Official Series Description


Lab Data Summary

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

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 HANGAARD 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 HANGAARD 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 HANGAARD 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 hills figure.

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

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with HANGAARD, 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. MN-2010-09-08-29 | Polk County - 2003

    Typical pattern of soils and underlying material in the Sandberg-Radium-Syrene association (Soil Survey of Polk County, Minnesota; 2003).

  2. MN-2010-09-10-08 | Roseau County -

    Relationship of soils, underlying materials, and landforms in the Karstad-Markey-Corliss association (Soil Survey of Roseau County, Minnesota).

Map Units

Map units containing HANGAARD 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
Rushlake and Hangaard soils, lake beaches11383448397428fbk8mn00519941:20000
Hangaard sandy loam111308397407fbjlmn00519941:20000
Hangaard sandy loam111658430383gfvbmn02919931:20000
Hangaard sandy loam, 0 to 2 percent slopesI28A4112798155prndmn02919931:20000
Hangaard sandy loamHa922397284fbdmmn04119701:12000
Hangaard sandy loam, dense till, 0 to 2 percent slopesI105A16352798851307d6mn06920071:12000
Hangaard sandy loam, 0 to 2 percent slopesI28A11992798913prndmn08919941:20000
Hangaard sandy loam111366357096czl7mn08919941:20000
Hangaard sandy loam, dense till, 0 to 2 percent slopesI105A52798980307d6mn08919941:20000
Hangaard sandy loam, 0 to 2 percent slopesI28A7372799041prndmn10719701:20000
Rushlake-Hangaard complex11204102435539gm6nmn11119961:20000
Hangaard loamy sand, lake beaches1114980435538gm6mmn11119961:20000
Hangaard sandy loam, 0 to 2 percent slopesI28A8362799650prndmn11919961:20000
Hangaard sandy loam111190352159ctfzmn11919961:20000
Hangaard sandy loam, 0 to 2 percent slopesI28A3872799775prndmn12520011:12000
Hangaard sandy loam, 0 to 2 percent slopes1111368394770f7sjmn13519991:24000
Hangaard sandy loam, 0 to 2 percent slopesI28A3222799825prndmn13519991:24000
Hangaard sandy loam1112027428495gcwfmn15319851:20000
Hangaard-Sioux complex823645428576gcz1mn15319851:20000

Map of Series Extent

Approximate geographic distribution of the HANGAARD 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 .