Soil Data Explorer - ADYEVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the ADYEVILLE soil series. This aggregation is based on all pedons with a current taxon name of ADYEVILLE, 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 ADYEVILLE were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 ADYEVILLE 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 ADYEVILLE 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 ADYEVILLE 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 ADYEVILLE 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 terrace figure.

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

Competing Series

Soil series competing with ADYEVILLE 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 ADYEVILLE 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 ADYEVILLE 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 ADYEVILLE, 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. IN-2010-09-24-15 | Owen County -

   Typical pattern of soils and parent materials in the Zanesville-Tulip-Wellston and Crider-Haggatt associations (Soil Survey of Owen County, Indiana).

2. IN-2010-09-24-20 | Perry County -

   Typical pattern of soils and parent materials of alluvial, stream terrace lacustrine and aeolian landforms adjacent to hills underlain with interbedded shale and limestone in Ohio River Valley (Soil Survey of Perry County, Indiana).

3. IN-2010-09-24-21 | Perry County -

   Typical pattern of soils and parent materials in the Adyeville-Ebal-Deuchars and Apalona associations (Soil Survey of Perry County, Indiana).

Map Units

Map units containing ADYEVILLE 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
Tipsaw-Adyeville complex, 25 to 75 percent slopes	TblG	34118	1652613	1sgp3	in025	1970	1:20000
Adyeville silt loam, 18 to 25 percent slopes, eroded	AbqE2	9244	1652606	1sgnw	in025	1970	1:20000
Adyeville-Tipsaw complex, 18 to 30 percent slopes	AciE	7630	1652609	1sgnz	in025	1970	1:20000
Adyeville silt loam, 18 to 25 percent slopes, severely eroded	AbqE3	4569	1652607	1sgnx	in025	1970	1:20000
Adyeville silt loam, 12 to 18 percent slopes, severely eroded	AbqD3	1423	1652837	1sgxb	in025	1970	1:20000
Adyeville-Tipsaw-Ebal complex, 20 to 50 percent slopes, very rocky	AccG	1397	1652540	1sglr	in025	1970	1:20000
Adyeville-Wellston silt loams, 18 to 50 percent slopes	AcmF	496	1652600	1sgnp	in025	1970	1:20000
Wellston-Ebal-Adyeville complex, 12 to 18 percent slopes, severely eroded	WpmD3	486	1652597	1sgnl	in025	1970	1:20000
Adyeville-Tipsaw complex, 20 to 60 percent slopes	AciG	289	1652610	1sgp0	in025	1970	1:20000
Wellston-Adyeville-Ebal silt loams, 12 to 18 percent slopes, eroded	WppD2	135	1652599	1sgnn	in025	1970	1:20000
Adyeville silt loam, 12 to 18 percent slopes, eroded	AbqD2	49	1652605	1sgnv	in025	1970	1:20000
Adyeville-Wellston-Deuchars silt loams, 8 to 20 percent slopes, eroded	AbvD2	31	1652538	1sglp	in025	1970	1:20000
Adyeville-Wellston-Deuchars silt loams, 8 to 20 percent slopes, severely eroded	AbvD3	19	1652539	1sglq	in025	1970	1:20000
Adyeville silt loam, 18 to 25 percent slopes	AbqE	8	1652838	1sgxc	in025	1970	1:20000
Caneyville-Adyeville-Rock outcrop complex, 25 to 75 percent slopes	CbxG	13241	1652078	1sg3v	in093	1982	1:15840
Adyeville-Tipsaw-Wellston complex, 18 to 50 percent slopes	AclF	10715	1651486	1sfhr	in093	1982	1:15840
Wellston-Adyeville silt loams, 12 to 18 percent slopes, eroded complex	WpoD2	8500	1651511	1sfjk	in093	1982	1:15840
