Soil Data Explorer - GRAINOLA

Official Series Description

Lab Data Summary

Aggregate lab data for the GRAINOLA soil series. This aggregation is based on all pedons with a current taxon name of GRAINOLA, 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 GRAINOLA were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
76	73-OK-57-18	73-OK113-57-18	Grainola	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.8249389,-96.740675
80A	90P0948	90OK103003	Grainola	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.3011093,-97.3227768
84B	76-OK-52-1	76-OK095-52-1	Grainola	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.0351639,-96.6912333
85	74-OK-10-3	74-OK019-10-3	Grainola	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.4339583,-97.3768917

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the GRAINOLA 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 GRAINOLA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the GRAINOLA 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 GRAINOLA 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).

There are insufficient data to create the 3D mountains figure.

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

Competing Series

Soil series competing with GRAINOLA share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the GRAINOLA 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the GRAINOLA 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).

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 GRAINOLA, 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. OK-2010-09-29-01 | Logan County - 2006

   Typical pattern of soils and underlying material in the Grainola-Masham-Ironmound general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

2. OK-2010-09-29-03 | Logan County - 2006

   Typical pattern of soils and underlying material in the Grainola-Renfrow-Piedmont general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

3. OK-2010-09-29-05 | Logan County - 2006

   Typical pattern of soils and underlying material in the Stephenville-Darsil-Harrah general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

4. OK-2010-09-29-07 | Noble County - 2005

   Typical pattern of soils and underlying material in the Grainola-Lucien-Masham general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

5. OK-2010-09-29-09 | Noble County - 2005

   Typical pattern of soils and underlying material in the Port-Ashport-Pulaski general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

6. OK-2010-09-29-10 | Noble County - 2005

   Typical pattern of soils and underlying material in the Teller-Konawa general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

7. OK-2010-09-29-11 | Noble County - 2005

   Typical pattern of soils and underlying material in the Darnell-Grainola-Newalla-Harrah general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

8. OK-2010-09-29-12 | Noble County - 2005

   Typical pattern of soils and underlying material in the Norge-Bethany-Kirkland general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

9. OK-2010-09-29-15 | Oklahoma County - 2004

   Typical pattern of soils and underlying material in the Renfrow-Grainola-Piedmont general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

10. OK-2010-09-29-16 | Oklahoma County - 2004

    Typical pattern of soils and underlying material in the Kirkland-Urban land-Renthin general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

11. OK-2010-09-29-17 | Oklahoma County - 2004

    Typical pattern of soils and underlying material in the Ashport-Miller general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

12. OK-2012-02-16-12 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Grainola-Grant map unit and the Port-Weswood map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

13. OK-2012-02-17-26 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Agra-Coyle and Steedman-Lucien-Grainola map units (Soil Survey of Payne County, Oklahoma; April 1987).

14. OK-2012-02-17-27 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Coyle-Grainola map unit (Soil Survey of Payne County, Oklahoma; April 1987).

15. OK-2012-02-17-28 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Grainola-Masham-Lucien map unit (Soil Survey of Payne County, Oklahoma; April 1987).

16. OK-2012-02-17-29 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Stephenville-Darnell map unit (Soil Survey of Payne County, Oklahoma; April 1987).

