Soil Data Explorer - CLAYBURN

Official Series Description

Lab Data Summary

Aggregate lab data for the CLAYBURN soil series. This aggregation is based on all pedons with a current taxon name of CLAYBURN, 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 CLAYBURN 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
48A	86P0852	86CO067003	Clayburn	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.5013885,-107.7388916
48A	13N57550	S2012UT037001	Clayburn	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4816611,-109.2916306

Water Balance

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

Competing Series

Soil series competing with CLAYBURN 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 CLAYBURN 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 CLAYBURN 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).

Soil series sharing subgroup-level classification with CLAYBURN, 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

No block diagrams are available.

Map Units

Map units containing CLAYBURN 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
Clayburn-Gelkie-Bowen families complex, 2 to 30 percent slopes	815G	1815	500989	jt9y	co634		1:24000
Clayburn loam, 6 to 15 percent slopes	16	38	3177083	jq19	co645		1:24000
Clayburn-Florey families, complex, 3 to 15 percent slopes	3	12322	509327	k2zx	co647		1:24000
Clayburn-Florey families, complex, 15 to 40 percent slopes	4	4756	509338	k308	co647		1:24000
Clayburn loam, warm, 3 to 25 percent slopes	33	538	3106839	jpcz	co648		1:24000
Clayburn-Foidel complex, 25 to 55 percent slopes, very bouldery	34	95	3106840	jpd0	co648		1:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery	221	67	3106836	jpch	co648		1:24000
Clayburn loam, 8 to 35 percent slopes	511	5	3106854	2nf41	co648		1:24000
Clayburn loam, 15 to 25 percent slopes	17	5288	497839	jq1b	co649	1977	1:24000
Clayburn loam, 25 to 50 percent slopes	18	3105	497840	jq1c	co649	1977	1:24000
Clayburn loam, 6 to 15 percent slopes	16	3105	497838	jq19	co649	1977	1:24000
Clayburn loam, 2 to 6 percent slopes	15	1277	497837	jq18	co649	1977	1:24000
Clayburn, warm-Booneville-Needleton family complex, 25 to 65 percent slopes	121	24164	509468	k34g	co660	1994	1:24000
Clayburn-Quander-Guero complex, 5 to 30 percent slopes	122	15788	509470	k34j	co660	1994	1:24000
Clayburn-Quander-Guero complex, 30 to 65 percent slopes	123	2126	509471	k34k	co660	1994	1:24000
Cochetopa-Clayburn complex, 12 to 40 percent slopes	125	1085	509473	k34m	co660	1994	1:24000
Clayburn-Quander-Guero complex, 5 to 30 percent slopes	122	1	2927467	k34j	co662	1968	1:24000
Booneville-Clayburn association, 5 to 40 percent slopes	107	4195	2453660	2nc7b	co664	1987	1:24000
Clayburn loam, 3 to 12 percent slopes	19	4617	58277	1ymx	co669	1982	1:24000
Clayburn cobbly loam, 6 to 25 percent slopes	20	2640	58279	1ymz	co669	1982	1:24000
Clayburn-Hourglass complex, 5 to 25 percent slopes	51	4240	737687	srmc	co672	2003	1:24000
Clayburn-Hourglass complex, 15 to 30 percent slopes	163	1921	507104	k0p6	co672	2003	1:24000
Clayburn-Heisspitz complex, 30 to 60 percent slopes	390	1612	507166	k0r6	co672	2003	1:24000
Ryman-Clayburn complex, 2 to 15 percent slopes	734	917	507253	k0v0	co672	2003	1:24000
Clayburn-Heisspitz complex, 15 to 30 percent slopes	394	732	507170	k0rb	co672	2003	1:24000
Clayburn cobbly loam, 6 to 25 percent slopes	920	169	507294	k0wb	co672	2003	1:24000
Clayburn loam, 3 to 12 percent slopes	919	138	507293	k0w9	co672	2003	1:24000
