Soil Data Explorer - FLUVAQUENTS

Official Series Description

Lab Data Summary

Aggregate lab data for the FLUVAQUENTS soil series. This aggregation is based on all pedons with a current taxon name of FLUVAQUENTS, 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 FLUVAQUENTS were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
147	88PA055065	1988PA055065	Fluvaquents	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	40.2277778,-77.6844444
n/a	X49-2220-1	S1988IA097926	Fluvaquents	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

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

There are insufficient data to create the water balance bar figure.

There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the FLUVAQUENTS 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).

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the FLUVAQUENTS 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).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the FLUVAQUENTS 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 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.

Competing Series

Soil series competing with FLUVAQUENTS 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).

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the FLUVAQUENTS 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 FLUVAQUENTS 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 FLUVAQUENTS, 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).

This figure is not available.

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. CA-2012-05-08-06 | Butte Area, Parts of Butte and Plumas Counties - 2006

   Block diagram 5.—This diagram shows the relationships between the Cascade volcanic flows and the metamorphic and granitic Sierra Nevada rocks. The flatter volcanic flows on the left buried the folded metamorphic rocks in the middle. The uniform intrusive igneous rocks weather to soils that are less resistant to geologic erosion and produce subtle, more evenly developed relief (Soil Survey of Butte Area, California, Parts of Butte and Plumas Counties; 2006).

2. DC-2011-05-31-05 | District of Columbia - 1976

   Diagram of Coastal Plain showing the pattern of soils and parent material (Soil Survey of District of Columbia; 1976).

3. IA-2010-09-09-23 | Webster County - 2008

   Typical pattern of soils and parent material in the Lester-Coland-Wadena association (Soil Survey of Webster County, Iowa; 2008).

4. MD-2012-02-03-12 | Dorchester County - 1998

   Typical profiles and landscape pattern of soils on flood plains adjacent to upland soils (Soil Survey of Dorchester County, Maryland; 1998).

5. NE-2010-09-09-04 | Garden County - 1999

   Typical pattern of the soils and underlying material in the Gothenburg, Lewellen-Jankosh, and Bayard-Scoville-Rushcreek associations (Soil Survey of Garden County, Nebraska; 1999).

6. NE-2012-02-08-08 | Blaine County - September 1993

   Typical pattern of soils and parent material in the Almeria-Ipage-Fluvaquents association (Soil Survey of Blaine County, Nebraska; September 1993).

7. NY-2010-09-28-04 | Clinton County - 2006

   Typical pattern of deltaic sands and associated soils in the Champlain-Adams-Croghan general soil map unit (Soil Survey of Clinton County, New York; 2006).

8. NY-2010-09-28-24 | Otsego County - 2006

   The relationship between the soils and underlying material in the Wayland-Canadaigua-Raynham general soil map unit and the Otego-Chenango-Scio general soil map unit (Soil Survey of Otsego County, New York; 2006).

9. NY-2010-09-28-31 | Akwesasne Territory: St. Regis Mohawk Reservation - 2005

   One of three major rivers flows through Akwesasne. The Raquetter River sliced through glacial till ridges (consisting of Grenville, Hogansburg, and Malone soils) and deposited fine-grained sands at varying depths over silt, clay, or loamy till. The silt and clay sediments of Adjidaumo and Muskellunge soils are remnants of proglacial lake and marine environments (Soil Survey of Akwesasne Territory; St. Regis Mohawk Reservation; 2005).

10. NY-2012-02-15-49 | Warren County - January 1989

    Typical relationship of upland and valley soils to landscape position and underlying deposits near the Schroon River (Soil Survey of Warren County, New York; January 1989).

11. PA-2012-03-13-34 | Greene and Washington Counties - September 1983

    Typical pattern of soils and underlying material in the Dormont-Culleoka association (Soil Survey of Greene and Washington Counties, PA; 1983).

12. PA-2012-03-13-76 | Montour County - April 1985

    Typical pattern of soils and underlying material in the Holly-Monongahela-Basher association (Soil Survey of Montour County, PA; 1985).

13. PA-2012-03-14-12 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Rayne-Gilpin-Wharton-Cavode soils (Soil Survey of Somerset County, PA; 1983).

