Soil Data Explorer - BLAIRTON

Official Series Description

Lab Data Summary

Aggregate lab data for the BLAIRTON soil series. This aggregation is based on all pedons with a current taxon name of BLAIRTON, 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 BLAIRTON 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
124	86KY-069-012	86KY-069-012	Blairton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4003296,-83.5232162
124	90KY-135-001	90KY-135-001	Blairton	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4522743,-83.4562683
147	65PA055007	1965PA055007	Blairton	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.9813889,-77.7477778
147	72PA041001	1972PA041001	Blairton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2158333,-77.4719444
147	72PA041002	1972PA041002	Blairton	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2072222,-77.4730556
147	88PA009013	1988PA009013	Blairton	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7958333,-78.4025
147	05N0349	S2004PA061005	Blairton	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.664917,-77.9037781

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLAIRTON 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 BLAIRTON 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 BLAIRTON 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 BLAIRTON 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 BLAIRTON 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 BLAIRTON 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 BLAIRTON 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 BLAIRTON, 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. KY-2010-09-03-17 | Lawrence and Martin Counties - 2005

   Typical pattern of soils, parent material, and topography in the Udorthents-Nelse-Allegheny and Shelocta-Hazleton-Blairton general soil map units. The Udorthents-Nelse-Allegheny general soil map unit is along the Tug and Lavista Forks of the Big Sandy River and their major tributaries, and the Shelocta-Hazleton-Blairton general soil map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

2. KY-2010-09-03-22 | Lewis County - 2004

   Typical pattern of soils and parent material in the Blairton-Berks-Brownsville general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

3. KY-2010-09-03-23 | Lewis County - 2004

   Typical pattern of soils and parent material in the Berks-Brownsville-Blairton general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

4. KY-2010-09-03-24 | Lewis County - 2004

   Typical pattern of soils and parent material in the Berks-Brownsville-Shelocta general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

5. KY-2012-01-27-74 | Fleming County - October 1993

   Typical pattern of soils and parent material in the Muse-Blairton-Brownsville soil map unit (Soil Survey of Fleming County, Kentucky; October 1993).

6. PA-2012-03-12-12 | Bedford County - 1998

   Typical pattern of soils and parent material in the Berks-Weikert-Blairton general soil map unit (Soil Survey of Bedford County, PA; 1998).

7. PA-2012-03-12-18 | Blair County - October 1981

   Typical pattern of soils and underlying material in the Berks-Brinkerton-Weikert association (Soil Survey of Blair County, PA; 1981).

8. PA-2012-03-13-17 | Cumberland and Perry Counties - April 1986

   Typical pattern of soils and underlying material in the Berks-Weikert-Bedington association (Soil Survey of Cumberland and Perry Counties, PA; 1986).

9. PA-2012-03-13-30 | Franklin County - August 1975

   Relationship of underlying material and topography in association 5 (Soil Survey of Franklin County, PA; 1975).

10. PA-2012-03-13-50 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Bedington unit (Soil Survey of Lancaster County, PA; 1985).

11. PA-2012-03-14-14 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Berks-Weikert soils (Soil Survey of Somerset County, PA; 1983).

