Soil Data Explorer - IRONMOUND

Official Series Description

Lab Data Summary

Aggregate lab data for the IRONMOUND soil series. This aggregation is based on all pedons with a current taxon name of IRONMOUND, 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 IRONMOUND 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
80A	75-OK-75-5	75-OK015-75-5	Ironmound	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.4493528,-98.5497583
80A	93P0392	S1992OK083005	Ironmound	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.0905571,-97.6586075

Water Balance

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

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

Competing Series

Soil series competing with IRONMOUND 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 IRONMOUND 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 IRONMOUND 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 IRONMOUND, 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. OK-2010-09-29-01 | Logan County - 2006

   Typical pattern of soils and underlying material in the Grainola-Masham-Ironmound general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

2. OK-2010-09-29-02 | Logan County - 2006

   Typical pattern of soils and underlying material in the Ashport-Pulaski-Lawrie general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

3. OK-2010-09-29-03 | Logan County - 2006

   Typical pattern of soils and underlying material in the Grainola-Renfrow-Piedmont general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

4. OK-2010-09-29-05 | Logan County - 2006

   Typical pattern of soils and underlying material in the Stephenville-Darsil-Harrah general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

5. OK-2010-09-29-06 | Logan County - 2006

   Typical pattern of soils and underlying material in the Coyle-Ironmound-Zaneis general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

6. OK-2010-09-29-15 | Oklahoma County - 2004

   Typical pattern of soils and underlying material in the Renfrow-Grainola-Piedmont general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

7. OK-2010-09-29-17 | Oklahoma County - 2004

   Typical pattern of soils and underlying material in the Ashport-Miller general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

