Official Series Description


Lab Data Summary

Aggregate lab data for the RINCON soil series. This aggregation is based on all pedons with a current taxon name of RINCON, 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 RINCON 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
1740A3063S1964CA113016Rincon7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7227783,-121.8583298
1740A3050S1964CA113017Rincon6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7811127,-122.0475006

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RINCON 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 RINCON 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 RINCON 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 RINCON 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 RINCON 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 RINCON 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 RINCON 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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Soil series sharing subgroup-level classification with RINCON, 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 RINCON 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
Rincon clay loam, 2 to 9 percent slopes, MLRA 14RbC69654558442tb8pca01319731:24000
Rincon clay loam, 0 to 2 percent slopes, MLRA 14RbA665528334082tb8nca01319731:24000
Rincon clay loam, 9 to 15 percent slopes, MLRA 14RbD8754558452tb8sca01319731:24000
Rincon clay loam, wet, 0 to 2 percent slopesRcA590455846h9bqca01319731:24000
Rincon clay loam, 2 to 9 percent slopes, MLRA 14RaC129454557042tb8pca05319721:24000
Rincon clay loam, 0 to 2 percent slopes, MLRA 14RaA547528334092tb8nca05319721:24000
Rincon clay loam, 9 to 15 percent slopes, MLRA 14RaD53604557052tb8sca05319721:24000
Rincon clay loam, 15 to 30 percent slopes, MLRA 14RaE18304557062tb8tca05319721:24000
Rincon clay loam, 2 to 9 percent slopes, MLRA 14RoCso718164852tb8pca05519741:24000
Rincon clay loam, 0 to 2 percent slopes, MLRA 14RoAso6428334102tb8nca05519741:24000
Rincon silty clay loam, 2 to 9 percent slopes, MLRA 14RsC53074562672tb8zca06919651:20000
Rincon silty clay loam, 0 to 2 percent slopesRsA44344562662tb8xca06919651:20000
Rincon silty clay loam, 9 to 15 percent slopes, eroded, MLRA 14RsD224874562682tb91ca06919651:20000
Rincon loam, 2 to 9 percent slopesRnC2228456264h9s6ca06919651:20000
Rincon loam, 9 to 15 prcent slopes, erodedRnD2629456265h9s7ca06919651:20000
Rincon loam, 0 to 2 percent slopesRnA498456263h9s5ca06919651:20000
Rincon clay loam, 0 to 2 percent slopeRoA8909456108h9m5ca09519691:24000
Rincon clay loam, 2 to 9 percent slopes, MLRA 14RoC33944561092tb8pca09519691:24000
Rincon loam, 2 to 9 percent slopesRnC450456107h9m4ca09519691:24000
Rincon silty clay loamRg24995459261hdwwca11319681:20000
Rincon clay loam, 0 to 3 percent slopesRdA3511456615hb4jca60919631:20000
Rincon loam, 0 to 3 percent slopesRc2075456614hb4hca60919631:20000
Rincon clay loam, 3 to 7 percent slopesRdB1069456616hb4kca60919631:20000
Rincon clay loam, 0 to 2 percent slopes, MLRA 14140aw5028334112tb8nca60919631:20000
Rincon clay loam, 0 to 2 percent slopes, MLRA 1414025644566932tb8nca61019751:24000
Rincon clay loam, 2 to 9 percent slopes, erodedRaC2835457043hblbca64619671:24000
Rincon clay loam, 0 to 2 percent slopes, MLRA 14RaA56328334132tb8nca64619671:24000
Rincon silty clay loam, 0 to 2 percent slopesRsAsb356996872tb8xca64619671:24000
Rincon clay loam, 2 to 9 percent slopes, MLRA 1418879304572912tb8pca66519771:24000
Rincon clay loam, 9 to 15 percent slopes, MLRA 1418918804572922tb8sca66519771:24000
Rincon clay loam, 0 to 2 percent slopes1871390457290hbv9ca66519771:24000
Rincon silty clay loam, 15 to 30 percent slopes, erodedRcE23328457758hcbdca67419681:24000
Rincon silty clay loam, 2 to 9 percent slopes, MLRA 19RcC32864577562tb90ca67419681:24000
Rincon silty clay loam, 9 to 15 percent slopes, eroded, warm MAAT, MLRA 19RcD221604577572tb92ca67419681:24000
Rincon silty clay loam, 9 to 30 percent slopes, severely erodedRcE3507457759hcbfca67419681:24000
Rincon clay loam, 2 to 9 percent slopes188700458089hcp2ca67819741:24000
Rincon clay loam, 9 to 15 percent slopes, MLRA 191893104580902tb8vca67819741:24000
Rincon clay loam, 15 to 30 percent slopes, MLRA 191902804580912tb8wca67819741:24000
Urban land-Rincon, landscaped-Antioch, landscaped complex, 0 to 8 percent slopes, residential44121524039672lpjbca69220011:24000
Kawenga-Sapwi-Rincon complex, 0 to 8 percent slopes, landscaped4493724039682lpjcca69220011:24000
Modesto-Rincon-Millsholm families association, 20 to 50 percent slopes3142310465298hm5mca77219811:24000
Rincon-Livermore-Modesto families association, 30 to 60 percent slopes4140355465309hm5zca77219811:24000
Rincon-Modesto-Los Osos families association, 30 to 60 percent slopes4213681465310hm60ca77219811:24000
Rincon silty clay loam, 2 to 9 percent slopes, MLRA 14RcC4914129012tb8zca77219811:24000
Rincon clay loam, 2 to 9 percent slopes, MLRA 14188pr1214128752tb8pca77219811:24000

Map of Series Extent

Approximate geographic distribution of the RINCON 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 .