Soil Data Explorer - NEGLEY

Official Series Description

Lab Data Summary

Aggregate lab data for the NEGLEY soil series. This aggregation is based on all pedons with a current taxon name of NEGLEY, 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 NEGLEY 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
113	86IL193020	1986IL193020	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.2199528,-88.1903417
113	84IL121025	S1984IL121025	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7739111,-88.9266139
114A	DU7607	1976IN037006	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.397225,-86.9807889
114B	77IL119024	1977IL119024	Negley	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7214679,-89.6444722
114B	JN7807	1978IN071007	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8824111,-85.8943778
114B	JN7808	1978IN071008	Negley	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.879925,-85.8920361
114B	94P0264	S1993IL027004	Negley	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.5208321,-89.5694427
120B	MT8004	1980IN101004	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.6494139,-86.8955222
n/a	AD-S01	1955-OH001-S01	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	AD-S02	1955-OH001-S02	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	SK-001	1956-OH151-001	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-077	1958-OH029-077	Negley	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-100	1959-OH029-100	Negley	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	HY-064	1967-OH071-064	Negley	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	CO-131	2017OH029001	Negley	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

Competing Series

Soil series competing with NEGLEY 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 NEGLEY 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 NEGLEY 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.

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

Soil series sharing subgroup-level classification with NEGLEY, 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. IL-2010-09-09-07 | Wayne County -

   Typical pattern of soils and parent material in the Parke-Negley association (Soil Survey of Wayne County, Illinois).

