Soil Data Explorer - RAYNESFORD

Official Series Description

Lab Data Summary

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

Competing Series

Soil series competing with RAYNESFORD 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 RAYNESFORD 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the RAYNESFORD 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 2D hillslope position figure.

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 terrace figure.

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

Soil series sharing subgroup-level classification with RAYNESFORD, 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

No block diagrams are available.

Map Units

Map units containing RAYNESFORD 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
Tiban-Raynesford-Woodhurst families, complex, gentle mountain slopes	524E	51	2024044	25y5r	id758	1998	1:24000
Raynesford-Hanson complex, 4 to 15 percent slopes	185	3779	342418	ch9r	mt027	1979	1:24000
Raynesford-Hanson complex, 0 to 4 percent slopes	184	3257	342417	ch9q	mt027	1979	1:24000
Bridger-Raynesford complex, 0 to 4 percent slopes	30	1815	342529	chfb	mt027	1979	1:24000
Hanson-Raynesford complex, rolling	HS	15984	146831	4xsh	mt600	1969	1:24000
Hanson-Raynesford complex, undulating	HR	8631	146830	4xsg	mt600	1969	1:24000
Raynesford-Hanson complex, hilly	RD	5081	146907	4xvy	mt600	1969	1:24000
Raynesford-Bear Lake complex, rolling	RC	2804	146906	4xvx	mt600	1969	1:24000
Raynesford-Fifer complex, hilly	FV	2171	146806	4xrp	mt600	1969	1:24000
Skaggs-Raynesford loams, 8 to 35 percent slopes	Ss	13296	147425	4ydn	mt602	1963	1:20000
Raynesford and Adel loams, 4 to 8 percent slopes	Rd	3509	147406	4yd1	mt602	1963	1:20000
Judith and Raynesford stony loams, 2 to 8 percent slopes	Jr	1844	147380	4yc6	mt602	1963	1:20000
Raynesford and Adel stony loams, 4 to 15 percent slopes	Rn	1410	147408	4yd3	mt602	1963	1:20000
Raynesford and Adel loams, 2 to 4 percent slopes	Ra	935	147405	4yd0	mt602	1963	1:20000
Raynesford and Adel loams, 8 to 15 percent slopes	Rf	764	147407	4yd2	mt602	1963	1:20000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes	664D	27	3039577	pg6s	mt602	1963	1:20000
Tiban-Raynesford-Woodhurst families, complex, gentle mountain slopes	524E	28015	148608	4zmt	mt605	2007	1:24000
Maciver-Tibson-Raynesford families, complex, pediment slopes	624D	1739	148730	4zrr	mt605	2007	1:24000
Raynesford gravelly loam, 15 to 35 percent slopes	5E	92	2450915	2n8cs	mt605	2007	1:24000
Raynesford-Bellcanyon complex, 15 to 35 percent slopes	305E	44	2597991	4zgk	mt605	2007	1:24000
Whitore, stony-Tropal, very stony-Raynesford, stony complex, 12 to 45 percent slopes	820E	40	1859717	20f5w	mt605	2007	1:24000
Whitore, very stony-Raynesford complex, 15 to 40 percent slopes	817E	32	1859716	20f5v	mt605	2007	1:24000
Raynesford-Nikat complex, 35 to 60 percent slopes, stony	416F	21	2598025	4zgt	mt605	2007	1:24000
Raynesford-Bellcanyon complex, 4 to 15 percent slopes	105D	20	2598024	4zf0	mt605	2007	1:24000
Raynesford loam, undulating	Ra	6398	346117	cm52	mt607	1970	1:24000
Crago, very stony-Raynesford-Farlin complex, 8 to 35 percent slopes	210E	3436	797982	vscc	mt612	2011	1:24000
Raynesford-Bellcanyon complex, 4 to 15 percent slopes	105D	2778	148397	4zf0	mt612	2011	1:24000
Levengood, very stony-Raynesford, very stony-Tropal, extremely stony complex, 8 to 35 percent slopes	410E	1759	2425168	2mdl7	mt612	2011	1:24000
