Soil Data Explorer - PORT

Official Series Description

Lab Data Summary

Aggregate lab data for the PORT soil series. This aggregation is based on all pedons with a current taxon name of PORT, 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 PORT 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
80A	68-OK-60-1	68-OK119-60-1	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1224639,-97.0955806
80A	72-OK-60-5	72-OK119-60-5	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1565528,-97.303625
80A	74-OK-60-1	74-OK119-60-1	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1223278,-97.1238139
80A	74-OK-60-3	74-OK119-60-3	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1209222,-97.01165
80A	75-OK-60-1	75-OK119-60-1	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1123944,-97.1062667
80A	76-OK-60-33	76-OK119-60-33	Port	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1182472,-97.0969028
80A	90P0949	90OK103004	Port	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.3477783,-97.2944412
80A	91P0875	91OK083004	Port	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.9255562,-97.2938919
80A	99P0224	99OK017001	PORT	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.5625,-98.0458298
80A	00P1354	S2000OK051001	Port	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.0653343,-97.793251

Water Balance

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

Select annual climate data summaries for the PORT 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 PORT 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 PORT share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the PORT 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).

Geomorphic description summaries for the PORT 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 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 PORT, 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. KS-2012-01-25-16 | Reno County - March 1966

   Cross section of the Renfrow-Vernon association downslope from the Clark-Ost association (Soil Survey of Reno County, Kansas; 1966).

2. KS-2012-01-25-17 | Reno County - March 1966

   Cross section of the Nash-Lucien association in the south-central part of the county (Soil Survey of Reno County, Kansas; 1966).

3. 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).

4. 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).

5. 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).

6. 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).

7. OK-2012-02-16-14 | Comanche County - August 1967

   Topography and underlying material of major soils in associations 1 and 7 (Soil Survey of Comanche County, Oklahoma; August 1967).

8. OK-2012-02-16-16 | Comanche County - August 1967

   Topography and underlying material of Lawton soils and other extensive soils in northwestern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

9. OK-2012-02-16-17 | Comanche County - August 1967

   Topography and underlying material of Waurika soils and other extensive soils in southeastern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

10. OK-2012-02-16-18 | Comanche County - August 1967

    Topography and underlying material of Windthorst soils and other extensive soils in southwestern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

11. OK-2012-02-16-19 | Cotton County - December 1963

    Typical pattern of Foard and Tillmans soils on gently undulating uplands in association 1 (Soil Survey of Cotton County, Oklahoma; December 1963).

12. OK-2012-02-16-22 | Cotton County - December 1963

    Typical pattern of moderately sloping Vernon soils in association 8 (Soil Survey of Cotton County, Oklahoma; December 1963).

13. OK-2012-02-16-23 | Cotton County - December 1963

    Schematic diagram showing the location of the Chickasha and other extensive soils in the east-central part of Cotton County (Soil Survey of Cotton County, Oklahoma; December 1963).

14. OK-2012-02-16-24 | Dewey County - December 1963

    Typical pattern of the soils in associations 1 and 2 (Soil Survey of Dewey County, Oklahoma; December 1963).

15. OK-2012-02-16-32 | Garfield County - October 1967

    Typical pattern of soils in the Grant-Pond Creek association, and Port, Reinach, and Pulaski soils of soil association 2 on the bordering flood plains (Soil Survey of Garfield County, Oklahoma; October 1967).

16. OK-2012-02-16-34 | Garfield County - October 1967

    Typical pattern of soils in the Kirkland-Bethany-Tabler association (Soil Survey of Garfield County, Oklahoma; October 1967).

17. OK-2012-02-16-51 | Jackson County - June 1961

    Typical pattern of La Casa and associated soils, Rough broken land, and Rock outcrop (Soil Survey of Jackson County, Oklahoma; June 1961).

18. OK-2012-02-17-01 | Lincoln County - January 1970

    Typical pattern of soils in associations 1 and 2 (Soil Survey of Lincoln County, Oklahoma; January 1970).

