Soil Data Explorer - WABASSO

Official Series Description

Lab Data Summary

Aggregate lab data for the WABASSO soil series. This aggregation is based on all pedons with a current taxon name of WABASSO, 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 WABASSO 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	S51_002	S1977FL101002	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.2862644,-82.395874
154	S53_012	S1981FL105012	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.0453167,-81.8496628
154	S60_001	S1982FL119001	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.8968773,-82.2310181
155	S64_021	1975-FL127-S64_021	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.8637581,-80.8754959
155	S49_016	S1974FL097016	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	28.1856422,-81.4909363
155	S36_015	S1978FL071015	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.7697201,-81.8660507
155	S26_013	S1983FL051013	Wabasso	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.7305412,-81.5326385
155	S14_017	S1985FL027017	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.2385769,-82.0158615
155	S18_003	S1986FL035003	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	29.5112667,-81.4347382
156B	S50_013	S1973FL099013	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	26.7532253,-80.2266388
156B	S56_016	S1975FL111016	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.4852505,-80.609787
156B	S43_024	S1978FL085024	Wabasso	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	27.1581059,-80.4246445

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WABASSO 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 WABASSO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the WABASSO 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 2023-10-09).

Geomorphic description summaries for the WABASSO 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 2023-10-04).

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

Competing Series

Soil series competing with WABASSO share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the WABASSO 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 2023-10-09).

Geomorphic description summaries for the WABASSO 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 2023-10-04).

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 WABASSO, 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 2023-10-02).

Block Diagrams

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

1. FL-2011-05-31-06 | Indian River County - 1987

   Typical pattern of soils and parent material in the Boca-Wabasso-Riviera map unit. The adjacent Riomar and Mckee soils are in the tidal marsh (Soil Survey of Indian River County, Florida; 1987).

Map Units

Map units containing WABASSO 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
Wabasso sand, 0 to 2 percent slopes	71	21182	1473356	2svyr	fl009	1990	1:24000
Copeland-Bradenton-Wabasso complex, limestone substratum	16	7738	1473302	1lg2w	fl009	1990	1:24000
Wabasso sand, 0 to 2 percent slopes	35	43200	1453451	2svyr	fl015	1982	1:20000
Wabasso sand, limestone substratum, 0 to 2 percent slopes	42	7732	1453458	2tzws	fl015	1982	1:20000
Wabasso sand, limestone substratum-Urban land complex, 0 to 2 percent slopes	138	4858	3045875	2x9c5	fl015	1982	1:20000
Wabasso sand-Urban land complex, 0 to 2 percent slopes	137	3345	3045874	2x9c6	fl015	1982	1:20000
Wabasso fine sand, 0 to 2 percent slopes	41	6430	1386935	2svzg	fl027	1986	1:24000
Wabasso fine sand, 0 to 2 percent slopes	4	20100	1529444	2svzg	fl035	1991	1:15840
Pineda-Wabasso complex	5	14500	1529447	1nbj0	fl035	1991	1:15840
Wabasso fine sand, 0 to 2 percent slopes	25	2130	1384403	2svzg	fl049	1981	1:20000
Wabasso sand, limestone substratum, 0 to 2 percent slopes	14	21790	1151415	2tzws	fl051	1986	1:24000
Wabasso sand, 0 to 2 percent slopes	6	12260	1151408	2svyr	fl051	1986	1:24000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	51	3363	322117	2y9dx	fl053	1976	1:20000
Wabasso fine sand, 0 to 2 percent slopes	57	11825	1407006	2svzg	fl057	1986	1:20000
Wabasso-Urban land complex	58	4295	1407007	1j73b	fl057	1986	1:20000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	13	23794	756738	2y9dx	fl061	1984	1:20000
Wabasso sand, limestone substratum-Urban land complex, 0 to 2 percent slopes	138	11799	3102914	2x9c5	fl071	1982	1:20000
Wabasso sand, limestone substratum, 0 to 2 percent slopes	42	8609	1483437	2tzws	fl071	1982	1:20000
Wabasso sand, 0 to 2 percent slopes	35	6341	1483429	2svyr	fl071	1982	1:20000
Wabasso sand-Urban land complex, 0 to 2 percent slopes	137	3527	3102913	2x9c6	fl071	1982	1:20000
Felda-Wabasso association, frequently flooded	24	15430	1384092	1hg84	fl081	1981	1:24000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	48	14732	1384118	2y9dx	fl081	1981	1:24000
Wabasso variant fine sand	50	1736	1384121	1hg92	fl081	1981	1:24000
Wabasso fine sand, rarely flooded	49	222	1384119	1hg90	fl081	1981	1:24000
Wabasso sand, 0 to 2 percent slopes	17	34218	1421568	2svyr	fl085	1979	1:20000
Wabasso and Oldsmar fine sands, depressional	56	4164	1421604	1jq96	fl085	1979	1:20000
Wabasso fine sand, 0 to 2 percent slopes	25	5340	1416174	2svzg	fl093	1998	1:24000
Wabasso-Urban land complex	52	3514	323168	bv8s	fl095	1986	1:20000
Wabasso fine sand, 0 to 2 percent slopes	51	2286	323167	2svzg	fl095	1986	1:20000
Wabasso fine sand, 0 to 2 percent slopes	45	9515	1483885	2svzg	fl097	1976	1:20000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	10	3185	323178	2y9dx	fl101	1980	1:20000
Wabasso soils and Urban land	31	7730	1017108	134cy	fl103	2003	1:24000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	62	7528	1425049	2y9dx	fl105	1987	1:20000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	50	1730	323417	2y9dx	fl107	1985	1:15840
Wabasso fine sand, 0 to 2 percent slopes	21	2975	1392019	2svzg	fl109	1981	1:20000
Wabasso sand, 0 to 2 percent slopes	48	26598	1421205	2svyr	fl111	1990	1:24000
Wabasso fine sand, gravelly substratum	49	3146	1421206	1jpwc	fl111	1990	1:24000
Wabasso fine sand, 0 to 2 percent slopes	41	2613	1460112	2svzg	fl115	1988	1:24000
Wabasso fine sand-Urban land complex, 0 to 2 percent slopes	74	807	3103033	2y0jc	fl115	1988	1:24000
Wabasso fine sand, 0 to 2 percent slopes	35	915	1478719	2svzg	fl117	1986	1:20000
Wabasso fine sand, bouldery subsurface	26	16334	323633	bvrs	fl119	1985	1:24000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	67	3070	323677	2y9dx	fl119	1985	1:24000
Wabasso fine sand, depressional	56	1231	323665	bvst	fl119	1985	1:24000
Wabasso-Wabasso, wet, fine sand, 0 to 2 percent slopes	73	9850	1544179	2y9dx	fl127	1977	1:20000
Wabasso fine sand, depressional	74	1865	1544180	1ntv8	fl127	1977	1:20000
Wabasso sand	48	1229	1542302	1nrwp	fl607	1970	1:20000
Wabasso fine sand, 0 to 2 percent slopes	49	12470	3102930	2svzg	fl611	1994	1:20000
Wabasso fine sand, 0 to 2 percent slopes	29	10108	1413475	2svzg	fl621	1989	1:24000
Wabasso fine sand-Urban land complex, 0 to 2 percent slopes	135	322	3045913	2y0jc	fl621	1989	1:24000

Map of Series Extent

Approximate geographic distribution of the WABASSO 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 2023-10-04).