Soil Data Explorer - KUMA

Official Series Description

Lab Data Summary

Aggregate lab data for the KUMA soil series. This aggregation is based on all pedons with a current taxon name of KUMA, 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 KUMA were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
119	76-OK-70-1	76-OK005-70-1	Kuma	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.6003639,-95.8856222
67B	91P0043	90CO063003	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.2991676,-102.5186081
67B	40A3910	S1954CO063004	Kuma	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1875,-102.3388901
72	05KS171041	05KS171041	Kuma	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.359333,-100.8318329
72	05KS171055	05KS171055	Kuma	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4020844,-100.820137
72	88P0535	88CO063183	Kuma	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.4174995,-102.5019455
72	90P0030	89CO063269A	Kuma	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1186104,-102.1294479
72	89P0556	89CO063269B	Kuma	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.1141663,-102.125
72	89P0738	89KS081017	Kuma	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.4405556,-101.0333328
72	90P0782	90NE029001	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6772232,-102.0500031
72	90P0784	90NE029001A	Kuma	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6772232,-102.0500031
72	90P0785	90NE029001B	Kuma	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.6772232,-102.0500031
72	40A3882	S1963CO115007	Kuma	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8058319,-102.3027802
72	40A3883	S1963CO115010	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.853611,-102.3291702
72	40A2126	S1974NE029001	KUMA	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.5830498,-102.0510406
72	40A2093	S1974NE029003	Kuma	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3636093,-101.5790787
72	81P0653	S1981KS179001	KUMA	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.3861122,-100.5888901
72	85P0844	S1985NE033051	Kuma	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3369806,-103.0200556
72	85P0840	S1985NE101020	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.1533583,-101.9300389
72	88P0912	S1988NE069076	Kuma	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2768,-102.5717449
72	90P0175	S1989NE049007	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2039806,-102.19725
72	03N0106	S2002KS199001	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7700958,-101.6745758
72	03N0107	S2002KS199002	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7700768,-101.6739349
72	03N0108	S2002KS199003	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.7696991,-101.6737595
72	06N0227	S2005KS171306	Kuma	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.6030273,-100.7999725
n/a	90P0025	89CO063269	Kuma	7	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 KUMA 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 KUMA 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 KUMA 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 KUMA 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 KUMA 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 KUMA 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 KUMA 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.

Soil series sharing subgroup-level classification with KUMA, 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. CO-2011-05-27-12 | Phillips County - 1971

   Typical landscape of the Rago-Platner-Kuma association showing the major soils and the minor Wages, Eckley, and Dix soils (Soil Survey of Phillips County, Colorado; 1971).

2. CO-2011-05-27-13 | Phillips County - 1971

   Cross section of Phillips County showing relationship of major soils to parent materials (Soil Survey of Phillips County, Colorado; 1971).

3. KS-2012-01-26-01 | Sheridan County - March 1984

   Typical pattern of soils in the Keith-Ulysses-Kuma association (Soil Survey of Sheridan County, Kansas; 1984).

4. NE-2010-09-09-05 | Garden County - 1999

   Typical pattern of the soils and underlying material in the Keith-Kuma-Duroc association (Soil Survey of Garden County, Nebraska; 1999).

5. NE-2012-02-10-07 | Chase County - November 1982

   Typical landscape pattern of the soils and underlying material in the Rosebud-Canyon association (Soil Survey of Chase County, Nebraska; November 1982).

6. NE-2012-02-10-08 | Chase County - November 1982

   Typical landscape pattern of the soils and underlying material in the Kuma association (Soil Survey of Chase County, Nebraska; November 1982).

7. NE-2012-02-13-43 | Keith County - November 1995

   Typical pattern of soils and parent material in the Satanta-Kuma association (Soil Survey of Keith County, Nebraska; November 1995).

