Official Series Description


Lab Data Summary

Aggregate lab data for the WATCHUNG soil series. This aggregation is based on all pedons with a current taxon name of WATCHUNG, 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 WATCHUNG 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
14887P018786MD510005Watchung5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3713875,-76.6869431

Water Balance

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

Soil series sharing subgroup-level classification with WATCHUNG, 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. MD-2010-09-10-04 | Cecil County -

    Neshaminy-Montalto-Chrome-Watchung association (Soil Survey of Cecil County, Maryland).

  2. PA-2010-09-30-02 | Adams County - 2005

    Typical pattern of soils and parent material in the Lehigh-Neshiminy general soil map unit (Soil Survey of Adams County, Pennsylvania; 2005).

Map Units

Map units containing WATCHUNG 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
Watchung silt loam, 0 to 3 percent slopesWaA45224798972p7jpde00320091:24000
Watchung silt loam, 3 to 8 percent slopesWaB25924798982p7jqde00320091:24000
Watchung silt loam, 0 to 8 percent slopes, very stonyWcB18524798992p7jrde00320091:24000
Watchung silt loam, 3 to 8 percent slopesWaB93524060832lrqlmd00520101:12000
Watchung-Urban land complex, 0 to 8 percent slopesWdB57424833862pc57md00520101:12000
Watchung silt loam, 3 to 8 percent slopes, stonyWcB48524060882lrqrmd00520101:12000
Watchung silt loam, 0 to 3 percent slopesWaA8624060802lrqhmd00520101:12000
Conowingo-Watchung complex, 0 to 8 percent slopes, very stonyCrB29024407752mxtpmd01520091:12000
Watchung silt loam, 0 to 3 percent slopesWaA22124407732mxtmmd01520091:12000
Watchung silt loam, 3 to 8 percent slopesWaB7324407742mxtnmd01520091:12000
Watchung silt loam, 0 to 8 percent slopesWcB449530780kt9ymd02120011:12000
Watchung silt loam, 3 to 8 percent slopes, stonyWcB423793659vmvxmd02720041:12000
Watchung silt loam, 0 to 3 percent slopesWaA97793658vmvwmd02720041:12000
Watchung silty clay loam, 0 to 3 percent slopes28A838533617kx8gmd03119891:15840
Watchung very stony silt loam, 0 to 8 percent slopesWcB2969533459kx3cmd60019721:15840
Watchung silt loam, 3 to 8 percent slopesWaB2281533458kx3bmd60019721:15840
Watchung silt loam, 0 to 3 percent slopesWaA1302533457kx39md60019721:15840
Mount Lucas-Watchung silt loams, 0 to 6 percent slopes, very stonyMopBb3323548634ldwwnj01919701:24000
Watchung silt loam, 0 to 2 percent slopesWasA13814277881jxqpnj01919701:24000
Watchung silt loam, 0 to 3 percent slopes, very rubblyWasAe236607168nct2nj02119691:24000
Watchung silt loam, 0 to 2 percent slopesWasA19714270421jwymnj02119691:24000
Mount Lucas-Watchung silt loams, 0 to 6 percent slopes, very stonyMopBb791351014jl3nj02119691:24000
Mount Lucas-Watchung silt loams, 6 to 12 percent slopes, very stonyMopCb141351024jl4nj02119691:24000
Watchung silt loam, 0 to 2 percent slopes, very stonyWasAb78813954391hv25nj02319851:24000
Mount Lucas-Watchung silt loams, 6 to 12 percent slopes, very stonyMopCb2114551791kv78nj02319851:24000
Mount Lucas-Watchung silt loams, 6 to 12 percent slopes, very stonyMopCb615914050481j524nj03519721:24000
Watchung silt loam, 0 to 2 percent slopesWasA171014439311kgjfnj03519721:24000
Mount Lucas-Watchung silt loams, 0 to 6 percent slopes, very stonyMopBb10514050471j523nj03519721:24000
Watchung silt loam, 0 to 3 percent slopesWaA5911545658l9swpa00119911:24000
Watchung silt loam, 3 to 8 percent slopesWaB809545659l9sxpa00119911:24000
Watchung silt loam, 0 to 8 percent slopes, extremely boulderyWbB512545660l9sypa00119911:24000
Watchung silt loam, 0 to 3 percent slopesWaA642641642pjp4pa02920081:24000
Watchung silt loam, 3 to 8 percent slopesWaB417641643pjp5pa02920081:24000
Watchung silt loamWa627540773l4q9pa04319671:15840
Watchung very stony silt loamWc380540774l4qbpa04319671:15840
Watchung silt loam, 3 to 8 percent slopesWaB149844562zhhwpa04519601:20000
Watchung silt loam, 0 to 3 percent slopesWaA139844552zhhvpa04519601:20000
Watchung silt loam, 0 to 8 percent slopes, very stonyWcB398453030cglpa04519601:20000
Watchung extremely stony silt loam, 0 to 8 percent slopesWbB48558454lr3npa07119821:15840
Watchung extremely stony silt loam, 0 to 8 percent slopesWbB970541342l59npa07519761:20000
Watchung silt loam, 0 to 5 percent slopesWaA809541341l59mpa07519761:20000
Watchung silt loam, 0 to 8 percent slopes, extremely stonyWcB1415541261l571pa09120081:12000
Watchung silt loam, 3 to 8 percent slopesWaB534541260l570pa09120081:12000
Watchung silt loam, 0 to 3 percent slopesWaA325541259l56zpa09120081:12000
Watchung silt loam, 0 to 8 percent slopes, extremely boulderyWbB4294542963l6zypa13319901:24000
Watchung silt loam, 0 to 3 percent slopesWaA1965542961l6zwpa13319901:24000
Watchung silt loam, 3 to 8 percent slopesWaB267542962l6zxpa13319901:24000

Map of Series Extent

Approximate geographic distribution of the WATCHUNG 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 .