Soil Data Explorer - CLOVER

Official Series Description

Lab Data Summary

Aggregate lab data for the CLOVER soil series. This aggregation is based on all pedons with a current taxon name of CLOVER, 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 CLOVER 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 CLOVER 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 CLOVER 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 CLOVER 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 CLOVER 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 CLOVER 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 CLOVER 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 CLOVER 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 flats position figure.

Soil series sharing subgroup-level classification with CLOVER, 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-2010-11-05-11 | Culpeper County -

   Relationship of soils and landscape in the Culpeper Triassic Basin Siltstone (Soil Survey of Culpeper County, Virginia).

2. VA-2010-11-05-24 | Fauquier County -

   Relationship of soils and landscape in the Culpeper Triassic Basin Siltstone (Soil Survey of Fauquier County, Virginia).

Map Units

Map units containing CLOVER 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
Clover silty clay loam, 2 to 8 percent slopes, moderately eroded	CnB2	6139	2424549	2mcy8	nc059	1988	1:24000
Clover silty clay loam, 8 to 15 percent slopes, moderately eroded	CnC2	4793	2424550	2mcy9	nc059	1988	1:24000
Clover silt loam, 15 to 25 percent slopes	CmD	1979	2424547	2mcy6	nc059	1988	1:24000
Clover silt loam, 25 to 45 percent slopes	CmE	1052	2424548	2mcy7	nc059	1988	1:24000
Clover silt loam, 2 to 8 percent slopes	CmB	899	2424545	2mcy4	nc059	1988	1:24000
Clover silt loam, 8 to 15 percent slopes	CmC	321	2424546	2mcy5	nc059	1988	1:24000
Clover sandy loam, 2 to 8 percent slopes	CmB	12412	2389940	2l6xv	nc157	1983	1:24000
Clover sandy loam, 8 to 15 percent slopes	CmD	7227	2389942	2l6xx	nc157	1983	1:24000
Clover sandy clay loam, 2 to 8 percent slopes, moderately eroded	CnB2	6771	2389946	2l6y1	nc157	1983	1:24000
Clover-Urban land complex, 2 to 10 percent slopes	CpC	3798	2389949	2l6y4	nc157	1983	1:24000
Clover sandy clay loam, 8 to 15 percent slopes, moderately eroded	CnD2	3217	2389947	2l6y2	nc157	1983	1:24000
Clover sandy loam, 15 to 25 percent slopes	CmE	3115	2389944	2l6xz	nc157	1983	1:24000
Clover sandy clay loam, 15 to 25 percent slopes, moderately eroded	CnE2	1513	2389948	2l6y3	nc157	1983	1:24000
Clover fine sandy loam, 2 to 8 percent slopes	CfB	4588	2387722	2l4m9	nc169	1992	1:24000
Clover fine sandy loam, 8 to 15 percent slopes	CfC	3969	2387724	2l4mc	nc169	1992	1:24000
Clover fine sandy loam, 15 to 25 percent slopes	CfD	3269	2387726	2l4mf	nc169	1992	1:24000
Clover sandy clay loam, 8 to 15 percent slopes, moderately eroded	CoC2	3142	2387964	2l4w3	nc169	1992	1:24000
Clover sandy clay loam, 2 to 8 percent slopes, moderately eroded	CoB2	2893	2387963	2l4w2	nc169	1992	1:24000
Clover-Pinkston complex, 25 to 45 percent slopes	CpE	1337	2388848	2l5sm	nc169	1992	1:24000
Clover sandy clay loam, 15 to 25 percent slopes, moderately eroded	CoD2	1111	2388201	2l53r	nc169	1992	1:24000
Clover-Urban land complex, 2 to 10 percent slopes	CrB	565	2388849	2l5sn	nc169	1992	1:24000
Clover fine sandy loam, 2 to 6 percent slopes	CmB	2410	2398274	2lhlp	nc197	1960	1:15840
Clover fine sandy loam, 6 to 10 percent slopes	CmC	764	2398276	2lhlr	nc197	1960	1:15840
Clover sandy clay loam, 6 to 10 percent slopes, moderately eroded	CoC2	757	2398277	2lhls	nc197	1960	1:15840
Clover sandy clay loam, 2 to 6 percent slopes, moderately eroded	CoB2	626	2398275	2lhlq	nc197	1960	1:15840
Clover fine sandy loam, 10 to 15 percent slopes	CmD	369	2398278	2lhlt	nc197	1960	1:15840
Clover-Pinkston complex, 25 to 45 percent slopes	CpF	252	2398273	2lhln	nc197	1960	1:15840
Clover sandy clay loam, 10 to 15 percent slopes, moderately eroded	CoD2	133	2398279	2lhlv	nc197	1960	1:15840
Clover loam, 2 to 7 percent slopes	54B	490	516411	2v7jq	va003	1981	1:15840
Clover loam, 7 to 15 percent slopes	54C	180	516412	2v7jr	va003	1981	1:15840
Clover-Penn complex, 0 to 2 percent slopes	9A	2661	1726300	1vyc3	va047	2006	1:24000
Clover-Penn complex, 2 to 7 percent slopes	9B	1673	1726301	1vyc4	va047	2006	1:24000
Chantilly-Clover complex, 2 to 7 percent slopes	19B	161	2250285	2fjlv	va059	2007	1:12000
Clover silt loam, 2 to 7 percent slopes	28B	62	2250312	2fjmq	va059	2007	1:12000
Clover loam, 2 to 7 percent slopes	75B	4651	1895382	21m9c	va061	2006	1:12000
Clover loam, 7 to 15 percent slopes	75C	2648	1895383	21m9d	va061	2006	1:12000
Clover fine sandy loam, 8 to 15 percent slopes	11C	1175	1472801	1lfkq	va083	2004	1:24000
Clover-Bentley complex, 2 to 8 percent slopes	12B	1045	1472803	1lfks	va083	2004	1:24000
Clover fine sandy loam, 15 to 25 percent slopes	11D	352	1472802	1lfkr	va083	2004	1:24000
Clover fine sandy loam, 2 to 7 percent slopes	MuB	554	119877	2zhfd	va137	1966	1:15840
Clover fine sandy loam, 2 to 7 percent slopes, moderately eroded	MuB2	482	119878	2zhff	va137	1966	1:15840
Clover fine sandy loam, 7 to 15 percent slopes, moderately eroded	MuC2	458	119879	2zhfg	va137	1966	1:15840
Clover fine sandy loam, 2 to 7 percent slopes	23B	26086	119972	2yzsf	va143	1989	1:24000
Clover fine sandy loam, 7 to 15 percent slopes	23C	24092	119973	2yzsg	va143	1989	1:24000
Clover fine sandy loam, 15 to 25 percent slopes	23D	6291	119974	2yzsh	va143	1989	1:24000
Pinkston-Clover complex, 15 to 35 percent slopes, very stony	29D	2547	119985	2yzst	va143	1989	1:24000
Pinkston-Clover complex, 7 to 15 percent slopes, very stony	29C	1867	119984	2yzss	va143	1989	1:24000
Pinkston-Clover complex, 35 to 50 percent slopes, very stony	29E	1644	119986	2yzsv	va143	1989	1:24000

Map of Series Extent

Approximate geographic distribution of the CLOVER 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).