Map Units

Map units containing IRONMOUND 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
Kingfisher-Ironmound silt loams complex, 1 to 5 percent slopes	5426	2423	3293153	30x69	ks077	1965	1:24000
Ironmound-Nash complex, 3 to 12 percent slopes	IrNE	1248	622474	nwqt	ok003	1971	1:24000
Ironmound loam, 1 to 3 percent slopes	IroB	363	622532	nwsp	ok003	1971	1:24000
Ironmound loam, 3 to 5 percent slopes, eroded	IroC2	95	775000	2tq5n	ok003	1971	1:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, eroded	KgID2	30	622376	nwmn	ok003	1971	1:24000
Ironmound-Dill complex, 3 to 12 percent slopes	LuD	33659	381897	dtd8	ok015	1967	1:24000
Ironmound-Nash complex, 5 to 12 percent slopes	QwD	23832	381916	dtdw	ok015	1967	1:24000
Ironmound-Dill complex, 12 to 30 percent slopes	LuE	3624	381898	dtd9	ok015	1967	1:24000
Nash-Ironmound complex, 3 to 8 percent slopes	NaD	12683	381962	dtgc	ok017	1972	1:24000
Grant-Ironmound complex, 5 to 8 percent slopes	GuD	6017	381949	dtfy	ok017	1972	1:24000
Nash-Ironmound complex, 3 to 8 percent slopes, eroded	NaD2	5730	381963	dtgd	ok017	1972	1:24000
Dill-Ironmound complex, 5 to 8 percent slopes	DuD	5267	381939	dtfm	ok017	1972	1:24000
Ironmound-Rock outcrop complex, 12 to 30 percent slopes	QrF	5040	381974	dtgr	ok017	1972	1:24000
Ironmound-Dill complex, 5 to 12 percent slopes	QdE	2924	381973	dtgq	ok017	1972	1:24000
Grant-Ironmound complex, 3 to 8 percent slopes, eroded	GuD2	2400	381950	dtfz	ok017	1972	1:24000
Nash-Ironmound complex, 3 to 8 percent slopes, severely eroded	NaD3	1230	381964	dtgf	ok017	1972	1:24000
Kingfisher-Ironmound complex, 1 to 5 percent slopes	9	7075	382153	2tq6c	ok027	1984	1:24000
Grainola-Ironmound complex, 5 to 12 percent slopes	6	5240	382122	dtmj	ok027	1984	1:24000
Ironmound very fine sandy loam, 5 to 8 percent slopes	29	599	382096	dtlp	ok027	1984	1:24000
Kingfisher-Urban land-Ironmound complex, 1 to 5 percent slopes	28	139	382095	2tq6g	ok027	1984	1:24000
Grainola-Masham-Ironmound complex, 5 to 12 percent slopes	VrD	38392	382533	dv1s	ok047	1965	1:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, eroded	GnD2	9974	382494	dv0j	ok047	1965	1:24000
Kingfisher-Ironmound complex, 8 to 20 percent slopes, eroded	GnE2	7568	382496	dv0l	ok047	1965	1:24000
Kingfisher-Ironmound complex, 8 to 20 percent slopes	GnE	7419	382495	dv0k	ok047	1965	1:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes	GnD	2701	382493	dv0h	ok047	1965	1:24000
Ironmound very fine sandy loam, 3 to 5 percent slopes	LuC	814	382503	dv0t	ok047	1965	1:24000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, eroded	KlD2	244	382499	dv0p	ok047	1965	1:24000
Ironmound-Nash complex, 5 to 12 percent slopes	47	8394	382580	dv39	ok049	1982	1:24000
Ironmound stony loam, 12 to 30 percent slopes	46	5732	382579	dv38	ok049	1982	1:24000
Ironmound-Rock outcrop complex, 12 to 30 percent slopes	42	7629	382663	dv5z	ok051	1975	1:24000
Ironmound-Nash complex, 3 to 12 percent slopes	46	5635	382736	dv8b	ok053	1983	1:24000
Ironmound loam, 1 to 3 percent slopes	44	3398	382734	dv88	ok053	1983	1:24000
Ironmound loam, 3 to 5 percent slopes, eroded	45	3137	382735	2tq5n	ok053	1983	1:24000
Kingfisher-Ironmound silt loams complex, 1 to 5 percent slopes	KgIC	545	3293154	30x69	ok053	1983	1:24000
Grainola-Ironmound complex, 5 to 15 percent slopes	VlE	34919	383544	dw3d	ok081	1966	1:24000
Coyle-Ironmound complex, 3 to 5 percent slopes, eroded	CoIC2	27851	383599	2wrk6	ok083	1994	1:12000
Ironmound-Coyle complex, 5 to 15 percent slopes	IrCE	19306	383631	2tq5p	ok083	1994	1:12000
Masham-Ironmound complex, 5 to 15 percent slopes	MaID	14389	383645	dw6n	ok083	1994	1:12000
Coyle-Ashport frequently flooded-Ironmound complex, 1 to 8 percent slopes	CAID	6262	383597	dw53	ok083	1994	1:12000
Ironmound-Coyle-Grainola complex, 5 to 8 percent slopes, severely eroded	ICGD3	3456	383630	dw65	ok083	1994	1:12000
Masham-Ironmound complex, 15 to 40 percent slopes	MaIG	1514	383646	dw6p	ok083	1994	1:12000
Ironmound loam, 3 to 5 percent slopes, eroded	IroC2	878	383632	2tq5n	ok083	1994	1:12000
Grainola-Ironmound complex, 3 to 12 percent slopes	GrIE	62	1587477	1q8wy	ok083	1994	1:12000
Kingfisher-Ironmound complex, 5 to 8 percent slopes, shallow, eroded	KgID2	50	1383569	1hfq8	ok093	1965	1:24000
Grainola-Ironmound complex, 3 to 12 percent slopes	GrIE	6478	384297	dwwp	ok109	1996	1:12000
Grainola-Urban land-Ironmound complex, 3 to 12 percent slopes	GUIE	4046	384291	dwwh	ok109	1996	1:12000
Ironmound-Coyle complex, 5 to 15 percent slopes	IrCE	1186	384307	2tq5p	ok109	1996	1:12000
Kingfisher-Ironmound complex, 1 to 5 percent slopes	KgIC	1080	384313	2tq6c	ok109	1996	1:12000
Coyle-Ironmound complex, 3 to 5 percent slopes, eroded	CoIC2	604	384277	2wrk6	ok109	1996	1:12000
Ironmound-Kingfisher complex, 1 to 8 percent slopes	IrKD	544	384308	dwx1	ok109	1996	1:12000
Kingfisher-Urban land-Ironmound complex, 1 to 5 percent slopes	KUIC	412	384309	2tq6g	ok109	1996	1:12000

Map of Series Extent

Approximate geographic distribution of the IRONMOUND 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).