Soil Data Explorer - CLAIREMONT

Official Series Description

Lab Data Summary

Aggregate lab data for the CLAIREMONT soil series. This aggregation is based on all pedons with a current taxon name of CLAIREMONT, 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 CLAIREMONT 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.

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CLAIREMONT 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.

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 CLAIREMONT, 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. KS-2012-01-20-38 | Comanche County - June 1989

   Typical pattern of soils and parent material in the Obaro-Abilen association (Soil Survey of Comanche County, Kansas; 1989).

2. OK-2010-09-29-18 | Woods County - 2003

   Typical pattern of soils and underlying material in the Burford-Knoco-Vernon general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

3. OK-2010-09-29-20 | Woods County - 2003

   Typical pattern of soils and underlying material in the Quinlan-Woodward-Deepwood general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

4. OK-2012-02-16-41 | Harmon County - September 1984

   Typical pattern of soils and underlying material in the Tipton-Westview-Altus map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

5. TX-2012-03-21-47 | McCulloch County - November 1974

   Pattern of soils in Pedernales-Sagerton-Clairemont association (Soil Survey of McCulloch County, TX; 1974).

6. TX-2012-03-21-71 | Shackelford County - February 1990

   Typical pattern of soils and parent material in the Clairemont-Grandfield-Clearfork map unit (Soil Survey of Shackelford County, TX; 1990).

7. TX-2012-03-21-84 | Stephens County - May 1994

   Typical pattern of soils and parent material in the Clearfork-Clairemont general soil map unit (Soil Survey of Stephens County, TX; 1994).

