Soil Data Explorer - DAKOTA

Official Series Description

Lab Data Summary

Aggregate lab data for the DAKOTA soil series. This aggregation is based on all pedons with a current taxon name of DAKOTA, 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 DAKOTA 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
103	40A1711	70MN047002	Dakota	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.5586128,-93.2741699
103	UMN1115	S1970MN0471115	Dakota	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.5598717,-93.2725754
104	UMN1161	S1970MN1091161	Dakota	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.8630371,-92.4552155
105	UMN5023	S1970MN0495023	Dakota	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.3163524,-92.7006937
105	UMN5022	S1970MN1095022	Dakota	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0612774,-92.4533099
105	78P0158	S1977WI111001	Dakota	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.3144444,-89.7402778
105	UMN2743	S1978MN1692743	Dakota	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9594498,-92.0239334
108B	70IL125002	1970IL125002	Dakota	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3827136,-89.7230156
108B	78IL103029	1978IL103029	Dakota	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.6209543,-89.543964
115C	84P0448	83IL179078	Dakota	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.4900017,-89.7977753
91A	UMN2560	S1978MN0372560	Dakota	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.6592598,-93.0753937
n/a	86IL179004	1986IL179004	Dakota	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 DAKOTA 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 DAKOTA 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 DAKOTA 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 DAKOTA 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 DAKOTA 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 DAKOTA 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 DAKOTA 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 DAKOTA, 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. IL-2010-09-01-45 | Mason County - 1995

   Typical pattern of soils and parent material in the Onarga-Dakota-Sparta association (Soil Survey of Mason County, Illinois; 1995).

2. IL-2010-09-01-48 | Mason County - 1995

   Typical pattern of soils and parent material in the Elburn-Plano-Thorp association (Soil Survey of Mason County, Illinois; 1995).

3. IL-2010-09-01-85 | Woodford County - 1999

   Typical pattern of soils and parent material in the Alvin-Coloma-Jasper association (Soil Survey of Woodford County, Illinois; 1999).

4. IL-2011-08-04-61 | Mason County - 1995

   Typical pattern of soils and parent material in the Onarga-Dakota-Sparta association (Soil Survey of Mason County, Illinois; 1995).

5. IL-2011-08-04-64 | Mason County - 1995

   Typical pattern of soils and parent material in the Elburn-Plano-Thorp association (Soil Survey of Mason County, Illinois; 1995).

6. WI-2012-03-22-06 | Grant County - June 1961

   Landscape of Grant County showing the relationship of the major soil series (Soil Survey of Grant County, WI; 1961).

7. WI-2012-03-23-02 | Iowa County - July 1962

   Two landscapes of terrace soils showing the relationship of the major soils. The upper illustration shows silty soils, and the lower one, sandy soils. By Soil Survey Division, University of Wisconsin (Soil Survey of Iowa County, WI; 1962).

