick silt loam, 6 to 10 percent slopes23C1546120328416kva14919801:15840
Peawick silt loam27460312081841qcva69519811:15840
Peawick-Urban land complex, 0 to 3 percent slopes1934112242743d8va71519951:12000

Map of Series Extent

Approximate geographic distribution of the PEAWICK 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 .