Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
154S51_0371979-FL101-S51_037Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties28.2700806,-82.3837204
155S05_0171967-FL009-S05_017Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties28.0699787,-80.7202454
155S50_0101971-FL099-S50_010Pineda2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.6494751,-80.1671143
155S64_0021973-FL127-S64_002Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.0003185,-81.1789856
155S14_0021982-FL027-S14_002Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.1092052,-81.7688599
155S18_0041986-FL035-S18_004Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.5067158,-81.4180984
15589P033389FL043002Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.065609,-81.0509415
155S26_004S1980FL051004Pineda2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.6408138,-81.4486694
155S26_010S1982FL051010Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.6072254,-81.2914429
155S22_001S1988FL043001Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.0656414,-81.0508499
156BS43_0051976-FL085-S43_005Pineda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.0587082,-80.3061447

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PINEDA 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the PINEDA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the PINEDA series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the PINEDA 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 .

Click the image to view it full size.

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

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

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with PINEDA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the PINEDA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the PINEDA 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with PINEDA, 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 PINEDA 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
Pineda sand, 0 to 2 percent slopes472357714733332x1nbfl00919901:24000
Malabar, Holopaw, and Pineda soils311154514733171lg3cfl00919901:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes264053614534452svypfl01519821:20000
Pineda fine sand, frequently ponded, 0 to 1 percent slopes731044314534802svz7fl01519821:20000
Pineda fine sand-Urban land complex, 0 to 2 percent slopes129225130458642x9cjfl01519821:20000
Pineda fine sand, limestone substratum, 0 to 2 percent slopes7784514534842x1n9fl01519821:20000
Pineda fine sand, ponded-Urban land complex, 0 to 1 percent slopes13027130458652x9ckfl01519821:20000
Cypress Lake-Pineda, limestone substratum complex51289932362352zlf2fl01719851:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes261101013869202svypfl02719861:24000
Pineda fine sand, frequently flooded27204013869211hk6dfl02719861:24000
Pineda-Pinellas fine sands29125013869231hk6gfl02719861:24000
Pineda fine sand, frequently ponded, 0 to 1 percent slopes2864013869222svz7fl02719861:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes141770015294162svypfl03519911:15840
Pineda-Wabasso complex51450015294471nbj0fl03519911:15840
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes152418014535742svypfl04319911:24000
Pineda sand, limestone substratum217630115140617n44fl05119861:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes10759011514122svypfl05119861:24000
Pineda sand, depressional623620115144817n5hfl05119861:24000
Pineda fine sand40245322105bt5hfl05319761:20000
Pineda sand, 0 to 2 percent slopes24715814135242x1nbfl05519821:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes16219957567412svypfl06119841:20000
Pineda fine sand, frequently ponded, 0 to 1 percent slopes5643667567762svz7fl06119841:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes261485414834232svypfl07119821:20000
Pineda fine sand-Urban land complex, 0 to 2 percent slopes1291205431028942x9cjfl07119821:20000
Pineda fine sand, frequently ponded, 0 to 1 percent slopes73649114834622svz7fl07119821:20000
Pineda fine sand, limestone substratum-Urban land complex, 0 to 2 percent slopes147466331029532x9fzfl07119821:20000
Pineda fine sand, limestone substratum, 0 to 2 percent slopes77357314834662x1n9fl07119821:20000
Pineda fine sand, ponded-Urban land complex, 0 to 1 percent slopes130273131028952x9ckfl07119821:20000
Holopaw-Pineda complex, frequently flooded15331014140591jgftfl07519901:24000
Pineda fine sand40251014140831jgglfl07519901:24000
Pineda fine sand, limestone substratum35204014140781jggffl07519901:24000
Pineda-Riviera fine sands association, 0 to 2 percent slopes214965431028972x9fyfl08519791:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes8414014161592svypfl09319981:24000
Pineda fine sand, frequently flooded311135323145bv81fl09519861:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes306973231442svypfl09519861:20000
Malabar-Pineda complex21625014838611lt2hfl09719761:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes30591514838702svypfl09719761:20000
Pineda fine sand3570323199bv9sfl10119801:20000
Pineda soils and Urban land2246601017085134c6fl10320031:24000
Pineda sand, 0 to 2 percent slopes324940814211892x1nbfl11119901:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes312553414601042svypfl11519881:24000
Pineda fine sand-Urban land complex, 0 to 2 percent slopes691904631030262x9cjfl11519881:24000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes25169314787092svypfl11719861:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes451295015441482svypfl12719771:20000
Pineda-Pineda, wet, fine sand, 0 to 2 percent slopes291593014072902svypfl61119941:20000
Pineda fine sand, limestone substratum-Urban land complex, 0 to 2 percent slopes1282326730458992x9fzfl62119891:24000
Pineda fine sand, limestone substratum, 0 to 2 percent slopes141156314134632x1n9fl62119891:24000
Pineda-Riviera fine sands association, 0 to 2 percent slopes28766730459272x9fyfl62119891:24000
Pineda-Riviera fine sands-Urban land association, 0 to 2 percent slopes12929330458982x9ftfl62119891:24000

Map of Series Extent

Approximate geographic distribution of the PINEDA 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 .