Soil Data Explorer - ONEILL

Official Series Description

Lab Data Summary

Aggregate lab data for the ONEILL soil series. This aggregation is based on all pedons with a current taxon name of ONEILL, 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 ONEILL were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ONEILL 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 ONEILL 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 ONEILL 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 ONEILL 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 ONEILL 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 ONEILL 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 ONEILL 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 ONEILL, 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 ONEILL 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
Oneill sandy loam, 2 to 6 percent slopes	3268	2686	426982	gb9m	ne003	1975	1:20000
Oneill sandy loam, 0 to 2 percent slopes	3267	993	426981	gb9l	ne003	1975	1:20000
Oneill loam, 0 to 2 percent slopes	3264	328	426983	gb9n	ne003	1975	1:20000
Meadin-Oneill complex, 2 to 30 percent slopes	3259	47	2215937	2dcvv	ne003	1975	1:20000
Oneill-Meadin fine sandy loams, 2 to 11 percent slopes	3272	2172	357650	d053	ne015	1976	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	1149	357648	2wgf4	ne015	1976	1:20000
Oneill fine sandy loam, 2 to 6 percent slopes	3261	708	357649	2ynvg	ne015	1976	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	3872	100015	2wgf4	ne017	1987	1:20000
Oneill-Meadin sandy loams, 2 to 6 percent slopes	3274	3430	100017	3c2c	ne017	1987	1:20000
Oneill-Meadin sandy loams, 6 to 11 percent slopes	3275	2523	100018	3c2d	ne017	1987	1:20000
Oneill loam, 0 to 2 percent slopes	3264	1066	100016	3c2b	ne017	1987	1:20000
Oneill and Pivot loams, 0 to 2 percent slopes	3110	161	2228196	2dsm9	ne019	1967	1:20000
Oneill and Pivot loams, 0 to 2 percent slopes	3110	10962	1700164	1v250	ne079	2003	1:12000
Boelus, Oneill, and Pivot complex, 0 to 3 percent slopes	6645	1896	1700102	1v230	ne079	2003	1:12000
Oneill sandy loam, 2 to 6 percent slopes	3268	1104	1700165	1v251	ne079	2003	1:12000
Oneill-Meadin fine sandy loams, 6 to 11 percent slopes	3273	26573	100141	3c6c	ne089	1981	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	25368	100137	2wgf4	ne089	1981	1:20000
Oneill-Meadin fine sandy loams, 2 to 6 percent slopes	3271	24882	100140	3c6b	ne089	1981	1:20000
Oneill-Meadin fine sandy loams, 11 to 30 percent slopes	3270	16058	100142	3c6d	ne089	1981	1:20000
Oneill loam, 0 to 2 percent slopes	3264	12499	100139	3c69	ne089	1981	1:20000
Anselmo-Oneill sandy loams, 0 to 3 percent slopes	8807	11544	100071	3c43	ne089	1981	1:20000
Anselmo-Oneill sandy loams, 3 to 6 percent slopes	9020	9060	100072	3c44	ne089	1981	1:20000
Oneill fine sandy loam, 2 to 6 percent slopes	3261	7256	100138	2ynvg	ne089	1981	1:20000
Oneill loamy sand, 0 to 2 percent slopes	3266	6775	100136	3c66	ne089	1981	1:20000
Meadin-Oneill complex, 2 to 30 percent slopes	3259	420	2220304	2djdq	ne089	1981	1:20000
Oneill sandy loam, 2 to 6 percent slopes	3268	201	2219607	2dhp7	ne089	1981	1:20000
Oneill loam, 0 to 2 percent slopes	3264	879	99735	3bs8	ne093	1968	1:12000
Oneill-Meadin fine sandy loams, 0 to 2 percent slopes	3269	6883	357718	d079	ne103	1977	1:20000
Oneill loamy fine sand, 0 to 2 percent slopes	3265	4568	357714	d075	ne103	1977	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	4238	357715	2wgf4	ne103	1977	1:20000
Oneill-Valentine complex, 2 to 11 percent slopes	3277	1870	357719	d07b	ne103	1977	1:20000
Oneill fine sandy loam, 2 to 6 percent slopes	3261	964	357716	2ynvg	ne103	1977	1:20000
Oneill fine sandy loam, 6 to 11 percent slopes	3263	577	357717	d078	ne103	1977	1:20000
Meadin-Oneill complex, 2 to 30 percent slopes	3259	9377	1144262	17dpp	ne107	1989	1:20000
Oneill sandy loam, 2 to 6 percent slopes	3268	926	1144273	17dq1	ne107	1989	1:20000
Oneill sandy loam, 0 to 2 percent slopes	3267	232	1144272	17dq0	ne107	1989	1:20000
Oneill loam, 0 to 2 percent slopes	3264	9287	1709674	1vd1s	ne121	1978	1:20000
Oneill sandy loam, 0 to 2 percent slopes	3267	6420	1709672	1vd1q	ne121	1978	1:20000
Oneill sandy loam, 2 to 6 percent slopes	3268	1565	1709673	1vd1r	ne121	1978	1:20000
Oneill and Pivot loams, 0 to 2 percent slopes	3110	1327	2228251	2dsp2	ne121	1978	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	275	427507	gbvk	ne125	1958	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	661	1691754	1tsdq	ne137	1967	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	1155	427670	gc0t	ne141	1984	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	333	1692307	1tszk	ne143	1967	1:20000
Oneill sandy loam, 2 to 6 percent slopes	3268	2769	100249	3c9v	ne149	1982	1:20000
Oneill sandy loam, 0 to 2 percent slopes	3267	2594	100248	3c9t	ne149	1982	1:20000
Oneill-Meadin sandy loams, 6 to 11 percent slopes	3275	1123	100250	3c9w	ne149	1982	1:20000
Oneill fine sandy loam, 0 to 2 percent slopes	3260	314	2219837	2wgf4	ne149	1982	1:20000
Oneill-Meadin sandy loams, 2 to 6 percent slopes	3274	67	2219838	2dhxp	ne149	1982	1:20000
Oneill fine sandy loam, 2 to 6 percent slopes	OeC	1845	355272	2ynvg	sd053	1982	1:20000

Map of Series Extent

Approximate geographic distribution of the ONEILL 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).