Official Series Description


Lab Data Summary

Aggregate lab data for the FIDDLER soil series. This aggregation is based on all pedons with a current taxon name of FIDDLER, 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 FIDDLER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FIDDLER 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 FIDDLER 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 FIDDLER 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 FIDDLER 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 FIDDLER 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 FIDDLER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the FIDDLER 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 terrace figure.

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

Soil series sharing subgroup-level classification with FIDDLER, 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 FIDDLER 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
Fiddler-Deven complex, 15 to 30 percent slopes165im46914689971l9m0ca60319741:24000
Fiddler-Deven complex, 30 to 50 percent slopes166im2914689981l9m1ca60319741:24000
Fiddler-Whitinger complex, 5 to 15 percent slopes1674965486924jbp7ca60419941:24000
Fiddler-Deven complex, 15 to 30 percent slopes1652224486920jbp3ca60419941:24000
Fiddler-Whitinger complex, 15 to 30 percent slopes1681310486926jbp9ca60419941:24000
Fiddler-Deven complex, 30 to 50 percent slopes166360486922jbp5ca60419941:24000
Devada-Petescreek-Fiddler association, 2 to 30 percent slopes17868542487449jc75ca60820001:24000
Fiddler-Orhood-Petescreek association, 5 to 30 percent slopes19718126487479jc84ca60820001:24000
Rubble land-Fiddler association, 15 to 50 percent slopes34316813487686jcgtca60820001:24000
Fiddler-Madeline association, 5 to 30 percent slopes19611168487478jc83ca60820001:24000
Ninemile-Petescreek-Fiddler association 2 to 30 percent slopes2986469487616jcdkca60820001:24000
Fiddler-Gavel-Rubble land association, 30 to 50 percent slopes1954639487477jc82ca60820001:24000
Fiddler-Gavel-Rubble land complex, 5 to 30 percent slopes1944387487475jc80ca60820001:24000
Lorella-Fiddler very complex, 5 to 30 percent slopes1456740486611jbc4ca68419861:24000
Bucklake-Fiddler association3263901103474013qqqca68520061:24000
Dosie-Fiddler-Rubble land association3873053103477013qrpca68520061:24000
Fiddler-Whitinger complex, 5 to 15 percent slopes167im1755189917921r7vca70319831:24000
Rubble land-Fiddler association, 15 to 50 percent slopes343su455189885921qxjca70319831:24000
Fiddler-Deven complex, 15 to 30 percent slopes165im415189917321r7nca70319831:24000
Devada-Petescreek-Fiddler association, 2 to 30 percent slopes178su363189882521qwfca70319831:24000
Fiddler-Whitinger complex, 15 to 30 percent slopes168im235189918221r7yca70319831:24000
Lorella-Fiddler very complex, 5 to 30 percent slopes145tl173189811821q4mca70319831:24000
Fiddler-Orhood-Petescreek association, 5 to 30 percent slopes197su115189883121qwmca70319831:24000
Fiddler-Deven complex, 30 to 50 percent slopes166im16189917621r7rca70319831:24000
Fiddler-Whitinger complex, 15 to 30 percent slopes168It31715280871n934ca70819841:24000
Rubble land-Fiddler association, 15 to 50 percent slopes343su3115283671n9d5ca70819841:24000
Fiddler-Gavel-Rubble land complex, 5 to 30 percent slopes194su515283311n9c0ca70819841:24000
Fiddler-Whitinger complex, 5 to 15 percent slopes167It215280841n931ca70819841:24000
Dosie-Fiddler-Rubble land association13674070474583hxv4nv75919951:24000
Bucklake-Fiddler association10813300474478hxqrnv75919951:24000

Map of Series Extent

Approximate geographic distribution of the FIDDLER 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 .