Map Units

Map units containing FLUVAQUENTS 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
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FaA	1245	2232045	2tjl0	al007	2007	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FaA	1040	328602	2tjl0	al023	1998	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FlA	2540	600097	2tjl0	al025	2004	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FlA	3860	328876	2tjl0	al041	2005	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	Fl	422	1715795	2tjl0	al063	2013	1:
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FuA	1508	329776	2tjl0	al065	2003	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FvA	1562	2494539	2tjl0	al075	2010	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FqA	277	2514616	2tjl0	al085	2011	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FuA	2485	330459	2tjl0	al087	1997	1:24000
Udifluvents-Fluvaquents complex, 0 to 3 percent slopes, frequently flooded	UfA	1857	2995053	2x5qt	al097	2018	1:24000
Fluvaquents silt loam, 0 to 1 percent slopes, frequently flooded	FlA	1281	2995060	2x5s4	al097	2018	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FuA	1710	331233	2tjl0	al105	1996	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FvA	18970	331294	2tjl0	al107	1997	1:24000
Fluvaquents silt loam, frequently ponded, 0 to 1 percent slopes, frequently flooded	FpA	1170	331347	2tjl0	al113	1997	1:24000
Fluvaquents, 0 to 1 percent slopes, ponded	FaA	140	1476409	1lkb3	al123	2005	1:24000
Fluvaquents silt loam, 0 to 1 percent slopes, frequently flooded	FaA	609	2642079	2x5s4	al129	2013	1:24000
Fluvaquents flooded	9	3504	565092	lz0s	ar003	1977	1:20000
Pits-Fluvaquents complex, occasionally flooded	56	545	3179391	lynn	ar019	1983	1:20000
Fluvaquents, 0 to 1 percent slopes, frequently flooded	Fl	846	1011978	30x8c	ar041	1968	1:20000
Fluvaquents, 0 to 1 percent slopes, frequently flooded	Fl	3502	1690251	30x8c	ar043	1972	1:24000
Pits-Fluvaquents complex, occasionally flooded	56	1210	3179281	lynn	ar059	1983	1:20000
Fluvaquents, frequently flooded	Ff	5040	564086	lxzb	ar077	1974	1:20000
Fluvaquents, frequently flooded	Ff	6740	564231	ly40	ar107	1971	1:20000
Oil-waste land-Fluvaquents complex, 0 to 1 percent slopes, frequently flooded	OfA	5213	579203	mfpz	ar139	1992	1:24000
Fluvaquents, frequently flooded	22	2773	564895	lytf	ar670	1981	1:20000
Riverwash-Fluvaquents association, 0 to 3 percent slopes	102	240	1507965	1mm51	az627	2005	1:24000
Brookline-Fluvaquents-Riverwash complex, 0 to 3 percent slopes	17	3528	55019	1v7t	az671	2000	1:24000
Haplustolls-Fluvaquents association, thermic, 0 to 4 percent slopes	87	2852	55002	1v78	az671	2000	1:24000
Quiburi-Fluvaquents-Riverwash complex, 0 to 5 percent slopes	123	815	55029	1v84	az671	2000	1:24000
Haplustolls-Fluvaquents association, mesic, 0 to 4 percent slopes	86	508	55001	1v77	az671	2000	1:24000
Fluvaquents-Psamments complex, warm, 2 to 6 percent slopes	41	157	615928	nnxn	az701	2001	1:24000
Fluvaquents-Psamments complex, 2 to 6 percent slopes	40	12	615927	nnxm	az701	2001	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded, MLRA 16	Fc	1000	455794	2yc98	ca013	1973	1:24000
Fluvaquents, organic substratum, 0 to 2 percent slopes, frequently flooded	150	1280	461894	2x4lr	ca067	1989	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded, MLRA 16	159	4985	462051	2yc98	ca077	1990	1:24000
Fluvaquents	139	7605	486414	jb4s	ca603	1974	1:24000
