Soil Data Explorer - DOUGHERTY

Official Series Description

Lab Data Summary

Aggregate lab data for the DOUGHERTY soil series. This aggregation is based on all pedons with a current taxon name of DOUGHERTY, 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 DOUGHERTY 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
118B	73-OK-32-2	73-OK063-32-2	Dougherty	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0774889,-96.0825389
80A	40A4703	56OK119001	Dougherty	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.0933342,-96.7664079
80A	73-OK-57-13	73-OK113-57-13	Dougherty	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.4825528,-96.9436944
80A	74-OK-14-1	74-OK027-14-1	Dougherty	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0731167,-97.3299194
84A	93P0400	92OK119001	Dougherty	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.9859161,-97.1850357
84B	76-OK-48-3	76-OK095-48-3	Dougherty	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.8749333,-96.7422667

Water Balance

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

Geomorphic description summaries for the DOUGHERTY 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 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with DOUGHERTY, 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. OK-2010-09-29-04 | Logan County - 2006

   Typical pattern of soils and underlying material in the Dougherty-Konawa-Derby general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

2. OK-2012-02-16-13 | Cleveland County - April 1987

   Typical pattern of soils and underlying material in the Norge-Teller-Vanoss map unit and Asher-Keokuk-Canadian map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

3. OK-2012-02-16-50 | Hughes County - December 1968

   Typical pattern of soils in associations 4 and 5 (Soil Survey of Hughes County, Oklahoma; December 1968).

4. OK-2012-02-17-05 | Logan County - June 1960

   Soils of central and western Logan County on recent alluvium and on loams and sands of Quaternary age. Red beds are exposed in the upper right corner (Soil Survey of Logan County, Oklahoma; June 1960).

5. OK-2012-02-17-06 | Love County - September 1966

   A diagram showing typical relief in the southern part of Love County and the relative position of the soils in associations 1, 3, and 6 (Soil Survey of Love County, Oklahoma; September 1966).

6. OK-2012-02-17-08 | Love County - September 1966

   Diagram showing typical relief in the northwestern corner of the county and the relative positions of the soils in association 4 (Soil Survey of Love County, Oklahoma; September 1966).

7. OK-2012-02-17-23 | Pawnee County - March 1959

   Prairie and forest soils formed in recent alluvium, and in adjoining areas of silty and sandy mantle material (Soil Survey of Pawnee County, Oklahoma; March 1959).

8. OK-2012-02-17-30 | Payne County - April 1987

   Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).

9. OK-2012-02-17-31 | Payne County - April 1987

   Typical pattern of soils and underlying material in the Konawa-Dougherty-Derby map unit (Soil Survey of Payne Oklahoma; April 1987).

10. OK-2012-02-17-32 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 1, 2, 3, and 7 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

