Soil Data Explorer - LINCOLN

Official Series Description

Lab Data Summary

Aggregate lab data for the LINCOLN soil series. This aggregation is based on all pedons with a current taxon name of LINCOLN, 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 LINCOLN 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
77E	93P0693	93OK059008	Lincoln	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.6836128,-99.8302765

Water Balance

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

Competing Series

Soil series competing with LINCOLN 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 LINCOLN 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 LINCOLN 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 LINCOLN, 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. CO-2011-05-27-17 | Prowers County - 1966

   Soils on bottom lands and terraces, and the underlying materials of soil association 7 (Soil Survey of Prowers County, Colorado; 1966).

2. CO-2011-05-27-19 | Prowers County - 1966

   Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

3. KS-2012-01-20-36 | Comanche County - June 1989

   Typical pattern of soils and parent material in the Albion-Shellabarger association (Soil Survey of Comanche County, Kansas; 1989).

4. KS-2012-01-23-02 | Finney County - November 1965

   Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

5. KS-2012-01-23-16 | Grant County - December 1969

   Relationships of soils in association 5 (Soil Survey of Grant County, Kansas; 1969).

6. KS-2012-01-23-20 | Gray County - January 1968

   Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

7. KS-2012-01-23-23 | Greeley County - December 1961

   Approximate geologic cross section (north and south) through central Greeley County (Soil Survey of Greeley County, Kansas; 1961).

8. KS-2012-01-23-24 | Greeley County - December 1961

   Cross section of the valley of White Woman Creek in Greeley County (Soil Survey of Greeley County, Kansas; 1961).

9. KS-2012-01-23-25 | Hamilton County - November 1961

   Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

10. KS-2012-01-24-20 | Morton County - December 1963

    Geologic cross section of the western part of the county. (Based on plate 6 of "Geology and Ground-Water Resources of Morton Co., Kans." (6).) (Soil Survey of Morton County, Kansas; 1963.)

11. KS-2012-01-26-30 | Wichita County - November 1965

    Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).

12. OK-2010-09-29-19 | Woods County - 2003

    Typical pattern of soils and underlying material in the Eda-Devol-Lovedale general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

13. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

14. OK-2012-02-16-09 | Cimarron County - June 1960

    Typical landscape in the central and eastern part of Cimarron County: Associations 1, 2, 3, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).

15. OK-2012-02-16-10 | Cimarron County - June 1960

    Typical landscape in the northwestern part of Cimarron County: Associations 3, 4, and 5 (Soil Survey of Cimarron County, Oklahoma; June 1960).

16. OK-2012-02-16-21 | Cotton County - December 1963

    Typical pattern of Pratt, Tivoli, and associated soils (Soil Survey of Cotton County, Oklahoma; December 1963).

17. OK-2012-02-16-27 | Dewey County - December 1963

    Typical pattern of most of the soils in association 5 (Soil Survey of Dewey County, Oklahoma; December 1963).

18. OK-2012-02-16-28 | Ellis County - April 1966

    Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

19. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

20. OK-2012-02-16-46 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed on alluvial plains and on windblown sands. The typical slope range is given for each soil (Soil Survey of Harper County, Oklahoma; June 1960).

21. OK-2012-02-17-06 | Love County - September 1966

    A diagram showing typical relief in the southern part of Love County and the relative position of the soils in associations 1, 3, and 6 (Soil Survey of Love County, Oklahoma; September 1966).

22. 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).

23. 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).

24. 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).

25. OK-2012-02-17-53 | Texas County - July 1961

    Typical pattern of the soils in association 3, Texas County, Okla (Soil Survey of Texas County, Oklahoma; July 1961).

26. 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).

27. OK-2012-02-17-61 | Woodward County - November 1963

    Typical pattern of soils of the Lincoln-Las Animas association (Soil Survey of Woodward County, Oklahoma; November 1963).

28. TX-2010-11-03-50 | King County - 2007

    Typical pattern of the Grandfield-Shrewder-Devol and Delwin-Nobscot general soil map units (Soil Survey of King County, Texas; 2007).

29. TX-2010-11-05-04 | Young County - 2009

    Pattern of soils and underlying material in the Grandfield-Gowen and Lincoln-Westola-Padgett general soil map units (Soil Survey of Young County, Texas; 2009).

30. TX-2012-03-21-36 | Lipscomb County - December 1975

    Pattern of soils and underlying material in association 3 (Soil Survey of Lipscomb County, TX; 1975).

