Official Series Description


Lab Data Summary

Aggregate lab data for the ABBAYE soil series. This aggregation is based on all pedons with a current taxon name of ABBAYE, 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE 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 ABBAYE, 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-2010-09-10-13 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Munising-Yalmer-Garlic association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  2. 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).

Map Units

Map units containing ABBAYE 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
Munising-Abbaye fine sandy loams, 1 to 12 percent slopes, dissected, stony158C601714553261kvd0mi00320071:24000
Munising-Abbaye fine sandy loams, 1 to 6 percent slopes211B535314553591kvf2mi00320071:24000
Abbaye-Zeba complex, 0 to 6 percent slopes, very stony233B79714553731kvfjmi00320071:24000
Abbaye loamy sand, 1 to 8 percent slopes50B3426414988fxtqmi01319841:20000
Deerton and Abbaye soils, dissected, 1 to 8 percent slopes93B576415042fxwgmi01319841:20000
Deerton and Abbaye soils, dissected, 8 to 35 percent slopes93D414415043fxwhmi01319841:20000
Abbaye loamy sand, 8 to 15 percent slopes50D310414989fxtrmi01319841:20000
Abbaye-Munising complex, 1 to 15 percent slopes8105C26424507122n857mi01319841:20000
Munising-Abbaye-Kalkaska complex, dissected, 1 to 12 percent slopes, rocky66B5698416148fz14mi06119891:20000
Munising-Abbaye-Kalkaska complex, dissected, 15 to 70 percent slopes, rocky66F4779416150fz16mi06119891:20000
Abbaye-Munising loamy fine sands, 1 to 8 percent slopes22B4398416109fyzwmi06119891:20000
Munising-Abbaye-Kalkaska complex, dissected, 8 to 35 percent slopes, rocky66D1945416149fz15mi06119891:20000
Abbaye-Munising complex, 1 to 15 percent slopes8105C182024838912pcpjmi06119891:20000
Abbaye-Munising complex, 1 to 15 percent slopes8105C60616748221t6sjmi13120071:24000
Munising-Abbaye-Yalmer complex, dissected, 8 to 35 percent slopes, stony183E2901801605vx47mi60520041:24000
Munising-Abbaye-Yalmer complex, dissected, 1 to 12 percent slopes, stony183C2535801606vx48mi60520041:24000
Abbaye-Lapoin complex, 0 to 6 percent slopes611B112514444601kh2hwi00320061:12000
Abbaye-Zeba complex, 0 to 6 percent slopes, very stony614B71714444611kh2jwi00320061:12000
Abbaye loamy sand, 6 to 15 percent slopes3609C14617026081v4pvwi00320061:12000
Abbaye-Lapoin complex, 0 to 6 percent slopes611B1606452765h64bwi00720051:12000
Abbaye loamy sand, 6 to 15 percent slopes3609C59813836621hft8wi00720051:12000
Abbaye-Zeba complex, 0 to 6 percent slopes, very stony614B27433692gk92wi00720051:12000

Map of Series Extent

Approximate geographic distribution of the ABBAYE 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 .