8. WI-2012-03-23-30 | Pepin County - March 1964

   Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing DAKOTA 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
Dakota loam, 0 to 2 percent slopes	379A	3771	1019393	136rn	il007	2006	1:12000
Dakota loam, 2 to 5 percent slopes	379B	435	615661	nnn1	il057	1997	1:12000
Dakota loam, 0 to 2 percent slopes	379A	203	615660	nnn0	il057	1997	1:12000
Dakota loam, 2 to 5 percent slopes	379B	146	175190	5w99	il067	1993	1:15840
Dakota loam, 2 to 5 percent slopes, rarely flooded	7379B	128	2604125	2r797	il067	1993	1:15840
Dakota sandy loam, 2 to 5 percent slopes, eroded	379B2	5161	937030	10g1s	il103	2004	1:12000
Dakota loam, 0 to 2 percent slopes	379A	8146	182694	643c	il111	1997	1:12000
Dakota loam, 2 to 4 percent slopes	379B	750	182695	643d	il111	1997	1:12000
Dakota loam, 0 to 2 percent slopes	379A	5637	182180	63ks	il123	1997	1:15840
Dakota loam, 2 to 5 percent slopes	379B	2745	182181	63kt	il123	1997	1:15840
Dakota fine sandy loam, 0 to 2 percent slopes	379A	10791	177796	5z0c	il125	1989	1:15840
Dakota fine sandy loam, 2 to 5 percent slopes	379B	1416	177797	5z0d	il125	1989	1:15840
Dakota loam, 0 to 2 percent slopes	379A	211	1406382	1j6g5	il129	2005	1:12000
Dakota loam, 0 to 2 percent slopes	379A	967	172805	5stc	il155	1987	1:15840
Dakota loam, 2 to 5 percent slopes, eroded	379B2	519	172807	5stf	il155	1987	1:15840
Dakota fine sandy loam, 0 to 2 percent slopes, rarely flooded	7379A	56	2650846	2r21s	il155	1987	1:15840
Dakota silt loam, 5 to 10 percent slopes, eroded	379C2	531	179099	60cd	il175	1992	1:15840
Dakota fine sandy loam, 0 to 2 percent slopes	379A	5042	179406	60p9	il179	1991	1:15840
Dakota fine sandy loam, 2 to 5 percent slopes	379B	1834	179407	60pb	il179	1991	1:15840
Dakota fine sandy loam, 2 to 5 percent slopes, rarely flooded	7379B	113	2509793	2qgxr	il179	1991	1:15840
Dakota fine sandy loam, 0 to 2 percent slopes, rarely flooded	7379A	92	2509792	2qgxq	il179	1991	1:15840
Dakota loam, 0 to 2 percent slopes	379A	340	174065	5v40	il201	1997	1:12000
Dakota loam, 0 to 2 percent slopes	379A	354	869218	y5h9	il203	2008	1:12000
Dakota and Rasset sandy loams, 0 to 2 percent slopes	DA	329	396410	f9hf	mn019	1987	1:12000
Dakota and Rasset sandy loams, 2 to 6 percent slopes	DB	290	396411	f9hg	mn019	1987	1:12000
Dakota silt loam, 0 to 3 percent slopes	M525A	2310	1386866	1hk4m	mn039	2005	1:12000
Dakota loam, 0 to 1 percent slopes	De	1083	2216716	2ddnz	mn045	2008	1:12000
Dakota fine sandy loam, 2 to 6 percent slopes	Db	581	2216715	2ddny	mn045	2008	1:12000
Dakota loam, 2 to 6 percent slopes	Df	483	2216717	2ddp0	mn045	2008	1:12000
Dakota fine sandy loam, 0 to 1 percent slopes	Da	281	2216714	2ddnx	mn045	2008	1:12000
Dakota fine sandy loam, 12 to 17 percent slopes, moderately eroded	Dd	63	2216712	2ddnv	mn045	2008	1:12000
Dakota loam, 2 to 6 percent slopes	5B	2690	397880	fc0v	mn047	1977	1:15840
Dakota loam, 0 to 2 percent slopes	5	1603	397872	fc0l	mn047	1977	1:15840
Dakota loam, 6 to 14 percent slopes	5C	728	397881	fc0w	mn047	1977	1:15840
Dakota silt loam, 0 to 3 percent slopes	N579A	6264	1690487	1tr2v	mn049	2007	1:12000
Dakota silt loam, 0 to 3 percent slopes	M525A	1116	1670742	1t2jx	mn049	2007	1:12000
Dakota loam, 0 to 2 percent slopes	DaA	1235	427949	gc9t	mn139	1988	1:20000
Dakota loam, 2 to 6 percent slopes	DaB	142	427950	gc9v	mn139	1988	1:20000
Dakota loam, 2 to 6 percent slopes, moderately eroded	DaB2	130	427951	gc9w	mn139	1988	1:20000
