Official Series Description


Lab Data Summary

Aggregate lab data for the MANFRED soil series. This aggregation is based on all pedons with a current taxon name of MANFRED, 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 MANFRED 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
5474ND02900374ND029003Manfred4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3135808,-100.3782541
5474ND05700274ND057002Manfred4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2416326,-101.437467
55A83ND01922583ND019225Manfred3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.615,-98.0605556
55A83ND01922783ND019227Manfred3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6055556,-98.0630556
55A83ND019226S1983ND019226Manfred3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.6152778,-98.0602778
55B78ND0350041978ND035004Manfred5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7102778,-97.8013889

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MANFRED 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 MANFRED 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 MANFRED 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 MANFRED 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.

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

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Competing Series

Soil series competing with MANFRED 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 MANFRED 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 MANFRED 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 MANFRED, 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-2012-02-07-39 | Foster County - July 1995

    Typical pattern of soils and parent material in the Cathay-Heimdal-Larson association (Soil Survey of Foster County, North Dakota; July 1995).

Map Units

Map units containing MANFRED 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
Vallers, saline-Manfred loams, 0 to 1 percent slopes, extremely stonyG624A235825736442q5smnd00319881:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A101125876222q4gdnd0051:12000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A7525737552q3vqnd0051:12000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A1225859052q4gdnd00919811:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A522725875192q4gdnd01919871:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A804925752792q3vqnd02119891:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A230225763902q3vqnd03119901:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A874425765122q3vqnd03519801:20000
Vallers, saline-Manfred clay loams, 0 to 1 percent slopesI228A24726425932ptwtnd03519801:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A123425765812q3vqnd03919911:24000
Vallers, saline-Manfred loams, 0 to 1 percent slopes, extremely stonyG624A1425766602q5smnd03919911:24000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A7125770432q3vqnd04519661:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A255025713412q3vqnd04919871:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A9625856002q4gdnd04919871:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A14425771802q3vqnd05519741:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A364225772652q3vqnd0631:12000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A172325873202q4gdnd0631:12000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A397925880222q4gdnd07919901:24000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A99025819452q3vqnd08319901:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A525797312q3vqnd09119911:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A250725861142q4gdnd09919671:20000
Manfred silty clay loam, 0 to 1 percent slopesI546A89526429022ptwlnd09919671:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesF120A1925851272q4gdnd10119671:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A81525796072q3vqnd10319661:12000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A127976492q3vqsd01319871:20000
Vallers, saline-Manfred complex, 0 to 1 percent slopesG120A2027987972q3vqsd08919801:20000

Map of Series Extent

Approximate geographic distribution of the MANFRED 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 .