Soil Data Explorer - KINROSS

Official Series Description

Lab Data Summary

Aggregate lab data for the KINROSS soil series. This aggregation is based on all pedons with a current taxon name of KINROSS, 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 KINROSS 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
94D	83P0044	82WI125003	Kinross	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.1188889,-89.2127762
98	08N0673	F2008MI121020	Kinross	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.1416664,-86.0872192

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KINROSS 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 KINROSS 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 KINROSS 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 KINROSS 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 KINROSS 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 KINROSS 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 KINROSS 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 KINROSS, 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. MI-2010-09-10-05 | Keweenaw County Area - 2006

   Typical pattern of soils and parent material in the Dawson-Au Gres-Croswell association (Soil Survey of Keweenaw County Area, Michigan; 2006).

2. MI-2012-02-06-09 | Chippewa County - February 1992

   Typical pattern of soils and parent material in the Markey-Kinross-Croswell association (Soil Survey of Chippewa County, Michigan; February 1992).

3. MI-2012-02-06-11 | Chippewa County - February 1992

   Typical pattern of soils and parent material in the Deer Park-Dawson-Au Gres association (Soil Survey of Chippewa County, Michigan; February 1992).

4. MI-2012-02-06-18 | Houghton County Area - October 1991

   Diagrammatic cross section of Houghton County showing the topography, elevation, general soil texture, landforms, and dominant soils and their drainage class (Soil Survey of Houghton County Area, Michigan; October 1991).

