Soil Data Explorer - BARNEY

Official Series Description

Lab Data Summary

Aggregate lab data for the BARNEY soil series. This aggregation is based on all pedons with a current taxon name of BARNEY, 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY 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 BARNEY, 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. NE-2012-02-08-12 | Butler County - February 1982

   Typical pattern of soils in the Alda-Boel-Barney association and the Gibbon-Muir-Zook association and relationship of the soils to topography and parent material (Soil Survey of Butler County, Nebraska; February 1982).

2. NE-2012-02-10-04 | Cedar County - October 1985

   Typical pattern of soils in the Sarpy-Blake-Albaton association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

3. NE-2012-02-10-22 | Custer County - July 1982

   Typical pattern of soils and relationship of soils to topography and parent material in three associations: No. 8—Cozad association; No. 13—Ipage-Valentine association; No. 14—Boel-Barney-Gannett association (Soil Survey of Custer County, Nebraska; July 1982).

4. NE-2012-02-13-18 | Greeley County - April 1993

   Typical pattern of soils and parent material in the Hord-Cozad and the Boel-Loup-Leshara associations (Soil Survey of Greeley County, Nebraska; April 1993).

5. NE-2012-02-13-60 | Morrill County - August 1985

   A generalized cross section of Morrill County that shows the relationship of parent material, soil associations, and elevation (Soil Survey of Morrill County, Nebraska; August 1985).

6. NE-2012-02-13-76 | Red Willow County - April 1967

   Typical pattern of soils in the Sandy alluvial land-Las-Glenberg association (Soil Survey of Red Willow County, Nebraska; April 1967).

7. NE-2012-02-13-82 | Saunders County - January 1965

   Soils in the Sarpy-Barney association (Soil Survey of Saunders County, Nebraska; January 1965).

8. NE-2012-02-13-99 | Sherman County - May 1990

   Typical pattern of soils and parent material in the Loup-Bolent-Barney and Gibbon-Wann-Saltine associations (Soil Survey of Sherman County, Nebraska; May 1990).

9. NE-2012-02-14-11 | Valley County - October 1985

   Typical pattern of soils and parent material in the Cozad-Hord and Boel-Loup-Leshara associations (Soil Survey of Valley County, Nebraska; October 1985).