Map Units

Map units containing KUMA 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
Kuma-Keith silt loams, 0 to 2 percent slopes	43	139904	96838	37rt	co063	1996	1:24000
Kuma-Keith very fine sandy loams, 1 to 3 percent slopes	42	2915	96837	37rs	co063	1996	1:24000
Kuma loam	52	3478	94535	35cj	co075	1974	1:24000
Rago and Kuma loams	Ra	179426	94784	35mk	co095	1971	1:20000
Rago and kuma silt loams, 0 to 3 percent slopes	RaB	77674	94954	35t1	co115	1969	1:15840
Keith-Kuma silt loams, 0 to 3 percent slopes	KkB	13640	94946	2s7w9	co115	1969	1:15840
Keith, goshen, and kuma silt loams, 0 to 3 percent slopes	KgB	6555	94945	35sr	co115	1969	1:15840
Rago and kuma silt loams, 3 to 5 percent slopes	RaC	2092	94955	35t2	co115	1969	1:15840
Keith-Kuma complex	33	29049	94994	2s7wb	co121	1982	1:24000
Keith-Kuma very fine sandy loams	32	8151	94993	2s7w7	co121	1982	1:24000
Kuma-Keith silt loams	25	158263	95068	35xq	co125	1976	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	126976	1149570	2v9g4	ks023	1987	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	37721	1150681	2v9g4	ks063	1974	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	2272	1150524	2v9g4	ks109	1962	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	87564	772984	2v9g4	ks153	1979	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	14251	1703765	2v9g4	ks171	1963	1:24000
Keith-Kuma silt loams, 0 to 1 percent slopes	1622	13442	1703767	1v5x7	ks171	1963	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	22911	1150000	2v9g4	ks179	1982	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	17490	1149623	2v9g4	ks181	1967	1:24000
Kuma-Keith silt loams, 0 to 2 percent slopes	1655	8040	1149624	17l8n	ks181	1967	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	47759	1150462	2v9g4	ks193	1978	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	13132	1150200	2v9g4	ks199	1984	1:24000
Kuma-Keith silt loams, 0 to 2 percent slopes	1655	64	1150201	17lw8	ks199	1984	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	18584	1699037	2v9g5	ne029	1980	1:20000
Kuma silt loam, 1 to 3 percent slopes	1653	5565	1699038	2wz9r	ne029	1980	1:20000
Kuma silt loam, 3 to 6 percent slopes	1654	945	1699039	1v0zq	ne029	1980	1:20000
Kuma loam, 0 to 1 percent slopes	1650	93469	1698692	2wz83	ne033	1989	1:20000
Kuma loam, 0 to 1 percent slopes	1650	2497	1698811	2wz83	ne049	2000	1:24000
Kuma loam, 1 to 3 percent slopes	1651	306	1698812	2wz93	ne049	2000	1:24000
Kuma loam, 0 to 1 percent slopes	1650	10294	1698755	2wz83	ne069	1995	1:20000
Kuma loam, 1 to 3 percent slopes	1651	35815	1698896	2wz93	ne101	1990	1:20000
Kuma loam, 0 to 1 percent slopes	1650	15166	1698895	2wz83	ne101	1990	1:20000
Kuma silt loam, 1 to 3 percent slopes	1653	2398	2219594	2wz9r	ne101	1990	1:20000
Kuma loam, 0 to 1 percent slopes	1650	1838	1692548	2wz83	ne105	2004	1:24000
Kuma loam, 1 to 3 percent slopes	1651	625	2219731	2wz93	ne111	1971	1:24000
Kuma silt loam, 1 to 3 percent slopes	1653	179	2219732	2wz9r	ne111	1971	1:24000
Kuma loam, 0 to 1 percent slopes	1650	44	2219730	2wz83	ne111	1971	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	28	2219776	2dhvp	ne111	1971	1:24000
Kuma silt loam, 0 to 1 percent slopes	1652	55130	1698973	2v9g5	ne135	1987	1:20000
Kuma silt loam, 1 to 3 percent slopes	1653	19820	1698974	2wz9r	ne135	1987	1:20000
Kuma loam, 0 to 1 percent slopes	1650	8396	2219564	2wz83	ne135	1987	1:20000
Kuma loam, 1 to 3 percent slopes	1651	6360	2219565	2wz93	ne135	1987	1:20000
Kuma loam, 1 to 8 percent slopes	KU	3724	56670	1wz2	nm636	1970	1:31680
Goshen-Kuma loams, 0 to 2 percent slopes	GkA	2171	104699	3hyd	wy615	1965	1:20000

Map of Series Extent

Approximate geographic distribution of the KUMA 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).