Official Series Description


Lab Data Summary

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

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

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

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Soil series sharing subgroup-level classification with ALLENDALE, 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-2012-02-06-10 | Chippewa County - February 1992

    Typical pattern of soils and parent material in the Pickford-Rudyard-Ontonagon association (Soil Survey of Chippewa County, Michigan; February 1992).

  4. MI-2012-02-06-12 | Chippewa County - February 1992

    Typical pattern of soils and parent material in the Fibre-Allendale-Pickford association (Soil Survey of Chippewa County, Michigan; February 1992).

Map Units

Map units containing ALLENDALE 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
Allendale loamy sand, 0 to 3 percent slopes62A30971903516d2cmi00119931:20000
Au Gres-Allendale-Croswell sands, nearly level253A19261902966d0lmi00119931:20000
Allendale loamy sand, nearly level264A2601902996d0pmi00119931:20000
Allendale loamy sand, 0 to 3 percent slopes62A771912996f1ymi00719981:12000
Allendale-Dorval-Blue Lake complex, 0 to 6 percent slopes361B51913756f4dmi00719981:12000
Allendale loamy sand, 0 to 2 percent slopesAmA41931891086bs8mi01119641:20000
Gladwin-Allendale association, undulatingGnB19521891656bv3mi01119641:20000
Allendale loamy sand, 2 to 6 percent slopesAmB2421891096bs9mi01119641:20000
Allendale loamy sand, 0 to 3 percent slopes76A254415019fxvqmi01319841:20000
Allendale sand, 0 to 3 percent slopes48A22241905936db5mi03119881:15840
Allendale loamy fine sand, 0 to 3 percent slopes32A11673415139fxzlmi03319891:15840
Allendale-Fibre complex, 0 to 3 percent slopes146A4965415102fxydmi03319891:15840
Allendale-Posen-Pickford complex, 0 to 6 percent slopes155B2536415113fxyrmi03319891:15840
Rudyard-Allendale complex, 0 to 3 percent slopes40A1232415147fxzvmi03319891:15840
Allendale-Croswell complex, 0 to 3 percent slopes83A568415171fy0mmi03319891:15840
Wakeley-Allendale complex, 0 to 3 percent slopes58A19521897266cf6mi03919931:15840
Allendale loamy sand, nearly level264A981897046cdhmi03919931:15840
Allendale loamy sand, 2 to 6 percent slopesAeB2221893046bzlmi04719681:20000
Pinconning-Allendale loamy fine sands, 0 to 2 percent slopesPnA427918689068gqmi04919671:20000
Allendale sand, 0 to 4 percent slopesAlB52221897416cfpmi05119661:15840
Allendale-Pinconning-Pickford associationAP3461897426cfqmi05119661:15840
Kellogg, sandy substratum-Allendale complex, 0 to 4 percent slopes277B2316076781qyxlmi05320071:24000
Allendale-Rudyard complex, 0 to 3 percent slopes51A2249416135fz0qmi06119891:20000
Kellogg, sandy substratum-Allendale complex, 0 to 4 percent slopes8277B138124849142pdrjmi06119891:20000
Allendale sand, 0 to 3 percent slopes62A38341919066fpjmi06919951:15840
Kawkawlin-Allendale-Aquepts complex, 0 to 4 percent slopes443B21741918846fntmi06919951:15840
Allendale loamy sand, nearly level264A4921918066fl9mi06919951:15840
Wakeley-Allendale complex, 0 to 3 percent slopes58A4871919026fpdmi06919951:15840
Eutroboralfs-Allendale complex, nearly level and undulating265B3341918076flbmi06919951:15840
Wakeley-Allendale complex, 0 to 3 percent slopes58A15211906856df4mi07919981:12000
Allendale-Algonquin complex, 0 to 3 percent slopes462A12011906866df5mi07919981:12000
Allendale-Springport complex, 0 to 3 percent slopes461A3541906846df3mi07919981:12000
Allendale sand, 0 to 3 percent slopes488A2681907326dgnmi07919981:12000
Allendale loamy sand, 0 to 2 percent slopesAoA3121919716frmmi08719661:15840
Allendale loamy sand, 2 to 6 percent slopesAoB2411919726frnmi08719661:15840
Allendale-Fibre complex, 0 to 3 percent slopes146A1150631316p5y1mi09520041:24000
Allendale loamy fine sand, 0 to 3 percent slopes32A171627485p1ygmi09520041:24000
Allendale fine sand, 0 to 3 percent slopes32A6369416392fz90mi09719941:20000
Allendale-Wakeley complex, 0 to 3 percent slopes146A2202416329fz6zmi09719941:20000
Rudyard-Allendale complex, 0 to 3 percent slopes40A804416400fz98mi09719941:20000
Allendale-Lenawee-Toledo complex, 0 to 3 percent slopesAlA1225085166903mi09919671:20000
