Soil Data Explorer - IOSCO

Official Series Description

Lab Data Summary

Aggregate lab data for the IOSCO soil series. This aggregation is based on all pedons with a current taxon name of IOSCO, 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 IOSCO 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
92	05N0181	S2004MI131004	Iosco	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.7872963,-89.0300674
95A	85P0249	84WI075004	Iosco	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.1344452,-87.921669

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the IOSCO 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 IOSCO 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 IOSCO 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 IOSCO 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 IOSCO 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 IOSCO 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the IOSCO 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 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with IOSCO, 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-2010-09-07-25 | Montmorency County - 2003

   Typical pattern of soils and underlying material in the Lupton-Tawas and Mancelona-Millersburg-Blue Lake associations (Soil Survey of Montmorency County, Michigan; 2003).

2. MI-2012-02-06-43 | Missaukee County - December 1985

   Pattern of soils and underlying material in the Nester-Kawkawlin-Manistee association (Soil Survey of Missaukee County, Michigan; December 1985).

Map Units

Map units containing IOSCO 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
Iosco loamy sand, 0 to 3 percent slopes	304A	6887	191320	6f2m	mi007	1998	1:12000
Iosco sand, 0 to 4 percent slopes	IoA	565	241500	839b	mi009	1976	1:15840
Iosco sand, 0 to 6 percent slopes	IosaaB	137	3155917	2ycxg	mi009	1976	1:15840
Iosco loamy sand, 0 to 2 percent slopes	ImA	4462	189174	6bvd	mi011	1964	1:20000
Iosco-Rubicon association, undulating	IrB	2066	189178	6bvj	mi011	1964	1:20000
Iosco loamy sand, 2 to 6 percent slopes	ImB	2007	189175	6bvf	mi011	1964	1:20000
Rubicon-Iosco association, undulating	RvB	546	189264	6by9	mi011	1964	1:20000
Nester-Iosco-Rubicon association, steep	NrE	541	189233	6bx9	mi011	1964	1:20000
Iosco sand, 2 to 6 percent slopes	IoB	90	189177	6bvh	mi011	1964	1:20000
Iosco sand, 0 to 2 percent slopes	IoA	63	189176	6bvg	mi011	1964	1:20000
Iosco-Kawkawlin-Brevort association	118	2	2508095	6chf	mi017	1978	1:20000
Iosco loamy sand, 0 to 6 percent slopes	IlB	732	190452	6d5m	mi029	1970	1:15840
Iosco sand, 0 to 6 percent slopes	IosaaB	7	3156027	2ycxg	mi029	1970	1:15840
Iosco-Kawkawlin complex, 0 to 3 percent slopes	IkA	10977	189621	6c9t	mi035	1977	1:15840
Iosco sand, 0 to 6 percent slopes	IoB	3800	1588060	1q9hr	mi041	1969	1:24000
Iosco loamy fine sand, 0 to 6 percent slopes	IlB	2953	189341	6c0s	mi047	1968	1:20000
Iosco-Brevort-Ingalls association	II	6924	189794	6chd	mi051	1966	1:15840
Iosco-Au Gres-Ingalls association	IA	3435	189790	6ch8	mi051	1966	1:15840
Iosco loamy sand, 0 to 2 percent slopes	IoA	2807	189797	6chh	mi051	1966	1:15840
Bowers-Iosco-Hettinger association	BI	2569	189752	6cg1	mi051	1966	1:15840
Iosco-Menominee-Brevort association	IM	2090	189796	6chg	mi051	1966	1:15840
Iosco-Pipestone-Ingalls association	IP	1904	2673493	2qz5z	mi051	1966	1:15840
Iosco-Brevort association	IB	1153	189791	6ch9	mi051	1966	1:15840
Iosco loamy sand, 2 to 6 percent slopes	IoB	745	189798	6chj	mi051	1966	1:15840
Iosco-Kawkawlin-Brevort association	IK	601	189795	6chf	mi051	1966	1:15840
Iosco-Kawkawlin complex, 0 to 3 percent slopes	IwA	72	2673462	6c9t	mi051	1966	1:15840
Iosco-Ogemaw loamy sands, 0 to 2 percent slopes	IsA	1396	189459	6c4l	mi055	1963	1:15840
Iosco loamy sand, 2 to 6 percent slopes	IlB	508	189456	6c4h	mi055	1963	1:15840
Iosco-Ogemaw loamy sands, 2 to 6 percent slopes	IsB	502	189460	6c4m	mi055	1963	1:15840
Iosco loamy sand, 6 to 12 percent slopes	IlC	463	189457	6c4j	mi055	1963	1:15840
Iosco-Ogemaw loamy sands, 0 to 2 percent slopes, overwash	IoA	101	189458	6c4k	mi055	1963	1:15840
Iosco loamy sand, 0 to 2 percent slopes	IsA	330	187988	69m4	mi067	1965	1:15840
Iosco loamy sand, 2 to 6 percent slopes	IsB	255	187989	69m5	mi067	1965	1:15840
Iosco-Kawkawlin complex, 0 to 3 percent slopes	106A	8	2673521	6c9t	mi073	1983	1:15840
Tonkey-Munuscong-Iosco sandy loams, 0 to 2 percent slopes	TmA	518	190851	6dlh	mi089	1967	1:20000
