Soil Data Explorer - SHUBUTA

Official Series Description

Lab Data Summary

Aggregate lab data for the SHUBUTA soil series. This aggregation is based on all pedons with a current taxon name of SHUBUTA, 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 SHUBUTA were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
133A	40A5099	S1953FL033024	SHUBUTA	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.838829,-87.3363953
133A	40A5100	S1953FL033026	SHUBUTA	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.8060513,-87.3422318

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHUBUTA 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 SHUBUTA 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 SHUBUTA 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 SHUBUTA 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 SHUBUTA 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 SHUBUTA 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 SHUBUTA 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 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 SHUBUTA, 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-2012-04-25-01 | Gadsden County - January 1961

   Main geologic formations and other topographic features in a segment of Gadsden County, and the positions of soils in some soil series (Soil Survey of Gadsden County, Florida; January 1961).

2. FL-2012-04-25-03 | Gadsden County - January 1961

   Geologic formations and some principal soils in relative positions (Soil Survey of Gadsden County, Florida; January 1961).

3. FL-2012-04-26-27 | Washington County - May 1965

   Geologic formations of Washington County and the position of most soil series (Soil Survey of Washington County, Florida; May 1965).

4. LA-2012-02-01-01 | Bossier Parish - August 1962

   Physiographic relationships of general soil areas in the northwestern part of Bossier Parish. The area represented is about 12 miles square (Soil Survey of Bossier Parish, Louisiana; August 1962).

5. MS-2012-04-27-11 | Newton County - February 1960

   Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

6. TN-2012-03-19-03 | Hardin County - June 1963

   Major soil series in associations 2 and 5 of their relation to the landscape (Soil Survey of Hardin County, TN; 1963).

7. TN-2012-03-19-05 | Hardin County - June 1963

   Major soil series in soil associations 8 and 10 and their relationship to the landscape (Soil Survey of Hardin County, TN; 1963).

