Soil Data Explorer - ADAIR

Official Series Description

Lab Data Summary

Aggregate lab data for the ADAIR soil series. This aggregation is based on all pedons with a current taxon name of ADAIR, 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 ADAIR 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
107B	40A1386	S1955IA165002	Adair	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.5341682,-95.2686081
108C	84P0424	83IA107001	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3400002,-92.269722
108C	84P0425	83IA107002	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.3391685,-92.2694473
108C	85P0462	84IA1070033	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4305573,-92.2444458
108C	87P0348	86IA1070058	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4286118,-92.2141647
108C	87P0349	86IA1070059	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.4288902,-92.2152786
108D	84P0382	83IA003003	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.0766678,-94.6627808
108D	84P0390	83IA029201	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2613907,-94.8527756
108D	85P0502	84IA0030043	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9422379,-94.7349701
108D	85P0503	84IA0030044	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9425125,-94.7358093
108D	85P0564	84IA1730011	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8194427,-94.8616638
108D	85P0565	84IA1730012	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.8194427,-94.8616638
108D	86P0319	85IA0030053	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9469452,-94.663887
108D	86P0320	85IA0030054	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.9469452,-94.6636124
108D	86P0333	85IA0290041	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	41.2555542,-94.8525009
108D	86P0465	85IA1730042	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7708321,-94.7050018
108D	86P0464	86IA1730041	Adair	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.7708321,-94.7052765
109	M8812909	1988MO129009m	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.416111,-93.6502762
109	M8912905	1989MO129005m	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.4150009,-93.4511108
109	M8912912	1989MO129012m	Adair	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2961121,-93.4280548
109	M8912915	1989MO129015m	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3236122,-93.4491653
109	M8912919	1989MO129019	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3005562,-93.7155533
109	M8912924	1989MO129024m	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.3024639,-93.6670333
115B	M8717109	1987MO171009	Adair	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012
115B	M8817108	1988MO171008	Adair	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.9672203,-92.3450012

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ADAIR 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 ADAIR 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 ADAIR 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 ADAIR 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 ADAIR 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 ADAIR 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 ADAIR 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 ADAIR, 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. IA-2010-09-09-21 | Shelby County - 2007

   Diagram showing the relationships of the upland soils in the eastern part of Shelby County to parent material and landforms (Soil Survey of Shelby County, Iowa; 2007).

2. IA-2011-05-31-05 | Audubon County - 1984

   Pattern of soils and parent material in the Marshall-Shelby-Adair association (Soil Survey of Audubon County, Iowa; 1984).

3. IA-2011-05-31-06 | Audubon County - 1984

   Pattern of soils and parent material in the Sharpsburg-Shelby-Marshall association (Soil Survey of Audubon County, Iowa; 1984).

4. IA-2011-05-31-08 | Audubon County - 1984

   Relationship of the major soils in Audubon County to the parent material (Soil Survey of Audubon County, Iowa; 1984).

5. IA-2011-06-01-18 | Montgomery County - 1989

   Typical pattern of soils and parent material in the Marshall-Exira association (Soil Survey of Montgomery County, Iowa; 1989).

6. IA-2011-06-01-19 | Montgomery County - 1989

   Typical pattern of soils and parent material in the Sharpsburg-Shelby association (Soil Survey of Montgomery County, Iowa; 1989).

7. IA-2011-06-01-41 | Ringgold County - 1992

   Typical pattern of soils and parent material in the Arispe-Shelby-Lamoni association (Soil Survey of Ringgold County, Iowa; 1992).

8. IA-2011-06-01-48 | Washington County - 1986

   Pattern of soils and parent material in the Otley-Nira association (Soil Survey of Washington County, Iowa; 1986).

9. NE-2012-02-08-17 | Gage County - May 1964

   Schematic diagram showing the relationship of major soil series to parent materials in Gage County, Nebraska (Soil Survey of Gage County, Nebraska; May 1964).

