Official Series Description


Lab Data Summary

Aggregate lab data for the LAS POSAS soil series. This aggregation is based on all pedons with a current taxon name of LAS POSAS, 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 LAS POSAS 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
18UCD665800966-CA-58-009LAS POSAS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2531738,-121.3216934

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAS POSAS 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 LAS POSAS 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 LAS POSAS 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 LAS POSAS 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 flats position figure.

Competing Series

Soil series competing with LAS POSAS 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 LAS POSAS 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 LAS POSAS 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 LAS POSAS, 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 LAS POSAS 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
Las Posas loam, 30 to 65 percent slopes, stonyLrG5484832959222zwscca63819671:24000
Las Posas stony fine sandy loam, 9 to 30 percent slopesLrE10477456869hbdqca63819671:24000
Las Posas fine sandy loam, 9 to 15 percent slopes, erodedLpD24649456867hbdnca63819671:24000
Las Posas fine sandy loam, 15 to 30 percent slopes, erodedLpE24404456868hbdpca63819671:24000
Las Posas stony fine sandy loam, 9 to 30 percent slopes, erodedLrE24348456870hbdrca63819671:24000
Las Posas fine sandy loam, 5 to 9 percent slopes, erodedLpC21053456866hbdmca63819671:24000
Las Posas fine sandy loam, 5 to 9 percent slopesLpC907456865hbdlca63819671:24000
Las Posas fine sandy loam, 2 to 5 percent slopesLpB314456864hbdkca63819671:24000
Blasingame-Las Posas rocky loams, 15 to 50 percent slopesBlF17607463254hk1pca64919671:24000
Blasingame-Las Posas rocky loams, 2 to 15 percent slopesBlD5321463253hk1nca64919671:24000
Blasingame-Las Posas loams, 2 to 15 percent slopesBgD3745463250hk1kca64919671:24000
Blasingame-Las Posas extremely rocky loams, 30 to 75 percent slopes, erodedBmG22452463255hk1qca64919671:24000
Blasingame-Las Posas loams, 15 to 30 percent slopesBgE1627463251hk1lca64919671:24000
Las Posas extremely rocky clay loam, 5 to 50 percent slopesLcF1177463278hk2gca64919671:24000
Las Posas very rocky clay loam, 9 to 30 percent slopesLbE815463277hk2fca64919671:24000
Las Posas-Rock outcrop complex, 9 to 50 percent slopes1445478463609hkf4ca66019771:24000
Las Posas loam, 30 to 50 percent slopes1434722463608hkf3ca66019771:24000
Las Posas loam, 15 to 30 percent slopes1422540463607hkf2ca66019771:24000
Las Posas loam, 9 to 15 percent slopes141890463606hkf1ca66019771:24000
Las Posas-Toomes rocky loams, 30 to 50 percent slopesLdF11895457856hcfkca67519681:24000
Las Posas loam, 9 to 30 percent slopesLaE784457855hcfjca67519681:24000
Las Posas gravelly loam, 15 to 50 percent slopes159970458060hcn4ca67819741:24000
Las Posas rocky loam, 15 to 50 percent slopes, severely erodedLkF39133458294hcwpca67919671:15840
Las Posas loam, 8 to 15 percent slopes, erodedLaD23331458290hcwkca67919671:15840
Las Posas loam, 2 to 8 percent slopesLaC3308458288hcwhca67919671:15840
Las Posas loam, 8 to 25 percent slopes, severely erodedLaE3675458291hcwlca67919671:15840
Las Posas rocky loam, 8 to 15 percent slopes, erodedLkD2541458293hcwnca67919671:15840
Las Posas loam, 5 to 8 percent slopes, erodedLaC2383458289hcwjca67919671:15840
Las Posas stony loam, 8 to 15 percent slopes, erodedLcD2196458292hcwmca67919671:15840

Map of Series Extent

Approximate geographic distribution of the LAS POSAS 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 .