Official Series Description


Lab Data Summary

Aggregate lab data for the EL PECO soil series. This aggregation is based on all pedons with a current taxon name of EL PECO, 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 EL PECO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EL PECO 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 EL PECO 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 EL PECO 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 EL PECO 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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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with EL PECO 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 EL PECO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the EL PECO 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

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 EL PECO, 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 EL PECO 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
Fresno and El Peco fine sandy loams, strongly saline-sodic, 0 to 1 percent slopesFecA30839329593830r9bca65119591:20000
El Peco-Dinuba fine sandy loams, strongly saline alkali, 0 to 1 percent slopesEdA7297463394hk66ca65119591:20000
Dinuba-El Peco fine sandy loams, slightly saline alkali, 0 to 1 percent slopesDpA7125463390hk62ca65119591:20000
Fresno and El Peco loams, strongly saline-sodic, 0 to 1 percent slopesFfcA6773329585830r8pca65119591:20000
Fresno and El Peco fine sandy loams, moderately saline-sodic, 0 to 1 percent slopesFebA5693329585630r8mca65119591:20000
Fresno and El Peco loams, moderately saline-sodic, 0 to 1 percent slopesFfbA5164329593730r9cca65119591:20000
Fresno, El Peco, and Lewis soils, moderately saline-sodic, 0 to 1 percent slopesFhbA50044634162ycblca65119591:20000
Fresno and El Peco fine sandy loams, slightly saline-sodic, 0 to 1 percent slopesFeaA4579329585730r8nca65119591:20000
Fresno and El Peco loams, slightly saline-sodic, 0 to 1 percent slopesFfaA3795329587030r98ca65119591:20000
Dinuba-El Peco fine sandy loams, moderately saline alkali, 0 to 1 percent slopesDsA3379463391hk63ca65119591:20000
Fresno, El Peco, and Chino soils, slightly saline-alkali, 0 to percent slopesFgaA2556463414hk6vca65119591:20000
Fresno, El Peco, and Pozo soils, slightly saline-sodic, 0 to 1 percent slopesFkaA6934634182ycbjca65119591:20000
Fresno, El Peco, and Lewis soils, strongly saline-sodic, 0 to 1 percent slopesFhcA5374634172ycbkca65119591:20000
Fresno, El Peco, and Pozo soils, moderately saline-sodic, 0 to 1 percent slopesFkbA4824634192ycbhca65119591:20000
Fresno, El Peco, and Chino soils, moderately saline-alkali, 0 t 1 percent slopesFgbA377463415hk6wca65119591:20000
Traver, Fresno, and El Peco fine sandy loams, moderately saline alkali, 0 to 1 percent slopesTsA212463531hkbmca65119591:20000
Traver, fresno, el peco fine sandy loams, strongly saline-alkal , 0 to 1 percent slopesTtA178463532hkbnca65119591:20000
Dinuba-El Peco loams, slightly saline alkali, 0 to 1 percent slopesDtA169463392hk64ca65119591:20000
Dinuba-El Peco loams, moderately saline alkali, 0 to 1 percent slopesDuA127463393hk65ca65119591:20000
El Peco fine sandy loamEd8600464279hl3rca65419661:24000
El Peco sandy loamEc1369464278hl3qca65419661:24000
El Peco loamEp734464280hl3sca65419661:24000

Map of Series Extent

Approximate geographic distribution of the EL PECO 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 .