Official Series Description


Lab Data Summary

Aggregate lab data for the RIDGEPORT soil series. This aggregation is based on all pedons with a current taxon name of RIDGEPORT, 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 RIDGEPORT 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
103UMN2702S1978MN015006(2702)Ridgeport2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2928505,-94.5235977
103UMN2758S1978MN015026(2758)Ridgeport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2509995,-94.7962494
103UMN3066S1979MN015004(3066)Ridgeport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.20261,-95.0270157
103UMN3219S1979MN015007(3219)Ridgeport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2047997,-95.0311813

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT 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 RIDGEPORT, 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-2010-09-02-11 | Humboldt County - 2005

    Typical pattern of soils and parent material in the Spillville-Ridgeport-Coland association (Soil Survey of Humboldt County, Iowa; 2005).

  2. IA-2010-09-02-14 | Humboldt County - 2005

    Typical pattern of soils and parent material in the Lester-Spillville-Coland association (Soil Survey of Humboldt County, Iowa; 2005).

  3. IA-2011-05-31-39 | Hancock, County - 1989

    Typical pattern of soils and parent material in the Fieldon-Harcot-Ridgeport association (Soil Survey of Hancock County, Iowa; 1989).

Map Units

Map units containing RIDGEPORT 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
Ridgeport sandy loam, 0 to 2 percent slopes8234872550300fjfmia01519771:15840
Ridgeport sandy loam, 2 to 5 percent slopes823B4702550301fjfnia01519771:15840
Ridgeport sandy loam, 5 to 9 percent slopes, moderately eroded823C23202550302fjfpia01519771:15840
Ridgeport sandy loam, 1 to 3 percent slopes823142403567fjy9ia02719791:15840
Ridgeport sandy loam, 2 to 5 percent slopes823B741404628fl1jia04919801:15840
Ridgeport sandy loam, 0 to 2 percent slopes823483404627fl1hia04919801:15840
Ridgeport sandy loam, 5 to 9 percent slopes823C266404629fl1kia04919801:15840
Ridgeport sandy loam, 1 to 3 percent slopes823496405665fm3zia06319891:15840
Ridgeport sandy loam, 0 to 2 percent slopes8233008406593fn2xia08119871:15840
Ridgeport sandy loam, 2 to 5 percent slopes823B2111406594fn2yia08119871:15840
Ridgeport sandy loam, 0 to 2 percent slopes8231765447583h0r5ia09119981:12000
Ridgeport sandy loam, 2 to 5 percent slopes823B755447584h0r6ia09119981:12000
Ridgeport sandy loam, 5 to 9 percent slopes, moderately eroded823C2168447586h0r8ia09119981:12000
Ridgeport sandy loam, 2 to 5 percent slopes823B1714408405fpzcia10919801:15840
Ridgeport sandy loam, 0 to 2 percent slopes8231298408404fpzbia10919801:15840
Ridgeport sandy loam, 5 to 9 percent slopes, moderately eroded823C2260408406fpzdia10919801:15840
Ridgeport sandy loam, 2 to 5 percent slopes823B14225065792q4msia14319851:15840
Ridgeport sandy loam, 5 to 9 percent slopes, moderately eroded823C210625065802q4mtia14319851:15840
Ridgeport sandy loam, 0 to 2 percent slopes8231811412338fv27ia18919841:15840
Ridgeport sandy loam, 2 to 5 percent slopes823B1624412339fv28ia18919841:15840
Ridgeport variant loam, 0 to 6 percent slopes1829B869396260f9blmn01519841:20000
Storden-Ridgeport variant loams, 15 to 50 percent slopes1911F802396265f9brmn01519841:20000
Ridgeport sandy loam639623396306f9d2mn01519841:20000
Ridgeport variant loam, 6 to 15 percent slopes1829C279396261f9bmmn01519841:20000
Estherville-Ridgeport complex, 0 to 6 percent slopesM534B209315919351qfjrmn04920071:12000
Ridgeport sandy loam, 2 to 6 percent slopes639B2042428174gck2mn14519801:15840
Ridgeport sandy loam, 0 to 2 percent slopes639A1714428173gck1mn14519801:15840
Ridgeport sandy loam, 1 to 6 percent slopes639B350428957gdcbmn16519871:20000

Map of Series Extent

Approximate geographic distribution of the RIDGEPORT 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 .