Map Units

Map units containing NEGLEY 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
Negley silt loam, 10 to 15 percent slopes	585D	505	173876	5txx	il005	1981	1:12000
Negley loam,15 to 30 percent slopes	585F	1007	173414	5tg0	il051	1991	1:15840
Negley loam, 30 to 60 percent slopes	585G	518	173415	5tg1	il051	1991	1:15840
Negley loam, 18 to 35 percent slopes	585F	369	198961	6p13	il119	2001	1:12000
Hickory and Negley loams, 18 to 35 percent slopes	998F	916	1721560	1vsf6	il135	2007	1:12000
Negley loam, 18 to 35 percent slopes, eroded	585F2	973	183087	64j1	il163	1997	1:12000
Negley loam, 10 to 15 percent slopes, eroded	585D2	592	179035	609b	il173	1990	1:15840
Negley loam, 5 to 10 percent slopes, eroded	585C2	558	179034	6099	il173	1990	1:15840
Negley loam, 18 to 35 percent slopes	585F	918	2025091	25z8j	il191	2008	1:12000
Negley silt loam, 10 to 18 percent slopes, eroded	585D2	299	2025103	25z8x	il191	2008	1:12000
Negley loam, 18 to 35 percent slopes	585F	124	1543921	1ntkx	il193	2006	1:12000
Negley loam, 25 to 50 percent slopes	NeF	805	162963	5gkw	in027	1969	1:20000
Negley loam, 12 to 18 percent slopes, severely eroded	NeD3	1643	535633	kzch	in037	1978	1:15840
Negley loam, 18 to 50 percent slopes	NeF	1115	535634	kzcj	in037	1978	1:15840
Negley silt loam, 12 to 18 percent slopes, eroded	NgD2	916	535636	kzcl	in037	1978	1:15840
Negley silt loam, 6 to 12 percent slopes, eroded	NgC2	475	535635	kzck	in037	1978	1:15840
Negley silt loam, 12 to 18 percent slopes, eroded	NerD2	1055	1907084	220gv	in071	1985	1:15840
Negley loam, 18 to 35 percent slopes	NehF	544	1907088	220gz	in071	1985	1:15840
Urban land-Parke-Medora-Negley complex, 6 to 18 percent slopes	UlbC	52	1947795	23cv3	in071	1985	1:15840
Negley silt loam, 6 to 12 percent slopes, eroded	NeC2	408	964668	11ctb	in077	1982	1:15840
Negley silt loam, 2 to 6 percent slopes, eroded	NeB2	200	964667	11ct9	in077	1982	1:15840
Negley clay loam, 12 to 22 percent slopes, severely eroded	NgD3	5	975402	11qzl	in077	1982	1:15840
Negley soils, 15 to 60 percent slopes	NsE	1111	159770	5c7w	in121	1965	1:20000
Negley silt loam, 18 to 35 percent slopes	NamF	142	165723	5kfx	in143	1995	1:12000
Negley clay loam, 12 to 22 percent slopes, severely eroded	NanD3	114	165724	5kfy	in143	1995	1:12000
Negley loam, 12 to 18 percent slopes, eroded	NeD2	214	160738	5d83	in145	1968	1:15840
Negley loam, 18 to 25 percent slopes	NeE	160	160739	5d84	in145	1968	1:15840
Negley loam, 25 to 40 percent slopes	NeF	452	159682	5c51	in167	1971	1:20000
Negley loam, 18 to 25 percent slopes	NeE	197	159681	5c50	in167	1971	1:20000
Negley silt loam, 12 to 20 percent slopes	NeD	805	552056	ljg8	ky603	1968	1:15840
Negley silt loam, 6 to 12 percent slopes	NeC	760	552055	ljg7	ky603	1968	1:15840
Negley silt loam, 2 to 6 percent slopes	NeB	607	552054	ljg6	ky603	1968	1:15840
Negley gravelly loam, 25 to 40 percent slopes	NgE	360	537375	l15p	oh009	1981	1:15840
Negley loam, 8 to 15 percent slopes	NeC	330	537374	l15n	oh009	1981	1:15840
Negley loam, 12 to 20 percent slopes, eroded	NaD2	757	172290	5s8r	oh045	1998	1:12000
Negley loam, 20 to 35 percent slopes	NaE	696	172291	5s8s	oh045	1998	1:12000
Negley loam, 12 to 18 percent slopes	NdD	1821	1420482	1jp40	oh071	1973	1:15840
Negley loam, 18 to 25 percent slopes	NdE	1612	1420483	1jp41	oh071	1973	1:15840
Negley loam, 6 to 12 percent slopes	NdC	1186	1420481	1jp3z	oh071	1973	1:15840
Negley-Fox complex, 18 to 35 percent slopes	NgF	1106	1420488	1jp46	oh071	1973	1:15840
Negley clay loam, 12 to 18 percent slopes, severely eroded	NfD3	731	1420487	1jp45	oh071	1973	1:15840
Negley loam, 25 to 35 percent slopes	NdF	655	1420484	1jp42	oh071	1973	1:15840
Negley silt loam, 2 to 6 percent slopes	NeB	191	1420485	1jp43	oh071	1973	1:15840
Negley clay loam, 6 to 12 percent slopes, severely eroded	NfC3	150	1420486	1jp44	oh071	1973	1:15840
Negley loam, 20 to 35 percent slopes, eroded	NeE2	50	1420559	1jp6h	oh071	1973	1:15840
Negley loam, 15 to 25 percent slopes	NcD	24	1420688	1jpbn	oh071	1973	1:15840
Negley loam, 6 to 12 percent slopes, eroded	NdC2	1	1420558	1jp6g	oh071	1973	1:15840
Negley silt loam, 40 to 70 percent slopes	NeF	735	1398088	1hxtm	oh073	1986	1:15840
Negley silt loam, 15 to 25 percent slopes	NeD	546	1398086	1hxtk	oh073	1986	1:15840
Negley silt loam, 25 to 40 percent slopes	NeE	512	1398087	1hxtl	oh073	1986	1:15840
Negley silt loam, 8 to 15 percent slopes	NeC	186	1398085	1hxtj	oh073	1986	1:15840
Negley loam, 6 to 12 percent slopes, eroded	NbC2	19	1398189	1hxxw	oh073	1986	1:15840
Negley loam, 12 to 18 percent slopes, eroded	NeD2	2060	171059	5r01	oh089	1986	1:15840
Negley loam, 18 to 25 percent slopes	NeE	670	171060	5r02	oh089	1986	1:15840
Negley loam, 6 to 12 percent slopes, eroded	NeC2	610	171058	5r00	oh089	1986	1:15840
Negley loam, 25 to 70 percent slopes	NeF	570	171061	5r03	oh089	1986	1:15840
Negley silt loam, 25 to 40 percent slopes	NeE	14	1403158	1j335	oh129	1977	1:15840
Negley loam, 8 to 15 percent slopes	NgC	654	537670	l1h6	oh131	1984	1:15840
Negley loam, 15 to 25 percent slopes	NgD	646	537671	l1h7	oh131	1984	1:15840
Negley loam, 25 to 35 percent slopes	NgE	540	537672	l1h8	oh131	1984	1:15840
Negley loam, 20 to 35 percent slopes, eroded	NeE2	182	1689011	1tpk7	oh131	1984	1:15840
Negley loam, 6 to 12 percent slopes, eroded	NeC2	85	1689009	1tpk5	oh131	1984	1:15840
Negley loam, 6 to 12 percent slopes	NeC	37	1689027	1tpkr	oh131	1984	1:15840
Negley loam, 12 to 20 percent slopes, eroded	NeD2	31	1689010	1tpk6	oh131	1984	1:15840
Negley silt loam, 2 to 6 percent slopes	NhB	3	1689026	1tpkq	oh131	1984	1:15840
Negley loam, 20 to 35 percent slopes, eroded	NeE2	7458	170926	5qvr	oh141	1997	1:15840
Negley loam, 12 to 20 percent slopes, eroded	NeD2	2382	170925	5qvq	oh141	1997	1:15840
Negley loam, 6 to 12 percent slopes, eroded	NeC2	520	170924	5qvp	oh141	1997	1:15840

Map of Series Extent

Approximate geographic distribution of the NEGLEY 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).