Clayburn-Jerry, moist-Bachus complex, 3 to 25 percent slopes	55	21487	506749	k09r	co680	1970	1:31680
Clayburn-Jerry, moist-Bachus complex, 25 to 65 percent slopes	55E	1682	506661	k06x	co680	1970	1:31680
Cochetopa-Clayburn complex, 12 to 40 percent slopes	24	11211	496684	jnv2	co682	1986	1:24000
Hapgood-Adel-Clayburn loams, 5 to 25 percent slopes	53	14044	496896	jp1x	co684	1984	1:24000
Clayburn loam, 3 to 15 percent slopes	15	10549	496854	jp0k	co684	1984	1:24000
Hapgood-Adel-Clayburn loams, 25 to 65 percent slopes	54	7632	496897	jp1y	co684	1984	1:24000
Lespate-Clayburn, cool loams, 3 to 25 percent slopes	69	6008	496913	jp2g	co684	1984	1:24000
Clayburn-Mayoworth-Adel loams, 5 to 30 percent slopes	16	5680	496855	jp0l	co684	1984	1:24000
Quander-Clayburn-Adel loams, 3 to 25 percent slopes	99	4233	496946	jp3j	co684	1984	1:24000
Hapgood-Clayburn-Cochetopa loams, 20 to 65 percent slopes	55	4172	496898	jp1z	co684	1984	1:24000
Cochetopa-Clayburn-Emerald loams, 5 to 25 percent slopes	21	4092	496861	jp0s	co684	1984	1:24000
Cochetopa-Clayburn-Emerald loams, 25 to 65 percent slopes	22	3206	496862	jp0t	co684	1984	1:24000
Winnemucca-Clayburn loams, 8 to 40 percent slopes	124	2911	496849	jp0d	co684	1984	1:24000
Winnemucca-Clayburn loams, 8 to 25 percent slopes	99	12188	497055	jp71	co685	1979	1:24000
Clayburn loam, 3 to 15 percent slopes	20	1738	496969	jp48	co685	1979	1:24000
Youga-Gelkie-Clayburn, warm complex, 25 to 45 percent slopes, extremely bouldery	221	6538	497193	jpch	co686	1992	1:31680
Clayburn-Foidel complex, 25 to 55 percent slopes, very bouldery	34	4754	497209	jpd0	co686	1992	1:31680
Clayburn loam, warm, 3 to 25 percent slopes	33	4095	497208	jpcz	co686	1992	1:31680
Clayburn-Youga, moist complex, 15 to 45 percent slopes	35	4086	497210	jpd1	co686	1992	1:31680
Heathcoat-Clayburn complex, 5 to 35 percent slopes, very stony	97	3236	497278	jpg7	co686	1992	1:31680
Clayburn family-Wiskisprings family, frequently flooded, complex, 0 to 5 percent slopes	899	275	3173271	2x03g	id712	2008	1:24000
Clayburn family-Wiskisprings family, frequently flooded, complex, 0 to 5 percent slopes	899	4104	2984162	2x03g	id713		1:24000
Clayburn family-Winnemucca, extremely stony surface, complex, 2 to 15 percent slopes	846	1131	2733456	2slrt	id713		1:24000
Clayburn family-Ezbin-Parkay complex, 5 to 30 percent slopes	939	584	2963848	2wv1p	id713		1:24000
Hymas-Northwater-Clayburn association, 20 to 60 percent slopes	46	4922	485640	j9bt	id715	1994	1:24000
Clayburn family-Wiskisprings family, frequently flooded, complex, 0 to 5 percent slopes	899	51	3163461	2x03g	id716		1:24000
Quazar-Clayburn-Agneston families complex, 20 to 55 percent slopes	3404	6464	2376439	2krwb	id758	1998	1:24000
Clayburn-Swede families complex, 50 to 90 percent slopes	3475	2819	2376436	2krw7	id758	1998	1:24000
Clayburn-Swede families complex, 15 to 50 percent slopes	3340	1657	2376440	2krwc	id758	1998	1:24000
Clayburn-Heath families complex, 15 to 50 percent slopes	3225	991	2376443	2krwg	id758	1998	1:24000
Clayburn family-Wander-Crubas, occasionally poned, complex, 0 to 40 percent slopes	CaE	2081	2862032	2vd1d	nm672		1:24000
Avaya-Clayburn-Curtis Creek complex, 2 to 15 percent slopes	QuA	3597	2503726	2pw02	ut013		1:24000
Clayburn loam, 15 to 25 percent slopes	CBD	3090	504208	jxns	ut622	1967	1:24000
Clayburn loam, 6 to 15 percent slopes	CBC	2650	504207	jxnr	ut622	1967	1:24000
Clayburn-Flygare association, hilly	CCD	1288	504209	jxnt	ut622	1967	1:24000
Clayburn soils, 25 to 40 percent slopes	CDE	987	504210	jxnv	ut622	1967	1:24000