Map Units

Map units containing SHUBUTA 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
Shubuta-Saffell complex, 10 to 30 percent slopes	SsE	3964	328093	c0dn	al001	1972	1:20000
Ruston-Shubuta-Troup association, steep	RTF	13693	328538	c0w0	al021	1967	1:20000
Ruston-Shubuta-Troup association, hilly	RTE	12045	328537	c0vz	al021	1967	1:20000
Shubuta sandy loam, 2 to 15 percent slopes, eroded	ShD2	2987	328548	c0wb	al021	1967	1:20000
Shubuta and Angie very fine sandy loams, eroded, gently sloping	ScC2	12867	329037	c1d3	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, eroded, very gently sloping	ScB2	8120	329035	c1d1	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, eroded, sloping	ScD2	7586	329039	c1d5	al045	1958	1:20000
Shubuta and Angie sandy clay loams, severely eroded, gently sloping	SbC3	2059	329033	c1cz	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, sloping	ScD	970	329038	c1d4	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, very gently sloping	ScB	766	329034	c1d0	al045	1958	1:20000
Shubuta and Angie sandy clay loams, severely eroded, very gently sloping	SbB3	584	329032	c1cy	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, gently sloping	ScC	554	329036	c1d2	al045	1958	1:20000
Shubuta and Boswell fine sandy loams, sloping phases	Sc	6410	329293	c1nc	al051	1948	1:20000
Shubuta and Boswell fine sandy loams	Sb	3887	329292	c1nb	al051	1948	1:20000
Shubuta fine sandy loam	S2	838	329297	c1nh	al051	1948	1:20000
Ruston-Cuthbert-Shubuta complex, 10 to 15 percent slopes, eroded	RxD2	18937	329505	c1w6	al057	1963	1:15840
Shubuta fine sandy loam, 6 to 10 percent slopes, eroded	SfC2	5976	329514	c1wh	al057	1963	1:15840
Ruston-Cuthbert-Shubuta complex, 6 to 10 percent slopes, eroded	RxC2	5873	329503	c1w4	al057	1963	1:15840
Ruston-Cuthbert-Shubuta complex, 10 to 15 percent slopes	RxD	5609	329504	c1w5	al057	1963	1:15840
Shubuta-Boswell complex, 15 to 50 percent slopes	ShE	5591	329519	c1wn	al057	1963	1:15840
Shubuta-Boswell complex, 10 to 15 percent slopes, eroded	ShD2	2861	329518	c1wm	al057	1963	1:15840
Shubuta-Boswell complex, 6 to 10 percent slopes, eroded	ShC2	2130	329517	c1wl	al057	1963	1:15840
Shubuta fine sandy loam, 10 to 15 percent slopes, eroded	SfD2	1767	329516	c1wk	al057	1963	1:15840
Ruston-Cuthbert-Shubuta complex, 6 to 10 percent slopes	RxC	1697	329502	c1w3	al057	1963	1:15840
Shubuta fine sandy loam, 6 to 10 percent slopes	SfC	965	329513	c1wg	al057	1963	1:15840
Shubuta fine sandy loam, 10 to 15 percent slopes	SfD	807	329515	c1wj	al057	1963	1:15840
Shubuta fine sandy loam, 2 to 6 percent slopes, eroded	SfB2	546	329512	c1wf	al057	1963	1:15840
Shubuta-Magnolia-Falaya association, hilly	SNE	62262	329700	c22h	al063	2013	1:
Shubuta-Boswell complex, 8 to 12 percent slopes, eroded	SmD2	7651	329710	c22t	al063	2013	1:
Shubuta fine sandy loam, 5 to 8 percent slopes, eroded	ShC2	4785	329709	c22s	al063	2013	1:
Shubuta-Boswell complex, 8 to 12 percent slopes, severely eroded	SmD3	3062	329711	c22v	al063	2013	1:
Shubuta fine sandy loam, 2 to 5 percent slopes, eroded	ShB2	2363	329708	c22r	al063	2013	1:
Shubuta fine sandy loam, 0 to 2 percent slopes	ShA	2320	329707	c22q	al063	2013	1:
Shubuta clay loam, 2 to 8 percent slopes, severely eroded	SgC3	1037	329706	c22p	al063	2013	1:
Shubuta fine sandy loam, 2 to 5 percent slopes	SdB	460	2995075	2x5sh	al097	2018	1:24000
Shubuta very fine sandy loam, eroded, gently sloping phase	SeC2	3666	330965	c3d9	al101	1958	1:20000
Shubuta-Cuthbert complex, eroded, 12 to 30 percent slopes	SfE	1439	330967	c3dc	al101	1958	1:20000