31. TX-2012-03-22-04 | Wheeler County - October 1975

    Relationship of soils in the Devol-Tivoli association to parent material and relief (Soil Survey of Wheeler County, TX; 1975).

Map Units

Map units containing LINCOLN 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
Lincoln sand	Lv	15134	94847	35pl	co099	1963	1:15840
Lincoln loam	Lu	195	94846	35pk	co099	1963	1:15840
Lincoln soils, frequently flooded	6060	23892	1382497	1hdlp	ks007	1973	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	2352	1382495	2wrw9	ks007	1973	1:24000
Lincoln sandy loam, occasionally flooded	6059	32	1382496	1hdln	ks007	1973	1:24000
Lincoln loamy fine sand, occasionally flooded	6056	15313	1381723	1hcsq	ks025	1980	1:24000
Lincoln-Krier complex, occasionally flooded	6062	6075	1381726	1hcst	ks025	1980	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	4079	1381724	2wrw9	ks025	1980	1:24000
Lincoln sandy loam, occasionally flooded	6059	17	1381725	1hcss	ks025	1980	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	17143	1381271	2wrw9	ks033	1987	1:24000
Lincoln-Krier complex, occasionally flooded	6062	4212	1381273	1hcb6	ks033	1987	1:24000
Lincoln sandy loam, occasionally flooded	6059	2299	1381272	1hcb5	ks033	1987	1:24000
Lincoln-Tivoli complex, 0 to 10 percent slopes	6063	4577	1382942	30yql	ks035	1977	1:24000
Pratt-Lincoln loamy fine sands, 0 to 4 percent slopes	5938	1247	1380388	2zt7f	ks047	1967	1:24000
Las Animas-Lincoln complex, occasionally flooded	1187	32	1380375	2zt78	ks047	1967	1:24000
Las Animas-Lincoln loamy sands, occasionally flooded	1188	4216	1152312	17p2c	ks055	1962	1:24000
Lincoln soils, occasionally flooded	6061	1639	1152320	17p2m	ks055	1962	1:24000
Las Animas-Lincoln complex, occasionally flooded	1187	6546	1380437	2zt78	ks057	1962	1:24000
Lincoln soils, frequently flooded	6060	1805	1380443	1hbgf	ks057	1962	1:24000
Lincoln soils, frequently flooded	6060	192	1380663	1hbpj	ks067	1965	1:24000
Lincoln soils, frequently flooded	6060	887	1380575	1hblp	ks069	1965	1:24000
Lincoln fine sandy loam, occasionally flooded	6055	3286	1151833	17nkx	ks071	1959	1:24000
Lincoln soils, occasionally flooded	6061	4795	1152226	17nzl	ks075	1959	1:24000
Lincoln loamy fine sand, occasionally flooded	6056	11106	1382705	1hdtd	ks077	1965	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	386	1382706	2wtxp	ks077	1965	1:24000
Lincoln soils, frequently flooded	6060	123	1382707	1hdtg	ks077	1965	1:24000
Lincoln soils, occasionally flooded	6061	2704	1152271	17p11	ks093	1961	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	10837	1444820	2wtxp	ks095	1977	1:24000
Lincoln sandy loam, occasionally flooded	6059	3839	1380527	1hbk4	ks097	1983	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	496	1380526	2wrw9	ks097	1983	1:24000
Lincoln soils, frequently flooded	6060	2910	1150530	17m6w	ks109	1962	1:24000
Lincoln soils, frequently flooded	6060	2723	1381785	1hcvq	ks119	1973	1:24000
Lincoln loamy fine sand, occasionally flooded	6056	294	1381784	1hcvp	ks119	1973	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	2817	1445178	2wtxp	ks151	1965	1:24000
Lincoln soils, frequently flooded	6060	191	1445179	1khtp	ks151	1965	1:24000
Lincoln soils, frequently flooded	6060	5866	1443999	1kglm	ks173	1976	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	6057	13	1443998	2wtxp	ks173	1976	1:24000
Lincoln soils, occasionally flooded	6061	3309	1382662	1hds0	ks175	1963	1:24000
Lincoln soils, occasionally flooded	6061	3900	1382563	1hdnt	ks187	1959	1:24000
Lincoln soils, frequently flooded	6060	6527	1444631	1kh80	ks191	1974	1:24000
Lincoln-Tivoli complex, 0 to 10 percent slopes	6063	881	1444632	30yql	ks191	1974	1:24000
Lincoln loamy fine sand, occasionally flooded	6056	66	1444630	1kh7z	ks191	1974	1:24000
Lincoln fine sandy loam, occasionally flooded	6055	827	1151943	17npg	ks203	1963	1:24000
Lincoln sand, 0 to 1 percent slopes, frequently flooded	LisA	719	3203435	2zc18	ok007	2021	1:24000
