Soil Data Explorer - KORONIS

Official Series Description

Lab Data Summary

Aggregate lab data for the KORONIS soil series. This aggregation is based on all pedons with a current taxon name of KORONIS, 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 KORONIS were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
102A	UMN2893	S1978MN067143 (2893)	Koronis	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.3250504,-95.0392609
102A	UMN2894	S1978MN067144 (2894)	Koronis	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.3265114,-95.0372162
103	UMN2913	S1979MN0932913	Koronis	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.3178902,-94.4627991
103	UMN2914	S1979MN0932914	Koronis	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.315979,-94.464119
103	UMN2938	S1979MN0932938	Koronis	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.2459373,-94.5509415

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KORONIS 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 KORONIS 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 KORONIS 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 KORONIS 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 KORONIS 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 KORONIS 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 KORONIS 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 KORONIS, 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. MN-2010-09-08-13 | Meeker County - 1999

   Typical pattern of soils and parent material in the Koronis-Forestcity-Houghton association (Soil Survey of Meeker County, Minnesota; 1999).

2. MN-2010-09-13-05 | Wright County -

   Typical pattern of soils and parent material in the Koronis-Forestcity-Houghton association (Soil Survey of Wright County, Minnesota).

Map Units

Map units containing KORONIS 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
Koronis-Kingsley complex, 2 to 6 percent slopes	L58B	1575	413391	fw56	mn053	2001	1:12000
Koronis-Kingsley complex, 6 to 12 percent slopes, eroded	L58C2	1237	434666	gl9h	mn053	2001	1:12000
Koronis-Kingsley-Malardi complex, 18 to 35 percent slopes	L62E	764	399488	fdpq	mn053	2001	1:12000
Koronis-Kingsley-Malardi complex, 6 to 12 percent slopes, eroded	L62C2	714	432654	gj6l	mn053	2001	1:12000
Koronis-Kingsley complex, 12 to 18 percent slopes, eroded	L58D2	321	434667	gl9j	mn053	2001	1:12000
Koronis-Kingsley complex, 18 to 25 percent slopes	L58E	234	434668	gl9k	mn053	2001	1:12000
Koronis-Kingsley-Malardi complex, 2 to 6 percent slopes	L62B	139	399470	fdp4	mn053	2001	1:12000
Koronis-Kingsley-Malardi complex, 12 to 18 percent slopes, eroded	L62D2	135	399484	fdpl	mn053	2001	1:12000
Koronis-Sunburg complex, 6 to 12 percent slopes, moderately eroded	L357C2	3246	2536646	2n801	mn067	1983	1:20000
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, moderately eroded	L355C2	2919	2536640	2n7zw	mn067	1983	1:20000
Koronis-Sunburg complex, 2 to 6 percent slopes	L357B	2824	2536645	2n800	mn067	1983	1:20000
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, moderately eroded	L355D2	2042	2536641	2n7zh	mn067	1983	1:20000
Koronis-Hawick complex, 12 to 20 percent slopes	804D	1395	398708	fcwk	mn067	1983	1:20000
Koronis-Hawick complex, 6 to 12 percent slopes	804C	1332	398707	fcwj	mn067	1983	1:20000
Koronis-Sunburg complex, 12 to 18 percent slopes, moderately eroded	L357D2	1297	2536647	2n7zk	mn067	1983	1:20000
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	L355B	858	2536639	2n7zv	mn067	1983	1:20000
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	L355E	806	2536642	2n7zj	mn067	1983	1:20000
Koronis loam, 18 to 40 percent slopes	L307E	671	2510835	2pf1t	mn067	1983	1:20000
Koronis-Hawick complex, 20 to 30 percent slopes	804E	458	398709	fcwl	mn067	1983	1:20000
Koronis-Hawick complex, 2 to 6 percent slopes	804B	333	398706	fcwh	mn067	1983	1:20000
Koronis loam, 2 to 6 percent slopes	L307B	14	2536648	2vvg8	mn067	1983	1:20000
