Soil Data Explorer - BASINGER

Official Series Description

Lab Data Summary

Aggregate lab data for the BASINGER soil series. This aggregation is based on all pedons with a current taxon name of BASINGER, 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 BASINGER were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
154	S27_017	1975-FL053-S27_017	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.4553909,-82.6316833
154	91P0244	90FL101001	Basinger	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.3033333,-82.4950027
154	S28_017	S1985FL055017	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.6337452,-81.355751
155	S49_018	1974-FL097-S49_018	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.111742,-81.2381439
155	S64_029	1976-FL127-S64_029	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.9624329,-81.0378952
155	40A5046	S1953FL115009	BASINGER	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.2661591,-82.4215317
155	40A5047	S1953FL115018	BASINGER	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.2372723,-82.3526459
155	S05_016	S1967FL009016	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.4290867,-80.7916489
155	S50_011	S1973FL099011	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.789917,-80.0927124
155	S50_022	S1973FL099022	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.6945305,-80.0775528
155	S14_006	S1984FL027006	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.1596355,-81.6108093
156A	S06_010	1972-FL011-S06_010	Basinger	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.0785999,-80.2518463

Water Balance

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

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BASINGER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the BASINGER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the BASINGER 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 (updated 2024-10-23).

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

Competing Series

Soil series competing with BASINGER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the BASINGER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the BASINGER 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 (updated 2024-10-23).

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.

Soil series sharing subgroup-level classification with BASINGER, 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 (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. FL-2012-04-25-30 | Polk County - October 1990

   Relationship of soils to topography (Soil Survey of Polk County, Florida; October 1990).