Map Units

Map units containing GRAINOLA 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
Renfrow-Grainola complex, 1 to 3 percent slopes	6421	12	1382729	1hdv5	ks077	1965	1:24000
Renfrow-Grainola complex, 1 to 3 percent slopes	6421	23	1444837	1khgn	ks095	1977	1:24000
Renfrow-Grainola complex, 1 to 3 percent slopes	6421	26213	1444666	1kh94	ks191	1974	1:24000
Grainola, Ashport frequently flooded, and Grant soils, 0 to 20 percent slopes	GAGF	56	622379	nwmr	ok003	1971	1:24000
Renthin-Grainola complex, 3 to 5 percent slopes, eroded	RnC2	13641	381766	dt81	ok011	1965	1:24000
Grainola-Port, frequently flooded, complex, 0 to 12 percent slopes	Bk	4733	381713	dt6b	ok011	1965	1:24000
Grainola-Rock outcrop complex, 5 to 15 percent slopes	VrE	6044	381986	dth4	ok017	1972	1:24000
Grainola clay loam, 3 to 5 percent slopes	VeC	3607	381985	2td64	ok017	1972	1:24000
Grainola soils, 3 to 5 percent slopes, eroded	VsC2	1856	381987	dth5	ok017	1972	1:24000
Tamford-Grainola complex, 5 to 12 percent slopes	42	11739	382027	dtjg	ok019	1977	1:24000
Kiti-Grainola complex, 5 to 20 percent slopes	19	9176	382001	dthm	ok019	1977	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	3	6873	382097	2tq76	ok027	1984	1:24000
Grainola-Ironmound complex, 5 to 12 percent slopes	6	5240	382122	dtmj	ok027	1984	1:24000
Lucien-Grainola-Zaneis complex, 5 to 12 percent slopes	LzD	36012	382191	dtpr	ok031	1965	1:24000
Zaneis-Grainola-Lucien complex, 5 to 20 percent slopes	Lz	16242	382237	dtr7	ok033	1961	1:24000
Grainola-Masham-Ironmound complex, 5 to 12 percent slopes	VrD	38392	382533	dv1s	ok047	1965	1:24000
Grainola, Ashport frequently flooded, and Grant soils, 0 to 20 percent slopes	Bk	32237	382484	dv06	ok047	1965	1:24000
Grainola-Masham complex, 3 to 5 percent slopes, eroded	VcC2	26472	382532	2wrk4	ok047	1965	1:24000
Grainola clay loam, 5 to 20 percent slopes	27	16039	382558	dv2l	ok049	1982	1:24000
Grainola clay loam, 3 to 5 percent slopes	26	4440	382557	2td64	ok049	1982	1:24000
Grainola cobbly clay loam, 5 to 20 percent slopes, eroded	28	698	382559	dv2m	ok049	1982	1:24000
Grainola-Urban land complex, 3 to 8 percent slopes	29	207	382560	dv2n	ok049	1982	1:24000
Grainola silty clay loam, 3 to 5 percent slopes	16	15037	382703	2tp6y	ok053	1983	1:24000
Grainola silty clay loam, 1 to 3 percent slopes	15	5310	382702	dv77	ok053	1983	1:24000
Zaneis, Lucien, and Grainola soils, 5 to 12 percent slopes	ZvD	107302	383269	2xm2m	ok067	1967	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	3059	383218	2tq76	ok067	1967	1:24000
Grainola clay loam, 3 to 5 percent slopes	VsC	1445	383259	2td64	ok067	1967	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	12392	383319	2tq76	ok071	1965	1:24000
Grainola clay loam, 3 to 5 percent slopes	VeC	2394	383378	2td64	ok071	1965	1:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely eroded	Es	1726	383328	2tp5m	ok071	1965	1:24000
Grainola-Shidler complex, 12 to 25 percent slopes	GrSF	1660	623391	nxpd	ok071	1965	1:24000
Dilworth-Grainola complex, 5 to 12 percent slopes	DiGE	184	623474	nxs2	ok071	1965	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Ab	34650	383384	2tq76	ok073	1960	1:24000
Grainola-Masham complex, 3 to 5 percent slopes, eroded	VcC3	31585	383424	2wrk4	ok073	1960	1:24000
Grainola clay loam, 1 to 3 percent slopes	VcB	6473	383423	dvzh	ok073	1960	1:24000
Renthin-Grainola complex, 3 to 5 percent slopes, severely eroded	RvC3	45226	383531	dw2z	ok081	1966	1:24000
Grainola-Ironmound complex, 5 to 15 percent slopes	VlE	34919	383544	dw3d	ok081	1966	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	19864	383497	2tq76	ok081	1966	1:24000
Grainola clay loam, 3 to 5 percent slopes	VcC	6023	383542	2td64	ok081	1966	1:24000
Grainola silty clay loam, 5 to 8 percent slopes, eroded	GraD2	17134	383624	dw5z	ok083	1994	1:12000
Grainola silty clay loam, 3 to 5 percent slopes	GraC	11026	383623	2tp6y	ok083	1994	1:12000
Ironmound-Coyle-Grainola complex, 5 to 8 percent slopes, severely eroded	ICGD3	3456	383630	dw65	ok083	1994	1:12000
Grainola-Masham-Gullied land complex, 5 to 15 percent slopes	GMGE4	1984	383613	dw5m	ok083	1994	1:12000
Grainola-Lucien complex, 5 to 12 percent slopes	GrLE	209	383622	2wrk2	ok083	1994	1:12000
