Official Series Description


Lab Data Summary

Aggregate lab data for the PLACID soil series. This aggregation is based on all pedons with a current taxon name of PLACID, 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 PLACID 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
155S25_0131968-FL049-S25_013Placid3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.4414463,-81.8159714
155S50_0151973-FL099-S50_015Placid3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.4105606,-80.1171799
155S49_0241975-FL097-S49_024Placid3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.8612194,-81.1676407
155S28_0231985-FL055-S28_023Placid3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.5582085,-81.2805099
15540A5093S1953FL115005PLACID4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.3256016,-82.2720871
15540A5094S1953FL115010PLACID4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.2661591,-82.4054184

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PLACID 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 PLACID 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 PLACID 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 PLACID 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 PLACID 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 PLACID 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 PLACID 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 PLACID, 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 PLACID 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
Placid sand, depressional343770320716brqpfl00119821:15840
Pompano-Placid complex801814733651lg4xfl00919901:24000
Placid, Basinger, and St. Johns soils, depressional121650015294141nbgyfl03519911:15840
Samsula and Placid soils, frequently flooded24206015294271nbhcfl03519911:15840
Placid fine sand, frequently ponded, 0 to 1 percent slopes21860013843992tzx9fl04919811:20000
Basinger, St. Johns, and Placid soils333566714135321jfwtfl05519821:24000
Placid fine sand, frequently ponded, 0 to 1 percent slopes71296114135072tzx9fl05519821:24000
Placid and Samsula soils, depressional113743014140551jgfpfl07519901:24000
Placid and Popash soils, depressional272526014140701jgg5fl07519901:24000
Placid fine sand10486014140541jgfnfl07519901:24000
Placid and Basinger fine sands, depressional13584714215641jq7xfl08519791:20000
Floridana, Riviera, and Placid soils, depressional74146014161581jjmjfl09319981:24000
Basinger and Placid soils, depressional32601014161541jjmdfl09319981:24000
Floridana, Placid, and Okeelanta soils, frequently flooded191616014161691jjmwfl09319981:24000
Placid fine sand, frequently ponded, 0 to 1 percent slopes323866414838722tzx9fl09719761:20000
Placid-Riviera-Samsula complex, frequently flooded48791524005102lkxtfl09719761:20000
Placid variant fine sand3358914838731lt2wfl09719761:20000
Placid fine sand701710323243bvc6fl10119801:20000
Placid fine sand, frequently ponded, 0 to 1 percent slopes2571010170982tzx9fl10320031:24000
Placid and Myakka fine sands, depressional251848614250161jtv8fl10519871:20000
Placid fine sand, frequently flooded37211314250271jtvmfl10519871:20000
Placid-Pompano association, frequently flooded4315600323409bvjkfl10719851:15840
Placid fine sand, frequently ponded, 0 to 1 percent slopes585303234162tzx9fl10719851:15840
Placid fine sand63920513920591hqk4fl10919811:20000
Placid fine sand, frequently ponded, 0 to 1 percent slopes3075013236382tzx9fl11919851:24000
Pompano-Placid complex53749515441571nttjfl12719771:20000
Placid fine sand, frequently ponded, 0 to 1 percent slopes48225015441512tzx9fl12719771:20000
Placid and Myakka sands, depressional402433715422941nrwffl60719701:20000
Placid sand, frequently ponded, 0 to 2 percent slopes38939815422922ttlnfl60719701:20000
Myakka and Placid sand, 2 to 8 percent slopes29426116031561qt6qfl60719701:20000
Placid-Pompano-Pomona complex59898517132031vhqmfl60819791:15840
Placid sand, depressional58727717129391vhg3fl60819791:15840

Map of Series Extent

Approximate geographic distribution of the PLACID 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 .