Map Units

Map units containing CLAIREMONT 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
Clairemont soils, channeled, frequently flooded	5314	26747	1382468	2wrw3	ks007	1973	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	5312	11601	1382467	2wrvy	ks007	1973	1:24000
Quinlan-Clairemont complex, 0 to 50 percent slopes	5451	10004	1382517	1hdmb	ks007	1973	1:24000
Clairemont soils, saline, channeled, frequently flooded	5316	2344	1382469	2wrw4	ks007	1973	1:24000
Clairemont loam, channeled, frequently flooded	5310	1144	1382466	2wrw8	ks007	1973	1:24000
Clairemont loam, channeled, frequently flooded	5310	4216	1381249	2wrw8	ks033	1987	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	5312	3459	1381250	2wrvy	ks033	1987	1:24000
Clairemont soils, saline, channeled, frequently flooded	5316	639	1382675	2wrw4	ks077	1965	1:24000
Clairemont soils, channeled, frequently flooded	5314	10	1380497	2wrw3	ks097	1983	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	8	9794	381708	2wrvy	ok009	1978	1:24000
Clairemont silt loam, 0 to 1 percent slopes, frequently flooded	9	3434	381709	2wrw1	ok009	1978	1:24000
Vernon-Clairemont frequently flooded complex, 0 to 12 percent slopes	Bk	16381	382165	2t025	ok031	1965	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	Cc	27742	382312	2wrvy	ok039	1973	1:24000
Woodward-Clairemont complex, 0 to 12 percent slopes	Wt	7565	382349	2w5q2	ok039	1973	1:24000
Clairemont silt loam, 0 to 1 percent slopes, frequently flooded	Cf	1990	382314	2wrw1	ok039	1973	1:24000
Clairemont silt loam, saline, 0 to 1 percent slopes, occasionally flooded	Ce	1213	382313	dttp	ok039	1973	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	12	1763	975443	2s7n7	ok057	1982	1:24000
Clairemont and Mangum soils, 0 to 1 percent slopes, frequently flooded	Cm	25389	383442	dw03	ok075	1973	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	No	17754	384758	2wrvy	ok129	1961	1:24000
Clairemont silty clay loam, 0 to 1 percent slopes, channeled, frequently flooded	Ca	19863	384938	dxkc	ok141	1968	1:24000
Clairemont silty clay loam, saline, 0 to 1 percent slopes, frequently flooded	Ce	6746	384939	dxkd	ok141	1968	1:24000
Wheatwood-Clairemont complex, 0 to 1 percent slopes, occasionally flooded	At	6386	384935	dxk8	ok141	1968	1:24000
Vernon-Clairemont frequently flooded complex, 0 to 12 percent slopes	Vn	4159	384987	2t025	ok141	1968	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	9	27309	385047	2wrvy	ok149	1976	1:24000
Woodward-Clairemont complex, 0 to 12 percent slopes	53	9987	385040	2w5q2	ok149	1976	1:24000
Clairemont silt loam, 0 to 1 percent slopes, frequently flooded	10	5676	384993	2wrw1	ok149	1976	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	ClgA	8167	385169	2wrvy	ok151	1995	1:24000
Clairemont silt loam, 0 to 1 percent slopes, frequently flooded	ClfA	931	385168	2wrw1	ok151	1995	1:24000
Clairemont silt loam, moist, 0 to 1 percent slopes, occasionally flooded	Cm	38530	362702	2s7n9	tx023	1971	1:24000
Clairemont silty clay loam, dry, 0 to 1 percent slopes, occasionally flooded	Cm	989	363274	2y85b	tx045	1972	1:20000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	3880	363967	2s7n7	tx081	1968	1:24000
Clairemont silt loam, 0 to 1 percent slopes, rarely flooded	Cm	1565	364008	2s7n8	tx083	1968	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	1777	365168	2s7n7	tx129	1975	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	2181	378327	2s7n7	tx169	1965	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	544	367909	dbv1	tx233	1972	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	5452	368475	2s7n7	tx263	1968	1:31680
Clairemont silt loam, 0 to 1 percent slopes, frequently flooded	6	12987	368751	2wrw1	tx275	1975	1:24000
Clairemont silt loam, moist, 0 to 1 percent slopes, occasionally flooded	5	3755	368750	2s7n9	tx275	1975	1:24000
Clairemont silt loam, 0 to 1 percent slopes, rarely flooded	Cn	4308	369938	2s7n8	tx307	1970	1:24000
Clairemont loam, saline, frequently flooded	Mm	1835	370343	dfck	tx317	1968	1:24000
Clairemont clay loam, slightly saline, rarely flooded	St	249	370356	dfcz	tx317	1968	1:24000
Clairemont silty clay loam, 0 to 2 percent slopes, occasionally flooded	Cc	11371	3124137	dg5b	tx359	1978	1:24000
Clairemont silty clay loam, 0 to 2 percent slopes, occasionally flooded	Cc	11046	3124214	dgd9	tx375	1974	1:24000
Clairemont and Mangum soils, 0 to 1 percent slopes, frequently flooded	Cm	6177	3124215	dgdb	tx375	1974	1:24000
Clairemont silt loam, frequently flooded	Cm	942	371941	dh13	tx411	1980	1:24000
Clairemont silty clay loam, moist, 0 to 1 percent slopes, occasionally flooded	Cm	3199	372054	2y85c	tx417	1985	1:24000
Clairemont silty clay loam, 0 to 2 percent slopes, frequently flooded, channeled	Cn	2898	372055	2y85d	tx417	1985	1:24000
Clairemont silty clay loam, 0 to 2 percent slopes, frequently flooded, channeled	Cn	3191	372175	2y85d	tx429	1985	1:24000
Clairemont silty clay loam, moist, 0 to 1 percent slopes, occasionally flooded	Cm	2310	372174	2y85c	tx429	1985	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded	Ca	3058	372263	2s7n7	tx433	1970	1:24000
Clairemont silty clay loam, 0 to 1 percent slopes, occasionally flooded	Ca	7856	391507	2y85g	tx441	1971	1:20000
Clairemont-Urban land complex, 0 to 1 percent slopes, occasionally flooded	Cn	2976	391508	2y85h	tx441	1971	1:20000
Clairemont silt loam, moist, 0 to 2 percent slopes, occasionally flooded	Cm	11827	372682	2z16c	tx447	1991	1:24000
Clairemont silt loam, 0 to 1 percent slopes, occasionally flooded, cool	Cm	1614	373285	2wrvy	tx483	1970	1:24000
Clairemont silt loam, moist, 0 to 1 percent slopes, occasionally flooded	Ca	14791	373338	2s7n9	tx485	1972	1:20000
Clairemont-Urban land complex	Cb	1145	373339	djh6	tx485	1972	1:20000
Clairemont soils, wet	Cc	456	373340	djh7	tx485	1972	1:20000
Clairemont clay loam, 0 to 1 percent slopes, frequently flooded	Lo	32730	373423	2z16d	tx487	1960	1:20000
Clairemont clay loam, 0 to 1 percent slopes, occasionally flooded	Nc	15141	373436	2rhnm	tx487	1960	1:20000
Clairemont silt loam, moist, 0 to 1 percent slopes, occasionally flooded	No	1312	373437	2s7n9	tx487	1960	1:20000
Clairemont soils, 0 to 1 percent slopes, frequently flooded	24	5264	390998	f3vv	tx602	1975	1:24000

Map of Series Extent

Approximate geographic distribution of the CLAIREMONT 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).