Soil Data Explorer - ARMO

Official Series Description

Lab Data Summary

Aggregate lab data for the ARMO soil series. This aggregation is based on all pedons with a current taxon name of ARMO, 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 ARMO 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
73	00KS105001	00KS105001ksu	Armo	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0881386,-98.3776093
73	40A1827	68KS051003	Armo	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.125,-99.0999985
73	40A1826	68KS051007	Armo	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0694427,-99.2147217
73	70KS051002	70KS051002	Armo	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0692101,-99.217453
73	10N0481	S10KS167002	Armo	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.0148888,-98.6322479
73	00P1386	S2000KS105001	Armo	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.8866959,-98.2211914

Water Balance

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

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

Competing Series

Soil series competing with ARMO 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 ARMO 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 ARMO 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 ARMO, 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. KS-2012-01-20-58 | Ellsworth County - February 1989

   Pattern of soils and parent material in the Harney-Armo association (Soil Survey of Ellsworth County, Kansas; 1989).

2. KS-2012-01-23-41 | Jewell County - May 1984

   Typical pattern of soils and underlying material in the Brownell-Wakeen-Bogue association (Soil Survey of Jewell County, Kansas; 1984).

3. KS-2012-01-23-42 | Jewell County - May 1984

   Typical pattern of soils and underlying material in the Harney-Roxbury-Corinth association (Soil Survey of Jewell County, Kansas; 1984).

4. KS-2012-01-24-01 | Lincoln County - May 1985

   Typical pattern of soils and parent material in the Harney-Nibson-Armo association (Soil Survey of Lincoln County, Kansas; 1985).

5. KS-2012-01-26-16 | Trego County - February 1990

   Pattern of soils and parent material in the Armo-Heizer-Brownell association (Soil Survey of Trego County, Kansas; 1990).

6. KS-2012-01-26-17 | Trego County - February 1990

   Pattern of soils and parent material in the Penden-Armo association (Soil Survey of Trego County, Kansas; 1990).

