Soil Data Explorer - DUDLEY

Official Series Description

Lab Data Summary

Aggregate lab data for the DUDLEY soil series. This aggregation is based on all pedons with a current taxon name of DUDLEY, 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 DUDLEY 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
55C	40A2506	S1971SD035001	DUDLEY	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4988899,-98.223053

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DUDLEY 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 DUDLEY 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 DUDLEY 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 DUDLEY 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 mountains figure.

Competing Series

Soil series competing with DUDLEY 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 DUDLEY 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 DUDLEY 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 hills figure.

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

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

Soil series sharing subgroup-level classification with DUDLEY, 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. SD-2012-03-15-58 | Jerauld County - September 1994

   Pattern of soils and parent material in the Clarno-Ethan-Prosper association (Soil Survey of Jerauld County, SD; 1994).

2. SD-2012-03-15-78 | Miner County - December 1984

   Pattern of soils and parent material in the Houdek-Dudley-Stickney association (Soil Survey of Miner County, SD; 1984).

3. SD-2012-03-15-79 | Miner County - December 1984

   Pattern of soils and parent material in the Clarno-Stickney association (Soil Survey of Miner County, SD; 1984).

Map Units

Map units containing DUDLEY 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
Dudley-Moody complex, 0 to 2 percent slopes	6520	878	427097	gbfb	ne027	1982	1:20000
Houdek-Dudley complex, 0 to 2 percent slopes	HdA	104423	354851	2wbpw	sd003	1979	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	DsA	23405	354844	2wkph	sd003	1979	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	HdB	18697	354852	2wbpx	sd003	1979	1:20000
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopes	BgB	13525	3333699	2yyg6	sd003	1979	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BdA	4006	354828	2yyg0	sd003	1979	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BdA	54735	354549	2yyg0	sd005	1976	1:20000
Dudley-Tetonka silt loams	DtA	52269	354566	cwym	sd005	1976	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	DsA	37876	354565	2wkpg	sd005	1976	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	DkA	7134	354564	2wkph	sd005	1976	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	HdB	5972	354583	2wbpx	sd005	1976	1:20000
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopes	BgB	1165	3333676	2yyg6	sd005	1976	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	Sy	2006	417791	2wkpg	sd025	1992	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	Dx	1267	417719	2wkph	sd025	1992	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BfA	914	417692	2yyg0	sd025	1992	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	SdA	5191	352935	2wkpg	sd035	1966	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BaA	3973	352899	2yyg0	sd035	1966	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	MnB	7956	355181	2wbpx	sd049	1981	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	NoA	4598	355187	2wkph	sd049	1981	1:20000
Houdek-Dudley complex, 0 to 2 percent slopes	WpA	4081	355205	2wbpw	sd049	1981	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	NaA	245	355184	2wkpg	sd049	1981	1:20000
Houdek-Dudley complex, 0 to 2 percent slopes	HlA	29779	352619	2wbpw	sd059	1959	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	HlB	16688	352620	2wbpx	sd059	1959	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	MdA	7494	352646	2wkph	sd059	1959	1:20000
Dudley silt loam, nearly level	CaA	6376	352582	ctwm	sd059	1959	1:20000
Stickney-Dudley silt loams, nearly level	CsA	4214	352590	ctww	sd059	1959	1:20000
Dudley-Stickney silt loams, nearly level	CcA	1360	352583	ctwn	sd059	1959	1:20000
Houdek-Dudley complex, 0 to 2 percent slopes	HrA	10457	356444	2wbpw	sd073	1987	1:20000
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopes	BgB	8070	356405	2yyg6	sd073	1987	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	DpA	3938	356423	2wkph	sd073	1987	1:20000
Houdek-Dudley-Jerauld complex, 2 to 6 percent slopes	HtB	1259	356445	2yyhf	sd073	1987	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BdA	194	356403	2yyg0	sd073	1987	1:20000
Stickney-Dudley-Hoven silt loams, 0 to 2 percent slopes	Sv	27878	417516	2wkpf	sd077	1992	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	Dx	4695	417475	2wkph	sd077	1992	1:20000
Beadle-Dudley complex, 0 to 2 percent slopes	BeA	4649	417456	2yyg0	sd077	1992	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	St	441	417515	2wkpg	sd077	1992	1:20000
Crossplain-Dudley complex	Cr	5548	418019	g0zh	sd087	1976	1:20000
Houdek-Dudley-Tetonka complex, 0 to 6 percent slopes	HgB	31292	355404	2yyhg	sd097	1983	1:20000
Houdek-Dudley complex, 0 to 2 percent slopes	HdA	19299	355401	2wbpw	sd097	1983	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	HdB	10769	355402	2wbpx	sd097	1983	1:20000
Stickney-Dudley silt loams, 0 to 2 percent slopes	Sd	9369	355409	2wkpg	sd097	1983	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	Do	8411	355394	2wkph	sd097	1983	1:20000
Houdek-Dudley complex, 2 to 6 percent slopes	HcB	9401	354792	2wbpx	sd111	1978	1:20000
Clarno-Dudley complex, 2 to 6 percent slopes	CkB	7324	354769	cx55	sd111	1978	1:20000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	DfA	3625	354778	2wkph	sd111	1978	1:20000
Stickney-Dudley-Hoven silt loams, 0 to 2 percent slopes	Su	15367	356710	2wkpf	sd115	1997	1:24000
Beadle-Dudley complex, 0 to 2 percent slopes	BdA	8976	356561	2yyg0	sd115	1997	1:24000
Dudley-Jerauld silt loams, 0 to 2 percent slopes	Du	3439	356592	2wkph	sd115	1997	1:24000
Stickney-Dudley silt loams, 0 to 2 percent slopes	St	3159	356709	2wkpg	sd115	1997	1:24000
Stickney-Dudley silt loams, 0 to 2 percent slopes	DsA	19321	417959	2wkpg	sd602	1975	1:20000

Map of Series Extent

Approximate geographic distribution of the DUDLEY 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).