Lincoln sand, 0 to 1 percent slopes, occasionally flooded	LsoA	500	3203436	2zc19	ok007	2021	1:24000
Lincoln clay loam, 0 to 1 percent slopes, rarely flooded	LncA	254	3203439	2zc1b	ok007	2021	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	34	13396	381671	dt4z	ok009	1978	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Ls	13810	382236	dtr6	ok033	1961	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, frequently flooded	LnfA	16509	1481084	1lq5x	ok043	1961	1:24000
Lincoln clay loam, 0 to 1 percent slopes, frequently flooded	Ln	9281	382374	dtwn	ok043	1961	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	Bf	3934	382354	dtw0	ok043	1961	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, occasionally flooded	LnnA	951	1481083	1lq5w	ok043	1961	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Ln	16084	382436	dtyn	ok045	1963	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, occasionally flooded	LnnA	6740	1914087	227rr	ok045	1963	1:24000
Lincoln fine sand, 0 to 1 percent slopes, frequently flooded	Rw	791	382467	dtzn	ok045	1963	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, frequently flooded	LnfA	6	1914084	227rn	ok045	1963	1:24000
Lincoln and Westola soils, 0 to 1 percent slopes, frequently flooded	LnWA	6051	648173	prgt	ok055	2005	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	LnuA	2932	648172	prgs	ok055	2005	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	37	2580	975470	11r1s	ok057	1982	1:24000
Lincoln sand, 0 to 1 percent slopes, occasionally flooded	LsoA	11829	382938	dvgv	ok059	1998	1:24000
Lincoln clay loam, 0 to 1 percent slopes, rarely flooded	LncA	6152	382937	dvgt	ok059	1998	1:24000
Lincoln-Jester complex, 0 to 5 percent slopes, rarely flooded	LiJC	4483	382948	dvh5	ok059	1998	1:24000
Lincoln sand, 0 to 1 percent slopes, frequently flooded	LisA	1036	382939	dvgw	ok059	1998	1:24000
Lincoln and Westola soils, 0 to 1 percent slopes, frequently flooded	LnWA	8049	392388	f59p	ok065	2000	1:24000
Lincoln loamy sand, 0 to 1 percent slopes, occasionally flooded	LnuA	4880	392389	f59q	ok065	2000	1:24000
Lincoln and Gracemore soils, 0 to 1 percent slopes, frequently flooded	Lo	6128	383466	dw0w	ok075	1973	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	Ln	1701	383465	dw0v	ok075	1973	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, frequently flooded	Ln	10348	384742	dxc1	ok129	1961	1:24000
Lincoln fine sandy loam, 0 to 1 percent slopes, occasionally flooded	LnnA	6230	1603721	1qtsy	ok129	1961	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	Br	493	384726	dxbj	ok129	1961	1:24000
Lincoln and Gracemore soils, 0 to 1 percent slopes, frequently flooded	Ln	28173	384961	dxl3	ok141	1968	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	Lo	2233	384962	dxl4	ok141	1968	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	LinA	5156	385209	dxv3	ok151	1995	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	LcnA	2979	385208	dxv2	ok151	1995	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Ln	18411	385277	dxx9	ok153	1961	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, occasionally flooded	Lf	10701	385276	dxx8	ok153	1961	1:24000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Sa	3014	362496	2z179	tx011	1963	1:20000
Lincoln and Westola soils, frequently flooded	Lc	11966	362718	d5fl	tx023	1971	1:24000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	Lf	5078	363281	2z178	tx045	1972	1:20000
Lincoln fine sand, cool, 0 to 1 percent slopes, frequently flooded	LNA	194	377977	2z17d	tx065	2000	1:24000
Lincoln fine sandy loam, frequently flooded	29	866	363881	d6n3	tx077	1977	1:24000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Ls	17251	364105	2z179	tx087	1965	1:20000
Lincoln soils	Lc	5132	364596	d7d5	tx101	1969	1:20000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Sa	1522	364740	2z179	tx107	1964	1:20000
