Official Series Description


Lab Data Summary

Aggregate lab data for the ARENDTSVILLE soil series. This aggregation is based on all pedons with a current taxon name of ARENDTSVILLE, 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 ARENDTSVILLE 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
130A61PA0010081961PA001008Arendtsville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9338889,-77.2775
130A61PA0010091961PA001009Arendtsville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9186111,-77.3108333

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARENDTSVILLE 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 ARENDTSVILLE 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 ARENDTSVILLE 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 ARENDTSVILLE 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 terrace figure.

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

Competing Series

Soil series competing with ARENDTSVILLE 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 ARENDTSVILLE 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 ARENDTSVILLE 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 flats position figure.

Soil series sharing subgroup-level classification with ARENDTSVILLE, 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 ARENDTSVILLE 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
Arendtsville gravelly loam, 2 to 6 percent slopesArnB97014050131j510nj03519721:24000
Arendtsville gravelly loam, 6 to 12 percent slopesArnC74114050151j512nj03519721:24000
Arendtsville gravelly loam, 8 to 15 percent slopesArC4469545548l9pbpa00119911:24000
Arendtsville gravelly loam, 3 to 8 percent slopesArB3502545547l9p9pa00119911:24000
Arendtsville gravelly loam, 15 to 25 percent slopesArD1769545549l9pcpa00119911:24000
Arendtsville gravelly loam, 25 to 40 percent slopesArE400545550l9pdpa00119911:24000
Arendtsville gravelly silt loam, 8 to 15 percent slopesArC1744543597l7ndpa01719971:24000
Arendtsville gravelly silt loam, 3 to 8 percent slopesArB1703543596l7ncpa01719971:24000
Arendtsville gravelly silt loam, 15 to 25 percent slopesArD684543598l7nfpa01719971:24000
Arendtsville gravelly silt loam, 3 to 8 percent slopesArB3075543104l74hpa07719971:24000
Arendtsville gravelly silt loam, 8 to 15 percent slopesArC1797543105l74jpa07719971:24000
Arendtsville gravelly silt loam, 15 to 25 percent slopesArD677543106l74kpa07719971:24000
Arendtsville gravelly silt loam, 0 to 3 percent slopesArA197543103l74gpa07719971:24000
Arendtsville gravelly loam, 3 to 8 percent slopesArB215543223l78bpa09520071:12000
Arendtsville gravelly loam, 8 to 15 percent slopesArC196543224l78cpa09520071:12000
Arendtsville gravelly loam, 15 to 25 percent slopesArD158543225l78dpa09520071:12000
Arendtsville gravelly loam, 8 to 15 percent slopesArC235542804l6ttpa13319901:24000
Arendtsville gravelly loam, 3 to 8 percent slopesArB128542803l6tspa13319901:24000
Arendtsville gravelly loam, 15 to 25 percent slopesArD109542805l6tvpa13319901:24000

Map of Series Extent

Approximate geographic distribution of the ARENDTSVILLE 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 .