Official Series Description


Lab Data Summary

Aggregate lab data for the ALCONA soil series. This aggregation is based on all pedons with a current taxon name of ALCONA, 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 ALCONA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
9203N0273S2002MI131011Alcona6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7816658,-88.9422913
93B04N0465S2003MI131012Alcona6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9549866,-88.9803848
94B99P0044S1998MI095008ALCONA7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.658886,-85.3429871
94C86P013386MI031005Alcona6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5308342,-84.2525024

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALCONA 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ALCONA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ALCONA series and siblings. 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 ALCONA 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 .

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.

Competing Series

Soil series competing with ALCONA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ALCONA 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 ALCONA 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.

Click the image to view it full size.

Soil series sharing subgroup-level classification with ALCONA, 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-2010-09-10-07 | Keweenaw County Area - 2006

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

Map Units

Map units containing ALCONA 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
Zimmerman-Alcona complex, 25 to 60 percent slopes80F13231903666d2vmi00119931:20000
Alcona loamy very fine sand, 12 to 18 percent slopes66D6451903556d2hmi00119931:20000
Alcona loamy very fine sand, 18 to 35 percent slopes66E2041903566d2jmi00119931:20000
Alcona very fine sandy loam, 0 to 6 percent slopes34B15011905766d9mmi03119881:15840
Alcona very fine sandy loam, 20 to 50 percent slopes34E6221905786d9pmi03119881:15840
Alcona very fine sandy loam, 6 to 15 percent slopes34C5101905776d9nmi03119881:15840
Rousseau, dark subsoil-Alcona complex, 0 to 6 percent slopes84B5188415172fy0nmi03319891:15840
Alcona loamy very fine sand, 0 to 6 percent slopes13B5032415096fxy6mi03319891:15840
Alcona-Markey complex, 0 to 50 percent slopes128F2817415085fxxvmi03319891:15840
Alcona loamy very fine sand, 25 to 50 percent slopes13F2152415098fxy8mi03319891:15840
Alcona loamy very fine sand, 6 to 15 percent slopes13D1703415097fxy7mi03319891:15840
Rousseau, dark subsoil-Alcona complex, 6 to 15 percent slopes84D1065415173fy0pmi03319891:15840
Rousseau, dark subsoil-Alcona complex, 25 to 50 percent slopes84F584415174fy0qmi03319891:15840
Munising-Alcona-Liminga complex, dissected, 15 to 70 percent slopes130F11302416065fyygmi06119891:20000
Kalkaska-Alcona complex, dissected, 15 to 70 percent slopes132F6545416069fyylmi06119891:20000
Munising-Liminga-Alcona complex, 1 to 8 percent slopes147B3849416088fyz6mi06119891:20000
Kalkaska-Alcona complex, dissected, 8 to 35 percent slopes132D2289416068fyykmi06119891:20000
Munising-Alcona-Liminga complex, dissected, 8 to 35 percent slopes130D1839416064fyyfmi06119891:20000
Alcona loamy fine sand, 1 to 8 percent slopes32B1675416118fz05mi06119891:20000
Munising-Alcona-Liminga complex, dissected, 1 to 12 percent slopes130B1630416063fyydmi06119891:20000
Kalkaska-Alcona complex, dissected, 1 to 12 percent slopes132B1383416067fyyjmi06119891:20000
Liminga-Alcona complex, 0 to 8 percent slopes133B979416070fyymmi06119891:20000
