Official Series Description


Lab Data Summary

Aggregate lab data for the CIENEBA soil series. This aggregation is based on all pedons with a current taxon name of CIENEBA, 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 CIENEBA 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
1869C0028S1969CA061023Cieneba6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7825012,-121.2052765
1940A2970S1955CA065008Cieneba5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.6861115,-117.0052795
2040A3376S1976CA037111Cieneba6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.4105568,-118.1386108

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CIENEBA 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 CIENEBA 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 CIENEBA 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 CIENEBA 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 CIENEBA 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 CIENEBA 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 CIENEBA 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 CIENEBA, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2012-05-08-20 | San Luis Obispo County, Carrizo Plain Area - 2003

    Idealized cross-section of the northwestern part of the survey area, showing soil-landscape-geology relationships (Soil Survey of San Luis Obispo County, California, Carrizo Plain Area; 2003).

Map Units

Map units containing CIENEBA 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
Cieneba fine gravelly sandy loam, 30 to 75 percent slopesCcG71200455570h91tca05319721:24000
Cieneba-Rock outcrop complex, 50 to 75 percent slopes, cool MAAT, MLRA 15Cd555004555712tb7xca05319721:24000
Cieneba-Sur-Rock outcrop complexCe42720455572h91wca05319721:24000
Cieneba gravelly sandy loam, 30 to 75 percent slopes, erodedCgG29136456167h9p2ca06919651:20000
Cieneba gravelly sandy loam, 15 to 75 percent slopes, severely erodedCgG33959456168h9p3ca06919651:20000
Cieneba-Rock outcrop complex, 30 to 75 percent slopes, very stonyCmrG12781432959212zwsbca63819671:24000
Cieneba-Fallbrook rocky sandy loams, 30 to 65 percent slopes, erodedCnG2103729456782hb9xca63819671:24000
Cieneba rocky coarse sandy loam, 9 to 30 percent slopes, erodedCmE232117456779hb9tca63819671:24000
Cieneba-Fallbrook rocky sandy loams, 9 to 30 percent slopes, erodedCnE220853456781hb9wca63819671:24000
Cieneba coarse sandy loam, 30 to 65 percent slopes, erodedClG213060456778hb9sca63819671:24000
Cieneba coarse sandy loam, 15 to 30 percent slopes, erodedClE21047932959202zws9ca63819671:24000
Cieneba coarse sandy loam, 5 to 15 percent slopes, erodedClD24668456776hb9qca63819671:24000
Cieneba-Rock outcrop complex, cool, 30 to 65 percent slopes1340367432958992zwr9ca63819671:24000
Cieneba sandy loam, 30 to 75 percent slopes, eroded1422830725845sc9cca63819671:24000
Cieneba-Rock outcrop complex, 30 to 75 percent slopes1451220725846sc9dca63819671:24000
Cieneba sandy loam, cool, 9 to 30 percent slopes134245232959032zwrkca63819671:24000
Cieneba-Rock outcrop complex, 15 to 75 percent slopes11660507463581hkd7ca66019771:24000
Cieneba-Kinkel variant loams, 30 to 75 percent slopes1185130457090hbmvca66419771:24000
Cieneba-Millsap loams, 30 to 75 percent slopes1191645457091hbmwca66419771:24000
Cieneba coarse sandy loam, 30 to 75 percent slopes, MLRA 151262213028333802tb7lca66519771:24000
Cieneba-Andregg complex, 30 to 75 percent slopes12710470457230hbscca66519771:24000
Vista-Cieneba complex, 15 to 30 percent slopes2114995457314hbw2ca66519771:24000