Lincoln fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	3322	365121	2z17b	tx125	1965	1:20000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, occasionally flooded	Lc	997	365120	2z17c	tx125	1965	1:20000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	23271	365176	2z178	tx129	1975	1:24000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Sa	1940	365805	2z179	tx151	1964	1:24000
Lincoln fine sand, cool, 0 to 1 percent slopes, frequently flooded	LNA	716	695950	2z17d	tx153	2004	1:24000
Lincoln soils, 0 to 1 percent slopes, frequently flooded	LnA	1560	3100973	2y7bx	tx155	2021	1:24000
Lincoln-Yahola complex	Lo	15327	378331	dpp7	tx169	1965	1:24000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	5724	378330	2z178	tx169	1965	1:24000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Ln	10544	391921	2z179	tx179	1965	1:20000
Lincoln loamy fine sand, dry, 0 to 2 percent slopes, frequently flooded	Sa	12202	366958	2z179	tx191	1965	1:20000
Lincoln and Yahola soils	Ly	5542	366943	d9tw	tx191	1965	1:20000
Lincoln fine sandy loam, 0 to 2 percent slopes, occasionally flooded	Ln	1509	367142	2z175	tx197	1965	1:20000
Lincoln soils, 0 to 1 percent slopes, frequently flooded	Ln	13819	367442	dbbz	tx205	1973	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Al	3559	367477	2z177	tx207	1960	1:20000
Lincoln loamy fine sand, 0 to 3 percent slopes	Sa	1155	367514	dbf9	tx207	1960	1:20000
Lincoln soils, 0 to 2 percent slopes, frequently flooded	Ln	23526	367567	dbh0	tx211	1967	1:20000
Lincoln soils, 0 to 2 percent slopes, frequently flooded	Ln	34402	367925	dbvk	tx233	1972	1:24000
Lincoln fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	8494	368483	2z17b	tx263	1968	1:31680
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	LnA	1066	368593	2z178	tx269	1999	1:31680
Lincoln-Westola complex, occasionally flooded	20	9749	368721	dcp7	tx275	1975	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	19	4350	368719	2z177	tx275	1975	1:24000
Lincoln soils, 0 to 2 percent slopes, frequently flooded	Ln	7399	369458	ddg0	tx295	1971	1:24000
Lincoln loamy fine sand, 0 to 2 percent slopes, occasionally flooded	Ln	1750	370821	dfvz	tx341	1968	1:24000
Yomont-lincoln soils	Ys	7094	370906	dfyq	tx345	1972	1:24000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, occasionally flooded	Ln	6935	370869	2z17c	tx345	1972	1:24000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	Lo	3983	370870	2z178	tx345	1972	1:24000
Lincoln soils, 0 to 2 percent slopes, frequently flooded	Ln	365	371084	dg4g	tx357	1966	1:20000
Lincoln soils, 0 to 1 percent slopes, frequently flooded	LNA	19425	3124145	dg5l	tx359	1978	1:24000
Lincoln soils, 0 to 1 percent slopes, frequently flooded	LNA	8234	3124220	dgdm	tx375	1974	1:24000
Yomont and Lincoln soils, 0 to 2 percent slopes, frequently flooded	YLA	1189	371413	dgh2	tx381	1999	1:24000
Lincoln fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	36215	371518	2z17b	tx393	1979	1:24000
Lincoln loamy fine sand, dry, 0 to 1 percent slopes, frequently flooded	Ln	9183	372282	2z178	tx433	1970	1:24000
Lincoln sandy loam, occasionally flooded	Ln	4128	372693	dhtc	tx447	1991	1:24000
Lincoln loamy fine sand, 0 to 2 percent slopes, occasionally flooded	Ln	11640	373308	2z176	tx483	1970	1:24000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Lw	4238	373367	2z177	tx485	1972	1:20000
Lincoln fine sandy loam, 0 to 2 percent slopes, occasionally flooded	Ln	1366	373366	2z175	tx485	1972	1:20000
Lincoln loamy fine sand, 0 to 1 percent slopes, frequently flooded	Sa	9774	373442	2z177	tx487	1960	1:20000
Lincoln fine sandy loam, 0 to 2 percent slopes, occasionally flooded	Ln	8749	373422	2z175	tx487	1960	1:20000
Lincoln sandy loam, 0 to 1 percent slopes, occasionally flooded	LnA	8912	373763	djxw	tx503	2003	1:24000

Map of Series Extent

Approximate geographic distribution of the LINCOLN 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).