Soil Data Explorer - FRIO

Official Series Description

Lab Data Summary

Aggregate lab data for the FRIO soil series. This aggregation is based on all pedons with a current taxon name of FRIO, 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 FRIO 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
85	81P0099	80TX099003	Frio	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	31.3172226,-97.4705582
86A	81P0602	81TX027006	Frio	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	31.0286102,-97.4116669

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FRIO 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 FRIO 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 FRIO 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 FRIO 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.

Competing Series

Soil series competing with FRIO 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 FRIO 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 FRIO 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 FRIO, 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. TX-2010-11-03-23 | Hamilton County - 2007

   Pattern of soils and underlying material in the Minwells-Bastsil and Bosque-Frio-Venus general soil map units (Soil Survey of Hamilton County, Texas; 2007).

2. TX-2010-11-04-06 | McLennan County - 2001

   Pattern of soils in the Crawford-Purves and Slidell-Sanger general soil map units (Soil Survey of McLennan County, Texas; 2001).

3. TX-2012-03-20-29 | Coryell County - May 1985

   Typical pattern of soils in the Bosque-Frio-Lewisville map unit and the Bastsil-Minwells map unit (Soil Survey of Coryell County, TX; 1985).

4. TX-2012-03-20-41 | Ellis County - August 1964

   Block diagram showing relation of eight soil associations in Ellis County to the underlying materials and surface relief (Soil Survey of Ellis County, TX; 1964).

5. TX-2012-03-20-42 | Ellis County - August 1964

   Geographical association of soils on benches. Burleson clay, terrace; Houston Black clay, terrace; and Lewisville soils are in soil association 1 (Soil Survey of Ellis County, TX; 1964).

6. TX-2012-03-20-44 | Ellis County - August 1964

   Relation of soils in soil association 4 to the underlying chalky bedrock. Eddy soils and Stephen silty clay soils are in soil association 4 (Soil Survey of Ellis County, TX; 1964).

7. TX-2012-03-20-46 | Ellis County - August 1964

   Geographical association of soils on flood plains. The Wilson and the Crockett soils are in soil association 7 (Soil Survey of Ellis County, TX; 1964).

8. TX-2012-03-21-17 | Johnson County - October 1985

   Typical pattern of soils and parent material in the Aledo-Bolar map unit (Soil Survey of Johnson County, TX; 1985).

9. TX-2012-03-21-46 | McCulloch County - November 1974

   Pattern of soils in Rowena-Mereta association (Soil Survey of McCulloch County, TX; 1974).

10. TX-2012-03-21-50 | Menard County - February 1967

    Soils of the Knippa-Uvalde soil association (Soil Survey of Menard County, TX; 1967).

11. TX-2012-03-21-67 | Shackelford County - February 1990

    Typical pattern of soils and parent material in the Lueders-Throck-Nukrum map unit (Soil Survey of Shackelford County, TX; 1990).

12. TX-2012-03-21-70 | Shackelford County - February 1990

    Typical pattern of soils and parent material in the Leeray-Pitzer-Wichita map unit (Soil Survey of Shackelford County, TX; 1990).

13. TX-2012-03-21-82 | Stephens County - May 1994

    Typical pattern of soils and parent material in the Gageby-Thurber-Frio general soil map unit (Soil Survey of Stephens County, TX; 1994).

14. TX-2012-03-21-84 | Stephens County - May 1994

    Typical pattern of soils and parent material in the Clearfork-Clairemont general soil map unit (Soil Survey of Stephens County, TX; 1994).

15. TX-2012-03-22-23 | Wise County - May 1989

    Typical pattern of the Venus-Aledo-Somervell general soil map unit (Soil Survey of Wise County, TX; 1989).

