Official Series Description


Lab Data Summary

Aggregate lab data for the STONYFORD soil series. This aggregation is based on all pedons with a current taxon name of STONYFORD, 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 STONYFORD 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
15UCD570600657-CA-06-006xSTONYFORDn/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3707199,-122.6076126
15UCD585202858-CA-52-028STONYFORD2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9078865,-122.6557541
15UCD624900262-CA-49-002xSTONYFORD2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7114639,-122.8171616
15UCD654502265-CA-45-022xSTONYFORD4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6643677,-122.5976563

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STONYFORD 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 STONYFORD 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 STONYFORD 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 STONYFORD 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 flats position figure.

Competing Series

Soil series competing with STONYFORD 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 STONYFORD 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 STONYFORD 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 STONYFORD, 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 STONYFORD 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
Stonyford-Guenoc complex, 20 to 50 percent slopes, MLRA 1552131544616392w8c7ca01119991:24000
Stonyford-Guenoc complex, 15 to 30 percent slopes5202161461638hhckca01119991:24000
Stonyford-Guenoc complex, 5 to 15 percent slopes519144461637hhcjca01119991:24000
Stonyford gravelly clay loam, 20 to 50 percent slopesSuE1545458866hdh4ca02119611:20000
Stonyford gravelly clay loam, 50 to 65 percent slopes, erodedSuF2925458869hdh7ca02119611:20000
Stonyford gravelly clay loam, 20 to 50 percent slopes, erodedSuE2761458867hdh5ca02119611:20000
Stonyford-Henneke complex, 30 to 65 percent slopesSvE222458870hdh8ca02119611:20000
Stonyford gravelly clay loam, 50 to 65 percent slopesSuF201458868hdh6ca02119611:20000
Stonyford clay, 30 to 65 percent slopesStE96458865hdh3ca02119611:20000
Stonyford-Guenoc complex, 20 to 50 percent slopes, MLRA 152366644596392w8c7ca03319851:24000
Stonyford gravelly loam, 50 to 75 percent slopes, erodedSoG13830459888hfk3ca09719681:20000
Stonyford gravelly loam, 30 to 50 percent slopesSoF1900459887hfk2ca09719681:20000
Stonyford-Boomer complex, 30 to 75 percent slopesSrG692459889hfk4ca09719681:20000
Stonyford very stony loam, 50 to 75 percent slopesSsG8670460141hft8ca60719671:20000
Stonyford very stony loam, 30 to 50 percent slopesSsE3891460140hft7ca60719671:20000
Stonyford complex, 15 to 50 percent slopes685455467003hnymca64219981:24000
Stonyford stony loam, 30 to 50 percent slopesStE7066460931hgmrca64519611:20000
Stonyford stony loam, 50 to 65 percent slopesStF3390460932hgmsca64519611:20000
Stonyford very stony loam, 30 to 50 percent slopesSsEsh142186868020qj0ca70719831:24000
Stonyford stony loam, 50 to 65 percent slopesStFtc39186829720q3nca70719831:24000
Stonyford very stony loam, 50 to 75 percent slopesSsGsh12186868220qj2ca70719831:24000
Millsholm-Exchequer-Stonyford families complex, 30 to 75 percent slopes29153835465295hm5jca77219811:24000
Yorba-Millsholm-Stonyford families association, 30 to 60 percent slopes51116440465320hm6bca77219811:24000
Stonyford-Millsholm families complex, 30 to 70 percent slopes2616480465333hm6rca77619811:24000

Map of Series Extent

Approximate geographic distribution of the STONYFORD 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 .