Grainola-Ironmound complex, 3 to 12 percent slopes	GrIE	62	1587477	1q8wy	ok083	1994	1:12000
Grainola-Masham-Lucien complex, 5 to 40 percent slopes, very bouldery	GMLG	46	383614	2wrk3	ok083	1994	1:12000
Tamford-Grainola complex, 5 to 12 percent slopes	Vc	3348	383753	dwb4	ok085	1963	1:24000
Grainola-Masham complex, 5 to 45 percent slopes	Vb	1208	383752	dwb3	ok085	1963	1:24000
Tamford-Grainola complex, 5 to 12 percent slopes	46	12697	383804	dwcs	ok087	1976	1:24000
Grainola clay loam, 3 to 5 percent slopes	12	3954	383767	2td64	ok087	1976	1:24000
Grainola cobbly clay loam, 5 to 20 percent slopes, eroded	35	889	383941	dwj6	ok099	1982	1:24000
Grainola-Lucien complex, 5 to 12 percent slopes	GrLE	34415	384059	2wrk2	ok103	1994	1:24000
Renfrow and Grainola soils, 3 to 5 percent slopes, eroded	ReGC2	24745	384106	2tp5s	ok103	1994	1:24000
Grainola-Masham-Lucien complex, 5 to 40 percent slopes, very bouldery	GMLG	21814	384052	2wrk3	ok103	1994	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	21143	1907375	2zh6v	ok103	1994	1:24000
Grainola-Lucien complex, 1 to 5 percent slopes	GrLC	17674	384058	dwmz	ok103	1994	1:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely eroded	RGPD3	4511	384105	2tp5m	ok103	1994	1:24000
Grainola silty clay loam, 3 to 5 percent slopes	GraC	3155	384060	2tp6y	ok103	1994	1:24000
Dilworth-Grainola complex, 5 to 12 percent slopes	DiGE	2437	384048	dwmn	ok103	1994	1:24000
Grainola silty clay loam, 3 to 5 percent slopes, eroded	GriC2	4683	384165	dwrf	ok107	1996	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	GrAD	6853	384295	2tq76	ok109	1996	1:12000
Grainola-Ironmound complex, 3 to 12 percent slopes	GrIE	6478	384297	dwwp	ok109	1996	1:12000
Grainola-Urban land-Ironmound complex, 3 to 12 percent slopes	GUIE	4046	384291	dwwh	ok109	1996	1:12000
Grainola-Piedmont complex, 3 to 5 percent slopes, eroded	GrPC2	3784	384299	dwwr	ok109	1996	1:12000
Grainola-Piedmont complex, 1 to 3 percent slopes, eroded	GrPB2	1242	384298	dwwq	ok109	1996	1:12000
Grainola silty clay loam, 3 to 5 percent slopes	GraC	748	384300	2tp6y	ok109	1996	1:12000
Grainola-Shidler complex, 12 to 25 percent slopes	25	27028	623420	nxqb	ok113	1975	1:24000
Grainola-Shidler-Lucien complex, 1 to 20 percent slopes, very rocky	GSLF	12967	1675936	1t7yg	ok117	2007	1:24000
Grainola-Lucien complex, 1 to 5 percent slopes	GrLC	12681	1677338	1t9dp	ok117	2007	1:24000
Grainola-Lucien complex, 5 to 12 percent slopes	GrLE	11992	1423157	2wrk2	ok117	2007	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	11104	1675948	2zh6v	ok117	2007	1:24000
Grainola-Rock outcrop-Lucien complex, 5 to 20 percent slopes	GRLF	6328	1675908	1t7xk	ok117	2007	1:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely eroded	RGPD3	2519	1677033	2tp5m	ok117	2007	1:24000
Grainola-Masham-Lucien complex, 5 to 40 percent slopes, very bouldery	GMLG	22	1883786	2wrk3	ok117	2007	1:24000
Grainola-Lucien complex, 5 to 12 percent slopes	GrLE	21975	1907386	2wrk2	ok119	1983	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	13234	384538	2zh6v	ok119	1983	1:24000
Grainola-Shidler-Lucien complex, 1 to 20 percent slopes, very rocky	GSLF	12181	1907651	22124	ok119	1983	1:24000
Grainola-Lucien complex, 1 to 5 percent slopes	GrLC	10364	1907385	220sk	ok119	1983	1:24000
Renfrow and Grainola soils, 3 to 8 percent slopes, severely eroded	49	9496	384547	dx4r	ok119	1983	1:24000
Grainola clay loam, 3 to 5 percent slopes	65	6329	384565	2td64	ok119	1983	1:24000
Grainola silty clay loam, 5 to 12 percent slopes	49	36826	384711	dxb1	ok125	1975	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	50	20891	384713	2tq76	ok125	1975	1:24000
Grainola clay loam, 3 to 5 percent slopes	48	3928	384710	2td64	ok125	1975	1:24000
Grainola-Lucien complex, 5 to 12 percent slopes	18	8749	384803	2wrk2	ok133	1976	1:24000
Grainola and Aydelotte soils, 3 to 8 percent slopes, severely eroded	17	5908	384802	dxdz	ok133	1976	1:24000
Zaneis-Grainola-Lucien complex, 5 to 12 percent slopes	Lz	37710	384867	dxh2	ok137	1960	1:24000

Map of Series Extent

Approximate geographic distribution of the GRAINOLA 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).