Map Units

Map units containing ARMO 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
Armo loam, 3 to 7 percent slopes	2519	4	1440460	2twcy	ks009	1979	1:24000
Armo silt loam, 3 to 7 percent slopes	2522	16355	1382019	2twd0	ks029	1972	1:24000
Armo loam, 3 to 7 percent slopes	2519	63	1382017	2twcy	ks029	1972	1:24000
Armo loam, 7 to 15 percent slopes	2521	20	1382018	2twcz	ks029	1972	1:24000
Lancaster-Armo loams, 3 to 7 percent slopes	3395	20	1382033	2tpw2	ks029	1972	1:24000
Armo loam, 3 to 7 percent slopes	2519	32405	1150098	2twcy	ks051	1970	1:24000
Armo loam, 7 to 15 percent slopes	2521	26672	1150100	2twcz	ks051	1970	1:24000
Harney-Armo complex, 3 to 7 percent slopes, eroded	2618	22893	1150132	2vvm4	ks051	1970	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	18405	1150105	2xmlr	ks051	1970	1:24000
Heizer-Armo complex, 8 to 25 percent slopes	2658	16433	1150139	2twfw	ks051	1970	1:24000
Armo loam, 1 to 3 percent slopes	2518	6061	1150097	2twcx	ks051	1970	1:24000
Armo loam, 3 to 7 percent slopes, eroded	2520	2077	1150099	2twf4	ks051	1970	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	455	1150101	2xmls	ks051	1970	1:24000
Armo loam, 3 to 7 percent slopes	2519	17696	1382200	2twcy	ks053	1985	1:24000
Armo loam, 7 to 15 percent slopes	2521	14176	1382201	2twcz	ks053	1985	1:24000
Armo loam, 3 to 7 percent slopes	2519	3917	1150787	2twcy	ks065	1985	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	14983	1381837	2xmlr	ks089	1981	1:24000
Armo loam, 1 to 3 percent slopes	2518	11879	1381834	2twcx	ks089	1981	1:24000
Armo loam, 3 to 7 percent slopes	2519	6368	1381835	2twcy	ks089	1981	1:24000
Armo loam, 7 to 15 percent slopes	2521	35835	1382077	2twcz	ks105	1983	1:24000
Armo loam, 3 to 7 percent slopes	2519	18250	1382076	2twcy	ks105	1983	1:24000
Lancaster-Armo loams, 3 to 7 percent slopes	3395	160	1382093	2tpw2	ks105	1983	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	8014	1381958	2xmlr	ks123	1977	1:24000
Roxbury-Armo complex, 0 to 3 percent slopes	2237	5039	1381996	307ny	ks123	1977	1:24000
Armo loam, 3 to 7 percent slopes	2519	4612	1381954	2twcy	ks123	1977	1:24000
Armo loam, 7 to 15 percent slopes	2521	4544	1381955	2twcz	ks123	1977	1:24000
Lancaster-Armo loams, 3 to 7 percent slopes	3395	1837	1381983	2tpw2	ks123	1977	1:24000
Armo silt loam, 3 to 7 percent slopes	2522	17	1381956	2twd0	ks123	1977	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	6	1381957	2xmls	ks123	1977	1:24000
Armo loam, 1 to 3 percent slopes	2518	6	1381953	2twcx	ks123	1977	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	58496	1151000	2xmls	ks141	1971	1:24000
Armo silt loam, 3 to 7 percent slopes	2522	4857	1150998	2twd0	ks141	1971	1:24000
Armo loam, 3 to 7 percent slopes	2519	327	1150996	2twcy	ks141	1971	1:24000
Armo silt loam, 3 to 7 percent slopes, eroded	2523	213	1150999	2twf5	ks141	1971	1:24000
Roxbury-Armo complex, 0 to 3 percent slopes	2237	191	1151031	307ny	ks141	1971	1:24000
Armo loam, 7 to 15 percent slopes	2521	186	1150997	2twcz	ks141	1971	1:24000
Armo silt loam, 3 to 7 percent slopes	2522	3685	1382110	2twd0	ks143	1978	1:24000
Armo loam, 3 to 7 percent slopes	2519	445	1382109	2twcy	ks143	1978	1:24000
Armo loam, 3 to 7 percent slopes	2519	3678	1150895	2twcy	ks147	1985	1:24000
Roxbury-Armo complex, 0 to 3 percent slopes	2237	129	1150922	307ny	ks147	1985	1:24000
Armo silt loam, 3 to 7 percent slopes	2522	177	1381887	2twd0	ks157	1965	1:24000
Armo loam, 3 to 7 percent slopes	2519	23	1381886	2twcy	ks157	1965	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	8	1381888	2xmlr	ks157	1965	1:24000
Armo loam, 3 to 7 percent slopes	2519	15098	1150221	2twcy	ks163	1980	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	5323	1150224	2xmls	ks163	1980	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	1937	1150227	2xmlr	ks163	1980	1:24000
Armo loam, 1 to 3 percent slopes	2518	1724	1150220	2twcx	ks163	1980	1:24000
Armo loam, 3 to 7 percent slopes, eroded	2520	151	1150222	2twf4	ks163	1980	1:24000
Heizer-Armo complex, 8 to 25 percent slopes	2658	78	1150244	2twfw	ks163	1980	1:24000
Armo loam, 7 to 15 percent slopes	2521	61	1150223	2twcz	ks163	1980	1:24000
Armo loam, 3 to 7 percent slopes	2519	158	1152113	2twcy	ks165	1978	1:24000
Armo loam, 1 to 3 percent slopes	2518	17	1152112	2twcx	ks165	1978	1:24000
Armo loam, 7 to 15 percent slopes	2521	17	1152114	2twcz	ks165	1978	1:24000
Harney-Armo complex, 3 to 7 percent slopes, eroded	2618	4	1152125	2vvm4	ks165	1978	1:24000
Armo loam, 3 to 7 percent slopes	2519	31870	1150939	2twcy	ks167	1980	1:24000
Armo loam, 7 to 15 percent slopes	2521	25600	1150940	2twcz	ks167	1980	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	70	1150941	2xmls	ks167	1980	1:24000
Harney-Armo complex, 3 to 7 percent slopes, eroded	2618	22	1150960	2vvm4	ks167	1980	1:24000
Bogue-Armo complex, 5 to 25 percent slopes	2540	13	1150944	2xmlr	ks167	1980	1:24000
Roxbury-Armo complex, 0 to 3 percent slopes	2237	10560	1151138	307ny	ks183	1974	1:24000
Armo loam, 3 to 7 percent slopes	2519	6122	1151102	2twcy	ks183	1974	1:24000
Armo-Bogue complex, 7 to 20 percent slopes	2524	240	1151103	2xmls	ks183	1974	1:24000
Armo loam, 3 to 7 percent slopes	2519	35969	1150829	2twcy	ks195	1986	1:24000
Armo loam, 7 to 15 percent slopes	2521	31409	1150831	2twcz	ks195	1986	1:24000
Armo loam, 1 to 3 percent slopes	2518	16004	1150828	2twcx	ks195	1986	1:24000
Harney-Armo complex, 3 to 7 percent slopes, eroded	2618	12	1150851	2vvm4	ks195	1986	1:24000
Heizer-Armo complex, 8 to 25 percent slopes	2658	7	1150854	2twfw	ks195	1986	1:24000
Armo loam, 3 to 7 percent slopes, eroded	2520	1	1150830	2twf4	ks195	1986	1:24000

Map of Series Extent

Approximate geographic distribution of the ARMO 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).