Richter-Alcona complex, 0 to 8 percent slopes150B490416092fyzbmi06119891:20000
Liminga-Alcona complex, 15 to 35 percent slopes133E376416072fyypmi06119891:20000
Liminga-Alcona complex, 8 to 15 percent slopes133D351416071fyynmi06119891:20000
Alcona sandy loam, 2 to 6 percent slopesAlB4741919686frjmi08719661:15840
Alcona sandy loam, 0 to 2 percent slopesAlA3981919676frhmi08719661:15840
Alcona sandy loam, 6 to 12 percent slopesAlC1221919696frkmi08719661:15840
Alcona-Richter sandy loams, 0 to 2 percent slopesArA23021907776dj3mi08919671:20000
Alcona-Richter sandy loams, 2 to 6 percent slopesArB8911907786dj4mi08919671:20000
Richter-Alcona sandy loams, 2 to 6 percent slopesRaB4891908486dldmi08919671:20000
Alcona sandy loam, 6 to 12 percent slopesAlC4841907766dj2mi08919671:20000
Richter-Alcona sandy loams, 0 to 2 percent slopesRaA2671908476dlcmi08919671:20000
Liminga-Alcona complex, 0 to 6 percent slopes84B2876631276p5wrmi09520041:24000
Liminga-Alcona complex, 6 to 15 percent slopes84D2175631278p5wtmi09520041:24000
Liminga-Alcona complex, 15 to 35 percent slopes84E1217627509p1z7mi09520041:24000
Wallace-Alcona complex, 0 to 6 percent slopes215B270631277p5wsmi09520041:24000
Wallace-Alcona complex, 6 to 15 percent slopes215D193631279p5wvmi09520041:24000
Wallace-Alcona complex, 0 to 6 percent slopes84B1966416426fzb3mi09719941:20000
Alcona fine sandy loam, 0 to 6 percent slopes13B1406416326fz6wmi09719941:20000
Wallace-Alcona complex, 35 to 60 percent slopes84F900416428fzb5mi09719941:20000
Wallace-Alcona complex, 6 to 15 percent slopes84D842416427fzb4mi09719941:20000
Alcona fine sandy loam, 6 to 15 percent slopes13D292416327fz6xmi09719941:20000
Garlic-Alcona-Voelker complex, 15 to 70 percent slopes, dissected76F12142395271f89pmi10319991:24000
Garlic-Alcona-Voelker complex, 8 to 35 percent slopes, dissected76E8951395270f89nmi10319991:24000
Garlic-Alcona-Voelker complex, 1 to 12 percent slopes, dissected76C6478395268f89lmi10319991:24000
Garlic-Alcona-Voelker complex, 6 to 18 percent slopes77D4556395272f89qmi10319991:24000
Garlic-Alcona-Voelker complex, 18 to 35 percent slopes77E386395273f89rmi10319991:24000
Alcona loamy very fine sand, 1 to 6 percent slopes22B380395171f86gmi10319991:24000
Alcona loamy fine sand, 2 to 6 percent slopes36B7201899126cm6mi12919871:15840
Garlic-Alcona complex, dissected, 1 to 12 percent slopes130C2965435361gm0xmi60520041:24000
Garlic-Alcona complex, dissected, 8 to 35 percent slopes130E2792435362gm0ymi60520041:24000
Alcona fine sandy loam, lake terrace, 15 to 30 percent slopes317D31114444011kh0lwi00320061:12000
Alcona fine sandy loam, 15 to 30 percent slopes817D90613836641hftbwi00720051:12000
Alcona fine sandy loam, lake terrace, 15 to 30 percent slopes317D408433431gk0nwi00720051:12000
Alcona fine sandy loam, lake terrace, 15 to 30 percent slopes317D364781180v6wcwi03120051:12000
Alcona fine sandy loam, lake terrace, 15 to 30 percent slopes317D515782048v7scwi05120061:12000
Alcona fine sandy loam, 0 to 6 percent slopesAcB1513421076g453wi08519881:20000
Alcona fine sandy loam, 6 to 15 percent slopesAcC380421077g454wi08519881:20000
Alcona fine sandy loam, 15 to 30 percent slopes817D2113830371hf53wi10720061:12000
Alcona fine sandy loam, 15 to 30 percent slopes817D83626795p176wi11320061:12000
Fence-Alcona complex, 0 to 6 percent slopesFeB2053421234g4b6wi12519851:20000
Fence-Alcona complex, 6 to 15 percent slopesFeC437421235g4b7wi12519851:20000

Map of Series Extent

Approximate geographic distribution of the ALCONA 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 .