Soil Data Explorer - ITMANN

Official Series Description

Lab Data Summary

Aggregate lab data for the ITMANN soil series. This aggregation is based on all pedons with a current taxon name of ITMANN, 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 ITMANN 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
125	07N0505	07KY650004	Itmann	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6648472,-84.5296667

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ITMANN 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 ITMANN 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 ITMANN 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 ITMANN 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 terrace figure.

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

Competing Series

Soil series competing with ITMANN 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 ITMANN 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 ITMANN 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 terrace figure.

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

Soil series sharing subgroup-level classification with ITMANN, 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

No block diagrams are available.

Map Units

Map units containing ITMANN 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
Itmann very channery loam, 25 to 70 percent slopes	Itm6F1	741	2896664	2rfb2	oh013	1978	1:15840
Itmann very channery loam, 0 to 8 percent slopes	Itm6B1	421	2896662	2rfb0	oh013	1978	1:15840
Itmann very channery loam, 8 to 25 percent slopes	Itm6D1	334	2896663	2rfb1	oh013	1978	1:15840
Itmann very channery loam, 0 to 8 percent slopes	Itm6B1	83	2899895	2rfb0	oh115	1992	1:15840
Itmann very channery loam, 25 to 70 percent slopes	Itm6F1	23	2899897	2rfb2	oh115	1992	1:15840
Itmann very channery loam, 8 to 25 percent slopes	Itm6D1	3	2899896	2rfb1	oh115	1992	1:15840
Itmann extremely channery loam, 8 to 25 percent slopes	ItD	137	2421744	2m90s	pa005	2012	1:24000
Itmann extremely channery loam, 25 to 70 percent slopes	IxF	42	2421745	2m90t	pa005	2012	1:24000
Itmann extremely channery loam, 0 to 8 percent slopes	ItB	20	2421743	2m90r	pa005	2012	1:24000
Itmann extremely channery loam, 0 to 8 percent slopes	ItB	48	557477	lq34	pa031	2012	1:24000
Itmann extremely channery loam, 8 to 15 percent slopes	ItC	37	3393301	30syj	pa031	2012	1:24000
Itmann extremely channery loam, 15 to 25 percent slopes	ItD	23	3393302	30syk	pa031	2012	1:24000
Mine dumps	Md	852	540755	l4pq	pa043	1967	1:15840
Itmann extremely channery loam, 8 to 25 percent slopes	ItD	1178	1591171	1qdr3	pa051	2005	1:24000
Itmann extremely channery loam, 0 to 8 percent slopes	ItB	776	1591170	1qdr2	pa051	2005	1:24000
Itmann extremely channery loam, 25 to 70 percent slopes	IxF	653	1591172	1qdr4	pa051	2005	1:24000
Itmann extremely channery loam, 8 to 25 percent slopes	ItD	1132	2393876	2lc0t	pa063	2012	1:24000
Itmann extremely channery loam, 0 to 8 percent slopes	ItB	340	2393875	2lc0s	pa063	2012	1:24000
Itmann extremely channery loam, 25 to 70 percent slopes	IxF	271	2393877	2lc0v	pa063	2012	1:24000
Itmann extremely channery loam, 25 to 70 percent slopes	IxF	156	2398985	2ljbm	pa065	2012	1:12000
Itmann extremely channery loam, 25 to 70 percent slopes	IxF	1231	544677	l8s7	pa129	2003	1:24000
Itmann extremely channery loam, 8 to 25 percent slopes	ItD	454	581191	mhs3	pa129	2003	1:24000
Itmann extremely channery loam, 0 to 8 percent slopes	ItB	345	581192	mhs4	pa129	2003	1:24000
Itmann very parachannery loam, 4 to 55 percent slopes	ItE	54	2406065	2lrq0	tn650	2008	1:12000
Itmann gravelly loam, 0 to 80 percent slopes	12F	116	1670923	1t2qr	va027	2006	1:24000
Itmann gravelly loam, 0 to 80 percent slopes	12F	70	2399869	2lk84	va051	2008	1:24000
Itmann extremely channery sandy loam, 0 to 80 percent slopes	19E	263	521705	khw6	va105	1997	1:24000
Itmann gravelly loam, 0 to 80 percent slopes	37G	47	2508562	2q7q9	va195	2010	1:24000
