Soil Data Explorer - ASHPORT

Official Series Description

Lab Data Summary

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

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

Competing Series

Soil series competing with ASHPORT 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 ASHPORT 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 ASHPORT 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 flats position figure.

Soil series sharing subgroup-level classification with ASHPORT, 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. 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-2010-09-29-02 | Logan County - 2006

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

3. OK-2010-09-29-06 | Logan County - 2006

   Typical pattern of soils and underlying material in the Coyle-Ironmound-Zaneis 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-2010-09-29-08 | Noble County - 2005

   Typical pattern of soils and underlying material in the Keokuk-Goodnight-Ashport and the McLain-Braman-Lela general soil map units (Soil Survey of Noble County, Oklahoma; 2005).

6. 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).

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-2010-09-29-16 | 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).

10. 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).

11. 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).

12. 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).

Map Units

Map units containing ASHPORT 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
Grainola, Ashport frequently flooded, and Grant soils, 0 to 20 percent slopes	GAGF	56	622379	nwmr	ok003	1971	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	3	6873	382097	2tq76	ok027	1984	1:24000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	96	5541	382160	2tq74	ok027	1984	1:24000
Norge-Ashport silt loams complex, 0 to 8 percent slopes, frequently flooded	33	4763	382100	30g73	ok027	1984	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	AstA	81	752390	2tq75	ok027	1984	1:24000
Ashport loam, 0 to 1 percent slopes, occasionally flooded	Po	31836	382196	2tq77	ok031	1965	1:24000
Ashport clay loam, 0 to 1 percent slopes, occasionally flooded	Pc	30816	382195	2tq71	ok031	1965	1:24000
Ashport, Port and Yahola soils, 0 to 1 percent slopes, frequently flooded	Br	12502	382166	2yh68	ok031	1965	1:24000
Ashport-Oscar complex, 0 to 1 percent slopes, occasionally flooded	Ps	10361	382197	2yh69	ok031	1965	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	Ga	22212	382286	2tq75	ok037	1952	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	304	2516362	2tq7b	ok037	1952	1:24000
Grainola, Ashport frequently flooded, and Grant soils, 0 to 20 percent slopes	Bk	32237	382484	dv06	ok047	1965	1:24000
Pulaski and Ashport soils, 0 to 1 percent slopes, frequently flooded	Br	19601	382485	30g74	ok047	1965	1:24000
Ashport silty clay loam, 0 to 1 percent slopes, occasionally flooded	2	1069	382550	2tq73	ok049	1982	1:24000
Masham-Ashport frequently flooded complex, 0 to 20 percent slopes	33	10521	382722	dv7w	ok053	1983	1:24000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	AspA	16	601438	2tq74	ok053	1983	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	3059	383218	2tq76	ok067	1967	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	12392	383319	2tq76	ok071	1965	1:24000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	Ps	9245	383358	2tq74	ok071	1965	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	8631	383321	2tq7b	ok071	1965	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	Pf	2772	383357	2tq75	ok071	1965	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Ab	34650	383384	2tq76	ok073	1960	1:24000
Ashport clay loam, 0 to 1 percent slopes, occasionally flooded	PoA	21300	383409	2tq71	ok073	1960	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	10328	383386	2tq7b	ok073	1960	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	Bk	19864	383497	2tq76	ok081	1966	1:24000
Ashport clay loam, 0 to 1 percent slopes, occasionally flooded	Pc	10189	383523	2tq71	ok081	1966	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	8385	383501	2tq7b	ok081	1966	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	AstA	17871	383592	2tq75	ok083	1994	1:12000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	AspA	7785	383591	2tq74	ok083	1994	1:12000
Coyle-Ashport frequently flooded-Ironmound complex, 1 to 8 percent slopes	CAID	6262	383597	dw53	ok083	1994	1:12000
Ashport clay loam, 0 to 1 percent slopes, occasionally flooded	Nc	1722	383729	2tq71	ok085	1963	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	39	6631	383796	2tq7b	ok087	1976	1:24000
Ashport loam, 0 to 1 percent slopes, occasionally flooded	1	4195	383764	2tq77	ok087	1976	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	28954	384030	2tq7b	ok103	1994	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	21143	1907375	2zh6v	ok103	1994	1:24000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	AspA	7040	384032	2tq74	ok103	1994	1:24000
Ashport silty clay loam, 0 to 1 percent slopes, occasionally flooded	AhpA	4026	384031	2tq73	ok103	1994	1:24000
Ashport silt loam, 1 to 3 percent slopes, occasionally flooded	AspB	504	384033	2yh67	ok103	1994	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	AstA	8489	384271	2tq75	ok109	1996	1:12000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	GrAD	6853	384295	2tq76	ok109	1996	1:12000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	AspA	3473	384270	2tq74	ok109	1996	1:12000
Ashport silty clay loam, 0 to 1 percent slopes, occasionally flooded	AhpA	1734	384267	2tq73	ok109	1996	1:12000
Agra-Ashport, frequently flooded complex, 0 to 12 percent slopes	18	26995	623413	2y2sc	ok113	1975	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	1	1427094	2tq7b	ok113	1975	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	18379	1423149	2tq7b	ok117	2007	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	11104	1675948	2zh6v	ok117	2007	1:24000
Ashport silt loam, 0 to 1 percent slopes, occasionally flooded	AspA	1984	1677023	2tq74	ok117	2007	1:24000
Ashport silty clay loam, 0 to 1 percent slopes, occasionally flooded	AhpA	93	1883787	2tq73	ok117	2007	1:24000
Grainola-Ashport frequently flooded-Mulhall complex, 0 to 8 percent slopes	GAMD	13234	384538	2zh6v	ok119	1983	1:24000
Ashport silty clay loam, 0 to 1 percent slopes, occasionally flooded	42	3257	384540	2tq73	ok119	1983	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	1639	1900485	2tq7b	ok119	1983	1:24000
Ashport silt loam, 0 to 1 percent slopes, frequently flooded	AstA	15	623491	2tq75	ok119	1983	1:24000
Grainola-Ashport, frequently flooded, complex, 0 to 12 percent slopes	50	20891	384713	2tq76	ok125	1975	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	34	7080	384695	2tq7b	ok125	1975	1:24000
Zaneis-Ashport frequently flooded complex, 0 to 12 percent slopes	Ba	24234	384846	dxgd	ok137	1960	1:24000

Map of Series Extent

Approximate geographic distribution of the ASHPORT 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).