Map Units

Map units containing ADAIR 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
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	6923	402217	2wxrz	ia001	1976	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	4910	402154	2wxrx	ia001	1976	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	2792	402153	2wxrs	ia001	1976	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	1916	402218	2wxs3	ia001	1976	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	3607	1404836	2wxs3	ia003	2008	1:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	3442	1404834	2wxrz	ia003	2008	1:12000
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	1272	1404824	2wxrx	ia003	2008	1:12000
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	192C2	3912	402655	2wjf9	ia007	1970	1:15840
Adair-Shelby complex, 9 to 14 percent slopes, moderately eroded	93D2	3638	402733	2wjfb	ia007	1970	1:15840
Adair-Shelby complex, 9 to 14 percent slopes, severely eroded	93D3	806	402734	fj2f	ia007	1970	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	597	402656	2wjf8	ia007	1970	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes	192C	255	402654	2wjf7	ia007	1970	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	9656	402789	2wxry	ia009	1982	1:15840
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, eroded	Z93E2	4741	402791	2wxs2	ia009	1982	1:15840
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, severely eroded	Z93E3	3955	402792	2wxs4	ia009	1982	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, severely eroded	Z93D3	3573	402790	2wxs0	ia009	1982	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	1681	402754	2wxrw	ia009	1982	1:15840
Adair clay loam, deep loess, 5 to 9 percent slopes, eroded	Z192C2	1033	402753	2wxrr	ia009	1982	1:15840
Adair clay loam, 9 to 14 percent slopes, severely eroded	192D3	372	402755	fj33	ia009	1982	1:15840
Burchard-Adair clay loams, 14 to 18 percent slopes, moderately eroded	924E2	2294	403573	fjyh	ia027	1979	1:15840
Burchard-Adair clay loams, 9 to 14 percent slopes, moderately eroded	924D2	1772	403572	fjyg	ia027	1979	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	347	403517	2wxrw	ia027	1979	1:15840
Adair-Shelby complex, MLRA 107B, 9 to 14 percent slopes, severely eroded	Z82D3	13203	2484912	2pdrg	ia029	2010	1:12000
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	6123	1868026	2wxrx	ia029	2010	1:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, severely eroded	Y93D3	2191	1868006	2wxs1	ia029	2010	1:12000
Shelby-Adair complex, MLRA 107B, 5 to 9 percent slopes, moderately eroded	Z93C2	1128	2484925	2pdrw	ia029	2010	1:12000
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	989	1868023	2wxrs	ia029	2010	1:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	779	1868005	2wxrz	ia029	2010	1:12000
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, eroded	Z93E2	341	2484928	2wxs2	ia029	2010	1:12000
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	241	1868007	2wxs3	ia029	2010	1:12000
Adair clay loam, MLRA 107B, 5 to 9 percent slopes, severely eroded	Z192C3	220	2507022	2q6cz	ia029	2010	1:12000
Adair-Shelby complex, MLRA 108D, 5 to 9 percent slopes, severely eroded	Y82C3	197	2422827	2mb4q	ia029	2010	1:12000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	12	2506590	2wxry	ia029	2010	1:12000
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	S192D2	3512	2962185	2wjf8	ia039	1987	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	2871	404185	2tkbw	ia039	1987	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	S192C2	1479	2962167	2wjf9	ia039	1987	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	1100	404115	2wxrx	ia039	1987	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	1016	2985915	2wxrz	ia039	1987	1:15840
Shelby-Adair clay loams, 9 to 14 percent slopes, severely eroded	93D3	855	404186	fkl8	ia039	1987	1:15840
Adair loam, heavy till, 9 to 14 percent slopes	192D	597	404114	2wbf3	ia039	1987	1:15840
Adair loam, heavy till, 5 to 9 percent slopes	192C	472	404112	2wbf2	ia039	1987	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	400	404113	2wxrs	ia039	1987	1:15840
Shelby-Adair loams, 9 to 14 percent slopes	93D	278	404184	fkl6	ia039	1987	1:15840
Adair clay loam, 9 to 14 percent slopes, severely eroded	192D3	244	404116	fkj0	ia039	1987	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes	Y192D	157	2985844	2wxrv	ia039	1987	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	2188	404636	2wxrz	ia049	1980	1:15840
