Official Series Description


Lab Data Summary

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

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

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

Competing Series

Soil series competing with KINZUA 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 KINZUA 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 KINZUA 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 .

Click the image to view it full size.

Click the image to view it full size.

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 KINZUA, 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-2010-09-28-01 | Cattarugus County - 2007

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Cattarugus County, New York; 2007).

  2. NY-2012-02-15-10 | Chautauqua County - August 1994

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Chautauqua County, New York; August 1994).

Map Units

Map units containing KINZUA 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
Kinzua channery silt loam, 25 to 35 percent slopes97E831300042b26sny00320131:24000
Kinzua channery silt loam, 25 to 35 percent slopes, extremely bouldery98E163318150bp1xny00320131:24000
Kinzua channery silt loam, 15 to 25 percent slopes97D128300041b26rny00320131:24000
Kinzua channery silt loam, 15 to 25 percent slopes, extremely bouldery98D47300046b26xny00320131:24000
Kinzua channery silt loam, 35 to 60 percent slopes, extremely bouldery98F33300047b26yny00320131:24000
Kinzua channery silt loam, 35 to 60 percent slopes97F28300043b26tny00320131:24000
Kinzua channery silt loam, 25 to 35 percent slopes97E155492897609qj3ny00920021:24000
Kinzua channery silt loam, 15 to 25 percent slopes97D44172897599qj2ny00920021:24000
Kinzua channery silt loam, 25 to 35 percent slopes, extremely bouldery98E31322897659qj8ny00920021:24000
Kinzua channery silt loam, 8 to 15 percent slopes97C19662897589qj1ny00920021:24000
Kinzua channery silt loam, 35 to 60 percent slopes97F10492897619qj4ny00920021:24000
Kinzua channery silt loam, 15 to 25 percent slopes, extremely bouldery98D9702897649qj7ny00920021:24000
Kinzua channery silt loam, 3 to 8 percent slopes97B4352897579qj0ny00920021:24000
Kinzua channery silt loam, 25 to 45 percent slopesKnE1112898479qlxny01319881:15840
Kinzua channery silt loam, 35 to 60 percent slopesKnF333914523881krb7pa08319841:20000
Kinzua channery silt loam, 25 to 35 percent slopesKnE64214523871krb6pa08319841:20000
Kinzua channery silt loam, 15 to 25 percent slopesKnD23114523861krb5pa08319841:20000
Kinzua channery silt loam, 8 to 15 percent slopesKnC13814523851krb4pa08319841:20000
Kinzua channery silt loam, 3 to 8 percent slopesKnB13314523841krb3pa08319841:20000
Kinzua channery silt loam, 25 to 65 percent slopes, extremely stonyKkF3938829990472x4x5pa10519531:24000
Kinzua-Madsheep channery silt loams, 25 to 65 percent slopes, extremely stonyKmF773129990492x4x7pa10519531:24000
Kinzua-Madsheep channery silt loams, 15 to 25 percent slopes, extremely stonyKmD114829990482x4x6pa10519531:24000
Kinzua channery silt loam, 35 to 60 percent slopesKnF94614513411kq7gpa60919791:20000
Kinzua channery silt loam, 3 to 8 percent slopesKnB24814513371kq7bpa60919791:20000
Kinzua channery silt loam, 15 to 25 percent slopesKnD14514513391kq7dpa60919791:20000
Kinzua channery silt loam, 8 to 15 percent slopesKnC1014513381kq7cpa60919791:20000

Map of Series Extent

Approximate geographic distribution of the KINZUA 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 .