Soil Data Explorer - SEBRING

Official Series Description

Lab Data Summary

Aggregate lab data for the SEBRING soil series. This aggregation is based on all pedons with a current taxon name of SEBRING, 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 SEBRING were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
n/a	AB-005	1953-OH007-005	Sebring	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AB-048	1954-OH007-048	Sebring	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-013	1956-OH029-013	Sebring	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-055	1958-OH029-055	Sebring	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-104	1959-OH029-104	Sebring	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-112	1959-OH029-112	Sebring	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AB-s12	1960-OH007-S12	Sebring	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MH-041	1964-OH099-041	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	SK-012	1964-OH151-012	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	ST-010	1966-OH153-010	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MD-017	1967-OH103-017	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	TR-022	1975-OH155-022	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WN-062	1976-OH169-062	Sebring	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SEBRING 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 SEBRING series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the SEBRING 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 SEBRING 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 SEBRING share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the SEBRING 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 SEBRING 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 3D mountains figure.

Soil series sharing subgroup-level classification with SEBRING, 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. OH-2010-09-29-03 | Ashtabula County - 2007

   Representative pattern of soils and parent materials in the Canadice-Caneadea-Fitchville association (Soil Survey of Ashtabula County, Ohio; 2007).

2. OH-2012-02-16-17 | Columbiana County - February 1968

   A schematic drawing showing the relationship of soils on the Wisconsin glacial outwash plain (in the valley to the right) and on the Wisconsin till plain (Soil Survey of Columbiana County, Ohio; February 1968).

3. OH-2012-02-16-43 | Trumbull County - March 1992

   Pattern of soils and parent material in the Wadsworth-Rittman association (Soil Survey of Trumbull County, Ohio; March 1992).

Map Units

Map units containing SEBRING 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
Sebring silt loam, 0 to 2 percent slopes	Sg	1130	288197	2v057	oh005	1976	1:15840
Sebring silt loam, 0 to 2 percent slopes	SbA	4626	298918	2v057	oh007	2001	1:12000
Sebring silt loam	Sb	5570	538007	l1v2	oh019	1981	1:15840
Sebring-Urban land complex	Sg	5	1670716	1t2j2	oh019	1981	1:15840
Sebring silt loam	Se	1060	536686	l0gg	oh031	1996	1:15840
Sebring silt loam	Sb	1005	168590	5nfd	oh033	1975	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	695	287265	2v057	oh035	1978	1:15840
Sebring silt loam, rarely flooded	Sc	531	172304	5s96	oh045	1998	1:12000
Sebring silt loam, 0 to 2 percent slopes	Sb	4214	287592	2v057	oh055	1979	1:15840
Sebring silt loam, 0 to 2 percent slopes	Se	1170	286934	2v057	oh075	1989	1:15840
Sebring silt loam	Sb	32	1605992	1qx56	oh077	1988	1:15840
Sebring silt loam	Se	2376	614627	nmkp	oh083	1983	1:15840
Sebring silt loam	Se	1485	171078	5r0n	oh089	1986	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	3115	287808	2v057	oh093	1972	1:15840
Sebring silt loam, sandstone substratum, 0 to 2 percent slopes	Sd	189	287809	2v059	oh093	1972	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	10095	816816	2v057	oh099	1966	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	Se	858	816817	2v05b	oh099	1966	1:15840
Sebring-Urban land complex, 0 to 2 percent slopes	Sg	598	816818	2v05c	oh099	1966	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sg	2515	288389	2v057	oh103	1974	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	St	592	288390	2v05b	oh103	1974	1:15840
Sebring silt loam	Se	2597	537935	l1rr	oh119	1989	1:15840
Sebring silt loam, rarely flooded	Sc	105	699498	rgwg	oh127	1984	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	9596	288495	2v057	oh133	1973	1:15840
Sebring silt loam, dark surface variant	Sv	759	288496	9p6b	oh133	1973	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	Sx	6	1717880	2v05b	oh133	1973	1:15840
Sebring silt loam, 0 to 2 percent slopes	Se	1967	170803	2v057	oh139	1971	1:15840
Sebring silt loam	Sb	336	170011	5px7	oh147	1978	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	11523	288073	2v057	oh151	1967	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	Se	1993	288074	2v05b	oh151	1967	1:15840
Sebring-Urban land complex, 0 to 2 percent slopes	Sg	370	288075	2v05c	oh151	1967	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	6414	825402	2v057	oh153	1969	1:20000
Sebring silt loam, till substratum, 0 to 2 percent slopes	Sh	1	1474197	2v05b	oh153	1969	1:20000
Sebring silt loam, 0 to 2 percent slopes	Sb	11915	287145	2v057	oh155	1986	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	Sc	11520	287146	2v05b	oh155	1986	1:15840
Sebring silt loam, dark surface variant	Sv	89	1721836	1vsq3	oh155	1986	1:15840
Sebring silt loam	Se	2100	536336	l035	oh157	1981	1:15840
Sebring silt loam, 0 to 2 percent slopes	Sb	3887	287232	2v057	oh169	1981	1:15840
Sebring silt loam, till substratum, 0 to 2 percent slopes	Se	1	2217047	2v05b	oh169	1981	1:15840
Sebring silt loam, 0 to 2 percent slopes	Se	1367	2633063	2v057	pa049	2012	1:12000
Sebring silt loam, 0 to 2 percent slopes	Sb	2	1612218	2v057	pa085	1967	1:20000

Map of Series Extent

Approximate geographic distribution of the SEBRING 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).