Shelby-Adair complex, 14 to 18 percent slopes	93E	290	404637	fl1t	ia049	1980	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	192C2	1409	404661	2wjf9	ia051	1988	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	943	404662	2wjf8	ia051	1988	1:15840
Adair-Shelby complex, 9 to 14 percent slopes, moderately eroded	93D2	867	404747	2wjfb	ia051	1988	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	3740	404772	2wjf8	ia053	1986	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	192C2	1197	404771	2wjf9	ia053	1986	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes	192C	644	404770	2wjf7	ia053	1986	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	1941	406105	2wxrw	ia071	1968	1:20000
Adair clay loam, deep loess, 9 to 14 percent slopes	Z192D	261	406104	2wxrt	ia071	1968	1:20000
Adair clay loam, deep loess, 5 to 9 percent slopes, eroded	Z192C2	226	406103	2wxrr	ia071	1968	1:20000
Adair soils, 9 to 14 percent slopes, severely eroded	192D3	175	406106	fml6	ia071	1968	1:20000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	7826	406435	2wxrz	ia077	1968	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	5839	406437	2wxs3	ia077	1968	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, severely eroded	Y93E3	1873	406438	2wxs5	ia077	1968	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	628	406351	2wxrx	ia077	1968	1:15840
Adair clay loam, 14 to 18 percent slopes, moderately eroded	192E2	349	406352	fmv4	ia077	1968	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, severely eroded	Y93D3	302	406436	2wxs1	ia077	1968	1:15840
Adair soils, 14 to 18 percent slopes, severely eroded	192E3	170	406353	fmv5	ia077	1968	1:15840
Adair loam, 9 to 14 percent slopes, moderately eroded	192D2	370	406825	fnbd	ia087	1982	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	1534	628331	p2tr	ia095	2005	1:12000
Adair silty clay loam, 9 to 14 percent slopes, moderately eroded	192D2	1349	452834	h66k	ia095	2005	1:12000
Shelby-Adair complex, 14 to 18 percent slopes, moderately eroded	93E2	941	628332	p2ts	ia095	2005	1:12000
Adair clay loam, 9 to 14 percent slopes, severely eroded	192D3	396	452838	h66p	ia095	2005	1:12000
Shelby-Adair complex, 9 to 14 percent slopes, severely eroded	93D3	349	1144451	17dws	ia095	2005	1:12000
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	7306	407703	fp7q	ia099	1975	1:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately erode	93E2	4323	407704	fp7r	ia099	1975	1:15840
Adair clay loam, 9 to 14 percent slopes, moderately eroded	192D2	1855	407629	fp5b	ia099	1975	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	2173	447246	h0d9	ia107	1998	1:12000
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	192C2	3127	408879	2wjf9	ia117	1991	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	1723	408882	2wjf8	ia117	1991	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	1626	409058	2tkbw	ia117	1991	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	1084	2985924	2wxrz	ia125	1976	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	431	412813	fvkk	ia125	1976	1:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately erode	93E2	969	409514	fr44	ia127	1978	1:15840
Adair clay loam, 9 to 14 percent slopes, moderately eroded	192D2	683	409444	fr1w	ia127	1978	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	536	409513	fr43	ia127	1978	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	781	409541	2wxrw	ia129	1979	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	501	409599	2wxry	ia129	1979	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	413	409753	2wjf8	ia135	1982	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	4787	2985904	2wxry	ia137	1987	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	1671	2985830	2wxrw	ia137	1987	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	690	409894	2wxrz	ia137	1987	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	241	409843	2wxrx	ia137	1987	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	7868	410196	2wxrx	ia145	1975	1:20000
Adair clay loam, dissected till plain, 9 to 14 percent slopes	Y192D	5373	410195	2wxrv	ia145	1975	1:20000
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	3660	2985831	2wxrw	ia145	1975	1:20000