Raynesford gravelly loam, 15 to 35 percent slopes	5E	1489	148472	4zhf	mt612	2011	1:24000
Raynesford-Bellcanyon complex, 15 to 35 percent slopes	305E	1328	148445	4zgk	mt612	2011	1:24000
Raynesford-Nikat complex, 35 to 60 percent slopes, stony	416F	1109	148453	4zgt	mt612	2011	1:24000
Raynesford-Skaggs loams, 4 to 8 percent slopes	158	3884	341821	cgph	mt613	1975	1:24000
Raynesford-Sheege complex, 4 to 15 percent slopes	160	2499	341824	cgpl	mt613	1975	1:24000
Raynesford-Skaggs loams, 8 to 20 percent slopes	159	2242	341822	cgpj	mt613	1975	1:24000
Raynesford loam, 20 to 40 percent slopes	157	1614	341820	cgpg	mt613	1975	1:24000
Raynesford loam, 8 to 20 percent slopes	156	817	341819	cgpf	mt613	1975	1:24000
Raynesford-Nikat-Levengood complex, 8 to 35 percent slopes	954E	2226	2486606	2pgj3	mt614	2012	1:24000
Raynesford-Nikat complex, 35 to 60 percent slopes, stony	416F	121	2520732	4zgt	mt614	2012	1:24000
Raynesford gravelly loam, 15 to 35 percent slopes	5E	25	2520741	4zhf	mt614	2012	1:24000
Raynesford, stony-Hanson, very stony complex, 8 to 25 percent slopes	681E	5402	155658	56z7	mt622	1997	1:24000
Farlin-Raynesford complex, 2 to 8 percent slopes	527C	426	2487018	2pgyd	mt624	2021	1:24000
Levengood-Raynesford complex, 8 to 35 percent slopes	526E	148	2487020	2pgyg	mt624	2021	1:24000
Raynesford silt loam, 4 to 15 percent slopes	1680D	162	150683	51sr	mt627	1998	1:24000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes, 8 to 15 percent slopes	664D	841	2486272	2pg5b	mt632		1:24000
Farlin-Raynesford complex, 2 to 8 percent slopes	527C	150	2512442	2pgyd	mt632		1:24000
Whitore, stony-Tropal, very stony-Raynesford, stony, complex, 12 to 45 percent slopes	820E	21	1703212	1v5bb	mt635	2006	1:24000
Skaggs-Raynesford-Tropal, very stony, complex, 8 to 35 percent slopes	823E	10	1703213	1v5bc	mt635	2006	1:24000
Hanson-Raynesford complex, 8 to 35 percent slopes	52	2813	146477	4xf2	mt636	1983	1:24000
Raynesford loam, 2 to 8 percent slopes	100	255	146371	4x9n	mt636	1983	1:24000
Farlin, stony-Raynesford complex, 8 to 15 percent slopes	664D	2867	639275	pg6s	mt637	2014	1:24000
Levengood-Skaggs, very stony-Raynesford complex, 15 to 35 percent slopes	156E	2446	2425971	2mff4	mt637	2014	1:24000
Raynesford, stony-Hanson, very stony complex, 8 to 25 percent slopes	9681E	205	2493523	56z7	mt637	2014	1:24000
Hanson-Raynesford complex, 0 to 4 percent slopes	195B	8324	348424	cpkh	mt657	1990	1:24000
Raynesford-Hanson complex, 4 to 15 percent slopes	485D	70	1531684	1ndv5	mt666	2008	1:24000
Hanson,stony -Raynesford - Tropal, stony complex, 8 to 45 percent slopes	4503E	1972	697945	rf8c	mt669		1:24000
Whitore, very stony-Raynesford complex, 15 to 40 percent slopes	817E	1273	1424811	1jtmn	mt670	2007	1:24000
Raynesford-Whitore, very stony complex, 4 to 20 percent slopes	818D	366	1424810	1jtmm	mt670	2007	1:24000
Raynesford-Whitore complex, 4 to 15 percent slopes, stony	819D	362	1424809	1jtml	mt670	2007	1:24000
Whitore, stony-Tropal, very stony-Raynesford, stony complex, 12 to 45 percent slopes	820E	311	1424808	1jtmk	mt670	2007	1:24000
Raynesford-Whitore-Skaggs complex, 12 to 30 percent slopes	826E	159	1424803	1jtmd	mt670	2007	1:24000
Skaggs-Raynesford-Tropal, very stony complex, 8 to 35 percent slopes	823E	112	1424806	1jtmh	mt670	2007	1:24000
Hanson-Raynesford association, 0 to 30 percent slopes	21	1765	158032	59ft	wy650	1982	1:24000

Map of Series Extent

Approximate geographic distribution of the RAYNESFORD 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).