Soil Data Explorer - KADOKA

Official Series Description

Lab Data Summary

Aggregate lab data for the KADOKA soil series. This aggregation is based on all pedons with a current taxon name of KADOKA, 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 KADOKA 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
64	40A2405	S1957SD113006	Kadoka	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.4208336,-102.1875

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KADOKA 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 KADOKA 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 KADOKA 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 KADOKA 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 KADOKA 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 KADOKA 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 KADOKA 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 KADOKA, 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-2012-03-15-93 | Shannon County - April 1971

   Representative pattern of soils in association 4 (Soil Survey of Shannon County, SD; 1971).

2. SD-2012-03-15-97 | Todd County - April 1974

   Typical pattern of soils in association 2 (Soil Survey of Todd County, SD; 1974).

Map Units

Map units containing KADOKA 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
Kadoka silt loam, 6 to 11 percent slopes	3212	4639	100602	3cp7	ne161	1992	1:20000
Kadoka silt loam, 2 to 6 percent slopes	3211	1271	100601	3cp6	ne161	1992	1:20000
Kadoka silt loam, 0 to 2 percent slopes	3210	187	100600	2tvvp	ne161	1992	1:20000
Kadoka silt loam, 3 to 6 percent slopes	KaB	696	352744	2tvtk	sd007	2004	1:20000
Epping-Kadoka silt loam, 9 to 40 percent slopes	EhF	545	352735	2tzzh	sd007	2004	1:20000
Kadoka-Epping silt loams, 6 to 15 percent slopes	KeD	1826	355114	cxj9	sd047	1980	1:24000
Kadoka silt loam, 0 to 6 percent slopes	KaB	390	355113	cxj8	sd047	1980	1:24000
Huggins-Kadoka silt loams, 2 to 5 percent slopes	HuB	7517	353375	cvq6	sd095	1971	1:20000
Kadoka-Kube silt loams	Ka	5477	353381	cvqd	sd095	1971	1:20000
Duroc and Kadoka silt loams, 2 to 5 percent slopes	DvB	2950	353361	cvpr	sd095	1971	1:20000
Duroc and Kadoka silt loams, 0 to 2 percent slopes	DvA	1268	353360	cvpq	sd095	1971	1:20000
Huggins-Kadoka silt loams, 0 to 2 percent slopes	HuA	768	353374	cvq5	sd095	1971	1:20000
Kadoka-Epping silt loams, 3 to 9 percent slopes	KbC	19691	353002	2tvtm	sd121	1967	1:31680
Keota-Kadoka silt loams, 9 to 15 percent slopes	KkD	14104	353009	cvbd	sd121	1967	1:31680
Kadoka-Huggins silt loams, 2 to 5 percent slopes	KdB	11708	353003	cvb6	sd121	1967	1:31680
Huggins-Kadoka silt loams, 2 to 9 percent slopes	HwB	11547	352998	cvb1	sd121	1967	1:31680
Kadoka-Huggins silt loams, 5 to 9 percent slopes	KdC	8270	353004	cvb7	sd121	1967	1:31680
Kadoka silt loam, 0 to 2 percent slopes	KaA	5087	353001	2tvvp	sd121	1967	1:31680
Huggins-Kadoka silt loams, 3 to 9 percent slopes	HkB	3696	354397	cws5	sd123	1975	1:20000
Kadoka-Epping silt loams, 6 to 12 percent slopes	KbD	882	354402	cwsb	sd123	1975	1:20000
Kadoka silt loam, 0 to 3 percent slopes	KaA	623	354401	cws9	sd123	1975	1:20000
Kadoka-Thirtynine silt loams, 3 to 6 percent slopes	U350B	83	2582917	2pf59	sd606	2011	1:24000
Kadoka-Thirtynine silt loams, 6 to 9 percent slopes	U350C	26	2582918	2pf5b	sd606	2011	1:24000
Epping-Kadoka silt loams, 9 to 18 percent slopes	EkE	42598	2925493	2tzzf	sd610	1965	1:20000
Kadoka-Epping silt loams, 3 to 9 percent slopes	KbC	29801	2925480	2tvtm	sd610	1965	1:20000
Kadoka silt loam, 6 to 9 percent slopes	KaC	23079	2925518	2tvtl	sd610	1965	1:20000
Epping-Kadoka silt loam, 9 to 40 percent slopes	EhF	20536	2925486	2tzzh	sd610	1965	1:20000
Kadoka silt loam, 3 to 6 percent slopes	KaB	16561	2925499	2tvtk	sd610	1965	1:20000
Kadoka-Huggins silt loams, 3 to 9 percent slopes	KdC	7838	2925503	cv5t	sd610	1965	1:20000
Kadoka silt loam, 0 to 2 percent slopes	KaA	2134	2925523	2tvvp	sd610	1965	1:20000
Kadoka-Thirtynine silt loams, 3 to 6 percent slopes	U350B	1306	2485310	2pf59	sd612	2011	1:20000
Kadoka-Epping silt loams, 3 to 9 percent slopes	U355C	912	2485312	2tvtm	sd612	2011	1:20000
Epping, moist-Kadoka silt loams, 9 to 20 percent slopes	U190D	318	2485299	2pf4y	sd612	2011	1:20000
Kadoka-Thirtynine silt loams, 0 to 3 percent slopes	U350A	203	2485308	2pf57	sd612	2011	1:20000
Kadoka-Thirtynine silt loams, 6 to 9 percent slopes	U350C	111	2485311	2pf5b	sd612	2011	1:20000
Epping-Kadoka silt loams, 9 to 18 percent slopes	EkE	35534	2582692	2tzzf	sd613	2011	1:24000
Kadoka-Epping silt loams, 3 to 9 percent slopes	KbC	10462	2582705	2tvtm	sd613	2011	1:24000
Epping-Kadoka silt loam, 9 to 40 percent slopes	EhF	8631	2582691	2tzzh	sd613	2011	1:24000
Kadoka silt loam, 3 to 6 percent slopes	KaB	5076	2582703	2tvtk	sd613	2011	1:24000
Kadoka silt loam, 6 to 9 percent slopes	KaC	4153	2582704	2tvtl	sd613	2011	1:24000
Kadoka silt loam, 0 to 2 percent slopes	KaA	1430	2582702	2tvvp	sd613	2011	1:24000
Epping, moist-Kadoka silt loams, 9 to 20 percent slopes	U190D	413	2582818	2pf4y	sd613	2011	1:24000
Kadoka-Thirtynine silt loams, 3 to 6 percent slopes	U350B	235	2582831	2pf59	sd613	2011	1:24000
Kadoka-Thirtynine silt loams, 0 to 3 percent slopes	U350A	139	2582830	2pf57	sd613	2011	1:24000
Kadoka-Thirtynine silt loams, 6 to 9 percent slopes	U350C	56	2582832	2pf5b	sd613	2011	1:24000
Kadoka loam, 6 to 10 percent slopes	P184C	5802	2745746	2qt3g	wy011	1978	1:24000
Kadoka loam, 1 to 6 percent slopes	P184B	4799	2745745	2qt3f	wy011	1978	1:24000
Kadoka loam, 1 to 6 percent slopes	85	271	349365	cqjv	wy011	1978	1:24000
Kadoka loam, 6 to 10 percent slopes	86	249	349366	cqjw	wy011	1978	1:24000
Thirtynine-Kadoka silt loams, 2 to 10 percent slopes	208	10605	349719	cqx8	wy027	1993	1:24000

Map of Series Extent

Approximate geographic distribution of the KADOKA 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).