Map Units

Map units containing FRIO 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
Frio silty clay, 0 to 1 percent slopes, frequently flooded	FsA	9587	391093	2wg92	tx027	1972	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FrA	9147	391092	2ssh3	tx027	1972	1:24000
Tinn and Frio soils, 0 to 1 percent slopes, frequently flooded	Tf	20460	390507	2y0v4	tx029	2000	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	26201	362998	2y2st	tx035	1977	1:24000
Frio-Gageby association, frequently flooded	18	25276	363591	d6br	tx059	1979	1:24000
Frio clay loam, occasionally flooded	17	9090	363590	d6bq	tx059	1979	1:24000
Frio silty clay loam	Fr	3129	363976	d6r5	tx081	1968	1:24000
Frio clay loam, frequently flooded	Fr	32842	364011	d6s9	tx083	1968	1:24000
Frio clay loam, 0 to 1 percent slopes, occasionally flooded	Fo	23038	364010	d6s8	tx083	1968	1:24000
Frio clay loam, occasionally flooded	Fo	4780	364071	d6v7	tx085	1965	1:20000
Frio clay loam, frequently flooded	Ff	2204	364070	d6v6	tx085	1965	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	10817	364373	2y2st	tx093	1974	1:20000
Frio silty clay loam, 0 to 2 percent slopes, occasionally flooded	Fo	10777	364430	2t26s	tx095	1985	1:24000
Frio soils, 0 to 2 percent slopes, frequently flooded	Fr	5264	364431	2t26w	tx095	1985	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	3574	364470	2y2st	tx097	1973	1:24000
Frio clay loam, 0 to 1 percent slopes, frequently flooded	23	3010	364471	2zht7	tx097	1973	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	10062	391159	2y2st	tx099	1983	1:24000
Frio clay loam, 0 to 1 percent slopes, frequently flooded	Fs	824	608920	2zht7	tx099	1983	1:24000
Frio silty clay, 0 to 1 percent slopes, frequently flooded	37	10411	364819	2wg92	tx113	1975	1:20000
Frio-Urban land complex, 0 to 1 percent slopes, frequently flooded	38	7764	364820	2ylmf	tx113	1975	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	36	5832	364818	2ssh3	tx113	1975	1:20000
Frio clay loam, 0 to 1 percent slopes, frequently flooded	34	18344	364985	2zht7	tx121	1975	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	6489	364984	2y2st	tx121	1975	1:24000
Frio silty clay, 0 to 1 percent slopes, frequently flooded	Fr	4960	365297	2wg92	tx139	1962	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	Fs	2426	365298	2ssh3	tx139	1962	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	20608	365372	2y2st	tx143	1966	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	6055	376663	2y2st	tx193	1994	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	8853	368166	2y2st	tx251	1981	1:20000
Frio silty clay loam, 0 to 2 percent slopes, occasionally flooded	Fr	9194	368550	2t26s	tx267	1980	1:31680
Frio soils, 0 to 2 percent slopes, frequently flooded	Fr	12327	369943	2t26w	tx307	1970	1:24000
Frio clay loam, 0 to 1 percent slopes, rarely flooded	Fo	9617	369942	2t26n	tx307	1970	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	13248	370096	2y2st	tx309	1992	1:24000
Frio clay loam, 0 to 1 percent slopes, rarely flooded	FcA	6166	370599	2t26n	tx327	1965	1:20000
Frio silty clay loam, 0 to 2 percent slopes, occasionally flooded	FcB	3535	370600	2t26s	tx327	1965	1:20000
Frio soils, 0 to 2 percent slopes, frequently flooded	Fr	1719	370601	2t26w	tx327	1965	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FrA	51857	370673	2ssh3	tx331	1988	1:24000
Frio silty clay loam, 0 to 1 percent slopes, occasionally flooded	FsoA	4119	390945	2zh6l	tx363	1979	1:24000
Frio silty clay loam, 0 to 1 percent slopes, frequently flooded	FsfA	1092	390946	2zh6p	tx363	1979	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	7622	390879	2y2st	tx367	1973	1:20000
Frio clay loam, 0 to 1 percent slopes, frequently flooded	Ff	6291	390880	2zht7	tx367	1973	1:20000
Frio silty clay loam, 0 to 2 percent slopes, occasionally flooded	Fr	16694	371947	2t26s	tx411	1980	1:24000
Frio soils, 0 to 2 percent slopes, frequently flooded	Fs	5058	371948	2t26w	tx411	1980	1:24000
Frio silty clay, occasionally flooded	Fr	38096	372057	dh4v	tx417	1985	1:24000
Frio silty clay loam, 0 to 1 percent slopes, occasionally flooded	FsoA	5346	372179	2zh6l	tx429	1985	1:24000
Frio silty clay loam, 0 to 1 percent slopes, frequently flooded	FsfA	1239	372180	2zh6p	tx429	1985	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	11178	372371	2y2st	tx439	1979	1:20000
Frio clay loam, 0 to 1 percent slopes, frequently flooded	Ff	7738	372372	2zht7	tx439	1979	1:20000
Frio-Urban land complex, 0 to 1 percent slopes, occasionally flooded	FoUA	6702	372373	2y2sv	tx439	1979	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FrA	3437	3130110	2ssh3	tx491	1981	1:20000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	10823	373663	2y2st	tx497	1984	1:20000
Frio silty clay loam, 0 to 1 percent slopes, occasionally flooded	FsoA	31808	391006	2zh6l	tx602	1975	1:24000
Frio silty clay loam, 0 to 1 percent slopes, frequently flooded	FsfA	14950	391007	2zh6p	tx602	1975	1:24000
Frio-Urban land complex, 0 to 1 percent slopes, very rarely flooded	FrUA	339	391008	2zh6t	tx602	1975	1:24000
Frio silty clay, 0 to 1 percent slopes, occasionally flooded	FriA	9260	374337	2y2st	tx609	1975	1:20000

Map of Series Extent

Approximate geographic distribution of the FRIO 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).