Soil Data Explorer - SEBEWA

Official Series Description

Lab Data Summary

Aggregate lab data for the SEBEWA soil series. This aggregation is based on all pedons with a current taxon name of SEBEWA, 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 SEBEWA 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
111B	DK7804	1978IN033004	Sebewa	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.45855,-84.9566889
111C	NO7002	1970IN113002	Sebewa	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.5135222,-85.6135861
111C	WH7510	1975IN181010	Sebewa	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7997472,-86.8909306
111C	FU8006	1980IN049006	Sebewa	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0473667,-86.0581139
111C	FU8106	1981IN049006	Sebewa	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0411944,-86.0200361
98	LP7203	1972IN091003	Sebewa	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3397361,-86.9116528
98	SR7703	1977IN149003	Sebewa	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3457917,-86.6974194
98	PR7805	1978IN127005	Sebewa	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4636694,-86.9365833
98	97P0175	S1994IN039033	Sebewa	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4489361,-85.7102667
n/a	PB-047	1960-OH135-047	Sebewa	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	MA-012	1962-OH097-012	Sebewa	3	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 SEBEWA 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 SEBEWA 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 SEBEWA 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 SEBEWA 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 SEBEWA 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 SEBEWA 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the SEBEWA 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.

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 SEBEWA, 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. IN-2010-09-24-06 | Elkhart County -

   Typical pattern of soils and underlying material in the Bainter-Bristol-Brady association (Soil Survey of Elkhart County, Indiana).

2. IN-2010-09-24-07 | Elkhart County -

   Typical pattern of soils and underlying material in the Desker-Matherton association (Soil Survey of Elkhart County, Indiana).

3. IN-2012-01-19-14 | Elkhart County - April 1974

   Relationship of soils to topography and underlying materials in the Oshtemo-Fox association (Soil Survey of Elkhart County, Indiana; 1974).

4. IN-2012-01-20-15 | Wabash County - February 1983

   Pattern of soils and underlying material in the Fox-Ockley-Kosciusko map unit (Soil Survey of Wabash County, Indiana; 1983).

5. MI-2010-09-07-02 | Calhoun County - 1997

   Typical pattern of soils and parent material in the Hillsdale-Kalamazoo-Oshtemo association (Soil Survey of Calhoun County, Michigan; 1997).

6. MI-2012-02-06-23 | Ingham County - August 1979

   Pattern of Houghton, Palms, and Edwards soils in association 3 (Soil Survey of Ingham County, Michigan; August 1979).