Fluvaquents-Typic Udifluvents complex, 0 to 2 percent slopes	130	169	466245	hn55	ca605	2013	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded, MLRA 16	Fccc		801711	2yc98	ca609	1963	1:20000
Fluvaquents, 0 to 1 percent slopes	155	340	460464	hg4p	ca618	1991	1:24000
Fluvaquents, channeled	186	2530	462838	hjm8	ca647	1984	1:24000
Cerini-Anela-Fluvaquents, saline-Sodic, association, 0 to 2 percent slopes	590	1189	467072	hp0v	ca653	2000	1:24000
Fluvaquents	Fa	1937	464023	hkvh	ca680	1974	1:24000
Fluvaquents, saline	104	12262	455493	h8zb	ca683	1976	1:24000
Fluvaquents-Riverwash complex, 2 to 8 percent slopes	399	544	488685	jdj1	ca685	2006	1:24000
Fluvaquents, 0 to 1 percent slopes	127	670	461012	hgqc	ca687	1985	1:24000
Fluvaquents-Riverwash complex, 0 to 5 percent slopes	202	290	469931	hs02	ca692	2001	1:24000
Fluvaquents-Riverwash complex, 2 to 8 percent slopes	399sv	8	1898160	21q5z	ca703	1983	1:24000
Oxyaquic Xerofluvents-Riverwash-Fluvaquents association, 0 to 2 percent slopes, mesic	101	65	466367	hn93	ca790	2006	1:24000
Fluvaquents, 0 to 1 percent slopes	12	1516	94299	353x	co017	1985	1:24000
Fluvaquents clay loam, 0 to 1 percent slopes, occasionally flooded	12	5282	94420	2zqss	co061	1977	1:24000
Fluvaquents	29	11310	94509	35bp	co075	1974	1:24000
Fluvaquents, 0 to 2 percent slopes	21	743	94981	35tx	co121	1982	1:24000
Haplaquolls-Fluvaquents complex, frequently flooded	28	1562	95119	35zc	co617	1980	1:24000
Fluvaquents, nearly level*	21	650	496411	jnk8	co623	1977	1:24000
Fluvaquents, sandy, 0 to 2 percent slopes	50	1138	497495	jpp7	co641	1980	1:24000
Fluvaquents, nearly level	33	1184	497680	jpw6	co644	1980	1:24000
Fluvaquents, 0 to 10 percent slopes	AG42	196	1415082	1jhht	co654		1:24000
Fluvaquents, 0 to 10 percent slopes	42	6244	497983	jq5z	co655	1984	1:24000
Fluvaquents, 0 to 3 percent slopes	A2W-B	2311	499261	jrj6	co668	2018	1:24000
Fluvaquents, sandy, frequently flooded	28	4267	58287	1yn7	co669	1982	1:24000
Fluvents-Fluvaquents complex, 0 to 3 percent slopes	35	1618	59441	1zvg	co670	2005	1:24000
Fluvents-Fluvaquents complex, 0 to 3 percent slopes	38	4759	57637	1xz8	co671	1997	1:24000
Fluvaquents-Haplustolls complex, 0 to 5 percent slopes	37	100	57636	1xz7	co671	1997	1:24000
Fluvaquents-Haplustolls complex, 0 to 5 percent slopes	17	1089	737684	srm8	co672	2003	1:24000
Fluvaquents, 0 to 6 percent slopes, frequently flooded	43	2707	502059	jvfg	co675	1986	1:24000
Fluvaquents, flooded	35	5734	496612	jnrr	co679	1976	1:24000
Fluvaquents, 0 to 3 percent slopes	36	1906	496697	jnvh	co682	1986	1:24000
Fluvaquents, frequently flooded	44	412	496886	jp1l	co684	1984	1:24000
Fluvaquents, frequently flooded	32	1104	496982	jp4p	co685	1979	1:24000
Green River-Fluvaquents complex, 0 to 2 percent slopes	116	6	927329	103yv	co685	1979	1:24000
Fluvaquents and Haplaquolls soils, frequently flooded	70	5212	497249	jpf9	co686	1992	1:31680
Green River-Fluvaquents complex, 0 to 2 percent slopes	231	74	629747	p49f	co686	1992	1:31680
Green River-Fluvaquents complex, 0 to 2 percent slopes	23	1153	506239	jzs9	co692	1998	1:24000
Tsetaa family-Bankard family-Fluvaquents complex, 0 to 45 percent slopes, very stony	65	282	506297	jzv5	co692	1998	1:24000
Fluvaquents, 0 to 1 percent slopes, frequently flooded	22	25	506238	jzs8	co692	1998	1:24000
Fluvaquents-Udifluvents complex, frequently flooded	109	5256	3395644	9ljw	ct601	2003	1:12000
Fluvaquents-Udifluvents complex, frequently flooded	109	3172	3396017	9ljw	ct602	2003	1:12000
Fluvaquents-Udifluvents-Urban land complex	FH	106	128600	49td	dc001	1975	1:12000
