Soil Data Explorer - DUNNING

Official Series Description

Lab Data Summary

Aggregate lab data for the DUNNING soil series. This aggregation is based on all pedons with a current taxon name of DUNNING, 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 DUNNING 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
115B	M9205772	1992MO057072	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M9305907	1993MO059007	Dunning	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
116A	59ID06	1959AR06306	Dunning	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.8267,-91.7746
116A	M9709139	1997MO091220	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.7602417,-91.8683389
116A	M9809125	1998MO091183	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.7454056,-91.7730222
116A	M9815334	1998MO153065H	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6020806,-92.2915222
116B	M9116747	1991MO167225	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.5832056,-93.4714806
120A	16N0952	S2016KY047001	Dunning	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.074855,-87.399419
121	09KY-021-001	09KY021001	Dunning	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.6561127,-84.8836136
121	09KY-021-002	09KY021 Dunning-OSD	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.6494446,-84.8238907
147	63PA027008	1963PA027008	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.815,-77.6416667
147	63PA027009	1963PA027009	Dunning	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7805556,-77.7602778

Water Balance

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

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

Soil series sharing subgroup-level classification with DUNNING, 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-2010-09-10-07 | Butler and Edmonson Counties -

   Relationship of soils to topography and underlying material in the Zanesville-Lawrence-Sadler association (Soil Survey of Butler and Edmonson Counties, Kentucky).

2. KY-2012-01-26-02 | Adair County - April 1964

   Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

3. KY-2012-01-26-06 | Adair County - April 1964

   Geological cross section of Adair County showing the relationship of the soils to the underlying rocks (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

4. KY-2012-01-26-23 | Bath County - September 1963

   Typical landscape showing the relative position of the principal soils in a limestone valley in association 9 (Soil Survey of Bath County, Kentucky; September 1963).

5. 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).

6. KY-2012-01-27-36 | Clark County - 1964

   Major soil series in soil association 3, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

7. TN-2012-03-19-23 | Maury County - October 1959

   Sketch showing relative positions of soils in the Etowah-Huntington (local allvuium phosphatic phase)-Emory and Huntington-Lindside-Armour (terrace phases)-Egam assciations (Soil Survey of Maury County, TN; 1959).

8. TN-2012-03-19-41 | Williamson County - August 1964

   Major and minor soils and underlying parent materials in the Rockland-Talbott-Egam association (Soil Survey of Williamson County, TN; 1964).

