Soil Data Explorer - EAKIN

Official Series Description

Lab Data Summary

Aggregate lab data for the EAKIN soil series. This aggregation is based on all pedons with a current taxon name of EAKIN, 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 EAKIN 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
53C	40A2373	S1956SD059007	EAKIN	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.330555,-99.1708298
53C	40A2374	S1956SD059010	EAKIN	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.2513885,-99.1208344

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the EAKIN 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 EAKIN 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 EAKIN 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 EAKIN 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 EAKIN 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 EAKIN 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 EAKIN 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 EAKIN, 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-2012-03-14-12 | Charles Mix County - February 1982

   Pattern of soils and parent material in the Eakin-Highmore-Ethan association (Soil Survey of Charles Mix County, SD; 1982).

2. SD-2012-03-15-22 | Douglas County - June 1981

   Pattern of soils and underlying material in the Eakin-Highmore-Ethan association (Soil Survey of Douglas County, SD; 1981).

3. SD-2012-03-15-23 | Douglas County - June 1981

   Pattern of soils and underlying material in the Highmore-Walke association (Soil Survey of Douglas County, SD; 1981).

4. SD-2012-03-15-45 | Hand County - April 1963

   A typical cross section of the southwestern part of the county (Soil Survey of Hand County, SD; 1963).

5. SD-2012-03-15-88 | Potter County - October 1985

   Pattern of soils and parent material in the Highmore association (Soil Survey of Potter County, SD; 1985).

Map Units

Map units containing EAKIN 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
Eakin-Ethan complex, 2 to 6 percent slopes	EeB	9528	354847	2xhbv	sd003	1979	1:20000
Eakin-DeGrey silt loams, 0 to 2 percent slopes	EdA	5797	354846	2wkq7	sd003	1979	1:20000
Eakin-Ethan complex, 2 to 6 percent slopes	EeB	85672	355020	2xhbv	sd023	1980	1:20000
Eakin-Ethan complex, 6 to 9 percent slopes	EeC	44276	355021	2xhc0	sd023	1980	1:20000
Eakin-DeGrey silt loams, 0 to 4 percent slopes	EdA	22497	355019	2xhd5	sd023	1980	1:20000
Eakin silt loam, 0 to 2 percent slopes	EaA	11160	355017	2yyhy	sd023	1980	1:20000
Eakin-Beadle complex, 2 to 6 percent slopes	EbB	6862	355018	2yyg5	sd023	1980	1:20000
Beadle-Eakin complex, 6 to 9 percent slopes	BbC	2679	355003	2yyg8	sd023	1980	1:20000
Eakin-Ethan complex, 2 to 6 percent slopes	EaB	52543	354893	2xhbv	sd043	1979	1:20000
Eakin-Ethan complex, 0 to 3 percent slopes	EaA	8232	354892	2yyhz	sd043	1979	1:20000
Eakin-Ethan complex, 6 to 9 percent slopes	EaC	6929	354894	2xhc0	sd043	1979	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	ReB	63438	352669	2wbpz	sd059	1959	1:20000
Raber-Eakin complex, 6 to 9 percent slopes	RaC	8837	352665	2wbq0	sd059	1959	1:20000
Eakin-Raber complex, 0 to 2 percent slopes	RaA	3324	352663	2wbpy	sd059	1959	1:20000
Eakin-Jerauld silt loams, 2 to 6 percent slopes	EmB	2276	352597	2yyhs	sd059	1959	1:20000
Eakin-DeGrey silt loams, 0 to 2 percent slopes	EcA	2030	352594	2wkq7	sd059	1959	1:20000
Eakin-DeGrey silt loams, 2 to 6 percent slopes	EcB	1969	352595	2yyhp	sd059	1959	1:20000
Eakin-Jerauld silt loams, 0 to 2 percent slopes	EmA	904	352596	2yyhr	sd059	1959	1:20000
Glenham-Eakin complex, undulating	WrA	382	352695	cv08	sd059	1959	1:20000
Jerauld-Eakin silt loams, 0 to 2 percent slopes	MeA	326	352647	2yyht	sd059	1959	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	ErB	11627	353279	2wbpz	sd065	1970	1:20000
Raber-Eakin complex, 6 to 9 percent slopes	ErC	5575	353280	2wbq0	sd065	1970	1:20000
Eakin-Raber complex, 0 to 2 percent slopes	ErA	2451	353278	2wbpy	sd065	1970	1:20000
Agar-Eakin silt loams, 2 to 6 percent slopes	AkB	1126	353262	2xhbq	sd065	1970	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	ErB	31865	353795	2wbpz	sd069	1992	1:20000
Eakin-Peno complex, 6 to 9 percent slopes	EpC	9162	353793	2xhc1	sd069	1992	1:20000
Eakin-Raber complex, 0 to 2 percent slopes	ErA	6395	353794	2wbpy	sd069	1992	1:20000
Eakin-Ethan-Onita complex, 2 to 6 percent slopes	EaB	11233	356427	2yyj0	sd073	1987	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	ErB	11	3333711	2wbpz	sd073	1987	1:20000
Eakin-Peno complex, 2 to 6 percent slopes	EpB	29418	355324	2yyhv	sd107	1983	1:20000
Eakin-Raber complex, 0 to 2 percent slopes	EaA	18569	355323	2wbpy	sd107	1983	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	RaB	10131	355363	2wbpz	sd107	1983	1:20000
Eakin-Peno complex, 6 to 9 percent slopes	EpC	3551	355325	30t2j	sd107	1983	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	RgB	32610	353118	2wbpz	sd119	1967	1:20000
Eakin-Raber complex, 0 to 2 percent slopes	RhA	26378	353120	2wbpy	sd119	1967	1:20000
Agar-Eakin silt loams, 0 to 2 percent slopes	AeA	7465	353062	2yyhw	sd119	1967	1:20000
Agar-Eakin silt loams, 2 to 6 percent slopes	AeB	4964	353063	2xhbq	sd119	1967	1:20000
Raber-Eakin complex, 6 to 9 percent slopes	RgC	3270	353119	2wbq0	sd119	1967	1:20000
Agar-Eakin silt loams, 5 to 9 percent slopes	AeC	2349	353064	2yyhx	sd119	1967	1:20000
Highmore-Eakin silt loams, cool, 2 to 6 percent slopes	C721B	27764	2800135	2rrrr	sd129	1975	1:20000
Highmore-Eakin silt loams, cool, 0 to 2 percent slopes	C721A	4430	2800134	2rrrq	sd129	1975	1:20000
Highmore-Eakin silt loams, cool, 6 to 9 percent slopes	C721C	3780	2800136	2rrrs	sd129	1975	1:20000
Raber-Eakin complex, 6 to 9 percent slopes	HmC	3711	354499	2wbq0	sd129	1975	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	HmB	2286	354498	2wbpz	sd129	1975	1:20000
Eakin-DeGrey silt loams, 0 to 2 percent slopes	EaA	75707	355497	2wkq7	sd603	1983	1:20000
DeGrey-Eakin-Jerauld silt loams, 0 to 2 percent slopes	DaA	6688	355493	2yyhq	sd603	1983	1:20000
Eakin-Beadle complex, 2 to 6 percent slopes	BeB	5127	355482	2yyg5	sd603	1983	1:20000
Beadle-Eakin complex, 6 to 9 percent slopes	BeC	1273	355483	2yyg8	sd603	1983	1:20000
Eakin-Raber complex, 2 to 6 percent slopes	ErB	1204	3333693	2wbpz	sd603	1983	1:20000

Map of Series Extent

Approximate geographic distribution of the EAKIN 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).