Shubuta very fine sandy loam, eroded, sloping phase	SeD2	1406	330966	c3db	al101	1958	1:20000
Shubuta very fine sandy loam, eroded, very gently sloping phase	SeB2	1358	330964	c3d8	al101	1958	1:20000
Shubuta-Cuthbert fine sandy loams, eroded, gently sloping phases	SgC2	693	330969	c3df	al101	1958	1:20000
Shubuta-Cuthbert sandy clay loams, severely eroded, sloping phases	ShD3	591	330972	c3dj	al101	1958	1:20000
Shubuta sandy clay loam, severely eroded, sloping phase	SdD3	559	330962	c3d6	al101	1958	1:20000
Shubuta-Cuthbert sandy clay loams, severely eroded, gently sloping phases	ShC3	407	330971	c3dh	al101	1958	1:20000
Shubuta sandy clay loam, severely eroded, gently sloping phase	SdC3	401	330961	c3d5	al101	1958	1:20000
Shubuta-Cuthbert fine sandy loams, eroded, sloping phases	SgD2	327	330970	c3dg	al101	1958	1:20000
Shubuta-Cuthbert fine sandy loams, eroded, very gently sloping phases	SgB2	290	330968	c3dd	al101	1958	1:20000
Shubuta very fine sandy loam, very gently sloping phase	SeB	195	330963	c3d7	al101	1958	1:20000
Shubuta fine sandy loam, eroded nearly level phase (kirvin)	ShB2	431	565201	lz49	ar011	1959	1:20000
Shubuta fine sandy loam, eroded gently sloping phase (kirvin)	ShC2	421	565202	lz4b	ar011	1959	1:20000
Shubuta gravelly fine sandy loam, moderately steep phase (kirvin)	ShE	281	565203	lz4c	ar011	1959	1:20000
Shubuta fine sandy loam, 3 to 8 percent slopes, eroded	SmC2	2461	565320	lz84	ar025	1965	1:15840
Shubuta fine sandy loam, 3 to 8 percent slopes	SmC	1089	565319	lz83	ar025	1965	1:15840
Shubuta gravelly fine sandy loam 3 to 8 percent slopes, eroded	SnC2	576	565322	lz86	ar025	1965	1:15840
Shubuta gravelly fine sandy loam 8 to 20 percent slopes	SnE	457	565323	lz87	ar025	1965	1:15840
Shubuta fine sandy loam, 8 to 12 percent slopes	SmD	366	565321	lz85	ar025	1965	1:15840
Shubuta fine sandy loam, 5 to 12 percent slopes	71	3840	324043	bw60	fl131	1985	1:20000
Shubuta fine sandy loam, 2 to 5 percent slopes	70	3720	324042	bw5z	fl131	1985	1:20000
Ruston-Shubuta-Linker association, hilly	RuE	28558	331752	c46p	ms003	1967	1:20000
Ora-Shubuta complex, 8 to 12 percent slopes	OsD	5355	331740	c469	ms003	1967	1:20000
Shubuta clay loam, 8 to 12 percent slopes, severely eroded	ScD3	1567	331754	c46r	ms003	1967	1:20000
Shubuta loam, 2 to 5 percent slopes, eroded	SbB2	186	331753	c46q	ms003	1967	1:20000
Shubuta fine sandy loam, 5 to 8 percent slopes, eroded	ShC2	7337	332053	c4jd	ms023	1963	1:15840
Shubuta fine sandy loam, 8 to 12 percent slopes, eroded	ShD2	6164	332055	c4jg	ms023	1963	1:15840
Shubuta fine sandy loam, 8 to 12 percent slopes	ShD	3974	332054	c4jf	ms023	1963	1:15840
Shubuta fine sandy loam, 5 to 8 percent slopes	ShC	3361	332052	c4jc	ms023	1963	1:15840
Shubuta fine sandy loam, 2 to 5 percent slopes, moderately eroded	ShB2	3174	332051	2x5b0	ms023	1963	1:15840
Shubuta sandy clay loam, 5 to 8 percent slopes, severely eroded	SnC3	1862	332056	c4jh	ms023	1963	1:15840
Shubuta sandy clay loam, 8 to 12 percent slopes, severely eroded	SnD3	1562	332057	c4jj	ms023	1963	1:15840
Shubuta fine sandy loam, 2 to 5 percent slopes	ShB	598	332050	2x5sh	ms023	1963	1:15840
Shubuta fine sandy loam, 5 to 8 percent slopes	SbC	9680	332653	c54r	ms061	1974	1:20000
Shubuta fine sandy loam, 2 to 5 percent slopes, moderately eroded	SbB2	1832	332652	2x5b0	ms061	1974	1:20000
Shubuta clay loam, severely eroded sloping phase (8 to 12 percent slopes)	ScD3	13228	333380	c5x6	ms101	1957	1:20000
Shubuta fine sandy loam, eroded sloping phase (8 to 12 percent slopes)	SdD2	13110	333387	c5xf	ms101	1957	1:20000