Fluvaquents, ponded	FD	68	128598	49tb	dc001	1975	1:12000
Fluvaquents, bouldery	FB	59	128597	49t9	dc001	1975	1:12000
Fluvaquents-Udifluvents complex, frequently flooded	FF	56	128599	49tc	dc001	1975	1:12000
Fluvaquents-Ousley association, occasionally flooded	25	1724	631637	p68d	fl007	1988	1:15840
Dorovan muck and Fluvaquents, frequently flooded	49	48120	1425355	1jv66	fl033	1998	1:24000
Bigbee-Garcon-Fluvaquents complex, flooded	50	10250	1425356	1jv67	fl033	1998	1:24000
Mantachie-Fluvaquents-Bigbee complex, frequently flooded	76	8870	1425381	1jv71	fl033	1998	1:24000
Elloree-Osier-Fluvaquents complex, frequently flooded	16	6020	321799	bsvm	fl041	1989	1:20000
Fluvaquents, frequently flooded	30	1310	321812	bsw1	fl041	1989	1:20000
Fluvaquents, frequently flooded	29	5300	886586	yrkk	fl067	1993	1:24000
Fluvaquents, frequently flooded	14	1638	1421171	1jpv7	fl111	1990	1:24000
Ousley-Blanton-Fluvaquents complex, 0 to 5 percent slopes, occasionally flooded	72	3179	1023386	13bxg	fl121	2003	1:24000
Fluvaquents-Meggett-Bigbee complex, frequently flooded	41	1241	1023355	13bwg	fl121	2003	1:24000
Fluvaquents-Ousley association, occasionally flooded	25	3140	1414590	1jgzy	fl125	1989	1:15840
Fluvaquents	24	2700	1544125	1ntsh	fl127	1977	1:20000
Fluvaquents, ponded	Fp	1525	124882	45yg	ga221	1984	1:20000
Fluvaquents, sandy and loamy	315	7535	402874	fj6y	ia011	1977	1:15840
Fluvaquents, nearly level	2315	1891	403522	fjwv	ia027	1979	1:15840
Fluvaquents, nearly level, occasionally flooded	1318	137	3088472	2y697	ia027	1979	1:15840
Fluvaquents-Omadi complex, 0 to 2 percent slopes, occasionally flooded	1610	3491	403905	2y6bb	ia035	1987	1:15840
Fluvaquents, frequently flooded, 0 to 3 percent slopes	1316	6315	405199	flmy	ia057	1980	1:15840
Fluvaquents-Coland complex, 0 to 3 percent slopes	2315	5423	406200	fmp7	ia073	1983	1:15840
Udifluvents-Fluvaquents complex, 0 to 2 percent slopes, flaggy, frequently flooded	5050	833	409191	2xbm3	ia121	1968	1:15840
Fluvaquents, frequently flooded	5044	678	447430	h0l7	ia133	1994	1:12000
Fluvaquents, ponded	5051	120	447434	h0lc	ia133	1994	1:12000
Fluvaquents, 0 to 2 percent slopes	5044	3644	411244	fsxy	ia167	1987	1:15840
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	715	3874	1453489	1ksgr	ia187	2006	1:12000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	5044	3288	401927	fh7d	ia193	2003	1:12000
Endoaquolls and Fluvaquents, 0 to 3 percent slopes	1200	17	2662873	nv3z	id606	1976	1:24000
Fluvaquents-Histic Endoaquolls complex, 0 to 3 percent slopes	66	1580	82118	2rfz	id681	1993	1:24000
Fluvaquents, channeled	60	3245	2519585	2r12	id685	2012	1:24000
Fluvaquents, 0 to 1 percent slopes	20	3477	83735	2t44	id762	1988	1:24000
Fluvaquents, nearly level	29	4503	83871	2t8j	id765	1975	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded, long duration	3646L	8314	1017898	1356f	il071	2005	1:12000
Fluvaquents, clayey, 0 to 2 percent slopes, occasionally flooded	8831A	1256	202263	6sgm	il119	2001	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded, long duration	3646L	3083	200750	6qwt	il131	2000	1:12000
Fluvaquents-Orthents complex, frequently flooded, long duration	3847L	2957	184081	65k3	il133	1998	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	3646A	1583	184080	65k2	il133	1998	1:12000
