Soil Data Explorer - FLOM

Official Series Description

Lab Data Summary

Aggregate lab data for the FLOM soil series. This aggregation is based on all pedons with a current taxon name of FLOM, 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 FLOM 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
102A	UMN1089	S1952MN1071089	Flom	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.1986427,-96.0925446
102A	UMN1131	S1970MN0831131	Flom	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.5313644,-96.0737991
102A	UMN1110	S1970MN1171110	Flom	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1816368,-96.1855927
102A	UMN2260	S1976MN0272260	Flom	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	46.9310989,-96.237236
55A	94P0679	94ND093002	Flom	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.9055556,-98.9280556
88	78P0603	78MN029001	Flom	7	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.9491653,-95.3977814
91A	UMN1586	S1972MN1451586	Flom	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.7474022,-95.0466995

Water Balance

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

Competing Series

Soil series competing with FLOM 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 FLOM 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 FLOM 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 3D hills figure.

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

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

Soil series sharing subgroup-level classification with FLOM, 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. MN-2010-09-08-04 | Becker County - 1998

   Typical pattern of soils and parent material in the Formdale-Langhei-Flom association (Soil Survey of Becker County, Minnesota; 1998).

Map Units

Map units containing FLOM 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
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	3020	3182503	2yw4z	mn005	1994	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	1669	3182513	2yw5c	mn005	1994	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	852	3182514	2yw5d	mn005	1994	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	555	3182510	2yw58	mn005	1994	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	362	3182511	2yw59	mn005	1994	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	30489	3182521	2yw4z	mn011	1990	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	5700	3182532	2yw5d	mn011	1990	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	3236	3182528	2yw58	mn011	1990	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	1523	3182531	2yw5c	mn011	1990	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	560	3182529	2yw59	mn011	1990	1:20000
Flom clay loam, 0 to 1 percent slopes	I683A	226	2798121	2ql18	mn027	1980	1:20000
Flom clay loam, very poorly drained, 0 to 1 percent slopes	I684A	166	2798122	2ql19	mn027	1980	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	18897	3182539	2yw4z	mn051	1974	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	16625	3182550	2yw5d	mn051	1974	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	4904	3182549	2yw5c	mn051	1974	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	1558	3182546	2yw58	mn051	1974	1:20000
Flom fine sandy loam, 0 to 1 percent slopes	I687A	1430	2798209	2ql1b	mn051	1974	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	322	3182547	2yw59	mn051	1974	1:20000
Flom clay loam	36	1179	1859410	20dvz	mn101	2008	1:12000
Flom and Vallers soils, depressional	Fv	2928	357228	czqh	mn107	1970	1:20000
Flom clay loam, 0 to 1 percent slopes	I683A	104	2799103	2ql18	mn107	1970	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	4276	3182557	2yw4z	mn111	1996	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	3877	3182568	2yw5d	mn111	1996	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	2935	3182567	2yw5c	mn111	1996	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	660	3182565	2yw59	mn111	1996	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	359	3182564	2yw58	mn111	1996	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	196	3182575	2yw4z	mn121	1968	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	173	3182585	2yw5c	mn121	1968	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	48	3182586	2yw5d	mn121	1968	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	26	3182583	2yw59	mn121	1968	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	25	3182582	2yw58	mn121	1968	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	27021	3182593	2yw4z	mn149	1966	1:15840
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	16431	3182604	2yw5d	mn149	1966	1:15840
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	4422	3182603	2yw5c	mn149	1966	1:15840
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	3558	3182600	2yw58	mn149	1966	1:15840
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	315	3182601	2yw59	mn149	1966	1:15840
Gonvick-Flom loams	825	1121	428579	gcz4	mn153	1985	1:20000
Flom-Aazdahl-Hamerly complex, 0 to 2 percent slopes	J113A	28830	3182611	2yw4z	mn155	1986	1:20000
Flom-Hamerly complex, 0 to 2 percent slopes	J115A	9023	3182622	2yw5d	mn155	1986	1:20000
Aazdahl-Balaton-Flom complex, 0 to 3 percent slopes	J109A	1713	3182618	2yw58	mn155	1986	1:20000
Flom-Quam silty clay loams, 0 to 1 percent slopes, occasionally ponded	J116A	809	3182621	2yw5c	mn155	1986	1:20000
Flom-Aazdahl-Quam complex, 0 to 4 percent slopes	J114B	185	3182619	2yw59	mn155	1986	1:20000
Flom clay loam, very poorly drained, 0 to 1 percent slopes	I684A	8	2800447	2ql19	mn167	1985	1:20000
Flom loam, 0 to 1 percent slopes	I322A	277	2640919	1nywp	nd017	1983	1:20000
Flom loam, 0 to 1 percent slopes	I322A	667	2641161	1nywp	nd077	2005	1:12000
Gilby-Flom loams, 0 to 2 percent slopes	I540A	7396	2641422	2nb77	nd091	1991	1:20000
Aastad-Flom complex	Aa	1469	418129	g131	sd051	1977	1:20000
Flom clay loam	Fa	1137	418146	g13l	sd051	1977	1:20000
Flom loam, 0 to 1 percent slopes	I322A	34	2800172	1nywp	sd109	1977	1:20000

Map of Series Extent

Approximate geographic distribution of the FLOM 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).