Soil Data Explorer - GAYNOR

Official Series Description

Lab Data Summary

Aggregate lab data for the GAYNOR soil series. This aggregation is based on all pedons with a current taxon name of GAYNOR, 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 GAYNOR 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 GAYNOR 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 GAYNOR 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 GAYNOR 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 GAYNOR 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).

Competing Series

Soil series competing with GAYNOR 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 GAYNOR 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 GAYNOR 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 GAYNOR, 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 GAYNOR 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
Limon-Gaynor silty clay loams, 3 to 12 percent slopes	62	5510	498330	jqk5	co637	1986	1:24000
Limon-Gaynor silty clay loams, 0 to 3 percent slopes	61	813	498329	jqk4	co637	1986	1:24000
Limon-Gaynor silty clay loams, moderately wet, 0 to 3 percent slopes	63	425	498331	jqk6	co637	1986	1:24000
Colby-Gaynor association	Ct	985	497566	jprj	co643	1975	1:20000
Shingle-Gaynor complex, 3 to 20 percent slopes	SgE	922	497605	jpss	co643	1975	1:20000
Gaynor silty clay loam, 3 to 9 percent slopes	GaD	878	497571	jprp	co643	1975	1:20000
Gaynor silty clay loam, 1 to 3 percent slopes	GaB	307	497570	jprn	co643	1975	1:20000
Midway-Gaynor silty clay loams, 10 to 40 percent slopes	56	10800	496635	jnsh	co679	1976	1:24000
Gaynor-Midway silty clay loams, dry, 2 to 25 percent slopes	35	5759	496985	jp4s	co685	1979	1:24000
Samsil-Gaynor complex, 2 to 10 percent slopes	156	19810	349238	cqdr	wy011	1978	1:24000
Gaynor clay loam, 2 to 10 percent slopes	65	10999	349345	cqj6	wy011	1978	1:24000
Samsil-Gaynor complex, 10 to 30 percent slopes	157	5045	349239	cqds	wy011	1978	1:24000
Renohill-Gaynor clay loams, 3 to 10 percent slopes	148	4059	349229	cqdg	wy011	1978	1:24000
Renohill-Gaynor clay loams, 10 to 30 percent slopes	149	3947	349230	cqdh	wy011	1978	1:24000
Samsil-Gaynor complex, cool, 10 to 30 percent slopes	Q0852E	3927	2440103	2mx40	wy011	1978	1:24000
Gaynor-Limon clay loams, 6 to 10 percent slopes	66	756	349346	cqj7	wy011	1978	1:24000
Samsil-Gaynor complex, cool, 2 to 10 percent slopes	Q0852C	495	2440102	2mx3z	wy011	1978	1:24000
Razor-Gaynor, dry-Samsil, dry complex, 6 to 30 percent slopes	RAD	41194	350910	2xtvj	wy619	1971	1:24000
Limon-Gaynor association	LR	9708	350878	cs3n	wy619	1971	1:24000
Samsil-Gaynor-Cadoma complex, rolling	SCD	6598	350922	cs52	wy619	1971	1:24000
Renohill-Danko association	RD	2637	350911	cs4q	wy619	1971	1:24000
Gaynor-Midway-Stutzman-like complex, 0 to 30 percent slopes -- Draft	358		152527	53q7	wy629		1:24000

Map of Series Extent

Approximate geographic distribution of the GAYNOR 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).