Official Series Description


Lab Data Summary

Aggregate lab data for the RACINE soil series. This aggregation is based on all pedons with a current taxon name of RACINE, 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 RACINE 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
104X191482S1959IA191011Racine1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1115794,-92.0482702
104X45-482-1S1965IA089927Racine2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.31667,-92.13712
105UMN1272S1971MN1091272Racine2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1718941,-92.4920731
105UMN3012S1981MN1693012Racine2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.96595,-91.9540176
105X49-482C2S1983IA097013Racine2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2608268,-90.8378027

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RACINE 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 RACINE 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 RACINE 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 RACINE 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 RACINE 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 RACINE 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 RACINE 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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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 RACINE, 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-2010-09-09-28 | Winneshiek County - 2007

    Typical pattern of soils and parent material in the Winneshiek-Marlean association (Soil Survey of Winneshiek County, Iowa; 2007).

  2. IA-2010-09-09-29 | Winneshiek County - 2007

    Typical pattern of soils and parent material in the Kasson-Floyd association (Soil Survey of Winneshiek County, Iowa; 2007).

  3. IA-2011-05-31-22 | Dubuque County - 1986

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

  4. MN-2010-09-10-04 | Rice County - 2000

    Typical pattern of soils and underlying material in the Racine-Kenyon-Nerwoods association (Soil Survey of Rice County, Minnesota; 2000).

  5. MN-2012-02-06-01 | Olmsted County - March 1980

    Pattern of soils and underlying material in the Readlyn-Maxfield-Kenyon association (Soil Survey of Olmsted County, Minnesota; March 1980).

Map Units

Map units containing RACINE 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
Racine loam, 2 to 5 percent slopes482B43094040482yvjvia03719891:15840
Racine loam, 5 to 9 percent slopes, moderately eroded482C22139404050fkfwia03719891:15840
Racine loam, 5 to 9 percent slopes482C1589405441flwria06119831:15840
Racine loam, 2 to 5 percent slopes482B10584054402yvjvia06119831:15840
Racine loam, 9 to 14 percent slopes, moderately eroded482D2629405443flwtia06119831:15840
Racine loam, 5 to 9 percent slopes, moderately eroded482C2365405442flwsia06119831:15840
Racine loam, 14 to 25 percent slopes, moderately eroded482F2141405444flwvia06119831:15840
Racine loam, 2 to 5 percent slopes482B124753552yvjvia06519751:15840
Racine loam, 2 to 5 percent slopes482B56194059392yvjvia06719891:15840
Racine silt loam, 0 to 2 percent slopes48210584059382yvkcia06719891:15840
Racine loam, 5 to 9 percent slopes482C864405940fmdvia06719891:15840
Racine loam, 5 to 9 percent slopes, moderately eroded482C2511405941fmdwia06719891:15840
Racine loam, 2 to 5 percent slopes482B61124069622yvjvia08919691:15840
Racine silt loam, 0 to 2 percent slopes482A5854069612yvkcia08919691:15840
Racine loam, 5 to 9 percent slopes482C525406963fngvia08919691:15840
Dickinson-Racine complex, 2 to 5 percent slopes576B440406968fnh0ia08919691:15840
Racine loam, 5 to 9 percent slopes, moderately eroded482C2233406964fngwia08919691:15840
Racine loam, 5 to 9 percent slopes, moderately eroded482C21158407519fp1sia09719881:15840
Racine loam, 2 to 5 percent slopes482B343407518fp1ria09719881:15840
Racine loam, 2 to 5 percent slopes482B36914096812yvjvia13119711:15840
Racine silt loam, 0 to 2 percent slopes48217524096802yvkcia13119711:15840
Racine silt loam, 5 to 9 percent slopes482C771409682fr9kia13119711:15840
Racine loam, 2 to 5 percent slopes482B104574373752yvjvia19120051:12000
Bassett-Racine complex, 18 to 25 percent slopesM522E25815969681qls3mn03920051:12000
Bassett-Racine complex, 12 to 18 percent slopes, moderately erodedM522D224513849861hh5zmn03920051:12000
Racine and Ostrander silt loams, 2 to 6 percent slopesRb1674222167662yvkbmn04520081:12000
Racine and Ostrander silt loams, 0 to 2 percent slopesRa544322167652yvk9mn04520081:12000
Racine and Ostrander silt loams, 7 to 11 percent slopes, moderately erodedRd92422167692ddqpmn04520081:12000
Racine and Ostrander loams, 12 to 17 percent slopes, moderately erodedRe15522167672ddqmmn04520081:12000
Bassett-Racine complex, 12 to 18 percent slopes, moderately erodedM522D2402316707401t2jvmn04920071:12000
Bassett-Racine complex, 18 to 25 percent slopesM522E114416707411t2jwmn04920071:12000
Racine silt loam, 0 to 2 percent slopes99A50584004872yvkcmn09919861:15840
Racine loam, 2 to 5 percent slopes99B47304004882yvjvmn09919861:15840
Racine silt loam, 6 to 12 percent slopes99C414400489ffr0mn09919861:15840
Racine loam, 2 to 5 percent slopes99B101924008212yvjvmn10919771:15840
Racine silt loam, 6 to 12 percent slopes99C2833400822fg2rmn10919771:15840
Lamont-Racine complex, 2 to 6 percent slopes1811B1553400719ffzfmn10919771:15840
Racine loam, 12 to 18 percent slopes, eroded99D2686400823fg2smn10919771:15840
Racine silt loam, moderately wet, 6 to 12 percent slopes, eroded1410C4042429572gf05mn13119961:12000
Racine silt loam, moderately wet, 2 to 6 percent slopes1410B3849429571gf04mn13119961:12000
Racine loam, 12 to 18 percent slopes, eroded99D2831429751gf5ymn13119961:12000
Racine silt loam, 6 to 12 percent slopes, moderately erodedRaC264622164182ddccmn15720081:12000
Racine silt loam, 2 to 6 percent slopesRaB56422164162ddc9mn15720081:12000
Racine silt loam, 12 to 18 percent slopes, moderately erodedRaD215422164152ddc8mn15720081:12000
Racine silt loam, 0 to 2 percent slopesRaA4422164142ddc7mn15720081:12000
Racine silt loam, 2 to 6 percent slopes99B1386429103gdj1mn16919871:20000
Racine silt loam, 6 to 12 percent slopes99C504429104gdj2mn16919871:20000

Map of Series Extent

Approximate geographic distribution of the RACINE 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 .