Official Series Description


Lab Data Summary

Aggregate lab data for the ARENZVILLE soil series. This aggregation is based on all pedons with a current taxon name of ARENZVILLE, 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 ARENZVILLE 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
104X53-320-1S1982IA105092Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1502614,-91.3074074
105UMN1252S1971MN0451252Arenzville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6455612,-92.2321167
105UMN1320S1971MN0451320Arenzville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6452103,-92.232811
105UMN1322S1971MN0451322Arenzville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6045723,-92.1425781
105UMN1391S1972MN0491391Arenzville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4625702,-92.4745865
105X22-320-1S1973IA043014Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0062907,-91.5971354
105X22-320-2S1973IA043016Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.86571,-91.6049039
105UMN1918S1975MN1091918Arenzville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8816566,-92.2287979
105UMN2353S1976MN0552353Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6278305,-91.4210587
10540A5202S1977WI049001ARENZVILLE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1508331,-89.9030533
105X49-320-1S1983IA097091Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0477332,-90.6467837
105X3-320-1S1987IA005016Arenzville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3677778,-91.4675
115C81IL0130251981IL013025Arenzville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1275948,-90.6724309

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE 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 ARENZVILLE, 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. IA-2010-09-02-02 | Allalmakee County - 1998

    Typical pattern of soils and parent material in the Fayette-Nordness-Dubuque association (Soil Survey of Allamakee County, Iowa; 1998).

  2. IA-2010-09-02-03 | Allamakee County - 1998

    Typical pattern of soils and parent material in the Lacrescent-Fayette-Village association (Soil Survey of Allamakee County, Iowal 1998).

  3. IA-2011-05-31-02 | Allamakee County - 1958

    Typical pattern of soils and parent material in the Fayette-Nordness-Dubuque association (Soil Survey of Allamakee County, Iowa; 1958).

  4. IA-2011-05-31-03 | Allamakee County - 1958

    Typical pattern of soils and parent material in the Lacrescent-Fayette-Village association (Soil Survey of Allamakee County, Iowa; 1958).

  5. IA-2011-05-31-19 | Dubuque County - 1986

    Typical pattern of soils and underlying material in the Fayette-Nordness association (Soil Survey of Dubuque County, Iowa; 1986).

  6. IA-2011-05-31-20 | Dubuque County - 1986

    Typical pattern of soils and underlying material in the Fayette-Rozetta-Eleroy association (Soil Survey of Dubuque County, Iowa; 1986).

  7. IA-2011-05-31-24 | Dubuque County - 1986

    A cross section of a typical pattern of soils and underlying material in a landscape controlled by limestone and shale (Soil Survey of Dubuque County, Iowa; 1986).

  8. IA-2011-05-31-50 | Jackson County - 1992

    Typical pattern of soils and parent material in the Fayette-Nordness-Rock outcrop association (Soil Survey of Jackson County, Iowa; 1992).

  9. IA-2011-05-31-51 | Jackson County - 1992

    Typical pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Jackson County, Iowa; 1992).

  10. IA-2011-06-01-01 | Jones County - 1991

    Typical pattern of soils and parent material in the Fayette-Downs-Exette association (Soil Survey of Jones County, Iowa; 1991).

  11. IL-2011-08-03-04 | Cass County - 1989

    Typical pattern of soils and parent material in the Sylvan-Rozetta-Bold general soil map unit (Soil Survey of Cass County, Illinois; 1989).

  12. IL-2011-08-03-05 | Cass County - 1989

    Typical pattern of soils and parent material in the Hamburg-Fayette-Seaton general soil map unit (Soil Survey of Cass County, Illinois; 1989).

  13. MN-2012-02-06-04 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Mt. Carroll-Marlean-Arenzville association (Soil Survey of Olmsted County, Minnesota; March 1980).

  14. WI-2010-11-08-06 | Pepin County - 2002

    Typical pattern of soils and parent material in the Ella-Orion-Plumcreek association (Soil Survey of Pepin County, Wisconsin; 2002).

  15. WI-2012-03-22-05 | Crawford County - December 1961

    Landscape showing relationships among soils of the bottom lands of Crawford County (Soil Survey of Crawford County, WI; 1961).

