Official Series Description


Lab Data Summary

Aggregate lab data for the HORSEHEAD soil series. This aggregation is based on all pedons with a current taxon name of HORSEHEAD, 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 HORSEHEAD 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
94A94P0553S1993MI119002Horsehead5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9880562,-84.2222214

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD 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 HORSEHEAD, 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. MI-2010-09-07-23 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Rubicon-Grayling-Tawas and Millersburg-Klacking-Horsehead associations (Soil Survey of Montmorency County, Michigan; 2003).

Map Units

Map units containing HORSEHEAD 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
Horsehead-Graycalm sands, 0 to 6 percent slopes390B45961922796g2kmi11919971:12000
Horsehead sand, 0 to 6 percent slopes391B45111922836g2pmi11919971:12000
Horsehead-Graycalm sands, 6 to 18 percent slopes390D42721922806g2lmi11919971:12000
Horsehead-Graycalm sands. 18 to 35 percent slopes390E29551922816g2mmi11919971:12000
Horsehead-Graycalm sands, 35 to 70 percent slopes390F16801922826g2nmi11919971:12000
Horsehead sand, 6 to 18 percent slopes391D12851922846g2qmi11919971:12000
Horsehead gravelly sand, 6 to 18 percent slopes389D9951922766g2gmi11919971:12000
Horsehead gravelly sand, 18 to 35 percent slopes389E4801922776g2hmi11919971:12000
Horsehead gravelly sand, 0 to 6 percent slopes389B4061922756g2fmi11919971:12000
Horsehead-Graycalm sands, 0 to 6 percent slopes390B272620904670jfmi13520031:12000
Coppler-Horsehead sands, 0 to 6 percent slopes504B201520907870kgmi13520031:12000
Bamfield, sandy substratum-Millersburg-Horsehead complex, 6 to 18 percent slopes503D173120907270k8mi13520031:12000
Horsehead-Graycalm sands, 6 to 18 percent slopes390D130020904770jgmi13520031:12000
Ossineke-Millersburg-Horsehead complex, 0 to 6 percent slopes505B76420908570kpmi13520031:12000
Horsehead-Graycalm sands, 18 to 35 percent slopes390E68620904870jhmi13520031:12000
Bamfield, sandy substratum-Millersburg-Horsehead complex, 18 to 35 percent slopes503E51220907670kdmi13520031:12000
Coppler-Horsehead sands, 6 to 18 percent slopes504D46320907970khmi13520031:12000
Ossineke-Millersburg-Horsehead complex, 6 to 12 percent slopes505C46220907570kcmi13520031:12000
Horsehead-Graycalm sands, 35 to 70 percent slopes390F28620904970jjmi13520031:12000
Coppler-Horsehead sands, 18 to 35 percent slopes504E13320908370kmmi13520031:12000
Horsehead sand, 0 to 6 percent slopes391B15241416836mmi13520031:12000

Map of Series Extent

Approximate geographic distribution of the HORSEHEAD 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 .