Map Units

Map units containing KINROSS 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
Kinross muck	35	226	190321	6d1d	mi001	1993	1:20000
Finch-Kinross complex, 0 to 3 percent slopes	252A	7956	1455397	1kvg9	mi003	2007	1:24000
Kinross muck, 0 to 2 percent slopes	18	4180	1455253	2xxhv	mi003	2007	1:24000
Croswell-Kinross complex, 0 to 6 percent slopes	176B	1382	1455339	1kvdf	mi003	2007	1:24000
Halfaday-Kinross complex, 0 to 4 percent slopes	285B	393	1455424	1kvh5	mi003	2007	1:24000
Kinross muck	35	822	191272	6f12	mi007	1998	1:12000
Kinross-Au Gres complex, 0 to 3 percent slopes	KinauA	775	3155922	2ythf	mi009	1976	1:15840
Kinross sand	Kr	2	2673430	6chm	mi011	1964	1:20000
Kinross-Croswell complex, 0 to 3 percent slopes	32A	3170	414972	fxt6	mi013	1984	1:20000
Kinross muck, 0 to 2 percent slopes	18	2766	414954	2xxhv	mi013	1984	1:20000
Grayling-Kinross complex, 0 to 15 percent slopes	29D	1218	414965	fxsz	mi013	1984	1:20000
Tawas-Kinross complex, 0 to 2 percent slopes	8061	172	2441881	2myzc	mi013	1984	1:20000
Kinross mucky sand	67	1715	190609	6dbp	mi031	1988	1:15840
Markey-Kinross-Au Gres complex, 0 to 3 percent slopes	94A	19740	415185	fy12	mi033	1989	1:15840
Kinross-Au Gres complex, 0 to 3 percent slopes	89A	17735	415179	fy0w	mi033	1989	1:15840
Deer Park-Kinross complex, 0 to 50 percent slopes	38F	15950	415145	fxzs	mi033	1989	1:15840
Wainola-Kinross-Rousseau complex, 0 to 35 percent slopes	48E	14871	415157	fy05	mi033	1989	1:15840
Kinross-Wainola complex, 0 to 3 percent slopes	137A	9803	415093	fxy3	mi033	1989	1:15840
Kinross muck, 0 to 2 percent slopes	22	8112	415132	2xxhv	mi033	1989	1:15840
Kinross-Dawson complex	102	5056	415054	fxwv	mi033	1989	1:15840
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	3543	189701	6cdd	mi039	1993	1:15840
Kinross muck	35	1894	189716	6cdw	mi039	1993	1:15840
Au Gres-Kinross-Croswell complex, 0 to 6 percent slopes	50B	984	189722	6cf2	mi039	1993	1:15840
Kinross muck, 0 to 2 percent slopes	Kr	4453	1588070	2xxhv	mi041	1969	1:24000
Kinross muck, 0 to 2 percent slopes	55	2068	415227	2xxhv	mi043	1985	1:20000
Pipestone-Kinross association	PX	5193	2673477	2qz5g	mi051	1966	1:15840
Kinross sand	Kr	2241	189801	6chm	mi051	1966	1:15840
Covert-Pipestone-Kinross association	CY	1594	2673489	2qz5v	mi051	1966	1:15840
Au Gres-Kinross loamy substratum association	AV	650	189746	6cfv	mi051	1966	1:15840
Au Gres-Kinross association	AU	639	189745	6cft	mi051	1966	1:15840
Croswell-Au Gres-Kinross association	CU	513	189772	6cgp	mi051	1966	1:15840
Pipestone-Kinross loamy substratum association	PY	191	2673478	2qz5h	mi051	1966	1:15840
Kinross mucky sand	Kn	5	2673465	686l	mi051	1966	1:15840
Tawas-Kinross complex, 0 to 2 percent slopes	61	267	1456240	1kwbh	mi053	2007	1:24000
Au Gres-Kinross complex, 0 to 3 percent slopes	76A	1268	416159	fz1h	mi061	1989	1:20000
Dawson-Kinross complex, 0 to 1 percent slopes	125	1006	416059	fyy8	mi061	1989	1:20000
Kellogg, sandy substratum-Au Gres-Kinross complex, 0 to 4 percent slopes	8232B	801	2485001	2pdvb	mi061	1989	1:20000
Tawas-Kinross complex, 0 to 2 percent slopes	8061	540	2483440	2pc6z	mi061	1989	1:20000
Deer Park-Kinross complex, 0 to 15 percent slopes	135D	232	416074	fyyr	mi061	1989	1:20000
Manido-Kinross complex, 0 to 4 percent slopes	8155	78	2483787	2pcl5	mi061	1989	1:20000
Kinross muck, 0 to 2 percent slopes	75	472	416016	2xxhv	mi071	1992	1:20000
Tawas-Kinross complex, 0 to 2 percent slopes	8061	165	2475140	2p2l7	mi071	1992	1:20000
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	1533	190641	6dcq	mi079	1998	1:12000
Kinross muck	35	1101	190648	6dcy	mi079	1998	1:12000
Au Gres-Kinross-Croswell complex, 0 to 6 percent slopes	50B	919	190662	6ddd	mi079	1998	1:12000
