Soil Data Explorer - REAVILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the REAVILLE soil series. This aggregation is based on all pedons with a current taxon name of REAVILLE, 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 REAVILLE 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
148	60PA091011	1960PA091011	Reaville	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2875,-75.5638889
148	61PA001010	1961PA001010	Reaville	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.9872222,-77.0941667
148	61PA001013	1961PA001013	Reaville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	39.7886111,-77.2902778
148	61PA091016	1961PA091016	Reaville	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2325,-75.4972222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the REAVILLE 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 REAVILLE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the REAVILLE 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 2023-10-09).

Geomorphic description summaries for the REAVILLE 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 2023-10-04).

Competing Series

Soil series competing with REAVILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the REAVILLE 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 2023-10-09).

Geomorphic description summaries for the REAVILLE 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 2023-10-04).

Soil series sharing subgroup-level classification with REAVILLE, 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 2023-10-02).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. MD-2010-09-07-04 | Frederick County - 2002

   Relationship of soils, topography, and underlying material in the Penn-Klinesville-Reaville general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

2. MD-2012-02-03-19 | Frederick County - 2002

   Relationship of soils, topography, and underlying material in the Penn-Klinesville-Reaville general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

3. PA-2010-09-30-01 | Adams County - 2005

   Typical pattern of soils and parent material in the Penn-Klinesville-Croton general soil map unit (Soil Survey of Adams County, Pennsylvania; 2005).

4. PA-2012-03-12-28 | Bucks and Philadelphia Counties - July 1975

   Typical pattern of soils and underlying material in the Abbottstown-Doylestown-Reaville soil association (Soil Survey of Bucks and Philadelphia Counties County, PA; 1975).

5. PA-2012-03-12-29 | Bucks and Philadelphia Counties - July 1975

   Typical pattern of soils and underlying material in the Abbottstown-Readington-Reaville soil association (Soil Survey of Bucks and Philadelphia Counties County, PA; 1975).

6. PA-2012-03-13-72 | Montgomery County - April 1967

   Typical landscape in the northern part of Montgomery County, showing the relationship of the soils formed on red shale and siltstone (Soil Survey of Montgomery County, PA; 1967).