Fluvaquents-Orthents complex, frequently flooded, long duration	3847L	2735	200555	6qpj	il157	2001	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	3646A	2124	200556	6qpk	il157	2001	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded, long duration	3646L	5039	271418	93ff	il161	2002	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, occasionally flooded	8646A	1620	183161	64lf	il163	1997	1:12000
Fluvaquents-Orthents complex, frequently flooded, long duration	3847L	1070	183002	64f9	il163	1997	1:12000
Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded, long duration	3646L	1486	793680	vmwl	il195	2003	1:12000
Fluvaquents, loamy	Fh	4150	272661	94qj	in091	1979	1:15840
Fluvaquents	Fh	4063	160647	5d55	in127	1978	1:15840
Fluvaquents, ponded	9980	250	1475399	1lj8j	ks005	1998	1:24000
Fluvaquents, clayey, frequently flooded	9978	850	1454564	1ktlf	ks041	1977	1:24000
Fluvaquents, ponded	9980	219	747156	t2gt	ks043	1977	1:24000
Fluvaquents, occasionally flooded	9979	676	1150125	17lst	ks051	1970	1:24000
Fluvaquents, ponded	9980	23	1862424	20j06	ks103	1973	1:24000
Fluvaquents, frequently flooded, 0 to 3 percent slopes	616A	714	791064	vk56	ma606	1981	1:15840
Endoaquods-Fluvaquents complex	272	1522	190301	6d0r	mi001	1993	1:20000
Fluvaquents, frequently flooded	104	825	2507992	688m	mi017	1978	1:20000
Histosols and Fluvaquents, frequently flooded	85	1491	188731	6bd3	mi025	1993	1:15840
Fluvaquents, loamy	23	11630	186775	68c0	mi063	1978	1:20000
Urban land-Fluvaquents complex	Uu	1065	186764	68bn	mi065	1977	1:15840
Borosaprists, euic-Fluvaquents-Aquic Udipsamments complex, nearly level	254A	4845	191797	6fl0	mi069	1995	1:15840
Endoaquods-Fluvaquents complex	272	2037	191810	6flf	mi069	1995	1:15840
Aquepts-Histosols-Fluvaquents complex, nearly level to very steep	356E	1897	191827	6flz	mi069	1995	1:15840
Ontonagon-Fluvaquents, frequently flooded complex, 0 to 35 percent slopes	169E	302	416343	fz7f	mi097	1994	1:20000
Udorthents-Fluvaquents complex, nearly level to very steep	98F	2178	192623	6gfn	mi105	1992	1:15840
Fluvaquents and Histosols, frequently flooded	64	3358	192441	6g7s	mi113	1983	1:15840
Endoaquods-Fluvaquents, occasionally flooded, complex	272	1535	241476	838k	mi135	2003	1:12000
Haplosaprists, euic-Fluvaquents-Aquic Udipsamments complex, nearly level, occasionally flooded	254A	228	654051	pylf	mi135	2003	1:12000
Histosols-Fluvaquents complex, frequently flooded	474	2916	190975	6dqh	mi143	1999	1:12000
Fluvaquents, frequently flooded	78	7459	186701	688m	mi145	1991	1:15840
Fluvaquents, loamy	Fn	23	2508268	68c0	mi151	1955	1:15840
Fluvaquents and Histosols	37	5018	190773	6dhz	mi600	1983	1:15840
Borosaprists and Fluvaquents soils, frequently flooded	1002	16066	432803	gjcd	mn001	1996	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	11717	3182434	2z19n	mn001	1996	1:20000
Fluvaquents, frequently flooded-Egglake-Sax complex, 0 to 2 percent slopes	2025A	1938	2603659	2qkjw	mn007	1991	1:24000
Fluvaquents, frequently flooded-Hapludalfs complex, 0 to 35 percent slopes	1057	1537	2527656	2ml29	mn007	1991	1:24000
Bowstring and Fluvaquents soils, des moines, 0 to 2 percent slopes, frequently flooded	B109A	1424	2474940	2p2cs	mn007	1991	1:24000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	7332	3182450	2z19n	mn009	2007	1:12000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	1020A	500	1899596	21rp9	mn009	2007	1:12000
Fluvaquents	1005	8849	396332	f9dx	mn017	1973	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	513	3182438	2z19n	mn017	1973	1:20000
Fluvaquents, frequently flooded	1002	8929	397688	fbtn	mn021	1993	1:20000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	5742	2798064	prn0	mn027	1980	1:20000
