Official Series Description


Lab Data Summary

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

Soil series competing with ALPENA 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 ALPENA series and competing. 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 ALPENA 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 .

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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.

Soil series sharing subgroup-level classification with ALPENA, 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

No block diagrams are available.

Map Units

Map units containing ALPENA 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
Alpena gravelly sandy loam, 0 to 6 percent slopes417B58711912866f1jmi00719981:12000
Alpena gravelly sandy loam, 6 to 12 percent slopes417C9481913506f3lmi00719981:12000
Alpena gravelly sandy loam, esker, 18 to 35 percent slopes418E3361912876f1kmi00719981:12000
Alpena, Kiva, and East Lake soilsAk99011903946d3rmi02919701:15840
Alpena gravelly sandy loam, 0 to 6 percent slopesAgB23141903916d3nmi02919701:15840
Alpena gravelly sandy loam, 6 to 18 percent slopesAgD5481903926d3pmi02919701:15840
Alpena gravelly sandy loam, 18 to 35 percent slopesAgF1641903936d3qmi02919701:15840
Shelter-Alpena complex, 0 to 15 percent slopes108D6062415062fxx3mi03319891:15840
Alpena very cobbly sandy loam, 0 to 15 percent slopes124D1544415081fxxqmi03319891:15840
Alpena gravelly sandy loam, 0 to 12 percent slopesAlC248315880142wpxxmi04119691:24000
Alpena gravelly loamy sand, sandy variant, 0 to 6 percent slopesAgB14131893056bzmmi04719681:20000
Alpena-East Lake gravelly loamy sands, 2 to 6 percent slopesAeB2741893856c26mi05519631:15840
Alpena-East Lake gravelly loamy sands, 0 to 2 percent slopesAeA2251893846c25mi05519631:15840
Ingalls-Alpena gravelly loamy sands, 0 to 2 percent slopesIaA2201894546c4fmi05519631:15840
Ingalls-Alpena gravelly loamy sands, 2 to 6 percent slopesIaB1121894556c4gmi05519631:15840
Alpena-East Lake gravelly loamy sands, 6 to 12 percent slopesAeC531893866c27mi05519631:15840
Alpena-East Lake gravelly loamy sands, 12 to 18 percent slopesAeD421893876c28mi05519631:15840
Alpena-East Lake gravelly loamy sands, 25 to 35 percent slopesAeE271893886c29mi05519631:15840
Alpena gravelly sandy loam, 0 to 12 percent slopesAsC16871907796dj5mi08919671:20000
Alpena gravelly loam, 0 to 15 percent slopes124D7623416318fz6mmi09719941:20000
Shelter-Alpena complex, 0 to 15 percent slopes, stony108D2427416306fz67mi09719941:20000
Alpena very gravelly sandy loam, 0 to 8 percent slopes6B70891909336dp4mi14119891:15840
Kiva-Alpena complex, 1 to 6 percent slopes83B8381909526dprmi14119891:15840
Alpena very gravelly sandy loam, 8 to 15 percent slopes6C6311909346dp5mi14119891:15840
Alpena cobbly sandy loam, bedrock substratum, 0 to 8 percent slopes91B5151909656dq5mi14119891:15840
Alpena gravelly sandy loam, 0 to 12 percent slopesApC33114222122wpxxwi02919751:15840
Alpena gravelly sandy loam, 12 to 35 percent slopesAkE44664223742wpxzwi07519871:20000
Alpena gravelly sandy loam, 6 to 12 percent slopesAkC5754223732wpxywi07519871:20000
Alpena gravelly sandy loam, 12 to 35 percent slopesAaE4374224582wpxzwi08319851:15840

Map of Series Extent

Approximate geographic distribution of the ALPENA 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 .