Official Series Description


Lab Data Summary

Aggregate lab data for the HERKIMER soil series. This aggregation is based on all pedons with a current taxon name of HERKIMER, 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 HERKIMER 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 HERKIMER 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 HERKIMER 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 HERKIMER 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 HERKIMER 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 HERKIMER 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 HERKIMER 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 HERKIMER 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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Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with HERKIMER, 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. NY-2010-09-28-21 | Otsego County - 2006

    Typical pattern of soils and underlying material in the Farmington-Wassaic general soil map unit (Soil Survey of Otsego County, New York; 2006).

  2. NY-2012-02-16-06 | Wyoming County - April 1974

    Typical pattern of soils in association 13 (Soil Survey of Wyoming County, New York; April 1974).

Map Units

Map units containing HERKIMER 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
Herkimer gravelly silt loam, 0 to 3 percent slopesHhA272725183239swrny04320181:24000
Herkimer gravelly silt loam, moderately well drained, 0 to 4 percent slopesHkB199625183259swtny04320181:24000
Herkimer gravelly silt loam, 3 to 8 percent slopesHhB186125183249swsny04320181:24000
Herkimer silt loam, 3 to 8 percent slopesHcB21402677701bmkzny04920181:24000
Herkimer silt loam, 0 to 3 percent slopesHbA20762677697bmkvny04920181:24000
Herkimer silt loam, 0 to 3 percent slopesHcA14902677700bmkyny04920181:24000
Herkimer silt loam, 3 to 8 percent slopesHbB8832677698bmkwny04920181:24000
Herkimer silt loam, 8 to 15 percent slopesHcC5292677702bml0ny04920181:24000
Herkimer silt loam, 15 to 25 percent slopesHbD48926777592dcr6ny04920181:24000
Herkimer silt loam, 8 to 15 percent slopesHbC2612677699bmkxny04920181:24000
Herkimer silt loam, 0 to 3 percent slopesGeA1522677678bmk7ny04920181:24000
Herkimer channery silt loam, 3 to 8 percent slopesHeB7642925629tfhny05319751:15840
Herkimer channery silt loam, calcareous subsoil variantHe3442928239tpxny05719731:24000
Herkimer channery silt loam, 3 to 8 percent slopes12B19132933329v7bny06519931:24000
Herkimer channery silt loam, 8 to 15 percent slopes12C2012933339v7cny06519931:24000
Herkimer channery silt loam, 3 to 8 percent slopes, cool816B55643761plwhny06519931:24000
Herkimer silt loamHe19222935719vh1ny06719731:20000
Herkimer channery silt loam, 2 to 8 percent slopesHeB3742941179w1nny07519731:15840
Herkimer channery silt loam, 8 to 15 percent slopesHeC1232941189w1pny07519731:15840
Herkimer gravelly silt loam, fan, 2 to 6 percent slopesHeB12192942179w4wny07719931:24000
Herkimer gravelly silt loam, fan, 0 to 2 percent slopesHeA8512942169w4vny07719931:24000
Herkimer channery silt loam, calcareous subsoil variantHe95309580bd4gny09319731:15840
Herkimer gravelly silt loam, 0 to 3 percent slopesHeA9032959759xzlny11519721:20000
Herkimer gravelly silt loam, 3 to 8 percent slopesHeB4012959769xzmny11519721:20000
Herkimer channery silt loam, 3 to 8 percent slopesHeB17062953609xbrny12119691:20000
Herkimer channery silt loam, 0 to 3 percent slopesHeA14862953599xbqny12119691:20000

Map of Series Extent

Approximate geographic distribution of the HERKIMER 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 .