Soil Data Explorer - SHROUTS

Official Series Description

Lab Data Summary

Aggregate lab data for the SHROUTS soil series. This aggregation is based on all pedons with a current taxon name of SHROUTS, 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 SHROUTS 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	85KY-069-009	85KY-069-009	Shrouts	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4156075,-83.6104431
n/a	86KY-069-011	86KY-069-011	Shrouts	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	99KY-011-006	99KY-011-006	Shrouts	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	99KY-011-011	99KY-011-011	Shrouts	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	99KY-151-UK4	99KY-151-UK4	Shrouts	2	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 SHROUTS 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 SHROUTS 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 SHROUTS 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 SHROUTS 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 flats position figure.

Competing Series

Soil series competing with SHROUTS 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 SHROUTS 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 SHROUTS 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 SHROUTS, 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-2010-09-03-06 | Garrard and Lincoln Counties - 2006

   Typical pattern of soils and underlying material in the Shrouts-Beasley-Garlin general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

2. KY-2010-09-03-21 | Lewis County - 2004

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

3. KY-2010-09-03-28 | Estill and Lee Counties - 2007

   Typical pattern of soils and their relationship to geology and topography in the Shrouts-Woolper-Allegheny general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

4. KY-2012-01-26-17 | Bath County - September 1963

   Typical landscape in the knobby areas of the county showing the topography, the relationship of some of the principal soils, and the parent rocks (Soil Survey of Bath County, Kentucky; September 1963).

5. KY-2012-01-26-18 | Bath County - September 1963

   Typical landscape in the southern part of association 4 showing the topography, the relationship of some of the principal soils, and the parent rocks (Soil Survey of Bath County, Kentucky; September 1963).

6. KY-2012-01-26-25 | Bath County - September 1963

   Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

7. KY-2012-01-27-44 | Clark County - 1964

   Major soil series in soil association 11, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

8. KY-2012-01-27-45 | Clark County - 1964

   Geolgic cross section of Clark County, showing some of the principal soils and their relation to the rock formations (Soil Survey of Clark County, Kentucky; 1964).

9. KY-2012-01-27-59 | Estill and Lee Counties - August 1974

   Pattern of soils and underlying material in the Fairmount-Shrouts-Allegheny association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

10. KY-2012-01-27-60 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Colyer-Shrouts-Allegheny association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

11. KY-2012-01-27-73 | Fleming County - October 1993

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

12. KY-2012-02-01-40 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Jessietown-Muse-Rohan general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

13. KY-2012-02-01-63 | Washington County - August 1986

    Typical pattern of soils and underlying material in the Fairmount-Shrouts-Faywood map unit (Soil Survey of Washington County, Kentucky; August 1986).

