Official Series Description


Lab Data Summary

Aggregate lab data for the FONTREEN soil series. This aggregation is based on all pedons with a current taxon name of FONTREEN, 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 FONTREEN 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
28A67C0024S1967UT039001Fontreen7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2113876,-111.6436081
4767C0025S1967UT039002Fontreen6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1722221,-112.0002747
4771C0033S1971UT039008Fontreen7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1705551,-112.0086136

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FONTREEN 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 FONTREEN 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 FONTREEN 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 FONTREEN 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 FONTREEN 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 FONTREEN 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 FONTREEN 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 FONTREEN, 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 FONTREEN 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
Fontreen-Borvant gravelly loams, 5 to 20 percent slopes3110317481239j4rvut60119851:24000
Fontreen-Bullump complex, 3 to 15 percent slopes326627481240j4rwut60119851:24000
Fontreen-Phage association, 15 to 40 percent slopes335259481241j4rxut60119851:24000
Fontreen-Rexmont, very shallow complex, 6 to 40 percent slopesFEE6750503848jx95ut60419801:24000
Fontreen-Borvant complex, 2 to 25 percent slopesFfD7076482501j62kut60819811:24000
Fontreen stony loam, 3 to 25 percent slopesFeD1799482499j62hut60819811:24000
Fontreen stony loam, 25 to 60 percent slopesFeF1213482500j62jut60819811:24000
Lodar-Amtoft-Fontreen complex, 30 to 70 percent slopesLYG2256124540042nclfut61819951:24000
Lodar-Fontreen complex, 40 to 70 percent slopesLSG13227482289j5vqut62719711:24000
Fontreen very cobbly loam, 20 to 40 percent slopes, erodedFRE211010482258j5tqut62719711:24000
Fontreen very cobbly loam, 40 to 70 percent slopes, erodedFRG210310482259j5trut62719711:24000
Fontreen cobbly loam, 4 to 20 percent slopesFOD7300482257j5tput62719711:24000
Fontreen-Borvant complex, 4 to 25 percent slopes, erodedFSD24655482260j5tsut62719711:24000
Lodar-Amtoft-Fontreen complex, 40 to 70 percent slopesLYG2187324539482ncjmut62719711:24000
Lodar-Amtoft-Fontreen complex, 40 to 70 percent slopes1665282483547j759ut6281:24000
Fontreen cobbly loam, 4 to 20 percent slopes13183483480j734ut6281:24000
Streuling-Fontreen very gravelly loams, 15 to 50 percent slopes4852491484027j7nsut63419971:24000
Atepic-Fontreen families complex, 20 to 50 percent slopes226547331284130gvjut6451:24000
Fontreen-Maple Mountain families complex, 20 to 50 percent slopes22C2440331284330gvlut6451:24000
Donnardo-Fontreen families complex, 3 to 15 percent slopes12L26532432802zscvut6451:24000
Fontreen family, 10 to 30 percent slopes22T101331284430gvmut6451:24000

Map of Series Extent

Approximate geographic distribution of the FONTREEN 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 .