Official Series Description


Lab Data Summary

Aggregate lab data for the CONEJO soil series. This aggregation is based on all pedons with a current taxon name of CONEJO, 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 CONEJO 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
1795P051395CA612004CONEJO7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6734842,-121.8121733

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CONEJO 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 CONEJO 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 CONEJO 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 CONEJO 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 CONEJO 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 CONEJO 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 CONEJO 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 CONEJO, 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 CONEJO 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
Conejo clay loam, 0 to 2 percent slopes, MLRA 14CeA50704557782xc94ca01319731:24000
Conejo clay loam, clay substratum, 0 to 2 percent slopesChA884455780h98lca01319731:24000
Conejo clay loam, 2 to 5 percent slopesCeB560455779h98kca01319731:24000
Conejo clay loam, 2 to 9 percent slopesCpC2487456176h9pcca06919651:20000
Conejo loam, 0 to 2 percent slopes, cool, MLRA 1412027144558962xc96ca08719761:24000
Conejo clay loam, 0 to 2 percent slopes, cool, MLRA 1412216484558982xc95ca08719761:24000
Conejo loam, 2 to 9 percent slopes121882455897h9dcca08719761:24000
Conejo soils, wetCs436456073h9l1ca09519691:24000
Conejo loamCn344456070h9kyca09519691:24000
Conejo clay loamCr300456072h9l0ca09519691:24000
Conejo gravelly loamCo210456071h9kzca09519691:24000
Conejo-Tisdale complex, 0 percent slopes, MLRA 17126227774593362y0fnca10119841:24000
Conejo loam, 0 to 1 percent slopes, MLRA 1712478404593342xc97ca10119841:24000
Conejo-Urban land complex, 0 percent slopes, MLRA 1712745464593372xc99ca10119841:24000
Conejo loam, 0 percent slopes, dense substratum, MLRA 1712517534593352y0fmca10119841:24000
Conejo clay loam, 2 to 5 percent slopesCeBcc801705vx7gca60919631:20000
Conejo clay loam, 0 to 1 percent slopes42012953461181hgwtca61220051:24000
Conejo fine sandy loam, 0 to 1 percent slopes, overwash419800461180hgwsca61220051:24000
Conejo loam, 0 to 1 percent slopes, MLRA 1714196954604462xc97ca61819911:24000
Conejo loam, 0 to 2 percent slopes, occasionally flooded, MLRA 1714227404604482y0flca61819911:24000
Conejo-Urban land complex, 0 percent slopes, MLRA 171432104604502y0fpca61819911:24000
Conejo-Urban land complex, 0 to 2 percent slopes, MLRA 19110110554560122xc98ca67619751:24000
Conejo-Urban land complex, 2 to 9 percent slopes1111310456013h9j3ca67619751:24000
Conejo-Urban land complex, 0 to 2 percent slopes110sf852670246h9j2ca69620161:24000
Conejo-Urban land complex, 2 to 9 percent slopes111sf62670247h9j3ca69620161:24000

Map of Series Extent

Approximate geographic distribution of the CONEJO 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 .