Official Series Description


Lab Data Summary

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

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

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Competing Series

Soil series competing with AYLMER 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 AYLMER 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 AYLMER 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with AYLMER, 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. ND-2012-02-08-21 | McHenry County - October 1990

    Typical pattern of soils and parent material in the Hecla-Aylmer-Ulen association (Soil Survey of McHenry County, North Dakota; October 1990).

Map Units

Map units containing AYLMER 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
Serden-Aylmer-Bantry complex, 0 to 9 percent slopesI96D2767279884621by4mn06920071:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B39425738072q5bxnd0051:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesF381B401425860562q54lnd00919811:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesF387B282725860852q54snd00919811:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesI348B124225216081nyx5nd01719831:20000
Bantry-Hamar-Aylmer complex, 0 to 6 percent slopesG337B62025753152q504nd02119891:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B52825753302q5bxnd02119891:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B236725762992q5bxnd0271:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B12425770732q5bxnd04519661:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesF381B10430925857772q54lnd04919871:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesF387B382125858042q54snd04919871:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B338825713672q5bxnd04919871:20000
Aylmer-Fossum complex, 0 to 6 percent slopesF386B136725857222q54rnd04919871:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesG387B11925713702q5c3nd04919871:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B60125773232q5bxnd0631:12000
Aylmer loamy sand, 0 to 6 percent slopesI569B410826430542pywynd06719721:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesF381B418325872842q54lnd06919751:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B322125823072q5bxnd06919751:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesF387B214925872972q54snd06919751:20000
Aylmer-Fossum complex, 0 to 6 percent slopesF386B136225872552q54rnd06919751:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesG387B110625823112q5c3nd06919751:20000
Aylmer-Rosewood-Serden complex, 0 to 9 percent slopesI348C1699226412871nyx6nd07319921:20000
Aylmer-Bantry fine sands, 0 to 6 percent slopesI348B560426412861nyx5nd07319921:20000
Aylmer-Rosewood-Serden complex, 0 to 9 percent slopesI348C1492526410361nyx6nd07720051:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesI348B1418026409931nyx5nd07720051:12000
Aylmer-Thiefriver, moderately saline-Serden complex, 0 to 9 percent slopesI291C302026409911nyvsnd07720051:12000
Ulen-Garborg-Aylmer complex, 0 to 2 percent slopesI358A240226411081nyxlnd07720051:12000
Aylmer-Bantry fine sands, clayey substratum, 0 to 6 percent slopesI291B65326410661nyvrnd07720051:12000
Bantry-Hamar-Aylmer complex, 0 to 6 percent slopesG337B1066825795182q504nd08119591:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesG381B192925795472q5bxnd08119591:12000
Aylmer-Bantry fine sands, 0 to 6 percent slopesI348B48226412171nyx5nd08119591:12000
Serden-Aylmer loamy sands, 0 to 9 percent slopesI569C21626425092qtvvnd09719741:20000
Serden-Aylmer loamy sands, 0 to 9 percent slopesI569C41826429382qtvvnd09919671:20000
Aylmer-Hamar-Venlo complex, 0 to 6 percent slopesG388B243527977662sd35sd01319871:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesG387B127976752q5c3sd01319871:20000
Bantry-Hamar-Aylmer complex, 0 to 6 percent slopesG337B127976652q504sd01319871:20000
Aylmer-Bantry, wet fine sands, 0 to 6 percent slopesG387B164927992952q5c3sd09119701:20000
Aylmer-Hamar-Venlo complex, 0 to 6 percent slopesG388B130827993392sd35sd09119701:20000
Bantry-Hamar-Aylmer complex, 0 to 6 percent slopesG337B527992852q504sd09119701:20000

Map of Series Extent

Approximate geographic distribution of the AYLMER 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 .