Adair clay loam, deep loess, 9 to 14 percent slopes	Z192D	1573	2985832	2wxrt	ia145	1975	1:20000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	1003	2985905	2wxry	ia145	1975	1:20000
Shelby-Adair clay loams, 9 to 14 percent slopes	93D	915	410234	frwc	ia145	1975	1:20000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	569	410235	2wxrz	ia145	1975	1:20000
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	546	410194	2wxrs	ia145	1975	1:20000
Adair clay loam, dissected till plain, 5 to 9 percent slopes	Y192C	430	410193	2wxrq	ia145	1975	1:20000
Adair clay loam, deep loess, 5 to 9 percent slopes, eroded	Z192C2	248	2985829	2wxrr	ia145	1975	1:20000
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, eroded	Z93E2	197	2985927	2wxs2	ia145	1975	1:20000
Adair clay loam, deep loess, 5 to 9 percent slopes	Z192C	115	2985828	2wxrp	ia145	1975	1:20000
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	29	410236	2wxs3	ia145	1975	1:20000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	5833	410520	2wxry	ia155	1986	1:15840
Adair clay loam, deep loess, 9 to 14 percent slopes, eroded	Z192D2	1188	410451	2wxrw	ia155	1986	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, severely eroded	Z93D3	802	410521	2wxs0	ia155	1986	1:15840
Adair clay loam, deep loess, 5 to 9 percent slopes, eroded	Z192C2	109	410450	2wxrr	ia155	1986	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	9441	410641	fs9h	ia157	1978	1:15840
Adair clay loam, 9 to 14 percent slopes, moderately eroded	192D2	5626	410558	fs6t	ia157	1978	1:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately eroded	93E2	1251	410642	fs9j	ia157	1978	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	S192C2	6305	2962171	2wjf9	ia159	1987	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	1629	410748	2tkbw	ia159	1987	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	1605	2985920	2wxrz	ia159	1987	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	1478	410666	2wxrs	ia159	1987	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	S192D2	1406	2962186	2wjf8	ia159	1987	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes	S192C	988	2962164	2wjf7	ia159	1987	1:15840
Shelby-Adair clay loams, 9 to 14 percent slopes	93D	365	410747	fsdx	ia159	1987	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	361	410667	2wxrx	ia159	1987	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes	Y192C	163	410665	2wxrq	ia159	1987	1:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, eroded	Z93D2	6348	991679	2wxry	ia165	2005	1:12000
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	9842	411594	2wxrs	ia173	1989	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	6827	411664	2wxrz	ia173	1989	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes	Y192C	2368	411593	2wxrq	ia173	1989	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	1179	411596	2wxrx	ia173	1989	1:15840
Shelby-Adair complex, 9 to 14 percent slopes	93D	697	411663	ftcg	ia173	1989	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes	Y192D	286	411595	2wxrv	ia173	1989	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	10926	2985922	2wxrz	ia175	1975	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes, eroded	Y192C2	3540	411684	2wxrs	ia175	1975	1:15840
Adair-Shelby clay loams, 9 to 14 percent slopes	93D	2707	411738	ftfw	ia175	1975	1:15840
Adair-Shelby clay loams, 9 to 14 percent slopes, moderately eroded	93D2	1667	411739	ftfx	ia175	1975	1:15840
Adair clay loam, dissected till plain, 5 to 9 percent slopes	Y192C	846	411683	2wxrq	ia175	1975	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	728	411685	2wxrx	ia175	1975	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	S192C2	674	2962172	2wjf9	ia175	1975	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	643	411740	2wxs3	ia175	1975	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes	S192C	162	2962165	2wjf7	ia175	1975	1:15840
Adair clay loam, 9 to 14 percent slopes, moderately eroded	192D2	1043	411775	fth2	ia179	1978	1:15840
Adair clay loam, 5 to 9 percent slopes, moderately eroded	192C2	700	411773	fth0	ia179	1978	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	494	411869	2tkbw	ia179	1978	1:15840
Adair silty clay loam, 9 to 14 percent slopes	192D	38	411774	fth1	ia179	1978	1:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, eroded	Y93D2	5548	2985923	2wxrz	ia181	1975	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, eroded	Y93E2	2948	2985936	2wxs3	ia181	1975	1:15840
