Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
9205N0188S2004MI131017Algonquin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7198944,-89.1545792
9205N0191S2004MI131021Algonquin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7442017,-89.0581665
94A92P037891MI119005Algonquin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1122208,-83.9263916
94A93P0037S1992MI069002Algonquin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2030525,-83.580986

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN 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 ALGONQUIN, 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-2010-09-07-06 | Kalkaska County - 2005

    Typical pattern of soils and parent material in the Algonquin-Allendale-Negwegon general soil map unit (Soil Survey of Kalkaska County, Michigan; 2005).

  2. MI-2010-09-07-22 | Montmorency County - 2003

    Typical pattern of soils and underlying material in the Algonquin-Negwegon-Springport association (Soil Survey of Montmorency County, Michigan; 2003).

  3. MI-2012-02-06-02 | Alcona County - 1998

    Typical pattern of soils and parent material in the Algonquin-Negwegon-Springport association (adjacent to the Au Gres-Wakeley-Tawas association) (Soil Survey of Alcona County, Michigan; 1998).

Map Units

Map units containing ALGONQUIN 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
Algonquin silt loam, 0 to 3 percent slopes54A91861903406d20mi00119931:20000
Algonquin-Springport complex, 0 to 6 percent slopes59B72241903456d25mi00119931:20000
Negwegon-Algonquin-Lupton complex, 0 to 6 percent slopes480B33491913936f4zmi00719981:12000
Algonquin-Springport complex, 0 to 6 percent slopes59B28431912986f1xmi00719981:12000
Algonquin silt loam, 0 to 3 percent slopes54A22351913846f4pmi00719981:12000
Algonquin silt loam, till substratum, 0 to 3 percent slopes479A17461913246f2rmi00719981:12000
Algonquin till substratum-Springport till substratum complex, 0 to 4 percent slopes477B10261913926f4ymi00719981:12000
Algonquin-Negwegon-Dorval complex, 0 to 12 percent slopes359C1821913746f4cmi00719981:12000
Algonquin-Pickford complex, 0 to 4 percent slopesPkA115515881011q9k2mi04119691:24000
Algonquin silt loam, 0 to 4 percent slopesPfA82215881001q9k1mi04119691:24000
Algonquin clay, 0 to 3 percent slopes378A32661918386fmbmi06919951:15840
Algonquin-Springport complex, 0 to 3 percent slopes379A11391918396fmcmi06919951:15840
Skeel-Algonquin-Aquepts complex, 0 to 6 percent slopes435B5251918736fngmi06919951:15840
Algonquin silt loam, 0 to 3 percent slopes54A2561918986fp8mi06919951:15840
Algonquin-Springport complex, 0 to 6 percent slopes59B151919036fpfmi06919951:15840
Allendale-Algonquin complex, 0 to 3 percent slopes462A12011906866df5mi07919981:12000
Algonquin silt loam, 0 to 3 percent slopes54A4251906666ddjmi07919981:12000
Algonquin-Springport complex, 0 to 6 percent slopes59B41701923196g3vmi11919971:12000
Algonquin silt loam, 0 to 3 percent slopes54A30031923186g3tmi11919971:12000
Algonquin-Negwegon-Dorval complex, 0 to 12 percent slopes359C14781922536g1qmi11919971:12000
Richter-Algonquin complex, 0 to 6 percent slopes423B12561922966g33mi11919971:12000
Algonquin silty clay, 1 to 4 percent slopes82B873514564921kwlmmi13120071:24000
Algonquin-Springport silt loams, 0 to 3 percent slopes512A2854654006pyjzmi13520031:12000
Algonquin silt loam, 0 to 3 percent slopes54A23951975906mlwmi13520031:12000

Map of Series Extent

Approximate geographic distribution of the ALGONQUIN 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 .