Koronis loam, 6 to 10 percent slopes, moderately eroded	L307C2	4	2510834	2vvgq	mn067	1983	1:20000
Koronis loam, 2 to 6 percent slopes	L307B	16882	2536650	2vvg8	mn093	1996	1:20000
Koronis loam, 6 to 10 percent slopes, moderately eroded	L307C2	8680	2536651	2vvgq	mn093	1996	1:20000
Koronis-Sunburg complex, 12 to 18 percent slopes, moderately eroded	L357D2	2657	2536682	2n7zk	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	L355E	1821	2536677	2n7zj	mn093	1996	1:20000
Rohrbeck-Koronis complex, 1 to 6 percent slopes	L326B	1445	2536686	2n809	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, moderately eroded	L355C2	1099	2536675	2n7zw	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, moderately eroded	L355D2	680	2536676	2n7zh	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	L355B	559	2536674	2n7zv	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, eroded	804D2	230	436420	gn42	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	804E	125	436421	gn43	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, eroded	804C2	70	436419	gn41	mn093	1996	1:20000
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	804B	43	436418	gn40	mn093	1996	1:20000
Koronis-Sunburg complex, 6 to 12 percent slopes, moderately eroded	L357C2	19	2536681	2n801	mn093	1996	1:20000
Koronis-Sunburg complex, 2 to 6 percent slopes	L357B	1	2536680	2n800	mn093	1996	1:20000
Koronis loam, 18 to 40 percent slopes	L307E	1	2536652	2pf1t	mn093	1996	1:20000
Koronis loam, 2 to 6 percent slopes	L307B	20093	2536690	2vvg8	mn145	1980	1:15840
Koronis loam, 6 to 10 percent slopes, moderately eroded	L307C2	8539	2536691	2vvgq	mn145	1980	1:15840
Koronis-Sunburg complex, 12 to 18 percent slopes, moderately eroded	L357D2	1705	2536718	2n7zk	mn145	1980	1:15840
Koronis loam, 18 to 40 percent slopes	L307E	1335	2536692	2pf1t	mn145	1980	1:15840
Koronis-Estherville complex, 12 to 25 percent slopes	804D	1099	428181	gck9	mn145	1980	1:15840
Rohrbeck-Koronis complex, 1 to 6 percent slopes	L326B	648	2536720	2n809	mn145	1980	1:15840
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, moderately eroded	L355D2	486	2536712	2n7zh	mn145	1980	1:15840
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	L355E	475	2536713	2n7zj	mn145	1980	1:15840
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	L355B	301	2536710	2n7zv	mn145	1980	1:15840
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, moderately eroded	L355C2	211	2536711	2n7zw	mn145	1980	1:15840
Koronis-Sunburg complex, 6 to 12 percent slopes, moderately eroded	L357C2	5	2536717	2n801	mn145	1980	1:15840
Koronis-Sunburg complex, 2 to 6 percent slopes	L357B	2	2536716	2n800	mn145	1980	1:15840
Koronis loam, 6 to 10 percent slopes, moderately eroded	L307C2	955	2536724	2vvgq	mn171	1998	1:12000
Koronis loam, 2 to 6 percent slopes	L307B	625	2536723	2vvg8	mn171	1998	1:12000
Koronis-Sunburg complex, 12 to 18 percent slopes, moderately eroded	L357D2	427	2527623	2n7zk	mn171	1998	1:12000
Koronis loam, 18 to 40 percent slopes	461E	412	433753	gkc1	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	L355E	267	2536738	2n7zj	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, moderately eroded	L355C2	251	2536736	2n7zw	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, moderately eroded	L355D2	218	2536737	2n7zh	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	L355B	172	2536735	2n7zv	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 12 to 18 percent slopes, eroded	804D2	29	433792	gkd9	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 2 to 6 percent slopes	804B	18	433794	gkdc	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 18 to 40 percent slopes	804E	11	433791	gkd8	mn171	1998	1:12000
Koronis-Sunburg-Hawick complex, 6 to 12 percent slopes, eroded	804C2	10	433793	gkdb	mn171	1998	1:12000
Koronis-Sunburg complex, 12 to 18 percent slopes, eroded	807D2	9	433788	gkd5	mn171	1998	1:12000

Map of Series Extent

Approximate geographic distribution of the KORONIS 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).