Fluvaquents-Haploborolls complex	1006	878	356934	czf0	mn027	1980	1:20000
Fluvaquents, loamy	1005	230	356933	czdz	mn027	1980	1:20000
Hapludolls-Fluvaquents, occasionally flooded complex, 0 to 30 percent slopes	I773E	46	2798116	2qjyr	mn027	1980	1:20000
Bowstring and Fluaquents soils, des moines, 0 to 2 percent slopes, frequently flooded	B109A	2083	2474808	2p27j	mn029	1993	1:20000
Fluvaquents, frequently flooded-Hapludalfs complex, 0 to 35 percent slopes	1057	593	2527657	2ml29	mn029	1993	1:20000
Bowstring-Fluvaquents complex, frequently flooded	1325	17	430380	gfv7	mn029	1993	1:20000
Bowstring and Fluvaquents soils, 0 to 2 percent slopes, frequently flooded	K2-10A	35053	2774503	2t222	mn031	2013	1:24000
Fluvaquents, clayey, 0 to 1 percent slopes, frequently flooded	K2-14A	1912	2774616	2t226	mn031	2013	1:24000
Entisols, frequently flooded, rubbly and Histosols soils, 0 to 1 percent slope, ponded	K2-12	1479	2774695	2t224	mn031	2013	1:24000
Sanborg-Fluvaquents, frequently flooded complex, 0 to 18 percent slopes	E2-21D	559	2774685	2t572	mn031	2013	1:24000
Mesaba, stony-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 50 percent slopes	E1-13F	541	2774596	2rn1f	mn031	2013	1:24000
Fluvaquents-Udifluvents complex, 0 to 3 percent slopes, frequently flooded, rubbly	K2-11A	505	2774658	2t223	mn031	2013	1:24000
Augustanna-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E1-18B	255	2774692	2rn1g	mn031	2013	1:24000
Badriver-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E2-20B	212	2774652	2t571	mn031	2013	1:24000
Odanah-Fluvaquents, frequently flooded complex, 0 to 45 percent slopes	E2-23E	209	2774624	2t574	mn031	2013	1:24000
Badriver-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E1-26B	146	2774726	2rn1j	mn031	2013	1:24000
Normanna-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 8 percent slopes	E1-9B	145	2774636	2rn1b	mn031	2013	1:24000
Quetico, stony-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 50 percent slopes	E1-12F	138	2774537	2rn11	mn031	2013	1:24000
Augustanna-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E2-10B	131	2774615	2t56w	mn031	2013	1:24000
Sanborg-Fluvaquebts, frequently flooded-Rock outcrop complex, 0 to 18 percent slopes	E1-27D	57	2774505	2rn1k	mn031	2013	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded complex 0 to 50 percent slopes	E1-10F	38	2774607	2rn0x	mn031	2013	1:24000
Bowstring muck and Fluvaquents, loamy soils, 0 to 1 percent slopes, frequently flooded	3-11A	8734	2840448	2v44r	mn035	2009	1:24000
Hapludalfs-Fluvaquents, frequently flooded complex, 0 to 35 percent slopes	3-11D	371	2840450	2v445	mn035	2009	1:24000
Fluvaquents, loamy	1034	753	397791	fbxz	mn047	1977	1:15840
Fluvaquents, 0 to 2 percent slopes, frequently flooded	I109A	220	2798198	21wnl	mn051	1974	1:20000
Lamoure-Fluvaquents, channeled complex, 0 to 6 percent slopes, frequently flooded	I146B	4	2798203	2ptx2	mn051	1974	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	30	3182442	2z19n	mn059	1956	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	11479	3182458	2z19n	mn065	2006	1:12000
Bowstring muck and Fluvaquents, loamy, 0 to 1 percent slopes, frequently flooded	1020A	797	1673437	1t5bv	mn065	2006	1:12000
Fluvaquents and Udifluvents, loamy, 0 to 2 percent slopes, frequently flooded	1025A	318	1673439	1t5bx	mn065	2006	1:12000
