Official Series Description


Lab Data Summary

Aggregate lab data for the FIDDYMENT soil series. This aggregation is based on all pedons with a current taxon name of FIDDYMENT, 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 FIDDYMENT 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
1779P022979CA067004Fiddyment6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5187874,-121.2415848
1783P030182CA067008Fiddyment6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.603611,-121.3411102
1769C0015S1969CA061006FIDDYMENT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7666664,-121.3555527
1769C0016S1969CA061007FIDDYMENT7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7666664,-121.355278
1769C0017S1969CA061008FIDDYMENT7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7666664,-121.355278
1769C0021S1969CA061013Fiddyment6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8233337,-121.3047256
1769C0022S1969CA061016FIDDYMENT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.810276,-121.3102798
1769C0023S1969CA061017FIDDYMENT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8105545,-121.3102798

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FIDDYMENT 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 FIDDYMENT 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 FIDDYMENT 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 FIDDYMENT 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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Click the image to view it full size.

Competing Series

Soil series competing with FIDDYMENT 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 FIDDYMENT 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 FIDDYMENT 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.

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 FIDDYMENT, 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. CA-2011-05-27-07 | Sacramento County - 1993

    Idealized cross section of the geomorphic surface, soils, and geology south of the American River in Sacramento County. The vertical scale is exaggerated (Soil Survey of Sacramento County, California; 1993).

  2. CA-2011-05-27-08 | Sacramento County - 1993

    Cross section showing the relationship of geomorphic surfaces, soils, and geology in the eastern part of Sacramento County. The vertical scale is exaggerated. The number 1 indiates Deer Creek; 2, the Cosumnes River; 3, Arkansas Creek; and 4, the Sacramento- Amador County line (Soil Survey of Sacramento County, California; 1993).

Map Units

Map units containing FIDDYMENT 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
Urban land-Xerarents-Fiddyment complex, 0 to 8 percent slopes22920890461973hhqcca06719891:24000
Fiddyment fine sandy loam, 1 to 8 percent slopes1455620461889hhmnca06719891:24000
Fiddyment-Urban land complex, 1 to 8 percent slopes1494100461893hhmsca06719891:24000
Fiddyment-Orangevale-Urban land complex, 2 to 8 percent slopes1484010461892hhmrca06719891:24000
Xerarents-Urban land-Fiddyment complex, 8 to 15 percent slopes2411740461985hhqrca06719891:24000
Fiddyment loam, 1 to 15 percent slopes1461480461890hhmpca06719891:24000
Kaseberg-Fiddyment-Urban land complex, 2 to 15 percent slopes1621030461906hhn6ca06719891:24000
Fiddyment fine sandy loam, 0 to 1 percent slopes144950461888hhmmca06719891:24000
Fiddyment-Orangevale complex, 2 to 8 percent slopes147490461891hhmqca06719891:24000
Cometa-Fiddyment complex, 1 to 5 percent slopes14124262460305hfzkca62019751:24000
Fiddyment-Kaseberg loams, 2 to 9 percent slopes1478810460311hfzrca62019751:24000
Alamo-Fiddyment complex, 0 to 5 percent slopes1047000460268hfycca62019751:24000
Fiddyment loam, 1 to 8 percent slopes1464200460310hfzqca62019751:24000
Urban land-Xerarents-Fiddyment complex, 0 to 8 percent slopes229sa17461414769hhqcca62019751:24000

Map of Series Extent

Approximate geographic distribution of the FIDDYMENT 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 .