Official Series Description


Lab Data Summary

Aggregate lab data for the FLEWSIE soil series. This aggregation is based on all pedons with a current taxon name of FLEWSIE, 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 FLEWSIE 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
43A75-ID-408875ID079002Flewsie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.1471,-116.2725
43A89P075089ID079006Flewsie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.1005554,-116.296669

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FLEWSIE 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 FLEWSIE 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 FLEWSIE 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 FLEWSIE 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 terrace figure.

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

Competing Series

Soil series competing with FLEWSIE 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 FLEWSIE 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 FLEWSIE 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.

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

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

Soil series sharing subgroup-level classification with FLEWSIE, 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. ID-2010-08-31-06 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 6 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  2. ID-2010-08-31-10 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 5 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  3. ID-2011-06-01-18 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 5 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  4. ID-2011-06-01-19 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 6 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

Map Units

Map units containing FLEWSIE 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
Flewsie, warm-Flewsie, dry-Secunda complex, 35 to 70 percent slopesSf39224704721rn9yid05720131:24000
Bouldercreek-Flewsie-Secunda complex, 35 to 75 percent slopesSf43843814019wb1pid05720131:24000
Flewsie-Bouldercreek complex, 30 to 55 percent slopesFb43442657112q1s5id05720131:24000
Flewsie, moist-Secunda complex, 35 to 65 percent slopesFw72681704723rnb0id05720131:24000
Secunda-Flewsie complex, 25 to 60 percent slopesPa12627657114q1s7id05720131:24000
Brodeer-Flewsie complex, 30 to 60 percent slopesBm2j12012501166v11rid05720131:24000
Flewsie-Threebear silt loams, 15 to 35 percent slopes231892115343554njid60819941:24000
Flewsie silt loam, 35 to 65 percent slopes21911515343354ngid60819941:24000
Nakarna-Flewsie silt loams, high precipitation, 35 to 65 percent slopes75182215349254qcid60819941:24000
Flewsie ashy silt loam, high precipitation, 35 to 65 percent slopes22158215343454nhid60819941:24000
Brodeer-Flewsie complex, 30 to 60 percent slopes3813601775581v11rid61220031:24000
Flewsie, low precipitation-Flewsie, dry complex, 30 to 60 percent slopes77526776655v25did61220031:24000
Flewsie ashy silt loam, 35 to 65 percent slopes76435776654v25cid61220031:24000
Hubub-Flewsie-Hugus families, complex, belts, lower sideslopes toesloes and stream bottoms of incised drainages in rolling uplands, north aspects456181623970112lg8yid6701:24000
Flewsie ashy silt loam, high precipitation, 35 to 65 percent slopes54nh23285096554nhid6701:24000
Flewsie-Threebear silt loams, 15 to 35 percent slopes54nj13285096654njid6701:24000

Map of Series Extent

Approximate geographic distribution of the FLEWSIE 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 .