Kinross-Au Gres complex, 0 to 3 percent slopes	60A	4881	627505	p1z3	mi095	2004	1:24000
Kinross muck, 0 to 2 percent slopes	30	783	627478	2xxhv	mi095	2004	1:24000
Kinross muck, 0 to 2 percent slopes	18	2274	395136	2xxhv	mi103	1999	1:24000
Kinross mucky fine sand	6	1637	192582	6gdb	mi105	1992	1:15840
Kinross mucky sand	Kn	6708	186638	686l	mi111	1976	1:15840
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	312	192225	6g0t	mi119	1997	1:12000
Manido-Kinross complex, 0 to 4 percent slopes	8155	1648	1674844	1t6t7	mi131	2007	1:24000
Dawson-Kinross complex, 0 to 1 percent slopes	8157	1221	1674846	1t6t9	mi131	2007	1:24000
Kellogg, sandy substratum-Au Gres-Kinross complex, 0 to 4 percent slopes	8232B	674	1674869	1t6v1	mi131	2007	1:24000
Kinross sand	Kx	80	190089	6csx	mi133	1966	1:15840
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	114	241388	835q	mi135	2003	1:12000
Au Gres-Kinross-Croswell complex, 0 to 6 percent slopes	50B	5	241390	835s	mi135	2003	1:12000
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	419	191462	6f76	mi137	1998	1:12000
Au Gres-Kinross-Croswell complex, 0 to 6 percent slopes	50B	190	191504	6f8k	mi137	1998	1:12000
Kinross muck	92	516	190966	6dq6	mi141	1989	1:15840
Au Gres-Kinross-Croswell complex, 0 to 6 percent slopes	50B	14740	191003	6drd	mi143	1999	1:12000
Kinross-Au Gres complex, 0 to 3 percent slopes	24A	4118	191000	6dr9	mi143	1999	1:12000
Kinross muck	35	1019	191001	6drb	mi143	1999	1:12000
Deford-Kinross mucks	473	661	190974	6dqg	mi143	1999	1:12000
Dawson-Kinross complex	499	218	191047	6dst	mi143	1999	1:12000
Kinross-Au Gres-Rubicon complex, 0 to 15 percent slopes	541D	11167	1650342	1sd9v	mi153	2007	1:24000
Kinross muck, 0 to 2 percent slopes	18	9234	1456977	2xxhv	mi153	2007	1:24000
Neconish-Kinross-Wainola complex, 0 to 6 percent slopes	525B	8560	1457046	1kx5h	mi153	2007	1:24000
Dawson-Kinross complex	84	4111	1456920	1kx1f	mi153	2007	1:24000
Halfaday-Kinross complex, 0 to 4 percent slopes	563B	1392	1538079	1nmhg	mi153	2007	1:24000
Croswell-Kinross complex, 0 to 6 percent slopes	562B	881	1538080	1nmhh	mi153	2007	1:24000
Au Gres-Kinross complex, 0 to 3 percent slopes	127A	1008	435360	gm0w	mi605	2004	1:24000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes	3826B	1150	1700374	1v2cs	wi003	2006	1:12000
Kinross muck, 0 to 2 percent slopes	445A	245	1444420	2xxhv	wi003	2006	1:12000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes	3826B	7811	1383665	1hftc	wi007	2005	1:12000
Kinross muck, 0 to 2 percent slopes	445A	482	433547	2xxhv	wi007	2005	1:12000
Kinross muck, 0 to 2 percent slopes	445A	1729	781248	2xxhv	wi031	2005	1:12000
Kinross muck, 0 to 2 percent slopes	Kr	449	430011	2xxhv	wi037	1995	1:12000
Kinross muck, 0 to 2 percent slopes	Kr	868	429840	2xxhv	wi041	1995	1:12000
Kinross-Au Gres-Markey complex, 0 to 3 percent slopes	455A	3527	1702181	1v482	wi051	2006	1:12000
Kinross muck, 0 to 2 percent slopes	445A	797	782116	2xxhv	wi051	2006	1:12000
Allendale-Wakeley-Kinross complex, 0 to 6 percent slopes	3826B	327	782362	v83h	wi051	2006	1:12000
Kinross muck, 0 to 2 percent slopes	Kr	3004	3119049	2xxhv	wi075	1987	1:20000
Kinross muck, 0 to 2 percent slopes	Kr	108	3119051	2xxhv	wi083	1985	1:15840
Kinross muck, 0 to 2 percent slopes	Ks	8733	421097	2xxhv	wi085	1988	1:20000
Kinross muck, 0 to 2 percent slopes	445A	421	627376	2xxhv	wi099	2006	1:12000
Kinross muck, 0 to 2 percent slopes	445A	435	625817	2xxhv	wi113	2006	1:12000
Kinross muck, 0 to 2 percent slopes	Kr	5695	421250	2xxhv	wi125	1985	1:20000

Map of Series Extent

Approximate geographic distribution of the KINROSS 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).