Official Series Description


Lab Data Summary

Aggregate lab data for the JOPPA soil series. This aggregation is based on all pedons with a current taxon name of JOPPA, 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 JOPPA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
149A87P018886MD510006Joppa5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2457133,-76.61998

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JOPPA 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 JOPPA 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 JOPPA 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 JOPPA 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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Competing Series

Soil series competing with JOPPA 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 JOPPA 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 JOPPA 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.

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

Soil series sharing subgroup-level classification with JOPPA, 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-2010-09-03-03 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Joppa-Sassafras association (Soil Survey of City of Baltimore, Maryland; 1998).

  2. MD-2012-02-03-04 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Joppa-Sassafras association (Soil Survey of City of Baltimore, Maryland; 1998).

Map Units

Map units containing JOPPA 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
Urban land-Joppa complex, 0 to 15 percent slopesUoC21112868149x0dc00119751:12000
Joppa gravelly sandy loam, 15 to 40 percent slopesJtD15312861749tydc00119751:12000
Joppa gravelly sandy loam, 8 to 15 percent slopesJtC8212861649txdc00119751:12000
Joppa-Urban land complex, 8 to 15 percent slopesJuC7712861949v0dc00119751:12000
Joppa-Urban land complex, 0 to 8 percent slopesJuB5912861849tzdc00119751:12000
Joppa-Urban land complex, 15 to 25 percent slopesJuD3312862049v1dc00119751:12000
Joppa gravelly sandy loam, 0 to 8 percent slopesJtB1512861549twdc00119751:12000
Joppa-Urban land complex, 0 to 8 percent slopes13UB1323533895kxkfmd51019931:12000
Joppa-Urban land complex, 8 to 15 percent slopes13UC1123533896kxkgmd51019931:12000
Urban land-Joppa complex, 0 to 8 percent slopes14UB544533897kxkhmd51019931:12000
Sassafras-Joppa complex, 0 to 8 percent slopes30B194533941kxlxmd51019931:12000
Joppa gravelly sandy loam, 8 to 15 percent slopes13C188533893kxkcmd51019931:12000
Joppa gravelly sandy loam, 0 to 8 percent slopes13B121533892kxkbmd51019931:12000
Joppa gravelly sandy loam, 15 to 60 percent slopes13E74533894kxkdmd51019931:12000
Joppa gravelly sandy loam, 5 to 10 percent slopesJpC823533398kx1dmd60019721:15840
Sassafras and Joppa soils, 15 to 30 percent slopesSsE562533453kx35md60019721:15840
Joppa gravelly sandy loam, 2 to 5 percent slopesJpB484533397kx1cmd60019721:15840
Sassafras and Joppa soils, 10 to 15 percent slopesSsD387533452kx34md60019721:15840

Map of Series Extent

Approximate geographic distribution of the JOPPA 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 .