Map Units

Map units containing DOUGHERTY 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
Dougherty fine sand, 0 to 3 percent slopes	DoB	4482	381421	dswx	ok003	1971	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	DuD	31083	381882	2tq7w	ok015	1967	1:24000
Dougherty-Konawa loamy fine sands association and 0 to 3 percent slopes	DoB	11666	381881	30g72	ok015	1967	1:24000
Dougherty-Konawa complex, 3 to 8 percent slopes	11	779	382084	dtl9	ok027	1984	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	DoED	232	1380055	2tq7w	ok031	1965	1:24000
Dougherty and Stidham soils, 3 to 8 percent slopes	Dk	2875	382282	dtsp	ok037	1952	1:24000
Dougherty and Stidham soils, 0 to 3 percent slopes	Dl	1310	382283	dtsq	ok037	1952	1:24000
Dougherty-Eufaula complex, 8 to 20 percent slopes	DoEF	251	2516364	1t7xb	ok037	1952	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	DouD	67	2516365	2tq7s	ok037	1952	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	7	11609	382690	2tq7w	ok051	1975	1:24000
Dougherty fine sand, 0 to 3 percent slopes	6	1041	382682	dv6l	ok051	1975	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	DoB	5819	383224	2tq7r	ok067	1967	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	DoC	903	383225	2tq7s	ok067	1967	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	13	3763	383275	dvtq	ok069	1976	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	DxC	3069	383327	2tq7w	ok071	1965	1:24000
Dougherty-Eufaula complex, 0 to 3 percent slopes	DxB	687	383326	2tq7x	ok071	1965	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	DeC	21423	383390	2tq7w	ok073	1960	1:24000
Dougherty-Eufaula complex, 0 to 3 percent slopes	DeB	20614	383389	2tq7x	ok073	1960	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	DuD	8595	383510	2tq7s	ok081	1966	1:24000
Eufaula-Dougherty complex, 5 to 12 percent slopes	EdE	5347	383511	dw2b	ok081	1966	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	DouB	5163	383610	2tq7r	ok083	1994	1:12000
Dougherty loamy fine sand, 3 to 8 percent slopes	DouD	4838	383611	2tq7s	ok083	1994	1:12000
Dougherty and Konsil soils, 5 to 8 percent slopes	DoD	23080	383708	dw8p	ok085	1963	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	DoB	17637	383706	dw8m	ok085	1963	1:24000
Dougherty and Konsil soils, 3 to 5 percent slopes	DoC	5389	383707	dw8n	ok085	1963	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	6	8077	383908	dwh4	ok095	1978	1:24000
Derby-Urban land-Dougherty complex, 0 to 15 percent slopes	DUDE	2222	384282	dww6	ok109	1996	1:12000
Derby-Dougherty complex, 0 to 15 percent slopes	DeDE	1703	384285	dww9	ok109	1996	1:12000
Dougherty loamy fine sand, 3 to 8 percent slopes	20	10015	623415	2tq7s	ok113	1975	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	19	8463	623414	2tq7r	ok113	1975	1:24000
Eufaula-Dougherty complex, 0 to 3 percent slopes	22	5170	623417	nxq7	ok113	1975	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	DouD	2176	1423155	2tq7s	ok117	2007	1:24000
Dougherty-Eufaula complex, 8 to 20 percent slopes	DoEF	1418	1675901	1t7xb	ok117	2007	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	DouB	856	1423154	2tq7r	ok117	2007	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	15	4889	384510	2tq7s	ok119	1983	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	95	2433	384593	2tq7r	ok119	1983	1:24000
Dougherty-Eufaula complex, 8 to 20 percent slopes	DoEF	2123	1907679	22131	ok119	1983	1:24000
Dougherty-Eufaula loamy fine sands, 8 to 20 percent slopes	DrE	2834	384616	dx6z	ok123	1967	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	DoD	2020	384615	2tq7s	ok123	1967	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	DoB	1298	384614	2tq7r	ok123	1967	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	11	2343	384670	2tq7s	ok125	1975	1:24000
Dougherty loamy fine sand, 0 to 3 percent slopes	10	818	384669	2tq7r	ok125	1975	1:24000
Eufaula-Dougherty complex, 5 to 15 percent slopes	11	7101	384796	dxds	ok133	1976	1:24000
Eufaula-Dougherty complex, 0 to 5 percent slopes	10	1516	384795	dxdr	ok133	1976	1:24000
Dougherty loamy fine sand, 3 to 8 percent slopes	8	1268	384843	2tq7s	ok133	1976	1:24000
Dougherty and Konawa soils, 3 to 8 percent slopes	DoC	4656	384858	dxgs	ok137	1960	1:24000
Dougherty-Konawa loamy fine sands association and 0 to 3 percent slopes	DoB	1464	384857	30g72	ok137	1960	1:24000
Konawa and Dougherty soils, 1 to 5 percent slopes, eroded	DuB2	354	384859	dxgt	ok137	1960	1:24000
Dougherty-Eufaula complex, 3 to 8 percent slopes	23	982	385007	2tq7w	ok149	1976	1:24000

Map of Series Extent

Approximate geographic distribution of the DOUGHERTY 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).