Adyeville-Wellston silt loams, 18 to 50 percent slopes complex	AcmF	647	1651485	1sfhq	in093	1982	1:15840
Wellston-Tipsaw-Adyeville complex, 18 to 70 percent slopes	WpfG	373	1651508	1sfjg	in093	1982	1:15840
Wellston-Adyeville-Ebal silt loams, 12 to 18 percent slopes, eroded complex	WppD2	284	1651512	1sfjl	in093	1982	1:15840
Adyeville-Ebal silt loams, 18 to 30 percent slopes complex	AcjE	39	1651526	1sfk1	in093	1982	1:15840
Wellston-Tipsaw-Adyeville complex, 18 to 70 percent slopes	WpfG	60650	1443115	1kfp3	in101	1984	1:15840
Wellston-Adyeville complex, 12 to 30 percent slopes	WpnE	30029	1443116	1kfp4	in101	1984	1:15840
Adyeville-Wellston silt loams, 18 to 50 percent slopes	AcmF	1036	1443061	1kfmc	in101	1984	1:15840
Adyeville-Tipsaw-Wellston complex, 18 to 50 percent slopes	AclF	1020	1443059	1kfm9	in101	1984	1:15840
Adyeville-Tipsaw complex, 20 to 60 percent slopes	AciG	510	1443058	1kfm8	in101	1984	1:15840
Adyeville silt loam, 18 to 25 percent slopes	AbqE	142	1443056	1kfm6	in101	1984	1:15840
Adyeville silt loam, 12 to 18 percent slopes, severely eroded	AbqD3	133	1443055	1kfm5	in101	1984	1:15840
Wellston-Adyeville-Ebal silt loams, 12 to 18 percent slopes, eroded	WppD2	109	1443118	1kfp6	in101	1984	1:15840
Adyeville silt loam, 12 to 18 percent slopes, eroded	AbqD2	24	1443054	1kfm4	in101	1984	1:15840
Adyeville-Wellston silt loams, 18 to 25 percent slopes	AcmE	18	1443060	1kfmb	in101	1984	1:15840
Adyeville silt loam, 18 to 25 percent slopes, severely eroded	AbqE3	6	1443057	1kfm7	in101	1984	1:15840
Wellston-Adyeville silt loams, 12 to 18 percent slopes, eroded	WpoD2	1	1443117	1kfp5	in101	1984	1:15840
Adyeville-Wellston silt loams, 18 to 50 percent slopes	AcmF	59151	1442963	1kfj6	in117	1980	1:15840
Wellston-Adyeville-Ebal silt loams, 12 to 18 percent slopes, eroded	WppD2	44506	1443012	1kfks	in117	1980	1:15840
Wellston-Ebal-Adyeville complex, 12 to 18 percent slopes, severely eroded	WpmD3	6616	1443010	1kfkq	in117	1980	1:15840
Wellston-Tipsaw-Adyeville complex, 18 to 70 percent slopes	WpfG	115	1443009	1kfkp	in117	1980	1:15840
Adyeville-Tipsaw complex, 20 to 60 percent slopes	AciG	40	1442958	1kfj1	in117	1980	1:15840
Tipsaw-Adyeville complex, 25 to 75 percent slopes	TblG	31	1442998	1kfkb	in117	1980	1:15840
Adyeville silt loam, 12 to 18 percent slopes, eroded	AbqD2	29	1442954	1kfhx	in117	1980	1:15840
Adyeville silt loam, 18 to 25 percent slopes, eroded	AbqE2	21	1442955	1kfhy	in117	1980	1:15840
Adyeville silt loam, 18 to 25 percent slopes, severely eroded	AbqE3	5	1442956	1kfhz	in117	1980	1:15840
Adyeville-Tipsaw-Ebal complex, 18 to 50 percent slopes	AcgF	4	1442959	1kfj2	in117	1980	1:15840
Wellston-Adyeville silt loams, 12 to 18 percent slopes, eroded	WpoD2	4	1443011	1kfkr	in117	1980	1:15840
Adyeville-Tipsaw complex, 18 to 30 percent slopes	AciE	1	1442957	1kfj0	in117	1980	1:15840
Hickory-Adyeville complex, 35 to 60 percent slopes	HepG	6047	166062	5ksv	in119	1997	1:12000
Tulip-Wellston-Adyeville silt loams, 18 to 25 percent slopes	TtcE	4561	166321	5l26	in119	1997	1:12000
Adyeville-Tipsaw-Ebal complex, 20 to 50 percent slopes, very rocky	AccG	80319	535667	kzdl	in123	1997	1:12000
Adyeville-Wellston-Deuchars silt loams, 8 to 20 percent slopes, severely eroded	AbvD3	19432	535666	kzdk	in123	1997	1:12000
Adyeville-Wellston-Deuchars silt loams, 8 to 20 percent slopes, eroded	AbvD2	15607	535665	kzdj	in123	1997	1:12000

Map of Series Extent

Approximate geographic distribution of the ADYEVILLE 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).