19. OK-2012-02-17-02 | Lincoln County - January 1970

    Typical pattern of soils in association 3 (Soil Survey of Lincoln County, Oklahoma; January 1970).

20. OK-2012-02-17-03 | Logan County - June 1960

    Soils of the Zaneis-Lucien-Chickasha and the Renfrow-Vernon-Kirkland associations on red clays, sandstone, siltstone, and alluvium. They have developed largely on the Wellington, Garber, and Hennessey formations that dip successively toward the west (Soil Survey of Logan County, Oklahoma; June 1960).

21. OK-2012-02-17-04 | Logan County - June 1960

    Soils of southeastern Logan County on reddish sandstone, colluvium, and alluvium (Soil Survey of Logan County, Oklahoma; June 1960).

22. OK-2012-02-17-08 | Love County - September 1966

    Diagram showing typical relief in the northwestern corner of the county and the relative positions of the soils in association 4 (Soil Survey of Love County, Oklahoma; September 1966).

23. OK-2012-02-17-12 | Major County - October 1968

    Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; October 1968).

24. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

25. OK-2012-02-17-21 | Pawnee County - March 1959

    Prairie soils of central and eastern Pawnee County formed in sandstone, shale, and limestone, and in accompanying alluvium (Soil Survey of Pawnee County, Oklahoma; March 1959).

26. OK-2012-02-17-22 | Pawnee County - March 1959

    Prairie soils of western Pawnee County formed in clay and sandy strata of the Permian "redbeds" area, and in accompanying alluvium (Soil Survey of Pawnee County, Oklahoma; March 1959).

27. OK-2012-02-17-37 | Pontotoc County - April 1973

    Pattern of soils in the Stephenville-Darnell-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

28. OK-2012-02-17-38 | Pontotoc County - April 1973

    Pattern of soils in the Chigley-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

29. OK-2012-02-17-41 | Roger Mills County - August 1963

    Typical pattern of soils in associations 6, 7, and 9 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

30. OK-2012-02-17-48 | Stephens County - 1964

    Typical pattern of soils in associations 1 and 5 (Soil Survey of Stephens County, Oklahoma; 1964).

31. OK-2012-02-17-49 | Stephens County - 1964

    Typical pattern of soils in association 3 (Soil Survey of Stephens County, Oklahoma; 1964).

32. OK-2012-02-17-51 | Stephens County - 1964

    Typical pattern of soils in associations 6, 7, and 8 (Soil Survey of Stephens County, Oklahoma; 1964).

33. OK-2012-02-17-60 | Woodward County - November 1963

    Typical pattern of soils of the Port association (Soil Survey of Woodward County, Oklahoma; November 1963).

34. TX-2012-03-19-10 | Archer County - April 1995

    Typical pattern of soils and parent material in the Bluegrove-Jolly-Weswind general soil map unit (Soil Survey of Archer County, TX; 1995).

35. TX-2012-03-19-11 | Archer County - April 1995

    Typical pattern of soils and parent material in the Kamay-Deandale general soil map unit (Soil Survey of Archer County, TX; 1995).

36. TX-2012-03-19-13 | Archer County - April 1995

    Typical pattern of soils and parent material in the Tillman-Vernon general soil map unit (Soil Survey of Archer County, TX; 1995).