Fluvaquents, ponded, 0 to 1 percent slopes, frequently flooded	1017A	69	1673436	1t5bt	mn065	2006	1:12000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	3437	2798405	prn0	mn069	2007	1:12000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	I109A	3436	2798875	21wnl	mn069	2007	1:12000
Hapludolls-Fluvaquents, occasionally flooded complex, 0 to 6 percent slopes	I773A	690	2798888	2qjys	mn069	2007	1:12000
Bowstring and Fluvaquents soils, 0 to 2 percent slopes, frequently flooded	K2-10A	57618	2774465	2zw3m	mn075	2013	1:24000
Amnicon-Fluvaquents, frequently flooded, complex, 0 to 18 percent slopes	E2-31D	4344	2742204	2t577	mn075	2013	1:24000
Miskoaki-Fluvaquents, frequently flooded, complex, 0 to 45 percent slopes	E2-33E	3908	2742206	2t579	mn075	2013	1:24000
Entisols, frequently flooded, rubbly and Histosols soils, 0 to 1 percent slope, ponded	K2-12	2380	2774467	2t224	mn075	2013	1:24000
Fluvaquents-Udifluvents complex, 0 to 3 percent slopes, frequently flooded, rubbly	K2-11A	2348	2774466	2t223	mn075	2013	1:24000
Cuttre-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E2-30B	1834	2742203	2t576	mn075	2013	1:24000
Augustanna-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E2-10B	1064	2742193	2t56w	mn075	2013	1:24000
Forbay-Fluvaquents, frequently flooded complex, 0 to 18 percent slopes	E2-11D	919	2742194	2t56x	mn075	2013	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded complex 0 to 50 percent slopes	E1-10F	811	2742176	2rn0x	mn075	2013	1:24000
Forbay-Fluvaquents, frequently flooded complex, 0 to 45 percent slopes	E2-13E	611	2742196	2t56z	mn075	2013	1:24000
Miskoaki-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 45 percent slopes	E1-39E	461	2742177	2rn0q	mn075	2013	1:24000
Quetico, stony-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 50 percent slopes	E1-12F	392	2742180	2rn11	mn075	2013	1:24000
Fluvaquents, clayey, 0 to 1 percent slopes, frequently flooded	K2-14A	254	2774469	2t226	mn075	2013	1:24000
Odanah-Fluvaquents, frequently flooded complex, 0 to 45 percent slopes	E2-23E	185	2742201	2t574	mn075	2013	1:24000
Badriver-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E2-20B	157	2742198	2t571	mn075	2013	1:24000
Mesaba, stony-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 50 percent slopes	E1-13F	148	2742183	2rn1f	mn075	2013	1:24000
Normanna-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 8 percent slopes	E1-9B	113	2742181	2rn1b	mn075	2013	1:24000
Odanah-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 45 percent slopes	E1-29E	78	2742189	2rn1m	mn075	2013	1:24000
Amnicon-Fluvaquents, frequently flooded-Rock outcrop complex, 0 to 18 percent slopes	E1-37D	52	2742191	2t56t	mn075	2013	1:24000
Augustanna-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 8 percent slopes	E1-18B	48	2742184	2rn1g	mn075	2013	1:24000
Sanborg-Fluvaquents, frequently flooded complex, 0 to 18 percent slopes	E2-21D	33	2742199	2t572	mn075	2013	1:24000
Sanborg-Fluvaquebts, frequently flooded-Rock outcrop complex, 0 to 18 percent slopes	E1-27D	30	2742187	2rn1k	mn075	2013	1:24000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	11916	2798903	prn0	mn089	1994	1:20000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	I109A	1	2798998	21wnl	mn089	1994	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	14217	3182462	2z19n	mn095	2006	1:12000
Bowstring muck and Fluvaquents, loamy, 0 to 1 percent slopes, frequently flooded	1020A	540	1676338	1t8cf	mn095	2006	1:12000
Fluvaquents and Udifluvents, loamy, 0 to 2 percent slopes, frequently flooded	1025A	496	1676340	1t8ch	mn095	2006	1:12000
