Official Series Description


Lab Data Summary

Aggregate lab data for the CALIFON soil series. This aggregation is based on all pedons with a current taxon name of CALIFON, 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 CALIFON 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
14884P048883NJ019001Califon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6616669,-74.9561081

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CALIFON 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 CALIFON 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 CALIFON 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 CALIFON 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 CALIFON 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 CALIFON 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 CALIFON 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 CALIFON, 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 CALIFON 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
Califon gravelly loam, 0 to 8 percent slopes, very stonyCanBb512214828241ls01nj01919701:24000
Califon loam, 3 to 8 percent slopesCakB2626548587ldvcnj01919701:24000
Califon loam, 0 to 3 percent slopesCakA215548586ldvbnj01919701:24000
Califon loam, 0 to 8 percent slopes, very stonyCakBb3902298486b0llnj02719741:24000
Califon loam, 3 to 8 percent slopesCakB3899298485b0lknj02719741:24000
Califon loam, 0 to 3 percent slopesCakA1361298484b0ljnj02719741:24000
Califon variant loam, 3 to 8 percent slopesCapfB1332298490b0lqnj02719741:24000
Califon loam, 8 to 15 percent slopesCakC992298487b0lmnj02719741:24000
Califon gravelly loam, 3 to 8 percent slopesCanB948298489b0lpnj02719741:24000
Califon loam, 8 to 15 percent slopesCakCb685298488b0lnnj02719741:24000
Califon gravelly loam, 0 to 8 percent slopes, very stonyCanBb7414829581ls4cnj02719741:24000
Califon gravelly loam, 0 to 8 percent slopes, very stonyCanBb354548455ldq3nj03519721:24000
Califon gravelly loam, 3 to 8 percent slopesCanB339548456ldq4nj03519721:24000
Califon loam, 3 to 8 percent slopesCakB9548538ldssnj03519721:24000
Califon loam, somewhat poorly drained, 0 to 8 percent slopes, very stonyCaoBb25931910247223rwnj04120071:12000
Califon loam, somewhat poorly drained, 8 to 15 percent slopes, very stonyCaoCb17091910248223rxnj04120071:12000
Califon loam, 3 to 8 percent slopesCaB110194795923d0dpa01719971:24000
Califon loam, 3 to 8 percent slopesCaB9523886525yrhlpa02920081:24000
Califon loam, 0 to 3 percent slopesCaA1577886526yrhmpa02920081:24000
Urban land-Califon complex, 0 to 8 percent slopesUrcB36616119631r3ctpa02920081:24000
Califon loam, 8 to 15 percent slopesCaC213886527yrhnpa02920081:24000
Califon loam, 0 to 8 percent slopes, extremely stonyCbB193886524yrhkpa02920081:24000
Califon loam, 0 to 3 percent slopesCaA1523961972zhhtpa04519601:20000
Califon loam, 3 to 8 percent slopesCaB88223871102l3zkpa09120081:12000
Califon loam, 0 to 3 percent slopesCaA8523961412lfcwpa09120081:12000
Califon loam, 3 to 8 percent slopesCaB13211914217227wypa09520071:12000
Cokesbury-Califon channery silt loams, 0 to 8 percent slopes, very stonyCoB4601914220227x1pa09520071:12000
Califon loam, 0 to 8 percent slopes, extremely stonyCbB1101914218227wzpa09520071:12000

Map of Series Extent

Approximate geographic distribution of the CALIFON 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 .