Map Units

Map units containing PORT 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
Woodward-Port complex, 0 to 20 percent slopes	5492	32	1382533	2w5ql	ks007	1973	1:24000
Port silt loam, occasionally flooded	5334	1990	1381281	1hcbg	ks033	1987	1:24000
Woodward-Port complex, 0 to 20 percent slopes	5492	25606	1382751	2w5ql	ks077	1965	1:24000
Woodward-Port complex, 0 to 20 percent slopes	5492	3	1444611	2w5ql	ks191	1974	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	GuE	10113	381430	2tq64	ok003	1971	1:24000
Yahola and Port soils, 0 to 1 percent slopes, frequently flooded	Yp	7463	381451	2tq6w	ok003	1971	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Pr	7286	381436	2tq60	ok003	1971	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	42	1701	381680	dt58	ok009	1978	1:24000
Yahola and Port soils, 0 to 1 percent slopes, frequently flooded	Br	9869	381714	2tq6w	ok011	1965	1:24000
Port loam, 0 to 1 percent slopes, occasionally flooded	Po	7105	381759	2tq5z	ok011	1965	1:24000
Port clay loam, 0 to 1 percent slopes, occasionally flooded	Pc	5753	381758	2tq6j	ok011	1965	1:24000
Grainola-Port, frequently flooded, complex, 0 to 12 percent slopes	Bk	4733	381713	dt6b	ok011	1965	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Po	24968	381913	2tq60	ok015	1967	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	Bk	9334	381870	2tq64	ok015	1967	1:24000
Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded, channeled	Pp	3019	381914	2tq6r	ok015	1967	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	GpE	23719	381948	2tq64	ok017	1972	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Po	19708	381971	2tq60	ok017	1972	1:24000
Port silty clay loam, 0 to 1 percent slopes, frequently flooded	Pw	6021	381972	dtgp	ok017	1972	1:24000
Port silt loam, 0 to 1 percent slopes, frequently flooded	94	5401	382158	2tq62	ok027	1984	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	93	3483	382157	2tq60	ok027	1984	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	92	3045	382156	2tq6k	ok027	1984	1:24000
Port-Urban land complex, 0 to 1 percent slopes, occasionally flooded	98	82	382162	dtnt	ok027	1984	1:24000
Ashport, Port and Yahola soils, 0 to 1 percent slopes, frequently flooded	Br	12502	382166	2yh68	ok031	1965	1:24000
Port clay loam, 0 to 1 percent slopes, occasionally flooded	Po	26210	382240	2tq6j	ok033	1961	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	Ps	13179	382242	2tq6q	ok033	1961	1:24000
Port loam, 0 to 1 percent slopes, occasionally flooded	Pr	12406	382241	2tq5z	ok033	1961	1:24000
Port loam, 0 to 1 percent slopes, frequently flooded	Bd	11648	382221	dtqq	ok033	1961	1:24000
Vernon-Port, frequently flooded, complex, 0 to 12 percent slopes	Ba	1652	382220	dtqp	ok033	1961	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Ve	18707	382306	2tq60	ok037	1952	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	Vd	8350	382305	2tq6k	ok037	1952	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	304	2516362	2tq7b	ok037	1952	1:24000
Port clay loam, 0 to 1 percent slopes, occasionally flooded	Pa	72	382292	2tq6j	ok037	1952	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Po	1696	382385	dtx0	ok043	1961	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	PrA	25657	382517	2tq60	ok047	1965	1:24000
Port clay loam, 0 to 1 percent slopes, occasionally flooded	Po	3730	382516	2tq6j	ok047	1965	1:24000
Port silt loam, 1 to 3 percent slopes, occasionally flooded	PrB	2323	382518	dv19	ok047	1965	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	57	13389	382591	2tq60	ok049	1982	1:24000
Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	58	10875	382592	dv3p	ok049	1982	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	56	7598	382590	2tq6k	ok049	1982	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	40	34100	382661	2tq60	ok051	1975	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	15	18000	382633	2tq64	ok051	1975	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	39	10897	382659	2tq6k	ok051	1975	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	41	10734	382731	2tq60	ok053	1983	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	22	8922	382710	2tq64	ok053	1983	1:24000
Port and Pocasset soils, 0 to 1 percent slopes, frequently flooded	42	7134	382732	dv86	ok053	1983	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	Po	35372	383237	2tq6q	ok067	1967	1:24000
Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded, channeled	Pp	6420	383238	2tq6r	ok067	1967	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	Pm	6033	383236	2tq6l	ok067	1967	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	Kc	24353	383332	2tq6l	ok071	1965	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	8631	383321	2tq7b	ok071	1965	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Ka	5500	383331	2tq60	ok071	1965	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	PsA	17737	383410	2tq60	ok073	1960	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	10328	383386	2tq7b	ok073	1960	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	Po	37841	383473	dw13	ok075	1973	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	Br	8385	383501	2tq7b	ok081	1966	1:24000
Port clay loam, 0 to 1 percent slopes, frequently flooded	Pf	1060	383524	dw2r	ok081	1966	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	37	13102	383794	2tq60	ok087	1976	1:24000
Grant-Port, frequently flooded, complex, 0 to 12 percent slopes	17	12615	383772	2tq64	ok087	1976	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	39	6631	383796	2tq7b	ok087	1976	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	Pr	18184	383848	2tq60	ok093	1965	1:24000
Yahola and Port soils, 0 to 1 percent slopes, frequently flooded	Ad	8607	383812	2tq6w	ok093	1965	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	Pf	1511	383847	2tq6k	ok093	1965	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	28954	384030	2tq7b	ok103	1994	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	PorA	15755	384101	2tq60	ok103	1994	1:24000
Port silt loam, 0 to 1 percent slopes, frequently flooded	PoaA	6978	384100	2tq62	ok103	1994	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	PoOA	3284	384099	2tq6q	ok103	1994	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	PotA	3077	384102	2tq6l	ok103	1994	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
Port silt loam, 0 to 1 percent slopes, occasionally flooded	PorA	6030	1423182	2tq60	ok117	2007	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	PotA	178	1883795	2tq6l	ok117	2007	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	PoOA	18	1883796	2tq6q	ok117	2007	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	37	2424	384534	2tq60	ok119	1983	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	APPA	1639	1900485	2tq7b	ok119	1983	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	39	435	384536	2tq6q	ok119	1983	1:24000
Port loam, 0 to 1 percent slopes, occasionally flooded	33	24233	384694	2tq5z	ok125	1975	1:24000
Ashport, Port and Pulaski soils, 0 to 1 percent slopes, frequently flooded	34	7080	384695	2tq7b	ok125	1975	1:24000
Port silt loam, 1 to 3 percent slopes, occasionally flooded	SpB	5388	384778	dxd6	ok129	1961	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	SpA	4909	384777	dxd5	ok129	1961	1:24000
Port fine sandy loam, 0 to 1 percent slopes, occasionally flooded	Pf	19645	384875	2tq6k	ok137	1960	1:24000
Port loam, 0 to 1 percent slopes, occasionally flooded	Pr	19312	384877	2tq5z	ok137	1960	1:24000
Port-Oscar complex, 0 to 1 percent slopes, occasionally flooded	Ps	13655	384878	2tq6q	ok137	1960	1:24000
Port clay loam, 0 to 1 percent slopes, occasionally flooded	Po	1989	384876	2tq6j	ok137	1960	1:24000
Port silty clay loam, 0 to 1 percent slopes, occasionally flooded	Po	4860	384967	dxl9	ok141	1968	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	35	11308	385020	dxn0	ok149	1976	1:24000
Yahola and Port soils, 0 to 1 percent slopes, frequently flooded	YaPA	448	385260	2tq6w	ok151	1995	1:24000
Port silt loam, 0 to 1 percent slopes, occasionally flooded	PorA	291	385223	2tq60	ok151	1995	1:24000
Port and Wheatwood soils, frequently flooded	Pw	27624	362444	d54r	tx009	1986	1:24000
Port-Wheatwood complex, occasionally flooded	Po	16628	362443	d54q	tx009	1986	1:24000
Port soils, frequently flooded	44	30985	363898	d6nn	tx077	1977	1:24000
Port clay loam, occasionally flooded	43	3927	363897	d6nm	tx077	1977	1:24000
Wheatwood and Port soils, frequently flooded	Aw	20111	373334	djh1	tx485	1972	1:20000
Port silt loam	Po	2585	373380	djjj	tx485	1972	1:20000

Map of Series Extent

Approximate geographic distribution of the PORT 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).