Map Units

Map units containing BASINGER 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
Basinger sand, 0 to 2 percent slopes	7	10671	1473293	2vbpc	fl009	1990	1:24000
Basinger sand, depressional	6	1609	1473292	1lg2k	fl009	1990	1:24000
Basinger fine sand, 0 to 2 percent slopes	5	8310	321083	2svym	fl017	1985	1:20000
Basinger fine sand, depressional, 0 to 1 percent slopes	6	7794	321094	2v16t	fl017	1985	1:20000
Basinger fine sand, 0 to 2 percent slopes	3	18000	1386897	2svym	fl027	1986	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	5	8860	1386899	2v16v	fl027	1986	1:24000
Basinger fine sand, frequently flooded	4	3030	1386898	1hk5n	fl027	1986	1:24000
Placid, Basinger, and St. Johns soils, depressional	12	16500	1529414	1nbgy	fl035	1991	1:15840
Basinger fine sand, 0 to 2 percent slopes	14	51920	1453573	2svym	fl043	1991	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	34	5510	1453587	2v16v	fl043	1991	1:24000
Basinger fine sand, 0 to 2 percent slopes	7	10800	1384386	2svym	fl049	1981	1:20000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	37	1390	1384415	2v16v	fl049	1981	1:20000
Basinger sand, 0 to 2 percent slopes	17	49240	1151417	2vbpc	fl051	1986	1:24000
Basinger fine sand, depressional, 0 to 1 percent slopes	10	4460	322072	2v16t	fl053	1976	1:20000
Basinger fine sand, 0 to 2 percent slopes	9	2186	322127	2svym	fl053	1976	1:20000
Floridana-Basinger association, occasionally flooded	24	918	322087	bt4x	fl053	1976	1:20000
Basinger fine sand, 0 to 2 percent slopes	12	63856	1413512	2svym	fl055	1982	1:24000
Basinger, St. Johns, and Placid soils	33	35667	1413532	1jfwt	fl055	1982	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	3	16370	1413503	2v16v	fl055	1982	1:24000
Paola-Basinger sands, rolling	45	5985	1413544	1jfx6	fl055	1982	1:24000
Tavares-Basinger-Sanibel complex, rolling	34	4541	1413533	1jfwv	fl055	1982	1:24000
Satellite-Basinger-Urban land complex	44	4263	1413543	1jfx5	fl055	1982	1:24000
Anclote-Basinger fine sand, frequently flooded	41	2894	1413540	1jfx2	fl055	1982	1:24000
Basinger, Holopaw, and Samsula soils, depressional	5	56275	1406998	1j731	fl057	1986	1:20000
Placid and Basinger fine sands, depressional	13	5847	1421564	1jq7x	fl085	1979	1:20000
Basinger fine sand, 0 to 2 percent slopes	55	1780	1421602	2svym	fl085	1979	1:20000
Basinger fine sand, 0 to 2 percent slopes	2	33510	1416153	2svym	fl093	1998	1:24000
Basinger and Placid soils, depressional	3	26010	1416154	1jjmd	fl093	1998	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	3	33228	323143	2v16v	fl095	1986	1:20000
Samsula-Hontoon-Basinger association, depressional	41	30158	323156	bv8d	fl095	1986	1:20000
Basinger fine sand, depressional, 0 to 1 percent slopes	6	47191	1483846	2v16t	fl097	1976	1:20000
Basinger fine sand, 0 to 2 percent slopes	5	44637	1483845	2svym	fl097	1976	1:20000
Basinger fine sand, depressional, 0 to 1 percent slopes	23	13780	323192	2v16t	fl101	1980	1:20000
Basinger fine sand, 0 to 2 percent slopes	22	3570	323191	2svym	fl101	1980	1:20000
Basinger fine sand-Urban land complex, 0 to 2 percent slopes	6	1120	3102979	2x9fl	fl103	2003	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	7	1020	1017112	2v16v	fl103	2003	1:24000
Basinger fine sand, 0 to 2 percent slopes	87	22607	3103035	2y9hy	fl105	1987	1:20000
Basinger mucky fine sand, frequently ponded, 0 to 1 percent slopes	36	22052	3103034	2y9hl	fl105	1987	1:20000
Basinger sand, 0 to 2 percent slopes	8	8068	1421165	2vbpc	fl111	1990	1:24000
Basinger, Samsula, and Hontoon soils, depressional	10	22896	1478694	1lmpt	fl117	1986	1:20000
Basinger and Smyrna fine sands, depressional	11	8124	1478695	1lmpv	fl117	1986	1:20000
Nittaw, Okeelanta, and Basinger soils, frequently flooded	23	7891	1478707	1lmq7	fl117	1986	1:20000
Basinger and Delray fine sands	9	5433	1478693	1lmps	fl117	1986	1:20000
Floridana-Basinger association, frequently flooded	63	3899	323673	bvt2	fl119	1985	1:24000
Basinger fine sand, depressional, 0 to 1 percent slopes	43	2913	323651	2v16t	fl119	1985	1:24000
Basinger fine sand, 0 to 2 percent slopes	24	447	323631	2svym	fl119	1985	1:24000
Basinger fine sand, frequently ponded, 0 to 1 percent slopes	8	9005	1544186	2v16v	fl127	1977	1:20000
Basinger fine sand, 0 to 2 percent slopes	4	3086	1389869	2svym	fl606	1981	1:20000
Basinger sand	Ba	1863	640576	phkr	fl609	1968	1:24000
Basinger fine sand, 0 to 2 percent slopes	6	23370	1407268	2svym	fl611	1994	1:20000
Basinger and Myakka sands, depressional	8	12830	1407270	1j7ct	fl611	1994	1:20000
Basinger fine sand-Urban land complex, 0 to 2 percent slopes	7	3330	3102980	2x9fl	fl611	1994	1:20000
Basinger fine sand, 0 to 2 percent slopes	17	14410	1413466	2svym	fl621	1989	1:24000
Basinger fine sand-Urban land complex, 0 to 2 percent slopes	101	7630	3045893	2x9fl	fl621	1989	1:24000
Holopaw-Basinger-Urban land complex, 0 to 2 perent slopes	115	6360	3045907	2y0j7	fl621	1989	1:24000
Basinger fine sand, occasionally flooded	56	860	1413497	1jfvp	fl621	1989	1:24000

Map of Series Extent

Approximate geographic distribution of the BASINGER 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 (updated 2024-10-30).