Cieneba-Vista complex, 30 to 50 percent slopes1284700457231hbsdca66519771:24000
Cieneba coarse sandy loam, 30 to 75 percent slopes, MLRA 15350366028333812tb7lca66720031:24000
Cieneba-Vista-Rock outcrop complex, 30 to 60 percent slopes26722369467359hpb3ca66820071:24000
Blasingame-Arujo-Cieneba association, 15 to 45 percent slopes26110943467354hp9yca66820071:24000
Feethill-Cibo-Cieneba complex, 15 to 30 percent slopes3023674467392hpc5ca66820071:24000
Cieneba-Vista-Rock outcrop complex, 30 to 60 percent slopes267ne105222180952dg3gca67019771:24000
Cieneba-Rock outcrop complex, 30 to 50 percent slopes, MLRA 20Cr147904579522tb7zca67719721:24000
Cieneba-Friant sandy loams complexCp1060457951hcjmca67719721:24000
Cieneba sandy loam, 9 to 15 percent slopesCnD545457950hcjlca67719721:24000
Cieneba sandy loam, 30 to 75 percent slopes, eroded14242174458043hcmlca67819741:24000
Cieneba-Rock outcrop complex, 30 to 75 percent slopes14537461458046hcmpca67819741:24000
Rock outcrop-Cieneba complex, 30 to 75 percent slopes19217938458093hcp6ca67819741:24000
Cieneba-Blasingame-Rock outcrop complex, 9 to 30 percent slopes1433490458044hcmmca67819741:24000
Cieneba sandy loam, 15 to 30 percent slopes1412785458042hcmkca67819741:24000
Cieneba-Rock outcrop complex, 9 to 30 percent slopes1441600458045hcmnca67819741:24000
Cieneba rocky sandy loam, 15 to 50 percent slopes, erodedCkF2114945458193hcsfca67919671:15840
Cieneba sandy loam, 15 to 50 percent slopes, erodedChF28372458191hcscca67919671:15840
Cieneba rocky sandy loam, 8 to 15 percent slopes, erodedCkD26287458192hcsdca67919671:15840
Cieneba sandy loam, 8 to 15 percent slopes, erodedChD24923458190hcsbca67919671:15840
Cieneba sandy loam, 5 to 8 percent slopesChC1696458189hcs9ca67919671:15840
Cieneba sandy loam, 30 to 75 percent slopes, eroded1421517729090sgp1ca67919671:15840
Cieneba-Rock outcrop complex, 30 to 75 percent slopes145772729103sgpgca67919671:15840
Cieneba-Rock outcrop complex, 30 to 50 percent slopes, MLRA 20Cr6807291282tb7zca67919671:15840
Rock outcrop-Cieneba complex, 30 to 75 percent slopes192565734865snpbca67919671:15840
Cieneba-Rock outcrop complex, 9 to 30 percent slopes14442734859snp4ca67919671:15840
Vista-Cieneba complex, 30 to 85 percent slopes1147987726702302rshjca69620161:24000
Vista-Fallbrook-Cieneba complex, 30 to 75 percent slopes1148838026702372rshpca69620161:24000
Cieneba-rock outcrop complex, 50 to 75 percent slopes20254880465164hm19ca76019811:24000
Rock outcrop-Cieneba-Brader family complex, 50 to 75 percent slopes44544014465202hm2jca76019811:24000
Rock outcrop-Cieneba complex, 50 to 75 percent slopes42039767465190hm24ca76019811:24000
Auberry-Cieneba-Rock outcrop complex, 30 to 50 percent slopes21319723465168hm1fca76019811:24000
Rock outcrop-Cieneba-Chawanakee complex, 30 to 75 percent slopes42918030465194hm28ca76019811:24000
Cieneba-Rock outcrop complex, 15 to 502018646465163hm18ca76019811:24000
Auberry-Cieneba-rock outcrop complex, 10 to 30 percent slopes2127511465167hm1dca76019811:24000
Holland-Bohna-Cieneba association, very steep7013437465270hm4qca76019811:24000
Cieneba-Vista-Rock outcrop complex, 30 to 60 percent slopes267ne242323710222kl7lca76019811:24000
Rock outcrop-Cieneba complex, 30 to 50 percent slopes4191659465189hm23ca76019811:24000
Cieneba-Rock outcrop complex, 15 to 75 percent slopes116tc32123707372kkydca76019811:24000
Cieneba rocky sandy loam, 15 to 50 percent slopes, erodedCkF2210848225xgn3ca77719811:24000

Map of Series Extent

Approximate geographic distribution of the CIENEBA 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 .