Official Series Description


Lab Data Summary

Aggregate lab data for the SALINAS soil series. This aggregation is based on all pedons with a current taxon name of SALINAS, 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 SALINAS 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
1479P027979CA053002Salinas8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5224342,-121.5265656
1440A3059S1965CA053003SALINAS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.25,-121.1500015
1440A3062S1965CA053011SALINAS6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5513878,-121.5044479

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SALINAS 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 SALINAS 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 SALINAS 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 SALINAS 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 SALINAS 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 SALINAS 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 SALINAS 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 SALINAS, 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 SALINAS 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
Salinas clay loam, 0 to 2 percent slopes, MLRA 14SbA1965528333712tyy1ca05319721:24000
Salinas loam, 0 to 2 percent slopes, MLRA 14SaA255528333772tyxzca05319721:24000
Salinas clay loam, 2 to 9 percent slopes, MLRA 14SbC182528333752tyy3ca05319721:24000
Salinas clay loam, 0 to 2 percent slopes, MLRA 14SaA169828333722tyy1ca06919651:20000
Salinas clay loam, 2 to 9 percent slopes, MLRA 14SaC49928333762tyy3ca06919651:20000
Salinas clay loam, 0 to 2 percent slopesSbAmo153849248xhq3ca06919651:20000
Salinas clay loam, 2 to 9 percent slopesSbC8268456923hbggca63819671:24000
Salinas clay loam, 0 to 2 percent slopes, warm MAAT, MLRA 19SbA236228333732tyy2ca63819671:24000
Salinas clay, 0 to 2 percent slopesScA2128456924hbghca63819671:24000
Salinas clay, 2 to 5 percent slopesScB1139456925hbgjca63819671:24000
Salinas silty clay loam, 0 to 2 percent slopes, MLRA 1419760704571692tyxvca66419771:24000
Salinas silty clay loam, 2 to 9 percent slopes, MLRA 1419827654571702tyxyca66419771:24000
Salinas loam, 0 to 2 percent slopes, MLRA 14196172028333782tyxzca66419771:24000
Salinas loam, 0 to 2 percent slopes, MLRA 14SaA271328333792tyxzca67219661:20000
Salinas silty clay loam, 2 to 9 percent slopes, MLRA 14SdC24664574822tyxyca67219661:20000
Salinas silty clay loam, 0 to 2 percent slopes, MLRA 14SdA22754574812tyxvca67219661:20000
Salinas loam, 2 to 9 percent slopesSaC919457479hc1dca67219661:20000
Salinas and Sorrento loams, 9 to 15 percent slopesSeD401457483hc1jca67219661:20000
Salinas loam, overflow, 0 to 2 percent slopesSbA130457480hc1fca67219661:20000
Salinas clay loam, 2 to 9 percent slopesSaC2616457762hcbjca67419681:24000
Salinas clay loam, 0 to 2 percent slopes, warm MAAT, MLRA 19SaA138328333742tyy2ca67419681:24000
Salinas clay loam, 2 to 9 percent slopesSaCvt3003618hcbjca69220011:24000
Salinas clay loam, 2 to 9 percent slopesSaC5514129021jf7hca77219811:24000

Map of Series Extent

Approximate geographic distribution of the SALINAS 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 .