Map Units

Map units containing BARNEY 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
Barney-Boel-Calamus complex, channeled	6320	942	1152523	17p95	ne003	1975	1:20000
Barney silt loam, channeled, frequently flooded	6314	965	427070	gbdg	ne011	1966	1:20000
Barney silt loam, channeled, frequently flooded	6314	2037	357610	d03t	ne015	1976	1:20000
Barney loam, frequently flooded, wet	6304	160	2570432	2r98l	ne015	1976	1:20000
Inavale-Barney complex, channeled, occasionally flooded	2350	3260	99992	3c1k	ne017	1987	1:20000
Barney fine sandy loam, frequently flooded	6311	1281	99979	3c14	ne017	1987	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	1120	1700095	2y22g	ne019	1967	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	1365	1691260	2y22g	ne023	1979	1:20000
Platte-Barney complex, channeled, frequently flooded	8569	175	2219052	2dh3b	ne023	1979	1:20000
Barney silty clay loam, 0 to 2 percent slopes, frequently flooded	6315	6	2219037	2y22c	ne023	1979	1:20000
Barney variant fine sand, frequently flooded	6317	2122	427081	gbdt	ne027	1982	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	42	2216964	2y22g	ne037	1980	1:20000
Barney sandy loam, frequently flooded	6318	1406	427788	gc4m	ne039	1973	1:20000
Barney fine sandy loam, frequently flooded	6311	3463	1699571	1v1jw	ne041	1980	1:20000
Barney loam, channeled, frequently flooded	6313	122	2228171	2dslh	ne041	1980	1:20000
Barney fine sandy loam, occasionally flooded	6308	1761	426714	gb0z	ne043	1972	1:20000
Platte-Barney complex, channeled, frequently flooded	8569	1134	2217106	2df2k	ne053	1975	1:20000
Barney silty clay loam, 0 to 2 percent slopes, frequently flooded	6315	22	2217102	2y22c	ne053	1975	1:20000
Platte, Inglewood, and Barney soils, frequently flooded	8566	2256	1710948	1vfcw	ne055	2007	1:12000
Platte-Barney complex, channeled, frequently flooded	8569	3	2217111	2df2q	ne055	2007	1:12000
Barney soils, frequently flooded	6316	793	1699429	2zwld	ne063	1973	1:20000
Barney soils, frequently flooded	6316	804	1699728	2zwl5	ne065	1975	1:20000
Barney silty clay loam, 0 to 2 percent slopes, frequently flooded	6315	9	3411590	2zwlf	ne065	1975	1:20000
Barney loam, channeled, frequently flooded	6313	549	1699769	1v1r8	ne071	1984	1:20000
Barney loam, channeled, frequently flooded	6313	215	1699926	1v1xb	ne077	1987	1:20000
Barney-Bolent complex, frequently flooded	6322	1869	1700100	1v22y	ne079	2003	1:12000
Barney complex, channeled, frequently flooded	6310	1176	1700099	1v22x	ne079	2003	1:12000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	8	2218798	2y22g	ne081	1982	1:20000
Barney loam, occasionally flooded	6309	1701	1699310	2zwlg	ne087	1965	1:20000
Barney-Boel-Calamus complex, channeled	6320	15102	100126	3c5w	ne089	1981	1:20000
Barney silt loam, channeled, frequently flooded	6314	2344	100073	3c45	ne089	1981	1:20000
Barney loam, frequently flooded, wet	6304	114	2570449	2r98l	ne089	1981	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	41	2228922	2y22g	ne093	1968	1:12000
Barney-Bolent complex, channeled, occasionally flooded	6321	2072	1145691	17g5s	ne103	1977	1:20000
Barney fine sandy loam, frequently flooded	6311	1214	357680	d062	ne103	1977	1:20000
Barney-Boel complex, channeled	6319	98	2217598	2dflf	ne103	1977	1:20000
Barney loam, frequently flooded, wet	6304	1460	2570462	2r98l	ne107	1989	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	843	849184	2y22g	ne107	1989	1:20000
Barney soils, frequently flooded	6316	510	2219765	2zwld	ne111	1971	1:24000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	2083	1709622	2y22g	ne121	1978	1:20000
Barney complex, channeled, frequently flooded	6310	327	2228256	2dsp7	ne121	1978	1:20000
Barney-Bolent complex, frequently flooded	6322	3	2228257	2dsp8	ne121	1978	1:20000
Barney loam, frequently flooded	6312	7840	1692581	1tt8d	ne123	1981	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	33	2217199	2y22g	ne141	1984	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	1286	2218985	2y22g	ne143	1967	1:20000
Barney-Alda complex, frequently flooded	6307	1004	1692320	1tszz	ne143	1967	1:20000
Barney silty clay loam, 0 to 2 percent slopes, frequently flooded	6315	1565	1699444	2zwlf	ne145	1965	1:20000
Barney loam, occasionally flooded	6309	36	2219075	2zwlg	ne145	1965	1:20000
Barney soils, frequently flooded	6316	24	2219109	2zwld	ne145	1965	1:20000
Barney-Boel complex, channeled	6319	2899	100229	3c96	ne149	1982	1:20000
Inavale-Barney complex, channeled, occasionally flooded	2350	399	2219833	2dhxj	ne149	1982	1:20000
Platte, Inglewood, and Barney soils, frequently flooded	8566	601	1711012	1vffy	ne153	2007	1:12000
Platte-Barney complex, channeled, frequently flooded	8569	2679	1691441	1ts2m	ne155	1995	1:12000
Barney silty clay loam, 0 to 2 percent slopes, frequently flooded	6315	2495	1691412	2y22c	ne155	1995	1:12000
Barney loam, frequently flooded	6312	7481	1653800	1shxd	ne157	1965	1:20000
Barney loam, channeled, frequently flooded	6313	1967	1699978	1v1z0	ne163	1987	1:20000
Barney loam, 0 to 2 percent slopes, frequently flooded	6312	857	426812	2y22g	ne167	1980	1:20000
Barney loam, channeled, frequently flooded	6313	1824	1699870	1v1vj	ne175	1983	1:20000
Platte, Inglewood, and Barney soils, frequently flooded	8566	124	2217312	2df96	ne177	2000	1:12000

Map of Series Extent

Approximate geographic distribution of the BARNEY 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).