Official Series Description


Lab Data Summary

Aggregate lab data for the GERDA soil series. This aggregation is based on all pedons with a current taxon name of GERDA, 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 GERDA 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.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GERDA 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 GERDA 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 GERDA 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 GERDA 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 GERDA 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 GERDA 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 GERDA 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 GERDA, 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. ND-2010-09-27-02 | Billings County - 2005

    Typical pattern of soils and underlying material in the Patent-Badland, outcrop-Cabbart association (Soil Survey of Billings County, North Dakota; 2005).

Map Units

Map units containing GERDA 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
Gerda-Maltese complex, 0 to 6 percent slopesL0516B17132566602q2mlmt02519911:24000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C1354027070682q2n3nd00719981:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B816027070692qz6rnd00719981:24000
Gerda-Kirby complex, 2 to 15 percent slopesL3015D720727070542qxl9nd00719981:24000
Maltese-Gerda complex, 0 to 6 percent slopesL0454B539527070332qk3pnd00719981:24000
Gerda-Maltese complex, 0 to 6 percent slopesL0516B231925634552q2mlnd01119691:20000
Gerda-Gerda, barren complex, 0 to 6 percent slopesL0531B65725634562qk3znd01119691:20000
Maltese-Gerda complex, 0 to 6 percent slopesL0454B47525634542qk3pnd01119691:20000
Kremlin-Belfield, low precipitation-Gerda complex, 0 to 2 percent slopesL0627A18125634592q2mnnd01119691:20000
Oburn-Gerda, barren complex, 0 to 6 percent slopesL0533B14125634572qk40nd01119691:20000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C1527584652q2n3nd01119691:20000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C127927071302q2n3nd02519811:20000
Gerda-Maltese complex, 0 to 6 percent slopesL0516B70227071282q2mlnd02519811:20000
Gerda-Maltese complex, 0 to 6 percent slopesL0516B671927073172q2mlnd03319851:24000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C135127073422q2n3nd03319851:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B128627073432qz6rnd03319851:24000
Gerda-Kirby complex, 2 to 15 percent slopesL3015D627597662qxl9nd03319851:24000
Maltese-Gerda complex, 0 to 6 percent slopesL0454B621227151392qk3pnd05320031:24000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C539927151372q2n3nd05320031:24000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B155727151622qz6rnd05320031:24000
Gerda-Kirby complex, 2 to 15 percent slopesL3015D127327151532qxl9nd05320031:24000
Patent, occasionally flooded-Vanda-Gerda, barren complex, 0 to 9 percent slopesL3247C508927159412q2n3nd08719741:20000
Gerda-Maltese complex, 0 to 6 percent slopesL0516B214827158852q2mlnd08719741:20000
Maltese-Gerda complex, 0 to 6 percent slopesL0454B70227158842qk3pnd08719741:20000
Kremlin-Ethridge-Gerda complex, 0 to 6 percent slopesL3251B19027159442qz6rnd08719741:20000
Gerda-Kirby complex, 2 to 15 percent slopesL3015D8527585382qxl9nd08719741:20000
Gerda-Gerda, barren complex, 0 to 6 percent slopesL0531B127585272qk3znd08719741:20000
Kremlin-Belfield, low precipitation-Gerda complex, 0 to 2 percent slopesL0627A127585282q2mnnd08719741:20000

Map of Series Extent

Approximate geographic distribution of the GERDA 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 .