Soil Data Explorer - GALLIA

Official Series Description

Lab Data Summary

Aggregate lab data for the GALLIA soil series. This aggregation is based on all pedons with a current taxon name of GALLIA, 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 GALLIA were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
n/a	WS-001	1966-OH167-001	Gallia	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WS-020	1968-OH167-020	Gallia	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	WS-030	1969-OH167-030	Gallia	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	83P0593	82WV000008S	Gallia	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	83P0595	82WV000010M	Gallia	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	83P0597	82WV000012N	Gallia	6	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 GALLIA 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 GALLIA 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 GALLIA 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 GALLIA 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 hills figure.

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 GALLIA 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 GALLIA 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 GALLIA 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 hills figure.

There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with GALLIA, 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. WV-2010-11-08-07 | Jackson and Mason Counties -

   The dominant upland and high terrace soils in the Upper Flats area of northern Mason County. These high terrace soils have their origins associated with the ancient Teays River system (Soil Survey of Jackson and Mason Counties, West Virginia).

2. WV-2012-03-23-06 | Pleasants and Tyler Counties - July 1989

   Typical relationship of soils, landscapes, and underlying parent materials in Otwell-Gallia-Hackers general soil map unit (Soil Survey of Pleasants and Tyler Counties, WV; 1989).

Map Units

Map units containing GALLIA 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
Gallia loam, 6 to 12 percent slopes	Gal2C1	350	2441859	2myyn	oh009	1981	1:15840
Gallia loam, 6 to 12 percent slopes	Gal2C1	1132	2450423	2n7vx	oh053	1988	1:15840
Gallia loam, 6 to 12 percent slopes	Gal2C1	762	2451272	2n8r9	oh105	1991	1:15840
Gallia loam, 12 to 18 percent slopes	Gal2D1	255	2451273	2n8rb	oh105	1991	1:15840
Gallia loam, 6 to 12 percent slopes	Gal2C1	1507	2396098	2lfbh	oh167	1973	1:15840
Gallia loam, 2 to 6 percent slopes	Gal2B1	430	2396097	2lfbg	oh167	1973	1:15840
Gallia loam, 12 to 18 percent slopes	Gal2D1	400	2396099	2lfbj	oh167	1973	1:15840
Gallia silt loam, 8 to 15 percent slopes	GaC	94	532306	kvx5	wv017	2001	1:24000
Gallia silt loam, 10 to 20 percent slopes	GaC	363	513280	k73f	wv085	1980	1:20000
Gallia silt loam, 3 to 10 percent slopes	GaB	276	513279	k73d	wv085	1980	1:20000
Gallia loam, 8 to 15 percent slopes	GaC	2974	1384153	1hgb3	wv600	2005	1:24000
Gallia loam, 10 to 20 percent slopes	GaC	932	514579	k8gb	wv601	1966	1:15840
Gallia loam, 3 to 10 percent slopes	GaB	176	514578	k8g9	wv601	1966	1:15840
Gallia loam, 10 to 20 percent slopes, severely eroded	GaC3	142	514580	k8gc	wv601	1966	1:15840
Gallia loam, 20 to 30 percent slopes, severely eroded	GaD3	72	514581	k8gd	wv601	1966	1:15840
Gallia silt loam, 8 to 15 percent slopes	GaC	2305	514688	k8kv	wv612	1984	1:20000
Gallia silt loam, 15 to 25 percent slopes	GaD	415	514689	k8kw	wv612	1984	1:20000

Map of Series Extent

Approximate geographic distribution of the GALLIA 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).