Adair-Shelby clay loams, 9 to 14 percent slopes, moderately eroded	93D2	1272	411978	ftpm	ia181	1975	1:15840
Adair clay loam, dissected till plain, 9 to 14 percent slopes, eroded	Y192D2	762	411905	2wxrx	ia181	1975	1:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, severely eroded	Y93E3	289	2985938	2wxs5	ia181	1975	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	S192D2	238	2962187	2wjf8	ia181	1975	1:15840
Adair-Shelby clay loams, 14 to 18 percent slopes, moderately eroded	93E2	178	411979	ftpn	ia181	1975	1:15840
Adair-Shelby clay loams, 14 to 18 percent slopes, severely eroded	93E3	126	411980	ftpp	ia181	1975	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	1723	412120	ftv6	ia183	1983	1:15840
Shelby-Adair clay loams, 9 to 14 percent slopes, severely eroded	93D3	946	412121	ftv7	ia183	1983	1:15840
Adair silty clay loam, 9 to 14 percent slopes, moderately eroded	192D2	357	412017	ftqw	ia183	1983	1:15840
Adair silty clay loam, 5 to 9 percent slopes, moderately eroded	192C2	327	412016	ftqv	ia183	1983	1:15840
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	192C2	11703	2423566	2wjf9	ia185	1966	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded	93D2	2415	1860446	2tkbw	ia185	1966	1:15840
Shelby-Adair complex, 9 to 14 percent slopes, severely eroded	93D3	1899	1860447	20fyf	ia185	1966	1:15840
Adair loam, heavy till, 5 to 9 percent slopes	192C	1355	1860461	2wbf2	ia185	1966	1:15840
Adair clay loam, heavy till, 9 to 14 percent slopes, moderately eroded	192D2	1052	1860769	2wjf8	ia185	1966	1:15840
Adair loam, heavy till, 9 to 14 percent slopes	192D	76	1860463	2wbf3	ia185	1966	1:15840
Lamoni and Adair soils, 5 to 9 percent slopes, eroded	30127	22240	958969	115wh	mo025	1967	1:24000
Lamoni and Adair soils, 9 to 14 percent slopes, eroded	30130	5337	2531348	2qns0	mo025	1967	1:24000
Lamoni and Adair soils, 5 to 9 percent slopes	30126	4231	2531344	2qnry	mo025	1967	1:24000
Lamoni and Adair soils, 5 to 9 percent slopes, severely eroded	30128	3718	2531346	2qnrz	mo025	1967	1:24000
Lamoni and Adair soils, 2 to 5 percent slopes	30124	2100	887992	yt0x	mo025	1967	1:24000
Lamoni and Adair soils, 9 to 14 percent slopes, severely eroded	30131	1920	958973	115wm	mo025	1967	1:24000
Lamoni and Adair soils, 2 to 5 percent slopes, eroded	30125	638	887993	yt0y	mo025	1967	1:24000
Lamoni and Adair soils, 9 to 14 percent slopes	30129	448	887997	yt12	mo025	1967	1:24000
Lamoni and Adair soils, 9 to 14 percent slopes, eroded	30130	118	2531347	2qns0	mo061	1952	1:24000
Lamoni and Adair soils, 5 to 9 percent slopes	30126	14	2531343	2qnry	mo061	1952	1:24000
Lamoni and Adair soils, 5 to 9 percent slopes, severely eroded	30128	41	2531345	2qnrz	mo063	1974	1:24000
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	30004	25870	2528511	2wjf9	mo081	1975	1:24000
Adair loam, 3 to 9 percent slopes	30005	21741	2528513	2qmvp	mo081	1975	1:24000
Adair loam, 5 to 9 percent slopes, eroded	30007	28655	901269	z7v6	mo129	1993	1:24000
Adair loam, 9 to 14 percent slopes, eroded	30008	2221	901270	z7v7	mo129	1993	1:24000
Adair loam, 3 to 9 percent slopes, eroded	30006	1651	2528514	2qmvq	mo129	1993	1:24000
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	30004	55	2528510	2wjf9	mo129	1993	1:24000
Adair and Shelby loams, 5 to 9 percent slopes, eroded	30001	133	2528508	2qmvm	mo147	1983	1:24000
Adair and Shelby loams, 5 to 9 percent slopes	30000	73	2528506	2qmvl	mo147	1983	1:24000
Adair loam, 3 to 9 percent slopes, eroded	30006	21589	2528515	2qmvq	mo171	1989	1:24000
Adair and Shelby loams, 5 to 9 percent slopes, eroded	30001	11332	2528507	2qmvm	mo227	1965	1:24000
Adair and Shelby soils, 5 to 9 percent slopes, severely eroded	30003	5959	887672	yspl	mo227	1965	1:24000
Adair and Shelby loams, 5 to 9 percent slopes	30000	5034	2528505	2qmvl	mo227	1965	1:24000
Adair silt loam variant and Adair loam, 2 to 5 percent slopes, eroded	30009	1328	887669	ysph	mo227	1965	1:24000
Adair loam, 3 to 9 percent slopes	30005	60	2528512	2qmvp	mo227	1965	1:24000
Adair clay loam, heavy till, 5 to 9 percent slopes, moderately eroded	30004	56	2528509	2wjf9	mo227	1965	1:24000

Map of Series Extent

Approximate geographic distribution of the ADAIR 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).