Official Series Description


Lab Data Summary

Aggregate lab data for the FLAGLER soil series. This aggregation is based on all pedons with a current taxon name of FLAGLER, 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 FLAGLER 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
104X53-284-1S1985IA105007Flagler2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0221107,-91.1379171
105X3-284G-2S1988IA005009Flagler2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.416467,-91.5221711
105X3-788-1S1989IA005101Flagler2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3621677,-91.605744

Water Balance

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with FLAGLER, 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-2010-09-09-07 | Bremer County - 2009

    Typical pattern of soils and parent material in the Spillville-Waukee-Coland association (Soil Survey of Bremer County, Iowa; 2009).

  2. IA-2011-05-31-15 | Delaware County - 1986

    Pattern of soils and parent material in the Spillville-Saude-Marshan association (Soil Survey of Delaware County, Iowa; 1986).

  3. IA-2011-05-31-42 | Hardin County - 1985

    Pattern of soils and parent material in the Coland-Saude-Spillville association (Soil Survey of Hardin County, Iowa; 1985).

Map Units

Map units containing FLAGLER 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
Flagler sandy loam, 0 to 2 percent slopes284910402864fj6mia01119771:15840
Flagler sandy loam, 2 to 5 percent slopes284B489402865fj6nia01119771:15840
Flagler sandy loam, 0 to 2 percent slopes2845096413242fw0dia01320011:12000
Flagler sandy loam, 2 to 5 percent slopes284B1144413316fw2sia01320011:12000
Flagler-Urban land complex, 0 to 2 percent slopes4284893413315fw2ria01320011:12000
Flagler-Urban land complex, 2 to 5 percent slopes4284B159413243fw0fia01320011:12000
Flagler sandy loam, 1 to 4 percent slopes, rarely flooded284B111015859901q7bzia01720081:12000
Flagler sandy loam, 0 to 2 percent slopes2844257403226fjl9ia01919781:15840
Flagler sandy loam, 2 to 5 percent slopes284B910403227fjlbia01919781:15840
Flagler sandy loam, 0 to 2 percent slopes2848009403387fjrhia02319781:15840
Flagler sandy loam, 2 to 5 percent slopes284B1475403388fjrjia02319781:15840
Flagler sandy loam, 5 to 9 percent slopes284C401403389fjrkia02319781:15840
Flagler sandy loam, 2 to 5 percent slopes284B1145403824fk6lia03319781:15840
Flagler sandy loam, 5 to 9 percent slopes284C648403825fk6mia03319781:15840
Flagler sandy loam, 0 to 2 percent slopes284315403823fk6kia03319781:15840
Flagler sandy loam, 2 to 5 percent slopes284B2610404015fkdria03719891:15840
Flagler sandy loam, 5 to 9 percent slopes, moderately eroded284C2526404017fkdtia03719891:15840
Flagler sandy loam, 5 to 9 percent slopes284C224404016fkdsia03719891:15840
Flagler sandy loam, 0 to 2 percent slopes284224404014fkdqia03719891:15840
Flagler sandy loam, 0 to 2 percent slopes284717404249fkn9ia04319791:15840
Flagler sandy loam, 2 to 5 percent slopes284B218404250fknbia04319791:15840
Flagler sandy loam, 1 to 5 percent slopes284B753404395fkt0ia04519781:15840
Flagler sandy loam, 5 to 9 percent slopes284C664404396fkt1ia04519781:15840
Flagler fine sandy loam, 0 to 2 percent slopes2841681405030flghia05519841:15840
Flagler fine sandy loam, 2 to 5 percent slopes284B1076405031flgjia05519841:15840
Flagler sandy loam, 2 to 5 percent slopes284B355405413flvvia06119831:15840
Flagler sandy loam, 2 to 5 percent slopes284B3713405751fm6ria06519751:15840
Flagler sandy loam, 0 to 2 percent slopes2843091405750fm6qia06519751:15840
Flagler sandy loam, 5 to 9 percent slopes284C593405752fm6sia06519751:15840
Flagler sandy loam, 5 to 9 percent slopes, moderately eroded284C21024753582p2t8ia06519751:15840
Flagler sandy loam, 2 to 5 percent slopes284B991405896fmcfia06719891:15840
Flagler sandy loam, 0 to 2 percent slopes284795405895fmcdia06719891:15840
Flagler sandy loam, 5 to 9 percent slopes284C283405897fmcgia06719891:15840
Flagler sandy loam, 1 to 5 percent slopes284B874404896flb5ia06919771:15840
Flagler sandy loam, 5 to 9 percent slopes284C337404897flb6ia06919771:15840
Flagler sandy loam, 2 to 5 percent slopes284B595406652fn4tia08319821:15840
Flagler sandy loam, 5 to 9 percent slopes, moderately eroded284C2327406653fn4via08319821:15840
Flagler sandy loam, 0 to 2 percent slopes284289406651fn4sia08319821:15840
Flagler sandy loam, 1 to 4 percent slopes284B632407653fp63ia09919751:15840
Flagler sandy loam, 0 to 2 percent slopes284294407989fpjyia10319791:15840
Flagler sandy loam, 1 to 5 percent slopes284B293408132fppkia10519881:15840
Flagler sandy loam, 2 to 5 percent slopes284B1155408594fq5gia11319701:15840
Flagler sandy loam, 5 to 9 percent slopes284C1077408595fq5hia11319701:15840
Flagler sandy loam, 0 to 2 percent slopes284A768408593fq5fia11319701:15840
Flagler sandy loam, 5 to 9 percent slopes, moderately eroded284C2251408596fq5jia11319701:15840
Flagler fine sandy loam, 0 to 2 percent slopes284462409310fqxkia12319711:15840
Flagler sandy loam, 2 to 5 percent slopes284B400409658fr8sia13119711:15840
Flagler sandy loam, 0 to 2 percent slopes28475409657fr8ria13119711:15840
Flagler sandy loam, calcareous subsoil variant, 0 to 2 percent slopes8231024410303frylia14719731:15840
Flagler sandy loam, calcareous subsoil variant, 2 to 5 percent slopes823B472410304frymia14719731:15840
Flagler sandy loam, calcareous subsoil variant, 2 to 5 percent slopes823B864410838fshvia16119751:15840
Flagler sandy loam, calcareous subsoil variant, 5 to 9 percent slopes, moderately eroded823C2440410839fshwia16119751:15840
Flagler sandy loam, 0 to 2 percent slopes2841260410951fsmhia16319891:15840
Flagler sandy loam, 2 to 5 percent slopes284B617411310ft02ia16919811:15840
Flagler sandy loam, 0 to 2 percent slopes284556411309ft01ia16919811:15840
Flagler sandy loam, 0 to 5 percent slopes, rarely flooded284B37123987212lj23ia19520121:12000
Flagler sandy loam, 0 to 5 percent slopes1284B24425814562r18dia19520121:12000
Flagler sandy loam, 0 to 2 percent slopes783A40814072511j7c6il00720061:12000
Flagler sandy loam, 2 to 6 percent slopes783B8014832281lsf2il00720061:12000
Flagler sandy loam, 0 to 2 percent slopes783A85141741955v86il20119971:12000
Flagler sandy loam, 2 to 6 percent slopes783B12801741965v87il20119971:12000
Flagler sandy loam, bedrock substratum, 0 to 2 percent slopes1951A1079429005gddwmn16919871:20000
Flagler sandy loam, bedrock substratum. 2 to 6 percent slopes1951B686429006gddxmn16919871:20000

Map of Series Extent

Approximate geographic distribution of the FLAGLER 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 .