Official Series Description


Lab Data Summary

Aggregate lab data for the ELDER soil series. This aggregation is based on all pedons with a current taxon name of ELDER, 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 ELDER 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
1507N067405ca085641276Elder6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3143583,-122.0637

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELDER 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 ELDER 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 ELDER 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 ELDER 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 ELDER 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 ELDER 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 ELDER 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 mountains figure.

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Soil series sharing subgroup-level classification with ELDER, 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-2012-04-20-09 | Pinnacles National Monument - 2008

    Block diagram relating soils, landforms, and geology (Soil Survey of Pinnacles National Monument, California; 2008).

  2. 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 ELDER 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
Elder sandy loam, 0 to 2 percent slopes, MLRA 14EaA666528333982tyyjca05319721:24000
Elder loam, gravelly substratum, 0 to 2 percent slopesEcA3335455596h92nca05319721:24000
Elder very fine sandy loam, 2 to 9 percent slopesEbC1130455595h92mca05319721:24000
Elder gravelly sandy loam, 0 to 1 percent slopes11714186197920hjvca06919651:20000
Elder sandy loam, 0 to 2 percent slopes, MLRA 14129314328333992tyyjca08719761:24000
Elder sandy loam, 2 to 9 percent slopes, MLRA 14130216828334232tyyhca08719761:24000
Elder sandy loam, 9 to 15 percent slopes, MLRA 1413143828334032tyygca08719761:24000
Elder shaly fine sandy loam, 2 to 9 percent slopesEdC1360456801hbbjca63819671:24000
Urbanland-Elder complex, 0 to 2 percent slopes, protected169319524258942mfbnca64120091:24000
Elder fine sandy loam, 0 to 2 percent slopes, rarely flooded171112116028131qsvnca64120091:24000
Caninecreek-Elder complex, 0 to 2 percent slopes, rarely flooded1737731882924216bhca64120091:24000
Elder fine sandy loam, protected, 0 to 2 percent slopes16840424258932mfbmca64120091:24000
Urban Land-Caninecreek-Elder complex, 0 to 2 percent slopes17422424275962mh3kca64120091:24000
Caninecreek-Elder complex, 1 to 5 percent slopes, protected1781324258952mfbpca64120091:24000
Elder fine sandy loam, 0 to 2 percent slopes, rarely flooded171scl124838472pcn3ca64619671:24000
Elder sandy loam, occasionally flooded, 2 to 9 percent slopes1391650457111hbnjca66419771:24000
Elder sandy loam, 2 to 5 percent slopes1351055457107hbndca66419771:24000
Elder sandy loam, occasionally flooded, 0 to 2 percent slopes138560457110hbnhca66419771:24000
Elder sandy loam, 9 to 15 percent slopes, MLRA 1413728028334042tyygca66419771:24000
Elder sandy loam, 5 to 9 percent slopes136280457108hbnfca66419771:24000
Elder loam, 0 to 5 percent slopes, flooded1401785457243hbssca66519771:24000
Elder loam, 0 to 2 percent slopes, MLRA 14138149528333942tyydca66519771:24000
Elder loam, 2 to 9 percent slopes, MLRA 1413940528333962tyyfca66519771:24000
Elder sandy loam, 2 to 9 percent slopes, MLRA 1447530054585162tyyhca66720031:24000
Elder sandy loam, 0 to 2 percent slopes, MLRA 14474236528334002tyyjca66720031:24000
Elder sandy loam, 2 to 9 percent slopes, erodedEdC2417833563762zwt8ca67219661:20000
Elder loam, 2 to 9 percent slopes, MLRA 14EmC410428333972tyyfca67219661:20000
Elder shaly loam, 2 to 9 percent slopes, erodedEnC23005457397hbyrca67219661:20000
Elder sandy loam, 0 to 2 percent slopes, erodedEdA21818342283631d5zca67219661:20000
Elder shaly loam, 0 to 2 percent slopes, erodedEnA21410457396hbyqca67219661:20000
Elder shaly loam, 9 to 15 percent slopes, erodedEnD2987457398hbysca67219661:20000
Elder sandy loam, 9 to 15 percent slopes, erodedEdD2835342283731d60ca67219661:20000
Elder loam, 0 to 2 percent slopes, MLRA 14EmA78928333952tyydca67219661:20000
Elder sandy loam, 0 to 2 percent slopes, MLRA 14EdA38028334012tyyjca67219661:20000
Elder sandy loam, 0 to 2 percent slopes, MLRA 14EaA173328334022tyyjca67319741:24000
Elder sandy loam, 2 to 9 percent slopes, MLRA 14EaB54628334252tyyhca67319741:24000
Elder-Soboba complex, 2 to 9 percent slopesEb448457597hc56ca67319741:24000
Elder sandy loam, 2 to 9 percent slopes, erodedEdC221533563462zwt8ca67319741:24000
Elder sandy loam, 0 to 2 percent slopes, erodedEdA2202342284731d5zca67319741:24000
Elder sandy loam, 9 to 15 percent slopes, erodedEdD2153342284831d60ca67319741:24000
Urbanland-Elder complex, 0 to 2 percent slopes, protected169scl1124838092pclwca68919851:24000
Elder fine sandy loam, coastal, 0 to 2 percent slopes220365469977hs1kca69220011:24000
Elder sandy loam, 2 to 9 percent slopes475cp1214128671jf6cca77219811:24000
Elder gravelly sandy loam, 0 to 1 percent slopes11715424264302mfwyca78820071:24000
Elder coarse sandy loam, 1 to 3 percent slopes1206924264322mfx0ca78820071:24000
Elder-Oxyaquic Haploxerolls complex, 2 to 5 percent slopes1133224264272mfwvca78820071:24000

Map of Series Extent

Approximate geographic distribution of the ELDER 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 .