Clayburn loam, 3 to 6 percent slopes	CBB	404	504206	jxnq	ut622	1967	1:24000
Clayburn-Faim families complex, 5 to 40 percent slopes	561		3312885	30gwz	ut645		1:24000
Elwood-Clayburn-Castino family complex, 15 to 50 percent slopes	45		3312880	30gwt	ut645		1:24000
Faim-Clayburn-Geertsen families complex, 3 to 20 percent slopes	412		3312874	30gwm	ut645		1:24000
Faim-Clayburn-Castino families complex, 5 to 30 percent slopes	600		3314857	30hlr	ut645		1:24000
Faim-Clayburn families complex, 3 to 20 percent slopes	411		3312872	30gwk	ut645		1:24000
Clayburn-Behanin-Faim families complex, 5 to 30 percent slopes	561B		3312887	30gx1	ut645		1:24000
Skylick-Adel-Clayburn families complex, 15 to 60 percent slopes	mt48	15918	3314840	30hl3	ut645		1:24000
Wrenman-Geertsen-Clayburn families complex, 20 to 60 percent slopes	109A	5151	3243268	2zscj	ut645		1:24000
Clayburn-Faim-Wesdy families complex, 20 to 50 percent slopes	110A	3370	3243273	2zscn	ut645		1:24000
Clayburn family-Menbar family association, 1 to 15 percent slopes	241	2840	512442	k67d	ut646		1:24000
Clayburn family-Venable family, occasionally flooded association, 0 to 15 percent slopes	127		625214	nzl6	ut649		1:24000
Clayburn-Faim families association, 5 to 20 percent slopes	126		625215	nzl7	ut649		1:24000
Condie-Clayburn-Behanin families complex, 5 to 40 percent slopes	134		581657	mj84	ut649		1:24000
Clayburn-Bachus-Inchau association	12	28043	152055	5370	wy043	1976	1:24000
Clayburn-Wallrock association	13	5834	152056	5371	wy043	1976	1:24000
Clayburn-Bachus-Inchau association	12	505	816473	wdlv	wy619	1971	1:24000
Clayburn-Wallrock association	13	81	816474	wdlw	wy619	1971	1:24000
Clayburn family-Ezbin-Parkay complex, 5 to 30 percent slopes	939	96	3083482	2wv1p	wy623	1971	1:20000
Clayburn family-Winnemucca, extremely stony surface, complex, 2 to 15 percent slopes	846	46	3083462	2slrt	wy623	1971	1:20000
Clayburn family-Wiskisprings family, frequently flooded, complex, 0 to 5 percent slopes	899	46	3083476	2x03g	wy623	1971	1:20000
Kezar-Irson-Clayburn association, hilly	211	30272	502311	jvpl	wy625	1985	1:24000
Bachus-Clayburn association, undulating	115	8209	502193	jvks	wy625	1985	1:24000
Inchau-Clayburn-Chittum complex, 4 to 20 percent slopes	202	6818	502293	jvp0	wy625	1985	1:24000
Clayburn-Moslander association, gently sloping	156	3827	502244	jvmf	wy625	1985	1:24000
Clayburn-Ratiopeak complex, 12 to 45 percent slopes, landsides	635		2959845	2wsx5	wy630		1:24000
Crownmountain-Clayburn complex, 8 to 25 percent slopes	633		3005436	2x7fk	wy630		1:24000
Clayburn-Roxal complex, 8 to 40 percent slopes	501	16776	2421021	2m88g	wy630		1:24000
Clayburn loam, 8 to 35 percent slopes	511	16734	2455480	2nf41	wy630		1:24000
Clayburn-Venable complex, 3 to 30 percent slopes	627	3540	2531444	2qmgc	wy630		1:24000
Clayburn-Mult complex, 5 to 25 percent slopes	618	439	2516057	2qftx	wy630		1:24000
Sedimentary Sideslopes, Big Sagebrush-Tall Forb Complex	3622	3996	151862	530s	wy662	1998	1:24000
Sedimentary Residual Sideslopes, Big Sagebrush-Grassland Complex	3624	3634	151864	530v	wy662	1998	1:24000
Sedimentary Sideslopes, Big Sagebrush-Silver Sagebrush Complex	3621	2022	151861	530r	wy662	1998	1:24000
Buffork-Tongue River association *	5	2192	153300	54j5	wy666	1978	1:24000
Buffork-Tongue River-Clayburn association *	6	900	153311	54jj	wy666	1978	1:24000
Clayburn-Paulson-Beavet complex, 2 to 15 percent slopes	8102		3169685	2y0yb	wy723		1:24000

Map of Series Extent

Approximate geographic distribution of the CLAYBURN 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).