Shubuta fine sandy loam, eroded gently sloping phase (5 to 8 percent slopes)	SdC2	7665	333385	c5xc	ms101	1957	1:20000
Shubuta clay loam, severely eroded gently sloping phase (5 to 8	ScC3	6751	333379	c5x5	ms101	1957	1:20000
Shubuta fine sandy loam, sloping phase (8 to 12 percent slopes)	SdD	3330	333386	c5xd	ms101	1957	1:20000
Shubuta fine sandy loam, eroded very gently sloping phase (2 to	SdB2	2055	333383	c5x9	ms101	1957	1:20000
Shubuta fine sandy loam, gently sloping phase (5 to 8 percent slopes)	SdC	1164	333384	c5xb	ms101	1957	1:20000
Shubuta clay loam, severely eroded very gently sloping phase (2	ScB3	197	333378	c5x4	ms101	1957	1:20000
Shubuta fine sandy loam, very gently sloping phase (2 to 5 percent slopes)	SdB	53	333382	c5x8	ms101	1957	1:20000
Ruston-Cuthbert-Shubuta-Association, steep (smithdale, sweatman sweatman)	RuF	12968	334222	c6sc	ms139	1963	1:15840
Ruston-Cuthbert-Shubuta association, moderately steep, eroded (smithdale, sweatman, sweatman)	RuE2	1175	334221	c6sb	ms139	1963	1:15840
Shubuta and Boswell soils, 8 to 12 percent slopes, eroded	StD2	824	334333	c6wy	ms147	1965	1:20000
Shubuta and Boswell soils, 5 to 8 percent slopes, eroded	StC2	306	334332	c6wx	ms147	1965	1:20000
Shubuta and Boswell soils, 12 to 17 percent slopes	StE	212	334334	c6wz	ms147	1965	1:20000
Shubuta fine sandy loam, 2 to 5 percent slopes	ShB	341	2403460	2x5sh	ms153	2008	1:24000
SHUBUTA-SAVANNAH FINE SANDY LOAMS, ROLLING PHASES	Sr	1457	327369	bzn9	tn039	2008	1:24000
SHUBUTA-LUVERNE FINE SANDY LOAMS, ROLLING PHASES	Sn	1206	327366	bzn6	tn039	2008	1:24000
SHUBUTA-SAVANNAH CLAY LOAMS, SEVERELY ERODED ROLLING PHASES	Sp	742	327368	bzn8	tn039	2008	1:24000
SHUBUTA-SAVANNAH CLAY LOAMS, ERODED ROLLING PHASES	So	628	327367	bzn7	tn039	2008	1:24000
SHUBUTA-LUVERNE CLAY LOAMS, ERODED ROLLING PHASE	Sm	488	327365	bzn5	tn039	2008	1:24000
Shubuta-Cuthbert loams, moderately steep phases complex (Shubuta-Luverne)	Sb	4446	327788	c02t	tn077	1955	1:20000
Shubuta-Cuthbert-Silerton soils, moderately steep phases complex (Shubuta-Luverne-Silerton)	Sh	4142	327794	c030	tn077	1955	1:20000
Shubuta-Ruston-Silerton soils, moderately steep phases complex (Shubuta-Smithdale-Silerton)	Sn	3470	327798	c034	tn077	1955	1:20000
Shubuta-Ruston-Silerton soils, severely eroded moderately steep complex (Shubuta-Smithdale-Silerton)	So	3324	327799	c035	tn077	1955	1:20000
Shubuta-Cuthbert-Silerton soils, severely eroded phases complex (Shubuta-Luverne-Silerton)	Sk	2985	327795	c031	tn077	1955	1:20000
Shubuta-Cuthbert-Silerton soils, severely eroded sloping phases complex (Shubuta-Luverne-Silerton)	Sg	2961	327793	c02z	tn077	1955	1:20000
Shubuta-Cuthbert sandy clays, severely eroded moderately steep phases complex (Shubuta-Luverne)	Se	2295	327791	c02x	tn077	1955	1:20000
Shubuta-Ruston-Silerton soils, severely eroded phases complex (Shubuta-Smithdale-Silerton)	Sm	1725	327797	c033	tn077	1955	1:20000
Shubuta-Cuthbert-Silerton soils, sloping phases complex (Shubuta-Luverne-Silerton)	Sf	1389	327792	c02y	tn077	1955	1:20000
Shubuta-Ruston-Silerton soils, sloping phases complex (Shubuta-Smithdale-Silerton)	Sl	717	327796	c032	tn077	1955	1:20000
Shubuta-Cuthbert sandy clays, severely eroded sloping phases complex (Shubuta-Luverne)	Sd	421	327790	c02w	tn077	1955	1:20000
Shubuta-Cuthbert loams, steep phases complex (Shubuta-Luverne)	Sc	419	327789	c02v	tn077	1955	1:20000

Map of Series Extent

Approximate geographic distribution of the SHUBUTA 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).