  16. WI-2012-03-23-03 | Iowa County - July 1962

    Landscape of the soils of the bottom lands showing the relationship of the major soils. By Soil Survey Division, University of Wisconsin (Soil Survey of Iowa County, WI; 1962).

Map Units

Map units containing ARENZVILLE 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
Arenzville-Volney complex, 2 to 5 percent slopes1496B4558402354fhp5ia00519921:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B19954023452tc4lia00519921:15840
Arenzville-Volney complex, 0 to 2 percent slopes14961760402353fhp4ia00519921:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded32012914024312wtqsia00519921:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B61124042032tc4lia04319791:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded32033834042522wtqsia04319791:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B134494043482tc4lia04519781:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B31344049792tc4lia05519841:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B129664053752tc4lia06119831:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded32051904054172wtqsia06119831:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B21674056952tc4lia06519751:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B91744074502tc4lia09719881:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded32020644074942wtqsia09719881:15840
Nodaway-Arenzville silt loams, 1 to 4 percent slopes729B9747408042fplnia10319791:15840
Arenzville silt loam, 0 to 2 percent slopes3202529408001fpkbia10319791:15840
Arenzville-Chaseburg complex, 1 to 5 percent slopes129B127324080862tc4lia10519881:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded32031604081392wtqsia10519881:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded3206484373622wtqsia19120051:12000
Arenzville silt loam, 0 to 2 percent slopes, frequently flooded3078A5128731143sjt8il01720031:12000
Arenzville silt loam, 0 to 2 percent slopes, rarely flooded7078A162314449201khkbil01720031:12000
Arenzville silt loam, 0 to 2 percent slopes, occasionally flooded8078A26226508532rmm2il01720031:12000
Arenzville silt loam, 0 to 2 percent slopes, occasionally flooded8078A3751988826nykil11920011:12000
Arenzville silt loam, 0 to 2 percent slopes, occasionally flooded8078A8441778175z11il12519891:15840
Arenzville silt loam, 0 to 2 percent slopes, frequently flooded3078A496214063181j6d3il12920051:12000
Arenzville silt loam, 0 to 2 percent slopes, occasionally flooded8078A29318412865lmil13319981:12000
Arenzville silt loam, 0 to 2 percent slopes, frequently flooded3078A229316721761t415il13719841:15840
Arenzville silt loam, 0 to 2 percent slopes, occasionally flooded8078A9452005646qptil15720011:12000
Arenzville silt loam, 0 to 2 percent slopes, frequently flooded3078A245725420862qrcqil17119841:12000
Beavercreek-Arenzville complex, 1 to 12 percent slopes598B7700398309fcgpmn05519811:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded1642523982262wtqsmn05519811:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded1655894007162wtqsmn10919771:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedAz389822162892wtqsmn15720081:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A664825616732wtqswi01119601:20000
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedAoA12124214842wtqswi01719851:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A754624990202wtqswi02319601:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A390324990212wtqswi03320031:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A43044217402wtqswi03519741:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedAr381384241342wtqswi04319591:20000
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedAn37484251962wtqswi04519691:12000
Chaseburg and Arenzville silt loams, 0 to 2 percent slopesCn7944252122tc4mwi04519691:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A638828066412wtqswi04919601:20000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A148524990262wtqswi05319941:20000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A125615562wtqswi05719871:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A566224990222wtqswi06320011:12000
Arenzville silt loam, channeled, 0 to 2 percent slopes, occasionally flooded625A213725184842wtqtwi06320011:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedAn105654247362wtqswi06519641:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A86526850662wtqswi08119811:15840
Arenzville silt loam, channeled, 0 to 2 percent slopes, occasionally flooded625A8626851352wtqtwi08119811:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A169424990232wtqswi09119981:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A332216910092wtqswi09320061:12000
Arenzville silt loam, cobbly substratum, 1 to 3 percent slopes, occasionally flooded640A238116911861trtdwi09320061:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A882824990242wtqswi10320021:12000
Arenzville silt loam, 0 to 3 percent slopes, occasionally floodedArA25514231142wtqswi11119771:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A115926834972wtqswi12119691:15840
Arenzville silt loam, 0 to 3 percent slopes, occasionally flooded626A753124990252wtqswi12319651:12000

Map of Series Extent

Approximate geographic distribution of the ARENZVILLE 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 .