Official Series Description


Lab Data Summary

Aggregate lab data for the CHRISTIANA soil series. This aggregation is based on all pedons with a current taxon name of CHRISTIANA, 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 CHRISTIANA 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
149A40A531269MD005001Christiana5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3441172,-76.4704977
149A87P019186MD510009Christiana5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2533067,-76.6275918
149A95P0270S1994MD033002Christiana6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0275002,-76.8347244

Water Balance

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

Competing Series

Soil series competing with CHRISTIANA 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 CHRISTIANA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CHRISTIANA 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 CHRISTIANA, 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. DC-2011-05-31-02 | District of Columbia - 1976

    Typical pattern of soils and parent material in the Urban land-Christiana-Sunnyside association (Soil Survey of District of Columbia; 1976).

  2. DC-2011-05-31-04 | District of Columbia - 1976

    Diagram of fall line between the Piedmont Plateau and the Coastal Plain. Diagram also shows the relationship of parent material and topography (Soil Survey of District of Columbia; 1976).

  3. MD-2010-09-03-01 | City of Baltimore - 1998

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

  4. MD-2012-02-03-01 | Anne Arundel County - February 1973

    Representative pattern of soils and parent material in soil association 2 (Soil Survey of Anne Arundel County, Maryland; February 1973).

  5. MD-2012-02-03-05 | City of Baltimore - 1998

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

  6. MD-2012-02-03-08 | Baltimore County - March 1978

    Cross section showing relationships of parent material and topography to certain soil series of Baltimore County. Fall line shown in drawing separates soil of Piedmont Province (left) from soils of Atlantic Coastal Plain (right) (Soil Survey of Baltimore County, Maryland; March 1976).

Map Units

Map units containing CHRISTIANA 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
Christiana-Urban land complex, 8 to 15 percent slopesCfC111612858649sydc00119751:12000
Urban land-Christiana complex, 8 to 15 percent slopesUfC45112867849wxdc00119751:12000
Christiana-Urban land complex, 0 to 8 percent slopesCfB44812858549sxdc00119751:12000
Christiana-Urban land complex, 15 to 40 percent slopesCfD26112858749szdc00119751:12000
Christiana silt loam, 15 to 40 percent slopesCeD25212858449swdc00119751:12000
Christiana silt loam, 8 to 15 percent slopesCeC20612858349svdc00119751:12000
Urban land-Christiana complex, 0 to 8 percent slopesUfB8112867749wwdc00119751:12000
Christiana silt loam, 0 to 8 percent slopesCeB7412858249stdc00119751:12000
Russett-Christiana-Hambrook complex, 0 to 5 percent slopesRhB63751378144mdmmd00320031:12000
Russett-Christiana-Hambrook complex, 5 to 10 percent slopesRhC284524314542mm40md00320031:12000
Russett-Christiana-Urban land complex, 0 to 5 percent slopesRkB185324314562mm42md00320031:12000
Russett-Christiana-Hambrook complex, 10 to 15 percent slopesRhD142424314552mm41md00320031:12000
Christiana-Sassafras complex, 2 to 5 percent slopesCcrB920609562ng99md00320031:12000
Christiana-Sassafras-Urban land complex, 5 to 15 percent slopesCdD7881377214m9mmd00320031:12000
Christiana-Sassafras complex, 5 to 10 percent slopesCcrC588609563ng9bmd00320031:12000
Christiana-Sassafras-Urban land complex, 0 to 5 percent slopesCdB4421377044m92md00320031:12000
Christiana-Urban land complex, 5 to 15 percent slopesCdD24624813222p90nmd00520101:12000
Christiana silt loam, 5 to 10 percent slopesCcC19424041752lpr1md00520101:12000
Christiana-Urban land complex, 0 to 5 percent slopesCdB13424041762lpr2md00520101:12000
Christiana silt loam, 2 to 5 percent slopesCcB11424041742lpr0md00520101:12000
Russett-Christiana-Hambrook complex, 5 to 10 percent slopesRmC600424406332mxp3md01520091:12000
Russett-Christiana-Hambrook complex, 10 to 15 percent slopesRmD273124406342mxp4md01520091:12000
Russett-Christiana-Hambrook complex, 0 to 5 percent slopesRmB238924406322mxp2md01520091:12000
Russett-Christiana-Urban land complex, 0 to 5 percent slopesRxB46624407862mxv1md01520091:12000
Christiana-Sassafras-Urban land complex, 5 to 15 percent slopesCfD32324406492mxpmmd01520091:12000
Christiana-Sassafras-Urban land complex, 0 to 5 percent slopesCfB32224406482mxplmd01520091:12000
Christiana-Downer-Urban land complex, 5 to 15 percent slopesCdD698024552772ndxhmd03320091:12000
Russett-Christiana-Urban land complex, 0 to 5 percent slopesRuB694524552762ndxgmd03320091:12000
Christiana-Downer complex, 5 to 10 percent slopesCcC454324552722ndxbmd03320091:12000
Russett-Christiana complex, 2 to 5 percent slopesRcB438224552702ndx8md03320091:12000
Urban land-Russett-Christiana complex, 0 to 5 percent slopesUrrB396024552792ndxkmd03320091:12000
Urban land-Christiana-Downer complex, 5 to 15 percent slopesUrcD365524552802ndxlmd03320091:12000
Christiana-Downer complex, 10 to 15 percent slopesCcD171524552732ndxcmd03320091:12000
Christiana-Downer complex, 15 to 25 percent slopesCcE85124552742ndxdmd03320091:12000
Russett-Christiana complex, 0 to 2 percent slopesRcA54224552692ndx7md03320091:12000
Christiana-Downer-Urban land complex, 15 to 25 percent slopesCdE52324552782ndxjmd03320091:12000
Christiana-Downer complex, 25 to 40 percent slopesCcF22024552752ndxfmd03320091:12000
Urban land-Sunnyside-Christiana complex, 0 to 8 percent slopes34UB1210533948kxm4md51019931:12000
Urban land-Sunnyside-Christiana complex, 8 to 15 percent slopes34UC823533949kxm5md51019931:12000
Sunnyside-Christiana complex, 0 to 8 percent slopes33B240533944kxm0md51019931:12000
Christiana-Urban land complex, 0 to 8 percent slopes7UB203533973kxmymd51019931:12000
Christiana-Urban land complex, 8 to 15 percent slopes7UC92533974kxmzmd51019931:12000
Sunnyside-Christiana complex, 8 to 15 percent slopes33C44533945kxm1md51019931:12000
Urban land-Christiana complex, 0 to 8 percent slopes8UB44533975kxn0md51019931:12000

Map of Series Extent

Approximate geographic distribution of the CHRISTIANA 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 .