Official Series Description


Lab Data Summary

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

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

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Competing Series

Soil series competing with RUDYARD 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 RUDYARD 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 RUDYARD 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 RUDYARD, 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-2010-09-07-11 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Pickford-Rudyard association (Soil Survey of Mackinac County, Michigan; 1997).

  2. MI-2012-02-06-10 | Chippewa County - February 1992

    Typical pattern of soils and parent material in the Pickford-Rudyard-Ontonagon association (Soil Survey of Chippewa County, Michigan; February 1992).

  3. MI-2012-02-06-18 | Houghton County Area - October 1991

    Diagrammatic cross section of Houghton County showing the topography, elevation, general soil texture, landforms, and dominant soils and their drainage class (Soil Survey of Houghton County Area, Michigan; October 1991).

  4. MI-2012-02-06-35 | Mackinac County - 1997

    Typical pattern of soils and parent material in the Pickford-Rudyard association (Soil Survey of Mackinac County, Michigan; 1997).

Map Units

Map units containing RUDYARD 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
Rudyard silty clay loam, 0 to 2 percent slopesRyA1331892656bybmi01119641:20000
Rudyard silt loam, 0 to 3 percent slopes35A7794149752xtmxmi01319841:20000
Rudyard silt loam, 0 to 6 percent slopesRrB3671905076d7dmi02919701:15840
Rudyard loam, 0 to 3 percent slopes60A62291906036dbhmi03119881:15840
Rudyard silty clay loam, 0 to 3 percent slopes11A317994150762xtmzmi03319891:15840
Rudyard silt loam, 0 to 3 percent slopes129A100574150862xtmxmi03319891:15840
Rudyard-Pickford silty clay loams, 0 to 3 percent slopes130A6378415087fxxxmi03319891:15840
Rudyard-Urban land complex, 0 to 3 percent slopes139A1293415095fxy5mi03319891:15840
Rudyard-Allendale complex, 0 to 3 percent slopes40A1232415147fxzvmi03319891:15840
Rudyard loam, 0 to 2 percent slopesRyA13611898576ckfmi05119661:15840
Rudyard loam, 2 to 6 percent slopesRyB2721898586ckgmi05119661:15840
Froberg-Rudyard silt loams, 1 to 8 percent slopes73B3420416157fz1fmi06119891:20000
Allendale-Rudyard complex, 0 to 3 percent slopes51A2249416135fz0qmi06119891:20000
Rudyard silt loam, 0 to 3 percent slopes65A10954161472xtmxmi06119891:20000
Rudyard silt loam, 0 to 3 percent slopes129A23346313112xtmxmi09520041:24000
Rudyard-Pickford silt loams, 0 to 3 percent slopes130A796631312p5xxmi09520041:24000
Rudyard silty clay loam, 0 to 3 percent slopes11A77854163142xtmzmi09719941:20000
Engadine-Rudyard complex, 0 to 3 percent slopes165A986416337fz77mi09719941:20000
Rudyard-Allendale complex, 0 to 3 percent slopes40A804416400fz98mi09719941:20000

Map of Series Extent

Approximate geographic distribution of the RUDYARD 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 .