Map Units

Map units containing SEBEWA 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
Sebewa loam, disintegration moraine, 0 to 1 percent slopes	Se	4518	160341	2v4bv	in033	1980	1:15840
Sebewa loam, drained, 0 to 1 percent slopes	ScuA	4755	165466	2v2cb	in039	1997	1:12000
Sebewa mucky loam, 0 to 1 percent slopes	SdnA	30	165467	5k5n	in039	1997	1:12000
Sebewa sandy clay loam	Se	8779	162595	5g60	in049	1984	1:15840
Sebewa loam, drained, 0 to 1 percent slopes	Se	12613	160916	2v2cb	in085	1985	1:20000
Sebewa mucky loam	Sf	4349	160917	5dfw	in085	1985	1:20000
Sebewa loam, drained, 0 to 1 percent slopes	Se	14000	272632	2v2cb	in087	1978	1:20000
Sebewa loam, shaly sand substratum	Sb	13862	272690	94rg	in091	1979	1:15840
Sebewa loam, disintegration moraine, 0 to 1 percent slopes	Se	978	161990	2v4bv	in103	1977	1:20000
Sebewa loam, drained, 0 to 1 percent slopes	Se	8341	272577	2v2cb	in113	1974	1:15840
Sebewa loam, shaly sand substratum	Sb	19683	160684	5d6c	in127	1978	1:15840
Sebewa loam, drained, 0 to 1 percent slopes	ScuA	1784	184989	2v2cb	in131	2001	1:12000
Sebewa clay loam	Se	785	160755	5d8n	in145	1968	1:15840
Sebewa-Milford complex	Sf	1513	161234	5ds3	in169	1980	1:15840
Sebewa loam, disintegration moraine, 0 to 1 percent slopes	Se	1223	161233	2v4bv	in169	1980	1:15840
Sebewa loam, disintegration moraine, 0 to 1 percent slopes	Se	747	161818	2v4bv	in183	1985	1:15840
Sebewa loam, 0 to 2 percent slopes	23	5236	212446	2v2c9	mi005	1984	1:15840
Sebewa loam, loamy substratum	36	707	186093	67n0	mi015	1988	1:15840
Sebewa loam, 0 to 2 percent slopes	23	3543	186161	2v2c9	mi021	1979	1:15840
Sebewa loam, 0 to 2 percent slopes	24	17602	186968	2v2c9	mi023	1984	1:15840
Sebewa loam, 0 to 2 percent slopes	65	23694	188722	2v2c9	mi025	1993	1:15840
Sebewa loam, 0 to 2 percent slopes	Sb	7837	186396	2v2c9	mi037	1974	1:15840
Sebewa loam, 0 to 2 percent slopes	Sb	9864	186250	2v2c9	mi045	1974	1:15840
Sebewa loam, 0 to 2 percent slopes	Se	1645	186894	2v2c9	mi049	1967	1:20000
Sebewa loam, disintegration moraine, 0 to 2 percent slopes	17	3823	188629	2v4bw	mi059	1991	1:15840
Sebewa loam, 0 to 2 percent slopes	Sb	8517	186754	2v2c9	mi065	1977	1:15840
Sebewa loam, 0 to 2 percent slopes	Sd	7804	188184	2v2c9	mi067	1965	1:15840
Sebewa loam, 0 to 2 percent slopes	46	4021	188777	2v2c9	mi075	1979	1:15840
Houghton and Sebewa soils, ponded	Hs	10163	187067	68nf	mi077	1978	1:15840
Sebewa loam, 0 to 2 percent slopes	Sb	9306	187081	2v2c9	mi077	1978	1:15840
Sebewa loam, 0 to 2 percent slopes	73	645	187197	2v2c9	mi081	1984	1:15840
Sebewa loam, disintegration moraine, 0 to 2 percent slopes	Se	2473	192145	2v4bw	mi087	1966	1:15840
Sebewa loam, disintegration moraine, 0 to 2 percent slopes	Sf	1081	2509150	2v4bw	mi091	1957	1:20000
Sebewa sandy loam, 0 to 3 percent slopes	SbA	598	188563	6b6p	mi091	1957	1:20000
Sebewa loam, 0 to 2 percent slopes	Se	2530	187601	2v2c9	mi093	1968	1:20000
Sebewa sandy loam, 0 to 3 percent slopes	111A	2	2509170	6b6p	mi115	1980	1:15840
Sebewa loam, disintegration moraine, 0 to 2 percent slopes	19	2888	188825	2v4bw	mi125	1980	1:15840
Sebewa loam	123	4	2441689	2mys5	mi145	1991	1:15840
Sebewa loam, 0 to 2 percent slopes	14	5360	186267	2v2c9	mi149	1980	1:15840
Sebewa loam, 0 to 2 percent slopes	Sd	7217	187849	2v2c9	mi155	1967	1:12000
Sebewa loam, disintegration moraine, 0 to 2 percent slopes	Sb	9703	191668	2v4bw	mi161	1974	1:20000
Sebewa silt loam, 0 to 2 percent slopes	Sb	1449	426242	2szfk	wi009	1970	1:20000
Sebewa silt loam, 0 to 2 percent slopes	Sm	1253	423648	2szfk	wi027	1976	1:15840
Sebewa silt loam, 0 to 2 percent slopes	SmA	4944	425561	2szfk	wi039	1967	1:15840
Sebewa silt loam, deep, 0 to 2 percent slopes	SnA	1951	425563	g8tv	wi039	1967	1:15840
Sebewa silt loam, 2 to 6 percent slopes	SmB	285	425562	g8tt	wi039	1967	1:15840
Sebewa silt loam, loamy subsoil variant, 0 to 3 percent slopes	SpA	77	425564	g8tw	wi039	1967	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Se	4078	425366	2szfk	wi045	1969	1:12000
Sebewa silt loam, 0 to 2 percent slopes	Sm	8336	423829	2szfk	wi055	1976	1:15840
Sebewa silt loam, clayey substratum	Sn	6377	423830	g70y	wi055	1976	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	2211	3268714	2szfk	wi059	2023	1:15840
Sebewa silt loam, clayey substratum	So	923	3268715	g79x	wi059	2023	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	860	3403371	2szfk	wi079	2023	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	1311	426021	2szfk	wi089	1967	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	2028	3403248	2szfk	wi101	2023	1:15840
Sebewa silt loam, clayey substratum	So	975	3268822	g79x	wi101	2023	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Se	14320	426387	2szfk	wi105	1970	1:20000
Sebewa silt loam, 0 to 2 percent slopes	Sm	3309	423930	2szfk	wi117	1974	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	5574	425681	2szfk	wi127	1967	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	1798	425776	2szfk	wi131	1967	1:15840
Sebewa silt loam, 0 to 2 percent slopes	Sm	7301	3403491	2szfk	wi133	2023	1:15840

Map of Series Extent

Approximate geographic distribution of the SEBEWA 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).