Map Units

Map units containing BLAIRTON 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
Blairton-Cruze-Marrowbone complex, 12 to 25 percent slopes	BlD	18134	1884681	21855	ky063	2007	1:12000
Gilpin-Steinsburg-Blairton complex, 12 to 25 percent slopes	GtD	10638	1884684	21858	ky063	2007	1:12000
Marrowbone-Blairton-Matewan complex, 25 to 60 percent slopes, rocky	MaF	2589	1884682	21856	ky063	2007	1:12000
Gilpin-Blairton-Ramsey complex, 2 to 12 percent slopes	GbC	2197	1884683	21857	ky063	2007	1:12000
Blairton-Cruze-Marrowbone complex, 6 to 12 percent slopes	BlC	540	1884680	21854	ky063	2007	1:12000
Blairton silt loam, 12 to 30 percent slopes, eroded	BrE2	3870	552698	2xb0d	ky069	1989	1:20000
Blairton silt loam, 6 to 12 percent slopes, eroded	BrC2	3815	552697	2xb0c	ky069	1989	1:20000
Blairton silt loam, 2 to 6 percent slopes	BrB	331	552696	2xb0b	ky069	1989	1:20000
Blairton silt loam, 12 to 30 percent slopes, eroded	BrE2	13403	550281	2xb0d	ky135	1998	1:20000
Blairton silt loam, 6 to 12 percent slopes, eroded	BrC2	4478	550280	2xb0c	ky135	1998	1:20000
Blairton silt loam, 2 to 6 percent slopes	BrB	875	550279	2xb0b	ky135	1998	1:20000
Marrowbone-Blairton-Dekalb complex, 25 to 60 percent slopes, rocky	MaF	22141	550908	lh87	ky640	1996	1:24000
Blairton-Cruze-Marrowbone complex, 12 to 25 percent slopes	BlD	16756	550891	lh7p	ky640	1996	1:24000
Blairton-Cruze-Marrowbone complex, 6 to 12 percent slopes	BlC	729	550890	lh7n	ky640	1996	1:24000
Blairton silt loam, 8 to 15 percent slopes	BnC	2593	2401041	2llgy	md001	2009	1:12000
Blairton silt loam, 3 to 8 percent slopes	BnB	713	2401040	2llgx	md001	2009	1:12000
Blairton silt loam, 15 to 25 percent slopes	BnD	538	2401042	2llgz	md001	2009	1:12000
Blairton-Rarden-Gilpin association, rolling	BmC	7	1460516	1l0sf	oh079	1981	1:15840
Coolville-Blairton association, rolling	CpC	8657	537620	l1fl	oh131	1984	1:15840
Blairton-Rarden-Gilpin association, rolling	BdC	7864	537611	l1f9	oh131	1984	1:15840
Blairton channery silt loam, 8 to 15 percent slopes	BrC	10856	541771	l5rh	pa009	1989	1:24000
Blairton channery silt loam, 15 to 25 percent slopes	BrD	5638	541772	l5rj	pa009	1989	1:24000
Blairton channery silt loam, 3 to 8 percent slopes	BrB	3783	541770	l5rg	pa009	1989	1:24000
Blairton silt loam, 8 to 15 percent slopes	BoC	844	542328	l6bg	pa013	1978	1:20000
Blairton silt loam, 3 to 8 percent slopes	BoB	784	542327	l6bf	pa013	1978	1:20000
Blairton silt loam, 3 to 8 percent slopes	BmB	7360	541892	l5wd	pa021	1978	1:20000
Blairton silt loam, 8 to 15 percent slopes	BmC	2366	541893	l5wf	pa021	1978	1:20000
Blairton-Berks channery silt loams, 8 to 15 percent slopes	BpC	1622	541895	l5wh	pa021	1978	1:20000
Blairton very stony silt loam, 3 to 8 percent slopes	BnB	689	541894	l5wg	pa021	1978	1:20000
Blairton silt loam, 3 to 8 percent slopes	BpB	4134	693690	r8v3	pa041	1980	1:15840
Blairton channery silt loam, 3 to 8 percent slopes	BlB	5303	545080	l967	pa055	1999	1:24000
Blairton channery silt loam, 0 to 3 percent slopes	BlA	599	545079	l966	pa055	1999	1:24000
Blairton silt loam, 2 to 8 percent slopes	BoB	1080	541965	l5yr	pa061	1974	1:20000
Blairton silt loam, 8 to 15 percent slopes	BoC	613	541966	l5ys	pa061	1974	1:20000
Blairton silt loam, 3 to 10 percent slopes	Bm	1649	542722	l6r5	pa071	1982	1:15840
Blairton silt loam, 3 to 8 percent slopes	BpB	344	693915	r92c	pa099	1980	1:15840
Blairton channery silt loam, 3 to 8 percent slopes	BnB	2822	542065	l61z	pa111	1977	1:20000
Blairton channery silt loam, 8 to 15 percent slopes	BnC	521	542066	l620	pa111	1977	1:20000
Wharton-Blairton complex, 15 to 35 percent slopes	55D	552	834401	x085	va005	2003	1:24000
Wharton-Blairton complex, 8 to 15 percent slopes	55C	314	834400	x084	va005	2003	1:24000
Wharton-Blairton complex, 8 to 15 percent slopes	61C	524	1451426	1kqb6	va017	2005	1:24000
Wharton-Blairton complex, 15 to 35 percent slopes	61D	486	1451427	1kqb7	va017	2005	1:24000
Blairton-Wharton complex, 3 to 8 percent slopes	8B	255	1451425	1kqb5	va017	2005	1:24000
Blairton silt loam, 2 to 7 percent slopes	3B	7664	521118	kh88	va069	1983	1:15840
Blairton silt loam, 7 to 15 percent slopes	3C	2335	521119	kh89	va069	1983	1:15840
Wharton-Blairton complex, 15 to 35 percent slopes	58E	499	2512113	2q9jz	va091	2010	1:24000
Blairton-Wharton complex, 3 to 8 percent slopes	7B	316	2512026	2q7v6	va091	2010	1:24000
Wharton-Blairton complex, 8 to 15 percent slopes	58C	299	2512114	2q9k0	va091	2010	1:24000
Blairton silt loam, 7 to 15 percent slopes	4C	1137	520779	kgxb	va171	1988	1:15840
Blairton silt loam, 2 to 7 percent slopes	4B	868	520778	kgx9	va171	1988	1:15840
Blairton silt loam, 2 to 7 percent slopes	2B	1308	518838	kdwq	va187	1980	1:15840
Blairton silt loam, 7 to 15 percent slopes	2C	303	518839	kdwr	va187	1980	1:15840
Blairton-Urban land complex, 2 to 7 percent slopes	503B	110	3025548	2xd4z	va840	2017	1:12000
Blairton-Urban land complex, 7 to 15 percent slopes	503C	36	3025549	2xd50	va840	2017	1:12000
Blairton silt loam, 2 to 7 percent slopes	3B	17	3025637	2xr7q	va840	2017	1:12000
Blairton silt loam, 7 to 15 percent slopes	3C	1	3025638	2xr7r	va840	2017	1:12000
Blairton silt loam, 3 to 8 percent slopes	BoB	712	515376	k991	wv075	1992	1:24000

Map of Series Extent

Approximate geographic distribution of the BLAIRTON 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).