Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
103UMN2595S1978MN063006(2595)Collinwood3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7199821,-95.2764511
103UMN2577S1978MN091003(2577)Collinwood2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7002373,-94.2576141
103UMN3014S1979MN091019(3014)Collinwood2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8118629,-94.2919388
103UMN3018S1979MN0913018Collinwood2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8232956,-94.7538376
103UMN3427S1980MN063014(3427)Collinwood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5711517,-95.2332687
103UMN3428S1980MN063015(3428)Collinwood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5068398,-95.3777618
103UMN3429S1980MN063016(3429)Collinwood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5700493,-95.2338409
103UMN3254S1980MN1013254Collinwood2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9061775,-95.6635284

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COLLINWOOD 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the COLLINWOOD series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the COLLINWOOD series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the COLLINWOOD 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 .

Click the image to view it full size.

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.

Click the image to view it full size.

Competing Series

Soil series competing with COLLINWOOD share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the COLLINWOOD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the COLLINWOOD 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.

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

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 COLLINWOOD, 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-2010-09-02-07 | Emmet County - 1997

    Typical pattern of soils and parent material in the Clarion-Storden-Nicollet association (Soil Survey of Emmet County, Iowa; 1997).

  2. IA-2011-05-31-37 | Hancock, County - 1989

    Typical pattern of soils and parent material in the Lester-Kilkenny-Webster association (Soil Survey of Hancock County, Iowa; 1989).

  3. IA-2011-05-31-41 | Hancock, County - 1989

    Typical pattern of soils and parent material in the Bode-Collinwood-Waldorf association (Soil Survey of Hancock County, Iowa; 1989).

  4. IA-2011-06-01-30 | Osceola County - 1988

    Typical pattern of soils and parent material in the Nicollet-Clarion-Webster association (Soil Survey of Osceola County, Iowa; 1988).

  5. IA-2011-06-01-51 | Winnebago County - 1987

    Pattern of soils and parent material in the Kilkenny-Lester-Waldorf association (Soil Survey of Winnebago County, Iowa; 1987).

  6. IA-2011-06-01-53 | Winnebago County - 1987

    Pattern of soils and parent material in the Vinje-Collinwood association (Soil Survey of Winnebago County, Iowa; 1987).

Map Units

Map units containing COLLINWOOD 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
Collinwood silty clay loam, 1 to 3 percent slopes38418954032982wd8wia02119731:15840
Collinwood silty clay loam, 2 to 6 percent slopes384B4724032992wd8sia02119731:15840
Collinwood silty clay loam, 5 to 9 percent slopes384C203403300fjnpia02119731:15840
Collinwood silty clay loam, 1 to 3 percent slopes3842843993502wd8wia04120021:12000
Collinwood silty clay loam, 1 to 3 percent slopes3848844055682wd8wia06319891:15840
Collinwood silty clay loam, 2 to 6 percent slopes384B38984065512wd8sia08119871:15840
Collinwood silty clay loam, 1 to 3 percent slopes38428114065502wd8wia08119871:15840
Collinwood silty clay loam, 1 to 3 percent slopes3844024108022wd8wia16119751:15840
Collinwood silty clay loam, 1 to 3 percent slopes3849304123062wd8wia18919841:15840
Collinwood silty clay loam, 2 to 6 percent slopes384B5394123072wd8sia18919841:15840
Collinwood silty clay loam, 1 to 3 percent slopes9652603962292wd8wmn01319751:12000
Collinwood silty clay loam, 6 to 12 percent slopes96C615396235f99smn01319751:12000
Collinwood silty clay loam, 2 to 6 percent slopes96B4653962342wd8smn01319751:12000
Collinwood silty clay loam, 12 to 18 percent slopes96D406396236f99tmn01319751:12000
Collinwood silty clay loam, 1 to 3 percent slopes96A139923971352wd8wmn04319891:20000
Collinwood silty clay loam, 2 to 6 percent slopes96B71413971362wd8smn04319891:20000
Collinwood silty clay loam, 1 to 3 percent slopes96188103985272wd8wmn06319841:20000
Collinwood silty clay loam, 1 to 3 percent slopes966834000732wd8wmn09119851:20000
Collinwood silty clay loam, 1 to 3 percent slopes1387A13264362322wd8wmn09319961:20000
Collinwood silty clay loam, 2 to 6 percent slopes96B13144364832wd8smn09319961:20000
Collinwood silty clay loam, 1 to 3 percent slopes96A1111918594152wd8wmn10120081:12000
Collinwood silty clay loam, 2 to 6 percent slopes96B482618594162wd8smn10120081:12000
Collinwood silty clay loam, 1 to 3 percent slopes1387A2234295632wd8wmn13119961:12000

Map of Series Extent

Approximate geographic distribution of the COLLINWOOD 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 .