Soil Data Explorer - FAUQUIER

Official Series Description

Lab Data Summary

Aggregate lab data for the FAUQUIER soil series. This aggregation is based on all pedons with a current taxon name of FAUQUIER, 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 FAUQUIER were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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 FAUQUIER 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 FAUQUIER 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 FAUQUIER 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 FAUQUIER 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 FAUQUIER 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 FAUQUIER 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 FAUQUIER 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 terrace figure.

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

Soil series sharing subgroup-level classification with FAUQUIER, 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. VA-2010-11-05-13 | Culpeper County -

   Relationship of soils and landscape in the Piedmont Metabasalt (Soil Survey of Culpeper County, Virginia).

2. VA-2010-11-05-18 | Fauquier County -

   Relationship of soils and landscape in the Blue Ridge Metabasalt (Soil Survey of Fauquier County, Virginia).

Map Units

Map units containing FAUQUIER 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
Fauquier silt loam, 7 to 15 percent slopes	29C	1670	516340	kb94	va003	1981	1:15840
Fauquier silt loam, 2 to 7 percent slopes	29B	1300	516339	kb93	va003	1981	1:15840
Fauquier silt loam, 15 to 25 percent slopes	29D	1120	516341	kb95	va003	1981	1:15840
Fauquier very stony silt loam, 15 to 25 percent slopes	31D	600	516349	kb9f	va003	1981	1:15840
Fauquier very stony silt loam, 7 to 15 percent slopes	31C	500	516348	kb9d	va003	1981	1:15840
Fauquier silt loam, 25 to 45 percent slopes	29E	470	516342	kb96	va003	1981	1:15840
Fauquier silty clay loam, 7 to 15 percent slopes, severely eroded	30C3	440	516346	2xxxw	va003	1981	1:15840
Fauquier silty clay loam, 15 to 25 percent slopes, severely eroded	30D3	200	516347	kb9c	va003	1981	1:15840
Fauquier loam, 15 to 25 percent slopes, very stony	19D	258	136724	4l8g	va009	2004	1:24000
Fauquier loam, 25 to 50 percent slopes, very stony	19E	217	136725	4l8h	va009	2004	1:24000
Fauquier loam, 7 to 15 percent slopes, very stony	19C	190	136723	4l8f	va009	2004	1:24000
Fauquier silt loam, 7 to 15 percent slopes	22C	6289	1726331	1vyd3	va047	2006	1:24000
Fauquier silt loam, 2 to 7 percent slopes	22B	3478	1726330	1vyd2	va047	2006	1:24000
Fauquier silt loam, 7 to 15 percent slopes	45C	16135	1895316	21m77	va061	2006	1:12000
Fauquier silt loam, 2 to 7 percent slopes	45B	5825	1895315	21m76	va061	2006	1:12000
Fauquier and Eubanks soils, 7 to 15 percent slopes	28C	4696	1895281	21m63	va061	2006	1:12000
Elioak-Fauquier complex, 7 to 15 percent slopes	47C	2969	1895320	21m7c	va061	2006	1:12000
Fauquier silt loam, 15 to 25 percent slopes	45D	2259	1895317	21m78	va061	2006	1:12000
Elioak-Fauquier complex, 2 to 7 percent slopes	47B	1410	1895319	21m7b	va061	2006	1:12000
Fauquier and Eubanks soils, 15 to 25 percent slopes	28D	228	1895283	21m65	va061	2006	1:12000
Fauquier silt loam, 7 to 15 percent slopes	45C	1407	642061	pk3n	va107	2006	1:12000
Fauquier silt loam, 2 to 7 percent slopes	45B	998	642060	pk3m	va107	2006	1:12000
Fauquier silty clay loam, 7 to 15 percent slopes, eroded	FcC2	1558	516997	kbzb	va113	1967	1:15840
Fauquier silt loam, 2 to 7 percent slopes	FaB	395	516995	kbz8	va113	1967	1:15840
Fauquier silty clay loam, 2 to 7 percent slopes, eroded	FcB2	305	516996	kbz9	va113	1967	1:15840
Fauquier silty clay loam, 15 to 25 percent slopes, eroded	FcD2	260	516998	kbzc	va113	1967	1:15840
Fauquier loam, 25 to 50 percent slopes, very stony	18E	2798	136916	4lgn	va125	1992	1:24000
Fauquier loam, 15 to 25 percent slopes, very stony	18D	837	136915	4lgm	va125	1992	1:24000
Fauquier loam, 7 to 15 percent slopes, very stony	18C	414	136914	4lgl	va125	1992	1:24000
Fauquier clay, 7 to 15 percent slopes, severely eroded	DdC3	11388	119820	30yn0	va137	1966	1:15840
Fauquier clay loam, 2 to 7 percent slopes, moderately eroded	DaB2	4347	119813	30ymy	va137	1966	1:15840
Fauquier clay loam, 7 to 15 percent slopes, moderately eroded	DaC2	3804	119814	2z1wn	va137	1966	1:15840
Fauquier clay, 2 to 7 percent slopes, severely eroded	DdB3	2393	119819	30ymz	va137	1966	1:15840
Fauquier clay, 15 to 25 percent slopes, severely eroded	DdD3	1958	119821	2z1ww	va137	1966	1:15840
Fauquier clay loam, 15 to 25 percent slopes, stony	DcD	992	119817	2z1wr	va137	1966	1:15840
Fauquier clay loam, 25 to 45 percent slopes, stony	DcE	960	119818	2z1ws	va137	1966	1:15840
Fauquier clay loam, 15 to 25 percent slopes, moderately eroded	DaD2	784	119815	2z1wp	va137	1966	1:15840
Fauquier silt loam, 2 to 7 percent slopes, moderately eroded	FaB2	442	119833	2z1x8	va137	1966	1:15840
Fauquier clay loam, 7 to 15 percent slopes, stony	DcC	336	119816	2z1wq	va137	1966	1:15840
Fauquier silt loam, 7 to 15 percent slopes, moderately eroded	FaC2	258	119834	2z1x9	va137	1966	1:15840
Fauquier silty clay loam, 4 to 20 percent slopes, severely eroded	FcC3	201	119835	40pn	va137	1966	1:15840
Fauquier silt loam, 15 to 35 percent slopes, very stony	21D	3643	517206	kc62	va139	1995	1:20000
Fauquier silt loam, 15 to 25 percent slopes	20D	1610	517196	kc5r	va139	1995	1:20000
Fauquier silt loam, 25 to 35 percent slopes	20E	1277	517197	kc5s	va139	1995	1:20000
Fauquier silt loam, 7 to 15 percent slopes	20C	683	517195	kc5q	va139	1995	1:20000
Fauquier silt loam, 7 to 15 percent slopes, very stony	21C	117	517205	kc61	va139	1995	1:20000
Fauquier silt loam, 2 to 7 percent slopes	20B	41	517194	kc5p	va139	1995	1:20000
Fauquier silt loam, 25 to 50 percent slopes, very stony	27E	3532	518380	kddy	va165	1980	1:20000
Fauquier silt loam, 15 to 25 percent slopes, stony, eroded	26D2	536	518379	kddx	va165	1980	1:20000
Fauquier silt loam, 7 to 15 percent slopes, stony, eroded	26C2	233	518378	kddw	va165	1980	1:20000
Fauquier - Urban land complex, 15 to 25 percent slopes	129D	48	2519311	2qjh3	va540	2011	1:24000
Fauquier - Urban land complex, 25 to 45 percent slopes	129E	17	2519312	2qjh4	va540	2011	1:24000

Map of Series Extent

Approximate geographic distribution of the FAUQUIER 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).