Soil Data Explorer - TRELONA

Official Series Description

Lab Data Summary

Aggregate lab data for the TRELONA soil series. This aggregation is based on all pedons with a current taxon name of TRELONA, 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 TRELONA 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 TRELONA 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 TRELONA 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 TRELONA 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 TRELONA 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 TRELONA 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 TRELONA 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 TRELONA 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 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 TRELONA, 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. WY-2012-03-23-05 | Goshen County, Southern Part - November 1971

   Typical pattern of soils, topography, and parent material in association 2 (Soil Survey of Goshen County, Wyoming, Southern Part; 1971).

Map Units

Map units containing TRELONA 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
Jayem-Phiferson-Trelona fine sandy loams, 3 to 10 percent slopes	146	67994	349606	2tvv6	wy027	1993	1:24000
Phiferson-Trelona fine sandy loams, 3 to 10 percent slopes	174	21744	349661	cqvd	wy027	1993	1:24000
Trelona-Phiferson-Vetal fine sandy loams, 6 to 30 percent slopes	212	11031	349723	cqxd	wy027	1993	1:24000
Tassel-Trelona-Phiferson fine sandy loams, 3 to 10 percent slopes	200	10277	349711	cqx0	wy027	1993	1:24000
Cedak-Trelona complex, 6 to 20 percent slopes	114	36	349541	cqqj	wy027	1993	1:24000
Jayem-Phiferson-Trelona fine sandy loams, 3 to 10 percent slopes	178	4358	1669700	2tvv6	wy609	2006	1:24000
Phiferson-Trelona fine sandy loams, 3 to 10 percent slopes	205	446	1669717	1t1gv	wy609	2006	1:24000
Dunday-Trelona complex, 3 to 35 percent slopes	DeE	40647	104686	3hxz	wy615	1965	1:20000
Rosebud-Dunday-Trelona loamy fine sands, 0 to 3 percent sl opes	ReA	5509	104735	3hzk	wy615	1965	1:20000
Rosebud-Dunday-Trelona loamy fine sands, 3 to 10 percent s lopes	ReC	4353	104736	3hzl	wy615	1965	1:20000
Rosebud-Trelona fine sandy loams, 0 to 6 percent slopes	RuB	3882	104743	3hzt	wy615	1965	1:20000
Rosebud-Trelona complex, 0 to 6 percent slopes	RtB	3563	104742	3hzs	wy615	1965	1:20000
Rosebud-Trelona fine sandy loams, 6 to 10 percent slopes	RuC	1777	104744	3hzv	wy615	1965	1:20000
Anselmo-Trelona loamy fine sands, 0 to 3 percent slopes	AtA	876	104661	3hx5	wy615	1965	1:20000
Rosebud-Trelona fine sandy loams, 10 to 20 percent slopes	RuD	822	104745	3hzw	wy615	1965	1:20000
Jayem-Manter-Trelona complex, 3 to 20 percent slopes	16D	66023	104857	2wcbr	wy715	1974	1:20000
Rosebud-Trelona fine sandy loams, 6 to 10 percent slopes	24C	5016	104871	3j3y	wy715	1974	1:20000
Rosebud-Trelona fine sandy loams, 0 to 6 percent slopes	24B	3363	104870	3j3x	wy715	1974	1:20000
Jayem-Phiferson-Trelona fine sandy loams, 3 to 10 percent slopes	63	869	1415164	2tvv6	wy715	1974	1:20000
Rosebud-Trelona fine sandy loams, 10 to 20 percent slopes	24D	305	104872	3j3z	wy715	1974	1:20000
Cedak-Trelona complex, 6 to 20 percent slopes	57	41	1415153	1jhl3	wy715	1974	1:20000

Map of Series Extent

Approximate geographic distribution of the TRELONA 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).