Soil Data Explorer - NADEAU

Official Series Description

Lab Data Summary

Aggregate lab data for the NADEAU soil series. This aggregation is based on all pedons with a current taxon name of NADEAU, 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 NADEAU 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.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NADEAU 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 NADEAU 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 NADEAU 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 NADEAU 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 NADEAU 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 NADEAU 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 NADEAU 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 NADEAU, 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. MI-2010-09-07-15 | Marquette County - 2007

   Typical pattern of soils and parent material in the Emmet-Carbondale association (Soil Survey of Marquette County, Michiganl 2007).

Map Units

Map units containing NADEAU 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
Nadeau extremely gravelly loamy sand, 1 to 9 percent slopes	31B	1818	190569	6d9d	mi031	1988	1:15840
Nadeau fine sandy loam, 0 to 6 percent slopes	35B	3337	415214	fy20	mi043	1985	1:20000
Nadeau fine sandy loam, 6 to 18 percent slopes	35D	2768	415215	fy21	mi043	1985	1:20000
Nadeau fine sandy loam, 18 to 35 percent slopes	35F	797	415216	fy22	mi043	1985	1:20000
Nadeau-Mancelona complex, 1 to 6 percent slopes	110B	1882	394975	f804	mi103	1999	1:24000
Nadeau fine sandy loam, 1 to 6 percent slopes	70B	1402	395250	f890	mi103	1999	1:24000
Nadeau-Mancelona complex, 6 to 18 percent slopes	110D	485	394976	f805	mi103	1999	1:24000
Onaway-Nadeau fine sandy loams, 1 to 6 percent slopes	91B	429	395301	f8bn	mi103	1999	1:24000
Nadeau fine sandy loam, 6 to 18 percent slopes	70D	414	395251	f891	mi103	1999	1:24000
Nadeau fine sandy loam, 3 to 12 percent slopes	12B	16713	415450	fy9m	mi109	1985	1:20000
Onaway-Nadeau fine sandy loams, 3 to 12 percent slopes	52B	13502	2861562	2t04v	mi109	1985	1:20000
Mancelona-Nadeau complex, 0 to 8 percent slopes	37B	6113	415475	fybf	mi109	1985	1:20000
Tawas-Banat-Nadeau complex, 0 to 15 percent slopes	54C	4488	415489	fybw	mi109	1985	1:20000
Nadeau fine sandy loam, 15 to 35 percent slopes	12D	3067	415451	fy9n	mi109	1985	1:20000
Onaway-Nadeau fine sandy loams, 12 to 35 percent slopes	52D	1358	2861563	2t04w	mi109	1985	1:20000
Pemene-Nadeau complex, 3 to 12 percent slopes	61B	1307	415495	fyc2	mi109	1985	1:20000
Nadeau-Summerville fine sandy loams, 3 to 12 percent slopes	55B	872	415490	fybx	mi109	1985	1:20000
Emmet-Nadeau fine sandy loams, 3 to 12 percent slopes	H52B	816	2800275	2s5fw	mi109	1985	1:20000
Nadeau fine sandy loam, 2 to 6 percent slopes	NaB	6070	422426	g5kn	wi075	1987	1:20000
Nadeau fine sandy loam, 6 to 12 percent slopes	NaC	4776	422427	g5kp	wi075	1987	1:20000

Map of Series Extent

Approximate geographic distribution of the NADEAU 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).