Map Units

Map units containing DUNNING 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
Dunning silt loam, overwashed, 0 to 2 percent slopes	DuA	162	523318	kkk7	al015	1959	1:20000
Dunning silty clay	Dc	1000	329144	c1hk	al049	1953	1:20000
Dunning silty clay	Du	3076	329559	c1xy	al059	1962	1:15840
Dunning silty clay	Du	1384	522853	kk27	al071	1943	1:24000
Dunning silty clay	Dl	7305	330113	c2ht	al079	1950	1:20000
Dunning silty clay	Dw	2178	523120	kkbv	al089	1958	1:24000
Dunning silty clay	Dm	3747	331067	c3hl	al103	1949	1:15840
Dunning soils	Dn	51	128596	49t8	dc001	1975	1:12000
Dunning silty clay loam, rarely flooded	Du	134	1592397	1qg0n	ky001	2006	1:12000
Dunning soils	Du	1269	549050	lfb9	ky047	1977	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	705	550163	2zs5h	ky049	1962	1:15840
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	140	551812	2zs5h	ky097	1965	1:15840
Dunning silty clay, frequently flooded	Du	564	549311	lflq	ky139	1989	1:20000
Dunning silty clay loam	Du	2150	548703	ldz3	ky141	1972	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	1412	1397864	2zs5h	ky151	1968	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Du	110	549947	2wltd	ky179	1967	1:15840
Dunning silty clay loam, dark subsoil variant	Du	456	548861	lf46	ky209	1974	1:15840
Dunning silty clay loam	Du	305	549795	lg3b	ky213	1982	1:20000
Dunning silt loam, occasionally flooded	Du	930	551151	lhj2	ky219	1984	1:20000
Dunning silty clay loam, ponded	Du	657	553855	llb9	ky227	2004	1:12000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Du	230	551488	2wltb	ky229	1983	1:20000
Dunning silty clay loam, occasionally flooded	Du	1165	550069	lgd5	ky231	1985	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	446	551612	2zs5h	ky601	1982	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Du	2350	552077	2wltb	ky604	1978	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Du	2216	551532	2wltb	ky606	1979	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Dn	514	551034	2wltd	ky621	1975	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	1280	551870	2zs5h	ky624	1976	1:20000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	2369	1398858	2zs5h	ky643	1965	1:15840
Dunning silty clay loam, occasionally flooded	Du	232	2452854	2nbdb	ky709	1995	1:20000
Dunning silt loam	Dz	23	3098697	l975	md043	1998	1:12000
Dunning silty clay, 0 to 2 percent slopes, occasionally flooded	66083	79	887252	ys81	mo135	1962	1:24000
Dunning silty clay loam	Dy	968	545578	l9q9	pa001	1991	1:24000
Dunning silty clay loam	Du	1553	538268	l23h	pa027	1975	1:20000
Dunning silt loam	Du	1050	545109	l975	pa055	1999	1:24000
Dunning silty clay loam, 0 to 2 percent slopes, occasionally flooded	Du	171	524500	2wpky	tn025	1948	1:24000
Dunning silt loam, silty substratum phase	Dn	919	524898	km66	tn031	1956	1:20000
Dunning silt loam, drained, overwash phase	Dm	385	524897	km65	tn031	1956	1:20000
Dunning silty clay loam, drained phase	Do	364	524899	km67	tn031	1956	1:20000
Dunning silty clay loam, 0 to 3 percent slopes, occasionally flooded	D6	1350	527174	30v95	tn051	1950	1:20000
Dunning silty clay loam	D5	488	527173	kpkl	tn051	1950	1:20000
Dunning silty clay loam, 0 to 3 percent slopes, occasionally flooded, warm	111	41	525283	2wpkx	tn063	2007	1:24000
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded, warm	Du	212	1017845	2wpkz	tn065	1980	1:15840
Dunning silty clay loam, 0 to 2 percent slopes, frequently flooded	Du	214	327556	30v94	tn071	1961	1:15840
Dunning silt loam, occasionally flooded	Du	432	526532	knwx	tn091	2000	1:24000
Dunning silty clay loam, phosphatic phase	Dg	2012	527763	kq5m	tn119	1955	1:20000
Dunning silty clay loam, 0 to 3 percent slopes, occasionally flooded, warm	Du	166	527883	2wpkx	tn123	1974	1:20000
Dunning silty clay loam	Du	177	529880	kscx	tn177	1965	1:15840
Dunning silt loam, phosphatic	Du	1912	523500	kkr3	tn187	1961	1:15840
Dunning silty clay loam, 0 to 3 percent slopes, occasionally flooded, warm	Du	265	528550	2wpkx	tn602	1973	1:15840
Dunning silt loam, overwash, occasionally flooded	Dv	1669	529686	ks5n	tn608	2001	1:24000
Dunning silty clay loam, occasionally flooded	Du	322	529685	ks5m	tn608	2001	1:24000
Dunning silt loam, 0 to 3 percent slopes, occasionally flooded	21A	180	834344	x06b	va005	2003	1:24000
Dunning silty clay loam, frequently ponded, 0 to 2 percent slopes, frequently flooded	8	1051	521301	2wpl0	va155	1981	1:15840
Dunning silt loam	Dz	912	516238	kb5v	wv003	1997	1:24000
Dunning silty clay loam, karst	Du	1316	553107	lkk5	wv025	2002	1:24000
Dunning silt loam	Dz	113	3098700	l975	wv037		1:24000
Dunning silty clay loam, karst	Dz	296	1713201	1vhqk	wv063	1962	1:24000
Dunning silty clay loam	Dz	116	555669	ln6t	wv065	2003	1:24000
Dunning silt loam	Du	191	514151	k80j	wv071	1988	1:20000
Dunning silt loam	Du	129	1602555	1qslb	wv604	1970	1:20000
Dunning silty clay loam	Du	592	555894	lng2	wv608	1973	1:20000
Dunning silty clay loam	Du	730	515898	k9tw	wv628	1980	1:20000

Map of Series Extent

Approximate geographic distribution of the DUNNING 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).