Map Units

Map units containing REAVILLE 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
Reaville silt loam, 0 to 3 percent slopes	ReA	1161	2496035	2ptnl	md013	2010	1:12000
Reaville silt loam, 3 to 8 percent slopes	ReB	971	2496036	2ptnm	md013	2010	1:12000
Penn-Reaville silt loams, 3 to 8 percent slopes	PrB	8529	559054	lrr0	md021	2001	1:12000
Reaville silt loam, 0 to 3 percent slopes	RmA	1967	535065	kys5	md021	2001	1:12000
Penn-Reaville silt loam, 0 to 3 percent slopes	PrA	1738	535061	kys1	md021	2001	1:12000
Penn-Reaville-Urban land complex, 0 to 8 percent slopes	PqB	524	559055	lrr1	md021	2001	1:12000
Reaville silt loam, 2 to 6 percent slopes	RehB	6190	548670	ldy1	nj019	1970	1:24000
Reaville wet variant silt loam, 0 to 2 percent slopes	RepwA	965	1478516	1lmj2	nj019	1970	1:24000
Reaville silt loam, 0 to 2 percent slopes	RehA	891	548669	ldy0	nj019	1970	1:24000
Reaville wet variant silt loam, 2 to 6 percent slopes	RepwB	774	1478517	1lmj3	nj019	1970	1:24000
Reaville silt loam, 6 to 12 percent slopes, eroded	RehC2	722	548671	ldy2	nj019	1970	1:24000
Reaville silt loam, 2 to 6 percent slopes	RehB	1762	135206	4jph	nj021	1969	1:24000
Doylestown and Reaville variant silt loams, 0 to 2 percent slopes	DOZA	1653	1482257	1lrdr	nj021	1969	1:24000
Doylestown and Reaville variant silt loams, 2 to 6 percent slopes	DOZB	1075	1482258	1lrds	nj021	1969	1:24000
Reaville silt loam, 0 to 2 percent slopes	RehA	471	135205	4jpg	nj021	1969	1:24000
Reaville silt loam, 2 to 6 percent slopes, eroded	RehB2	439	135207	4jpj	nj021	1969	1:24000
Reaville silt loam, 6 to 12 percent slopes, eroded	RehC2	352	135208	4jpk	nj021	1969	1:24000
Doylestown and Reaville variant silt loams, 2 to 6 percent slopes, eroded	DOZB2	194	1482259	1lrdt	nj021	1969	1:24000
Doylestown and Reaville variant silt loams, 6 to 12 percent slopes	DOZC	108	1482260	1lrdv	nj021	1969	1:24000
Doylestown and Reaville variant silt loams, 6 to 12 percent slopes, eroded	DOZC2	9	1482261	1lrdw	nj021	1969	1:24000
Reaville poorly drained variant silt loam, 0 to 2 percent slopes	RepwA	6	1445357	1kj0f	nj021	1969	1:24000
Reaville silt loam, 0 to 2 percent slopes	RehA	1612	1455185	1kv7g	nj023	1985	1:24000
Reaville-Urban land complex, 0 to 6 percent slopes	RemB	1487	1455187	1kv7j	nj023	1985	1:24000
Reaville poorly drained variant silt loam, 0 to 2 percent slopes	RepwA	843	1426830	1jwqs	nj023	1985	1:24000
Reaville silt loam, 2 to 6 percent slopes	RehB	497	1455186	1kv7h	nj023	1985	1:24000
Reaville deep variant channery silt loam, 0 to 6 percent slopes	RerB7	1065	298539	b0n9	nj027	1974	1:24000
Reaville silt loam, 2 to 6 percent slopes	RehB	6726	1405081	1j536	nj035	1972	1:24000
Reaville silt loam, 0 to 2 percent slopes	RehA	4308	1405080	1j535	nj035	1972	1:24000
Reaville deep variant channery silt loam, 0 to 6 percent slopes	RerB7	35	1405083	1j538	nj035	1972	1:24000
Reaville silt loam, 6 to 12 percent slopes, eroded	RehC2	2	1405082	1j537	nj035	1972	1:24000
Reaville channery silt loam, 3 to 8 percent slopes	RfB	3173	545646	l9sh	pa001	1991	1:24000
Reaville channery silt loam, 0 to 3 percent slopes	RfA	708	545645	l9sg	pa001	1991	1:24000
Reaville channery silt loam, 8 to 15 percent slopes	RfC	656	545647	l9sj	pa001	1991	1:24000
Reaville silt loam, 0 to 3 percent slopes	RhA	79	543071	l73f	pa011	1997	1:24000
Reaville silt loam, 3 to 8 percent slopes	RhB	68	543072	l73g	pa011	1997	1:24000
Reaville channery silt loam, 3 to 8 percent slopes	RlB	15519	543716	l7s7	pa017	1997	1:24000
Reaville channery silt loam, 8 to 15 percent slopes	RlC	4188	543717	l7s8	pa017	1997	1:24000
Reaville channery silt loam, 0 to 3 percent slopes	RlA	3087	543715	l7s6	pa017	1997	1:24000
Urban land-Reaville complex, 0 to 8 percent slopes	UyB	1586	543751	l7tc	pa017	1997	1:24000
Reaville silt loam, 3 to 8 percent slopes	RhB	15839	2232631	2dy7c	pa091	2008	1:12000
Reaville silt loam, 8 to 15 percent slopes	RhC	3913	2232635	2dy7h	pa091	2008	1:12000
Reaville silt loam, 0 to 3 percent slopes	RhA	2006	2232630	2dy7b	pa091	2008	1:12000
Reaville channery silt loam, 3 to 8 percent slopes	RfB	705	542949	l6zh	pa133	1990	1:24000
Reaville channery silt loam, 8 to 15 percent slopes	RfC	79	542950	l6zj	pa133	1990	1:24000
Reaville silt loam, 0 to 4 percent slopes	48A	2122	521211	khc8	va153	1985	1:15840

Map of Series Extent

Approximate geographic distribution of the REAVILLE 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 2023-10-04).