Itmann very channery loam, 8 to 25 percent slopes	ImD	130	2900023	2rfb1	wv001	1965	1:12000
Itmann very channery loam, 0 to 8 percent slopes	ImB	118	2900022	2rfb0	wv001	1965	1:12000
Itmann very channery loam, 25 to 70 percent slopes	ImF	77	2900024	2rfb2	wv001	1965	1:12000
Itmann extremely channery sandy loam, very steep	ItF	1125	514859	k8rc	wv005	1988	1:24000
Itmann channery loam, steep	ImE	340	514858	k8rb	wv005	1988	1:24000
Itmann channery clay loam, very steep	ItF	696	516101	kb1f	wv015	1998	1:24000
Itmann channery clay loam, steep	ItE	111	514906	k8sw	wv021	1995	1:24000
Itmann very channery loam, 25 to 75 percent slopes, very stony, reclaimed	IrF	79	3054891	2xb1w	wv039	1976	1:20000
Itmann very channery loam, 0 to 8 percent slopes, very stony, reclaimed	IrB	69	3054889	2xb1t	wv039	1976	1:20000
Itmann very channery loam, 8 to 25 percent slopes, very stony, reclaimed	IrD	40	3054890	2xb1v	wv039	1976	1:20000
Itmann extremely channery loam, 8 to 25 percent slopes, very stony, unreclaimed	IuD	23	3054874	2xb0q	wv039	1976	1:20000
Itmann extremely channery loam, 25 to 75 percent slopes, very stony, unreclaimed	IuF	18	3054875	2xb0r	wv039	1976	1:20000
Itmann extremely channery sandy loam, very steep	ItF	2060	532213	kvt5	wv047	1993	1:24000
Itmann very channery loam, 8 to 25 percent slopes	ImD	341	2900079	2rfb1	wv051	2007	1:12000
Itmann very channery loam, 25 to 70 percent slopes	ImF	201	2900080	2rfb2	wv051	2007	1:12000
Itmann very channery loam, 0 to 8 percent slopes	ImB	92	2900078	2rfb0	wv051	2007	1:12000
Itmann channery clay loam, 0 to 8 percent slopes	ItB	223	1882994	216dr	wv077	1955	1:24000
Itmann channery clay loam, steep	ItF	131	1600445	1qqd8	wv077	1955	1:24000
Itmann extremely channery loam, 8 to 25 percent slopes, very stony, unreclaimed	IuD	141	3054895	2xb0q	wv079	1981	1:20000
Itmann extremely channery loam, 25 to 75 percent slopes, very stony, unreclaimed	IuF	61	3054896	2xb0r	wv079	1981	1:20000
Itmann very channery loam, 0 to 8 percent slopes, very stony, reclaimed	IrB	3	3054901	2xb1t	wv079	1981	1:20000
Itmann very channery loam, 0 to 8 percent slopes	ImB	92	2900093	2rfb0	wv097	1981	1:20000
Itmann very channery loam, 8 to 25 percent slopes	ImD	57	2900094	2rfb1	wv097	1981	1:20000
Itmann very channery loam, 25 to 70 percent slopes	ImF	53	2900095	2rfb2	wv097	1981	1:20000
Itmann channery loam, very steep	ItF	294	515129	k912	wv101	1992	1:24000
Itmann very channery sandy loam, very steep	ItF	1345	513499	k7bh	wv109	1984	1:24000
Itmann channery loam, steep	ImE	350	513498	k7bg	wv109	1984	1:24000
Itmann very channery sandy loam	It	20	514044	k7x2	wv602	1965	1:20000
Itmann very channery loam, 25 to 70 percent slopes	ImF	285	2900125	2rfb2	wv610	1973	1:20000
Itmann very channery loam, 0 to 8 percent slopes	ImB	280	2900123	2rfb0	wv610	1973	1:20000
Itmann very channery loam, 8 to 25 percent slopes	ImD	190	2900124	2rfb1	wv610	1973	1:20000
Itmann very channery loam, 8 to 25 percent slopes	ImD	1615	2900161	2rfb1	wv611	1977	1:20000
Itmann very channery loam, 25 to 70 percent slopes	ImF	1286	2900162	2rfb2	wv611	1977	1:20000
Itmann very channery loam, 0 to 8 percent slopes	ImB	1016	2900160	2rfb0	wv611	1977	1:20000
Itmann extremely channery sandy loam, very steep	ImF	250	1155547	17sfq	wv620	2005	1:24000
Itmann very channery sandy loam, very steep	ImF	44	2427116	2mgm2	wv622	2010	1:12000
Itmann very channery sandy loam, 0 to 15 percent slopes	ImC	6	2513083	2q9pv	wv622	2010	1:12000
Itmann very channery sandy loam, very steep	ItF	427	2453230	2nbsg	wv705	2009	1:24000
Itmann very channery sandy loam, 0 to 15 percent slopes	ItC	269	2453229	2nbsf	wv705	2009	1:24000
Itmann very channery sandy loam, very steep	ItF	370	2516662	261cm	wv713		1:24000
Itmann channery sandy loam, very steep	ItF	1378	2514096	k7ls	wv767	2011	1:20000

Map of Series Extent

Approximate geographic distribution of the ITMANN 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).