Soil Data Explorer - CALEB

Official Series Description

Lab Data Summary

Aggregate lab data for the CALEB soil series. This aggregation is based on all pedons with a current taxon name of CALEB, 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 CALEB 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
109	M9012912	1990MO129012m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.4905194,-93.5892667
109	M9112907	1991MO129007m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5680542,-93.6611099
109	M9112908	1991MO129008m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5680542,-93.628334
109	91P0892	1991MO129014	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5683327,-93.660553
109	M9311707	1993MO117007m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.8958321,-93.6244431
109	M9411713	1994MO117013m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7322502,-93.7252121
109	M9411714	1994MO117014m	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7461128,-93.6444473
115B	M9012911	1990MO129011	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9119715	1991MO197015	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9119768	1991MO197068	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9119769	1991MO197069	Caleb	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012

Water Balance

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

Soil series sharing subgroup-level classification with CALEB, 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. IA-2011-06-01-15 | Lucas County - 1999

   Typical pattern of soils and parent material in the Lindley-Keswick-Weller association (Soil Survey of Lucas County, Iowa; 1999).

2. IA-2011-06-01-42 | Ringgold County - 1992

   Relationship of the major soils in Ringgolg County to parent material and to position on the landscape (Soil Survey of Ringgold County, Iowa; 1992).

Map Units

Map units containing CALEB 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
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	354	402185	fhhq	ia001	1976	1:15840
Mystic-Caleb complex, 14 to 18 percent slopes, moderately eroded	94E2	872	402737	fj2j	ia007	1970	1:15840
Mystic-Caleb complex, 14 to 18 percent slopes, severely eroded	94E3	684	402738	fj2k	ia007	1970	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	552	402735	2wjf6	ia007	1970	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, severely eroded	94D3	212	402736	fj2h	ia007	1970	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	2658	404188	2wjf6	ia039	1987	1:15840
Caleb-Mystic loams, 9 to 14 percent slopes	94D	860	404187	2yy85	ia039	1987	1:15840
Caleb-Mystic complex, 14 to 18 percent slopes, moderately eroded	94E2	674	404189	2wbdb	ia039	1987	1:15840
Caleb-Mystic complex, 14 to 18 percent slopes, moderately eroded	94E2	344	404748	2wbdb	ia051	1988	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	160	404694	2wbd9	ia051	1988	1:15840
Caleb-Mystic complex, 9 to 18 percent slopes, moderately eroded	94E2	2747	404853	2yy83	ia053	1986	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	451E2	1353	404806	2wbd8	ia053	1986	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	1172	404805	2wbd9	ia053	1986	1:15840
Caleb-Mystic complex, 9 to 18 percent slopes	94E	333	404852	2yy82	ia053	1986	1:15840
Caleb loam, 5 to 9 percent slopes, moderately eroded	451C2	328	404804	fl76	ia053	1986	1:15840
Caleb and mystic soils, 9 to 14 percent slopes, moderately eroded	94D2	425	407705	fp7s	ia099	1975	1:15840
Caleb and mystic soils, 14 to 18 percent slopes, moderately eroded	94E2	354	407706	fp7t	ia099	1975	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	2048	409065	2wjf6	ia117	1991	1:15840
Mystic-caleb complex, 14 to 18 percent slopes, moderately eroded	94E2	1248	409068	fqnr	ia117	1991	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	451E2	511	408957	2wbd8	ia117	1991	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	267	408955	2wbd9	ia117	1991	1:15840
Caleb-Mystic loams, 9 to 14 percent slopes, moderately eroded	94D2	738	409168	2yy86	ia121	1968	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	427	409167	fqry	ia121	1968	1:15840
Caleb-Mystic loams, 14 to 18 percent slopes, moderately eroded	94E2	252	409169	2yy84	ia121	1968	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	451E2	1600	409332	fqy8	ia123	1971	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	272	409331	fqy7	ia123	1971	1:15840
Caleb loam, 18 to 25 percent slopes, moderately eroded	451F2	35	409333	fqy9	ia123	1971	1:15840
Caleb-Mystic loams, 9 to 14 percent slopes, moderately eroded	94D2	1711	412814	2yy86	ia125	1976	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	184	410593	fs7y	ia157	1978	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	3316	410750	2wjf6	ia159	1987	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	447	410704	2wbd9	ia159	1987	1:15840
Caleb loam, 14 to 25 percent slopes, moderately eroded	451F2	243	410705	2wbfb	ia159	1987	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes	94D	208	410749	2wbfc	ia159	1987	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	1470	411741	ftfz	ia175	1975	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	944	411717	ftf6	ia175	1975	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	S451D2	467	3006959	2wbd9	ia175	1975	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	451E2	443	411718	ftf7	ia175	1975	1:15840
Caleb loam, 5 to 9 percent slopes, moderately eroded	451C2	255	411716	ftf5	ia175	1975	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	S451E2	247	3006964	2wbd8	ia175	1975	1:15840
Caleb loam, 7 to 14 percent slopes, moderately eroded	451D2	606	411812	ftj8	ia179	1978	1:15840
Mystic-Caleb complex, 9 to 14 percent slopes, moderately eroded	94D2	3272	411981	ftpq	ia181	1975	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	939	411941	ftnf	ia181	1975	1:15840
Mystic-Caleb complex, 14 to 18 percent slopes, moderately eroded	94E2	745	411982	ftpr	ia181	1975	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	S451D2	328	3006960	2wbd9	ia181	1975	1:15840
Caleb clay loam, 9 to 14 percent slopes, severely eroded	451D3	2166	1860783	20g98	ia185	1966	1:15840
Caleb loam, 9 to 14 percent slopes, moderately eroded	451D2	1923	1860781	2wbd9	ia185	1966	1:15840
Caleb clay loam, 14 to 18 percent slopes, severely eroded	451E3	352	1860784	20g99	ia185	1966	1:15840
Caleb loam, 14 to 18 percent slopes, moderately eroded	451E2	331	1860782	2wbd8	ia185	1966	1:15840
Caleb silt loam, 9 to 14 percent slopes, eroded	30042	3	2531037	2qmwd	mo025	1967	1:24000
Caleb silt loam, 9 to 14 percent slopes, eroded	30042	3628	2531036	2qmwd	mo117	1996	1:24000
Caleb-Mystic complex, 5 to 14 percent slopes, eroded	30043	2016	901268	z7v5	mo129	1993	1:24000
Caleb-Mystic complex, 9 to 14 percent slopes, eroded	30044	254	888520	ytky	mo197	1993	1:24000

Map of Series Extent

Approximate geographic distribution of the CALEB 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).