Official Series Description


Lab Data Summary

Aggregate lab data for the FLYGARE soil series. This aggregation is based on all pedons with a current taxon name of FLYGARE, 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 FLYGARE 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
4768C0122S1968UT051002Flygare7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4547234,-111.2108307
48A90P099190CO033001Flygare6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6844444,-108.2319412
48A90P099290CO033002Flygare7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6844444,-108.2319412
48A90P099390CO083001Flygare7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4799995,-108.1791687
48A92P081892CO033003Flygare7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6938896,-108.2141647

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLYGARE 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 FLYGARE 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 FLYGARE 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 FLYGARE 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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Competing Series

Soil series competing with FLYGARE 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 FLYGARE 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 FLYGARE 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 flats position figure.

Soil series sharing subgroup-level classification with FLYGARE, 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

No block diagrams are available.

Map Units

Map units containing FLYGARE 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
Flygare-Foidel complex, 0 to 15 percent slopes3503351507146k0qkco67220031:24000
Flygare-Foidel complex, 15 to 30 percent slopes3551113507147k0qlco67220031:24000
Flygare loam, dry, 25 to 65 percent slopes716281497250jpfbco68619921:31680
Foidel, moist-Flygare-Skyway, moist complex, 3 to 25 percent slopes744172497253jpffco68619921:31680
Flygare-Datemark-Rock outcrop association6120320114755117j3snv77920041:24000
Flygare, very stony-Sisna complex, 10 to 60 percent slopesERE13899508488k23vut0131:24000
Faim-Wesdy, extremely bouldery-Flygare, very stony complex, 5 to 40 percent slopes551750724989282pzwjut0131:24000
Cluff, very stony-Biorkman-Flygare complex, 2 to 20 percent slopesNbB581225037382pw0gut0131:24000
Sisna-Flygare, very stony complex, 10 to 50 percent slopesEUE373508491k23yut0131:24000
FLYGARE SILT LOAM, 3 TO 20 PERCENT SLOPESFLD1597482716j69hut60319681:20000
Flygare gravelly loam, 25 to 50 percent slopesFDF700503847jx94ut60419801:24000
Flygare-Starley association, very steepFdF8307482498j62gut60819811:24000
Flygare loam, 30 to 70 percent slopesFbF8010482496j62dut60819811:24000
Sheep Creek-Flygare complex, 8 to 30 percent slopesSmE3775482620j66dut60819811:24000
Flygare-Parkay-Rock outcrop complex, 30 to 70 percent slopesFcF2592482497j62fut60819811:24000
Flygare loam, 30 to 60 percent slopesFcG2695506545k035ut60919741:24000
Flygare-Datemark-Rock outcrop association, 30 to 70 percent slopes209769482124j5pdut61119921:24000
Flygare-Dateman families-Rock outcrop association, 25 to 80 percent slopes222753331838462whrhut6171:24000
Flygare soils, 25 to 40 percent slopesFRE4949504240jxptut62219671:24000
Flygare loam, 6 to 15 percent slopesFBC2530504236jxpput62219671:24000
Flygare-Little Pole association, hillyFLD2168504238jxprut62219671:24000
Flygare soils, 40 to 60 percent slopesFRF2084504241jxpvut62219671:24000
Flygare loam, 15 to 25 percent slopesFBD1594504237jxpqut62219671:24000
Clayburn-Flygare association, hillyCCD1288504209jxntut62219671:24000
Flygare-Little Pole association, steepFLE1271504239jxpsut62219671:24000
Baird Hollow association, moderately steepBDC1058504182jxmyut62219671:24000
Flygare soils, sandy loam subsoil variant, 25 to 40 percent slopesFSE908504242jxpwut62219671:24000
Baird Hollow-Flygare association, steepBCE486504181jxmxut62219671:24000
Flygare loam, 3 to 6 percent slopesFBB400504235jxpnut62219671:24000
Baird Hollow-Flygare association, moderately steepBCC336504180jxmwut62219671:24000
Daybell-Flygare association, very steepDBG4230482240j5t4ut62719711:24000
Flygare loam, 25 to 50 percent slopes2911132553481vlfut63319831:24000
Flygare loam, 5 to 25 percent slopes286326553471vldut63319831:24000
Faim-Wesdy, extremely bouldery-Flygare, very stony complex, 5 to 40 percent slopes55125786742pzwjut6501:24000
Flygare family-Owlcan family-Savar complex, 0 to 30 percent slopes202152554759533qwy6351:24000
Flygare family-Owlcan family-Savar complex, 0 to 30 percent slopes20222160151953533qwy66320121:24000
Flygare family-Owlcan family-Savar complex, 0 to 30 percent slopes20229752611978533qwy7231:24000

Map of Series Extent

Approximate geographic distribution of the FLYGARE 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 .