Map Units

Map units containing SHROUTS 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
Shrouts-Beasley complex, 20 to 30 percent slopes, eroded	StE2	6432	1727507	1vzm1	ky011	2006	1:12000
Shrouts-Beasley-Rock outcrop complex, 6 to 20 percent slopes, eroded	SrD2	5598	1727506	1vzm0	ky011	2006	1:12000
Beasley-Shrouts silt loams, 12 to 20 percent slopes, eroded	BeD2	3595	1727505	1vzlz	ky011	2006	1:12000
Fleming-Shrouts complex, 12 to 20 percent slopes (beasley-shrouts)	FpD	2156	550147	lggp	ky049	1962	1:15840
Fleming-Shrouts complex, 12 to 20 percent slopes, severely eroded (beasley-shrouts)	FpD3	1707	550148	lggq	ky049	1962	1:15840
Fleming-Shrouts complex, 6 to 12 percent slopes (beasley-shrouts)	FpC	554	550146	lggn	ky049	1962	1:15840
Fleming-Shrouts complex, 20 to 30 percent slopes, severely eroded (beasley-shrouts)	FpE3	229	550150	lggs	ky049	1962	1:15840
Fleming-Shrouts complex, 20 to 30 percent slopes (beasley-shrouts)	FpE	226	550149	lggr	ky049	1962	1:15840
Beasley-Shrouts complex, rocky, 12 to 30 percent slopes, severely eroded	BhE3	14843	552694	lk3v	ky069	1989	1:20000
Muse-Shrouts complex, 6 to 20 percent slopes, severely eroded	MtD3	4084	552726	lk4w	ky069	1989	1:20000
Shrouts silty clay, 6 to 12 percent slopes, severely eroded	StC3	3789	552741	lk5c	ky069	1989	1:20000
Shrouts silty clay, 12 to 20 percent slopes, severely eroded	StD3	1368	552742	lk5d	ky069	1989	1:20000
Shrouts silty clay loam, 2 to 6 percent slopes	SsB	788	552740	lk5b	ky069	1989	1:20000
Shrouts silt loam, 12 to 25 percent slopes, severely eroded, very rocky	ShD3	9344	1533064	1ng8p	ky111	2005	1:12000
Faywood-Shrouts-Beasley complex, 25 to 50 percent slopes	FsF	5299	1533084	1ng9b	ky111	2005	1:12000
Shrouts silt loam, 6 to 12 percent slopes, severely eroded	ShC3	3495	1533063	1ng8n	ky111	2005	1:12000
Urban land-Alfic Udarents-Shrouts complex, 12 to 25 percent slopes	UwD	764	1536455	1nkt2	ky111	2005	1:12000
Urban land-Alfic Udarents-Shrouts complex, 0 to 12 percent slopes	UwC	227	1536454	1nkt1	ky111	2005	1:12000
Beasley-Shrouts complex, 12 to 30 percent slopes, very rocky, eroded	BhE2	13771	550276	lglv	ky135	1998	1:20000
Shrouts silty clay loam, 12 to 30 percent slopes, severely eroded	SrD3	12018	550324	lgnd	ky135	1998	1:20000
Shrouts-Beasley complex, 6 to 12 percent slopes, eroded	SsC2	1751	550325	lgnf	ky135	1998	1:20000
Covedale-Shrouts complex, 12 to 25 percent slopes, eroded	CsD2	1618	550291	lgmb	ky135	1998	1:20000
Shrouts silty clay loam, 2 to 6 percent slopes	SrB	103	550323	lgnc	ky135	1998	1:20000
Otway silty clay, 12 to 30 percent slopes (shrouts)	OtE	5648	1397901	1hxml	ky151	1968	1:20000
Shrouts silty clay loam, 12 to 30 percent slopes	SrE	3690	1397917	1hxn3	ky151	1968	1:20000
Shrouts clay, 6 to 30 percent slopes, severely eroded	SuE3	2886	1397918	1hxn4	ky151	1968	1:20000
Otway silty clay, 30 to 50 percent slopes (shrouts)	OtF	2874	1397902	1hxmm	ky151	1968	1:20000
Otway silty clay, 6 to 12 percent slopes (shrouts)	OtC	1555	1397900	1hxmk	ky151	1968	1:20000
Shrouts silty clay loam, 6 to 12 percent slopes	SrC	220	1397916	1hxn2	ky151	1968	1:20000
Shrouts-Brassfield complex, 12 to 30 percent slopes, eroded, very rocky	SrE2	2820	552371	ljsf	ky155	1986	1:20000
Brassfield-Shrouts-Beasley complex, 12 to 35 percent slopes, eroded	BsE	10010	550513	lgvh	ky173	1983	1:20000
Shrouts-Otway complex, 12 to 30 percent slopes	SoE	5275	550002	lgb0	ky179	1967	1:15840
Shrouts-Otway complex, 6 to 12 percent slopes	SoC	1320	550001	lg9z	ky179	1967	1:15840
Faywood-Shrouts silty clay loams, very rocky, 12 to 30 percent slopes, severely eroded	FyE3	5545	551500	lhwb	ky229	1983	1:20000
Shrouts silt loam, rocky, 6 to 12 percent slopes, eroded	ShC2	3830	551516	lhwv	ky229	1983	1:20000
Shrouts silt loam, 2 to 6 percent slopes	ShB	730	551515	lhwt	ky229	1983	1:20000
Shrouts-Beasley-Woolper complex, 12 to 30 percent slopes, eroded	SkE2	7371	557801	lqfl	ky616	2004	1:24000
Brassfield-Shrouts-Woolper complex, 25 to 75 percent slopes, eroded, stony	BsF2	2936	557791	lqf8	ky616	2004	1:24000
Shrouts-Cynthiana complex, 12 to 25 percent slopes, severely eroded, rocky	SfD3	8266	552995	lkfk	ky618	1993	1:12000
Garlin-Shrouts complex, 12 to 25 percent slopes, eroded, rocky	GaD2	6617	552957	lkdb	ky618	1993	1:12000
Shrouts silty clay loam, 6 to 12 percent slopes, eroded	SeC2	5562	552994	lkfj	ky618	1993	1:12000
Garlin-Shrouts complex, 6 to 12 percent slopes, eroded	GaC2	4796	552956	lkd9	ky618	1993	1:12000
Faywood-Shrouts complex, 12 to 25 percent slopes, eroded, rocky	FoD2	3515	552951	lkd4	ky618	1993	1:12000
Shrouts-Garlin-Cynthiana complex, 25 to 50 percent slopes, severely eroded, very rocky	SgF3	2146	552996	lkfl	ky618	1993	1:12000
Faywood-Shrouts complex, 25 to 60 percent slopes, eroded, rocky	FoF2	1585	552952	lkd5	ky618	1993	1:12000
Shrouts-Woolper complex, 15 to 35 percent slopes	SeE	1943	550851	lh6d	ky634	1989	1:20000

Map of Series Extent

Approximate geographic distribution of the SHROUTS 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).