Soil Data Explorer - TALMOON

Official Series Description

Lab Data Summary

Aggregate lab data for the TALMOON soil series. This aggregation is based on all pedons with a current taxon name of TALMOON, 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 TALMOON 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
90B	UMN1309	S1964MN0251309	Talmoon	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.6769676,-92.9809494
90B	UMN1307	S1971MN0251307	Talmoon	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.7030792,-92.9866867

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TALMOON 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 TALMOON 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 TALMOON 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 TALMOON series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

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

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

Competing Series

Soil series competing with TALMOON 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 TALMOON 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 TALMOON 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 mountains figure.

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

Soil series sharing subgroup-level classification with TALMOON, 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-2010-09-10-12 | Sherburne County -

   Pattern of soils and parent material in the Nebish-Braham-Stonelake association (Soil Survey of Sherburne County, Minnesota).

Map Units

Map units containing TALMOON 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
Talmoon fine sandy loam	346	12986	432905	gjgp	mn001	1996	1:20000
Talmoon muck, depressional	628	11040	432952	gjj6	mn001	1996	1:20000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	19	3247914	307cy	mn003	1972	1:15840
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	0	3247916	307cj	mn003	1972	1:15840
Talmoon muck	628	7394	397674	fbt6	mn007	1991	1:24000
Talmoon loam, 0 to 2 percent slopes	C128A	67	1914097	227s2	mn009	2007	1:12000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	13380	3247922	307ck	mn025	1990	1:15840
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	6970	3247919	307cy	mn025	1990	1:15840
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	3135	3247929	307cj	mn025	1990	1:15840
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	1775	3247921	307ch	mn025	1990	1:15840
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	805	3247928	307cp	mn025	1990	1:15840
Talmoon loam	346	3338	430489	gfyr	mn029	1993	1:20000
Talmoon loam, 0 to 2 percent slopes	346	491	436651	gncj	mn057	1998	1:24000
Talmoon muck, depressional, 0 to 1 percent slopes	628	126	436689	gndr	mn057	1998	1:24000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	6742	3247936	307ck	mn059	1956	1:20000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	4905	3247933	307cy	mn059	1956	1:20000
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	2707	3247943	307cj	mn059	1956	1:20000
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	1122	3247935	307ch	mn059	1956	1:20000
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	832	3247942	307cp	mn059	1956	1:20000
Talmoon silt loam	628	7913	398460	fcmk	mn061	1982	1:24000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	16	3247946	307cy	mn065	2006	1:12000
Talmoon loam	346	716	399228	fdfb	mn087	1992	1:20000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	88	3247952	307ck	mn095	2006	1:12000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	80	3247949	307cy	mn095	2006	1:12000
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	28	3247951	307ch	mn095	2006	1:12000
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	7	3247958	307cp	mn095	2006	1:12000
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	2	3247959	307cj	mn095	2006	1:12000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	6780	3247965	307ck	mn115	2009	1:24000
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	769	3247972	307cj	mn115	2009	1:24000
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	407	3247964	307ch	mn115	2009	1:24000
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	96	3247971	307cp	mn115	2009	1:24000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	64	3247962	307cy	mn115	2009	1:24000
Talmoon loam, 0 to 2 percent slopes	346	2253	431481	ggzr	mn141	1994	1:15840
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	596	3247975	307cy	mn163	1978	1:15840
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	233	3247978	307ck	mn163	1978	1:15840
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	34	3247984	307cp	mn163	1978	1:15840
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	32	3247977	307ch	mn163	1978	1:15840
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	12	3247985	307cj	mn163	1978	1:15840
Beltrami-Talmoon complex, 0 to 3 percent slopes	A25A	25147	2943761	sfwj	mn625	2015	1:24000
Talmoon-Beltrami complex, 0 to 3 percent slopes	A22A	19084	2943759	sfwg	mn625	2015	1:24000
Talmoon, depressional-Hamre complex, 0 to 1 percent slopes	A19A	9841	2943749	nl80	mn625	2015	1:24000
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	1802	3247998	307cp	wi013	2004	1:12000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	658	3247992	307ck	wi013	2004	1:12000
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	317	3247991	307ch	wi013	2004	1:12000
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	127	3247989	307cy	wi013	2004	1:12000
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	26	3247999	307cj	wi013	2004	1:12000
Talmoon-Alstad-Bluffton, frequently ponded, loams, 0 to 2 percent slopes	C79A	628	3248005	307ck	wi095	1978	1:15840
Alstad-Talmoon loams, 0 to 2 percent slopes	C76A	412	3248004	307ch	wi095	1978	1:15840
Branstad-Alstad-Talmoon loams, 0 to 4 percent slopes	C84B	255	3248011	307cp	wi095	1978	1:15840
Talmoon, Alstad, and Blomford soils, 0 to 2 percent slopes	C63A	92	3248002	307cy	wi095	1978	1:15840
Ricelake, Alstad, and Talmoon soils, 0 to 2 percent slopes	C90A	72	3248012	307cj	wi095	1978	1:15840

Map of Series Extent

Approximate geographic distribution of the TALMOON 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).