Tonkey-Munuscong-Iosco sandy loams, 2 to 6 percent slopes	TmB	502	190852	6dlj	mi089	1967	1:20000
Iosco-Epoufette loamy sands	Ie	438	190813	6dk8	mi089	1967	1:20000
Caffey-Ingalls-Iosco complex, 0 to 6 percent slopes	168B	5413	416342	fz7d	mi097	1994	1:20000
Iosco sand, 0 to 3 percent slopes	62A	3359	416417	fz9t	mi097	1994	1:20000
Iosco loamy sand, 0 to 3 percent slopes	40A	15296	192431	6g7g	mi113	1983	1:15840
Melita-Iosco-Kawkawlin complex, 0 to 2 percent slopes	Ms	1794	187307	68x5	mi117	1956	1:20000
Iosco loamy sand, 0 to 2 percent slopes	Ia	1383	187290	68wm	mi117	1956	1:20000
Iosco sand, 0 to 6 percent slopes	384B	1674	192266	6g24	mi119	1997	1:12000
Morganlake-Iosco-Deford complex, 0 to 6 percent slopes	422B	1640	192295	6g32	mi119	1997	1:12000
Iosco sand, 0 to 4 percent slopes	51B	7461	189931	6cmt	mi129	1987	1:15840
Iosco sandy loam, 2 to 6 percent slopes	IdB	1770	190043	6crf	mi133	1966	1:15840
Iosco loamy sand, 2 to 6 percent slopes	IcB	1668	190041	6crc	mi133	1966	1:15840
Iosco loamy sand, 0 to 2 percent slopes	IcA	550	190040	6crb	mi133	1966	1:15840
Iosco sandy loam, 0 to 2 percent slopes	IdA	361	190042	6crd	mi133	1966	1:15840
Iosco sand, 0 to 6 percent slopes	384B	57	654002	pyjv	mi135	2003	1:12000
Iosco loamy sand, 0 to 4 percent slopes	IoA	5439	192673	6gh8	mi139	1967	1:15840
Iosco and Allendale loamy sands, 0 to 4 percent slopes	IrA	3366	192674	6gh9	mi139	1967	1:15840
Iosco-Belding complex, 2 to 6 percent slopes	IsB	1283	192675	6ghb	mi139	1967	1:15840
Iosco loamy sand, 0 to 3 percent slopes	16A	7128	190866	6dlz	mi141	1989	1:15840
Saverine and Iosco fine sandy loams, 0 to 2 percent slopes	SbA0	21947	188398	6b1c	mi151	1955	1:15840
Iosco sandy loam and Covert loamy sand, 0 to 2 percent slopes	IcA0	6556	2673641	2qz3n	mi151	1955	1:15840
Iosco and Winegars sandy loams, 0 to 2 percent slopes	IbA0	5626	188293	69xz	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 2 to 7 percent slopes, slightly eroded	SbB1	2711	188399	6b1d	mi151	1955	1:15840
Iosco sandy loam and Covert loamy sand, 2 to 7 percent slopes, slightly eroded	IcB1	969	2673642	2qz3p	mi151	1955	1:15840
Iosco and Menominee loamy sands, 0 to 2 percent slopes	IaA0	854	188291	69xx	mi151	1955	1:15840
Iosco and Menominee loamy sands, 2 to 6 percent slopes, slightly eroded	IaB1	634	188292	69xy	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 7 to 14 percent slopes, slightly eroded	SbC1	350	188401	6b1g	mi151	1955	1:15840
Iosco sandy loam and Covert loamy sand, 7 to 14 percent slopes, slightly eroded	IcC1	176	2673643	2qz3q	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 7 to 14 percent slopes, moderately eroded	SbC2	145	188402	6b1h	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 14+ percent slopes, slightly eroded	SbD1	70	188403	6b1j	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 2 to 7 percent slopes, moderately eroded	SbB2	56	188400	6b1f	mi151	1955	1:15840
Iosco and Winegars sandy loams, 2 to 6 percent slopes, slightly eroded	IbB1	41	188294	69y0	mi151	1955	1:15840
Saverine and Iosco fine sandy loams, 14+ percent slopes, moderately eroded	SbD2	40	188404	6b1k	mi151	1955	1:15840
Iosco sandy loam and Covert loamy sand, 14+ percent slopes, slightly eroded	IcD1	12	2673644	2qz3r	mi151	1955	1:15840
Iosco sand, 0 to 3 percent slopes	249A	3	1650227	1sd64	mi153	2007	1:24000
Iosco loamy sand, deep variant	Iv	1084	187805	69f7	mi155	1967	1:12000
Iosco stony loamy sand, 0 to 2 percent slopes	ItA	55	187804	69f6	mi155	1967	1:12000
Iosco loamy sand, 0 to 4 percent slopes	514B	2129	1444435	1kh1p	wi003	2006	1:12000
Iosco loamy sand, 0 to 4 percent slopes	514B	655	433596	gk5z	wi007	2005	1:12000
Iosco loamy sand, 0 to 4 percent slopes	514B	1818	781306	v70f	wi031	2005	1:12000
Ellwood-Iosco-Vilas complex, 0 to 15 percent slopes	EnC	2865	430001	gfg0	wi037	1995	1:12000
Ellwood-Iosco-Morganlake complex, 0 to 6 percent slopes	EmB	1526	430000	gffz	wi037	1995	1:12000
Iosco loamy fine sand, 0 to 3 percent slopes	IsA	689	430010	gfg9	wi037	1995	1:12000
Iosco loamy sand, 0 to 4 percent slopes	514B	172	782174	v7xf	wi051	2006	1:12000
Iosco loamy fine sand, 0 to 3 percent slopes	IsA	7671	422402	g5jw	wi075	1987	1:20000
Iosco loamy sand, 0 to 4 percent slopes	IsB	405	395798	f8vp	wi078	1998	1:12000
Iosco loamy fine sand, 0 to 3 percent slopes	IsA	23477	422467	g5lz	wi083	1985	1:15840
Iosco loamy sand, 0 to 3 percent slopes	IsA	7712	422672	g5tl	wi115	1981	1:15840

Map of Series Extent

Approximate geographic distribution of the IOSCO 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).