Fluvaquents, ponded, 0 to 1 percent slopes, frequently flooded	1017A	11	1676337	1t8cd	mn095	2006	1:12000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	5123	3182446	2z19n	mn097	1987	1:20000
Hapludolls-Fluvaquents, occasionally flooded complex, 0 to 30 percent slopes	I773E	6160	2799098	2qjyr	mn107	1970	1:20000
Hapludolls-Fluvaquents, occasionally flooded complex, 0 to 6 percent slopes	I773A	5020	2799099	2qjys	mn107	1970	1:20000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	I109A	3590	2799078	21wnl	mn107	1970	1:20000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	430	2799035	prn0	mn107	1970	1:20000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	3288	2799176	prn0	mn113	2003	1:12000
Bowstring-Fluvaquents complex, 0 to 2 percent slopes, frequently flooded	I7A	436	2799169	prmp	mn113	2003	1:12000
Bowstring and Fluvaquents soils, des moines, 0 to 2 percent slopes, frequently flooded	B109A	265	680938	qvkr	mn113	2003	1:12000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	10478	3182454	2z19n	mn115	2009	1:24000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	3619	2799639	prn0	mn119	1996	1:20000
Bowstring-Fluvaquents complex, frequently flooded	1325	3167	352194	cth3	mn119	1996	1:20000
Bowstring-Fluvaquents complex, 0 to 2 percent slopes, frequently flooded	I7A	2388	2799630	prmp	mn119	1996	1:20000
Fluvaquents-Haploborolls complex, 0 to 30 percent slopes	1006	11	352142	ctff	mn119	1996	1:20000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	7709	2799763	prn0	mn125	2001	1:12000
Bowstring-Fluvaquents complex, 0 to 2 percent slopes, frequently flooded	I7A	3018	2799753	prmp	mn125	2001	1:12000
Bowstring and Fluvaquents soils, mlra 88, 0 to 2 percent slopes, frequently flooded	B109A	183	623929	ny7r	mn125	2001	1:12000
Fluvaquents,frequently flooded-Hapludolls complex, 0 to 30 percent slopes	I16F	7398	2799824	prn0	mn135	1999	1:24000
Fluvaquents, frequently flooded-Hapludalfs complex, 0 to 60 percent slopes	1067	4231	394768	f7sg	mn135	1999	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	I109A	4131	2799877	21wnl	mn135	1999	1:24000
Fluvaquents, 0 to 2 percent slopes, frequently flooded	1002	477	394764	f7sb	mn135	1999	1:24000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	C211	16	3182466	2z19n	mn141	1994	1:15840
Lamoure-Fluvaquents, channeled complex, 0 to 6 percent slopes, frequently flooded	I146B	12	2799964	2ptx2	mn155	1986	1:20000
Lamoure-Fluvaquents, channeled complex, 0 to 6 percent slopes, frequently flooded	I146B	3517	2800436	2ptx2	mn167	1985	1:20000
Fluvaquents, channeled	1002	864	428980	gdd2	mn169	1987	1:20000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	1020A	55895	2407778	2lth8	mn613	2016	1:24000
Bowstring and Fluvaquents soils, 0 to 2 percent slopes, frequently flooded	2srrt	1661	2943735	2srrt	mn613	2016	1:24000
Bowstring and Fluvaquents, loamy, 0 to 2 percent slopes, frequently flooded	1020A	29964	449516	h2rj	mn615	2007	1:24000
Miskoaki-Fluvaquents, frequently flooded, complex, 0 to 45 percent slopes	E9E	2059	626065	p0gn	mn615	2007	1:24000
Amnicon-Fluvaquents, frequently flooded, complex, 0 to 18 percent slopes	E8D	1414	626066	p0gp	mn615	2007	1:24000
Ahmeek-Rock outcrop-Fluvaquents, frequently flooded, complex, 0 to 50 percent slopes	F148F	1404	764970	tp0g	mn615	2007	1:24000

Map of Series Extent

Approximate geographic distribution of the FLUVAQUENTS 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).