Allendale sand, 0 to 4 percent slopesAlB7426735306cfpmi11119761:15840
Allendale-Dorval-Blue Lake complex, 0 to 6 percent slopes361B42181922556g1smi11919971:12000
Allendale-Wakeley-Dorval complex, 0 to 3 percent slopes351A39461922476g1jmi11919971:12000
Allendale loamy sand, 0 to 3 percent slopes62A20381923246g40mi11919971:12000
Belding and Allendale soils, 0 to 6 percent slopesBaB612518733368y0mi12119661:15840
Allendale loamy sand, 0 to 4 percent slopes54B32991899366cmzmi12919871:15840
Allendale loamy fine sand, 0 to 3 percent slopes10A81314563861kwh6mi13120071:24000
Kellogg, sandy substratum-Allendale complex, 0 to 4 percent slopes8277B51916748811t6vfmi13120071:24000
Allendale sandy loam, 2 to 6 percent slopesAmB1891899796cpcmi13319661:15840
Allendale loamy sand, 2 to 6 percent slopesAlB1011899786cpbmi13319661:15840
Wakeley-Allendale complex, 0 to 3 percent slopes58A6145241350834hmi13520031:12000
Allendale sand, 0 to 3 percent slopes488A102820907070k6mi13520031:12000
Glossudalfs-Allendale complex, nearly level and undulating265B202241475838jmi13520031:12000
Allendale loamy sand, nearly level264A272414658386mi13520031:12000
Allendale sandy loam, 0 to 4 percent slopesAlA47061926316gfxmi13919671:15840
Iosco and Allendale loamy sands, 0 to 4 percent slopesIrA33661926746gh9mi13919671:15840
Allendale sand, 0 to 3 percent slopes76A44271909446dphmi14119891:15840
Wakeley-Allendale complex, 0 to 3 percent slopes58A29891910316ds9mi14319991:12000
Allendale sand, 0 to 3 percent slopes, sandy substratum492A23601910426dsnmi14319991:12000
Pinconning-Allendale loamy fine sands, 0 to 2 percent slopes122A15423994002ljs0mi14519911:15840
Allendale-Lenawee-Toledo complex, 0 to 3 percent slopesAtA280961873986903mi14719691:20000
Allendale-Hoytville complex, 0 to 6 percent slopesAhB194991873966901mi14719691:20000
Allendale-Latty complex, 0 to 3 percent slopesAlA155651873976902mi14719691:20000
Allendale loamy fine sand, 0 to 3 percent slopesAeA15131873956900mi14719691:20000
Allendale loamy sand, 0 to 2 percent slopes138A325081386frmmi15719841:15840
Allendale loamy sand, 0 to 4 percent slopes14A92331907416dgymi60019831:15840
Allendale loamy fine sand222667396347f9fdmn01719731:20000
Kellogg-Allendale-Ashwabay complex, 2 to 6 percent slopes713B914614444811kh35wi00320061:12000
Kellogg-Allendale-Ashwabay complex, 0 to 15 percent slopes713C324714444821kh36wi00320061:12000
Allendale loamy fine sand, 0 to 3 percent slopes226A222814443881kh05wi00320061:12000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes3826B115017003741v2cswi00320061:12000
Kellogg-Allendale-Ashwabay complex, 2 to 6 percent slopes713B25725433300gjwfwi00720051:12000
Kellogg-Allendale-Ashwabay complex, 6 to 15 percent slopes713C15037433301gjwgwi00720051:12000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes3826B781113836651hftcwi00720051:12000
Allendale loamy fine sand, 0 to 3 percent slopes226A1884433379gjyzwi00720051:12000
Allendale loamy fine sand, 0 to 3 percent slopesAdA26914261602wpwmwi00919701:20000
Allendale fine sandy loam, 0 to 3 percent slopesAeA9124261612wpwpwi00919701:20000
Allendale loamy sand, 0 to 3 percent slopesAdA5594222112wpwnwi02919751:15840
Allendale loamy fine sand, 0 to 3 percent slopes226A2122781153v6vhwi03120051:12000
Kellogg-Allendale-Ashwabay complex, 2 to 6 percent slopes713B1507781445v74xwi03120051:12000
Kellogg-Allendale-Ashwabay complex, 6 to 15 percent slopes713C58613859731hj6twi03120051:12000
Kellogg-Allendale-Ashwabay complex, 2 to 6 percent slopes713B121116977101tzlvwi05120061:12000
Kellogg-Allendale-Ashwabay complex, 0 to 15 percent slopes713C67516977111tzlwwi05120061:12000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes3826B327782362v83hwi05120061:12000
Allendale loamy fine sand, 0 to 3 percent slopes226A82782021v7rhwi05120061:12000
Allendale loamy fine sand, 0 to 3 percent slopesAdA4794222872wpwmwi06119781:15840
Allendale loamy sand, 0 to 3 percent slopesAdA2099422372g5hxwi07519871:20000
Allendale loamy fine sand, 0 to 3 percent slopesAdA24974225262wpwmwi08719751:15840

Map of Series Extent

Approximate geographic distribution of the ALLENDALE 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 .