Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with HASSHOLLOW 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 HASSHOLLOW 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 HASSHOLLOW 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.

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

Soil series sharing subgroup-level classification with HASSHOLLOW, 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

No block diagrams are available.

Map Units

Map units containing HASSHOLLOW 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
Bata-Cabell-Hasshollow complex, 0 to 30 percent slopes0858NO85531202481q6x9or60720181:24000
Bearpawmeadow-Hasshollow complex, 30 to 60 percent slopes0877CO7031203231qy18or60720181:24000
Bearpawmeadow-Hasshollow-Rock outcrop complex, 15 to 30 percent slopes0879BR4931203541qygvor60720181:24000
Tyeecreek-Hasshollow complex, 15 to 30 percent slopes0870BO4631202641q70por60720181:24000
Tyeecreek-Hasshollow complex, 30 to 60 percent slopes0844CO1731203491qydyor60720181:24000
Bearpawmeadow-Marblepoint-Hasshollow complex, 15 to 30 percent slopes0861BO486124370251qyggor63120181:24000
Bearpawmeadow-Hasshollow complex, 30 to 60 percent slopes0877CO340224370341qy18or63120181:24000
Bata-Cabell-Hasshollow complex, 0 to 30 percent slopes0858NO161024850901q6x9or63120181:24000
Dollarlake-Clarkscreek-Hasshollow complex, 30 to 60 percent slopes0855CO126224370201qyg2or63120181:24000
Bearpawmeadow-Moodybasin-Hasshollow complex, 30 to 60 percent slopes0897CO107224370411qyjpor63120181:24000
Tyeecreek-Hasshollow complex, 30 to 60 percent slopes0844CO87324370101qydyor63120181:24000
Dollarlake-Bearpawmeadow-Hasshollow complex, 15 to 30 percent slopes0854BO78124370191qyg0or63120181:24000
Bearpawmeadow-Hasshollow complex, 0 to 15 percent slopes0877AO73824370331qygror63120181:24000
Tyeecreek-Hasshollow complex, 15 to 30 percent slopes0870BO50124370281q70por63120181:24000
Hasshollow-Ducklake complex, 15 to 30 percent slopes0876BO34624370311qygqor63120181:24000
Digit-Hasshollow-Bandarrow complex, 0 to 15 percent slopes0873AO31924370291qygnor63120181:24000
Bearpawmeadow-Hasshollow-Rock outcrop complex, 15 to 30 percent slopes0879BR30224370351qygvor63120181:24000
Hasshollow-Ducklake complex, 30 to 60 percent slopes0876CO16024370321q6z7or63120181:24000
Tyeecreek-Hasshollow complex, 60 to 90 percent slopes0844DO14724370111qydzor63120181:24000
Mudlakebasin-Hasshollow-Rock outcrop complex, 30 to 60 percent slopes0883CO8524370371qyhpor63120181:24000

Map of Series Extent

Approximate geographic distribution of the HASSHOLLOW 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 .