Dakota loam, 6 to 12 percent slopes, moderately eroded	DaC2	31	427952	gc9x	mn139	1988	1:20000
Dakota loam, 1 to 6 percent slopes	5B	775	431537	gh1k	mn143	1991	1:20000
Dakota loam, 2 to 6 percent slopes	5B	1457	428170	gcjy	mn145	1980	1:15840
Dakota loam, 0 to 2 percent slopes	5A	1385	428169	gcjx	mn145	1980	1:15840
Dakota loam, 2 to 6 percent slopes	DkB	815	428226	gclr	mn147	1967	1:20000
Dakota sandy loam, 2 to 6 percent slopes	DaB	788	428223	gcln	mn147	1967	1:20000
Dakota loam, 0 to 2 percent slopes	DkA	594	428225	gclq	mn147	1967	1:20000
Dakota sandy loam, 6 to 14 percent slopes	DaC	530	428224	gclp	mn147	1967	1:20000
Dakota sandy loam, 0 to 2 percent slopes	DaA	418	428222	gclm	mn147	1967	1:20000
Dakota silt loam, 0 to 3 percent slopes	403A	542	2561692	1lmx9	wi011	1960	1:12000
Dakota silt loam, 2 to 6 percent slopes	403B	121	2639461	2rhz2	wi011	1960	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	769	2504026	1lmx9	wi023	1960	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	2753	2504027	1lmx9	wi033	2003	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	326	3099678	1lmx9	wi035	1974	1:12000
Dakota fine sandy loam, 0 to 2 percent slopes	DaA	519	424151	g7c9	wi043	1959	1:20000
Dakota fine sandy loam, 2 to 6 percent slopes	DaB	167	424152	g7cb	wi043	1959	1:20000
Dakota fine sandy loam, 6 to 10 percent slopes, moderately eroded	DaC2	44	424153	g7cc	wi043	1959	1:20000
Dakota loam, 0 to 2 percent slopes	DaA	1186	425214	g8gl	wi045	1969	1:12000
Dakota loam, 2 to 6 percent slopes, moderately eroded	DaB2	435	425215	g8gm	wi045	1969	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	676	2774813	1lmx9	wi049	1960	1:20000
Dakota silt loam, 0 to 3 percent slopes	403A	444	2504028	1lmx9	wi063	2001	1:12000
Dakota loam, mottled subsoil variant, 0 to 3 percent slopes	DbB	137	424755	g7zs	wi065	1964	1:15840
Dakota loam, 2 to 6 percent slopes	DaB	133	424754	g7zr	wi065	1964	1:15840
Dakota loam, 0 to 2 percent slopes	DaA	38	424753	g7zq	wi065	1964	1:15840
Dakota silt loam, 0 to 3 percent slopes	403A	107	2504029	1lmx9	wi091	1998	1:12000
Dakota loam, strath terrace, 0 to 3 percent slopes	401A	8177	1697385	1tz8c	wi093	2006	1:12000
Dakota loam, till plain, 0 to 3 percent slopes	404A	855	1698631	1v0kk	wi093	2006	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	731	1690944	1trkl	wi093	2006	1:12000
Dakota loam, limestone substratum, 0 to 3 percent slopes	DlA	1357	421183	g48k	wi095	1978	1:15840
Dakota loam, 0 to 2 percent slopes	DaA	974	421181	g48h	wi095	1978	1:15840
Dakota variant silt loam, 0 to 3 percent slopes	DvA	705	421184	g48l	wi095	1978	1:15840
Dakota loam, 2 to 6 percent slopes	DaB	699	421182	g48j	wi095	1978	1:15840
Dakota silt loam, 0 to 3 percent slopes	403A	217	2504030	1lmx9	wi103	2002	1:12000
Dakota loam, 2 to 6 percent slopes	DaB	1998	422129	g582	wi109	1975	1:15840
Dakota-Pillot complex, 6 to 12 percent slopes, eroded	DcC2	860	422130	g583	wi109	1975	1:15840
Dakota loam, 0 to 2 percent slopes	DaA	808	422128	g581	wi109	1975	1:15840
Dakota loam, 0 to 2 percent slopes	DaA	4124	423137	g69l	wi111	1977	1:15840
Dakota loam, 2 to 6 percent slopes	DaB	2115	423138	g69m	wi111	1977	1:15840
Dakota silt loam, 2 to 6 percent slopes	403B	489	2683483	2rhz2	wi121	1969	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	198	2683472	1lmx9	wi121	1969	1:12000
Dakota silt loam, 0 to 3 percent slopes	403A	10	2504031	1lmx9	wi123	1965	1:12000

Map of Series Extent

Approximate geographic distribution of the DAKOTA 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).