Soil Data Explorer - LAMOILLE

Official Series Description

Lab Data Summary

Aggregate lab data for the LAMOILLE soil series. This aggregation is based on all pedons with a current taxon name of LAMOILLE, 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 LAMOILLE 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
105	UMN2383	S1976MN0552383	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.6229515,-91.43956
105	UMN2630	S1978MN1692630	Lamoille	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.1356392,-91.930336
105	UMN3096	S1979MN1693096	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9908905,-91.788887
105	UMN3098	S1979MN1693098	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0067596,-91.7201385
105	UMN3404	S1980MN1693404	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	44.0808983,-91.9407806
105	86IL085006	S1986IL085006	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3860333,-90.3239361
105	86IL085007	S1986IL085007	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3861694,-90.3239361
105	86IL085008	S1986IL085008	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3863056,-90.3241583
105	86IL085013	S1986IL085013	Lamoille	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.3930694,-90.2884667
105	01P0211	S2000WI063025	Lamoille	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9928818,-90.9734955
105	01P0232	S2000WI063046	Lamoille	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9930649,-90.973587
105	01P0233	S2000WI063047	Lamoille	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.9931412,-90.9737244

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LAMOILLE 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 LAMOILLE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the LAMOILLE 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 LAMOILLE 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.

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 LAMOILLE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the LAMOILLE 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 LAMOILLE 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 3D mountains figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with LAMOILLE, 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. IL-2011-08-04-35 | Jo Daviess County - 1996

   Typical pattern of soils and parent material in the NewGlarus-Lamoille-Lacrescent association (Soil Survey of Jo Daviess County, Illinois; 1996).

Map Units

Map units containing LAMOILLE 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
Newglarus-Lamoille silt loams, silurian landscape, 18 to 35 percent slopes	905F	5708	850720	2t7z6	il015	2005	1:12000
Newglarus-Lamoille silt loams, silurian landscape, 35 to 60 percent slopes	905G	2988	850714	2t7z7	il015	2005	1:12000
Newglarus-Lamoille silt loams, silurian landscape, 18 to 35 percent slopes	905F	14699	1949691	2t7z6	il085	1990	1:12000
Lamoille silt loam, 18 to 35 percent slopes, eroded	755F2	4011	2229502	2dtzf	il085	1990	1:12000
Newglarus-Lamoille silt loams, silurian landscape, 18 to 35 percent slopes	905F	281	1675997	2t7z6	il177	2006	1:12000
Lamoille-Elbaville silt loams, 20 to 30 percent slopes	592E	32224	398307	fcgm	mn055	1981	1:15840
Lamoille-Dorerton silt loams, 30 to 45 percent slopes	584F	16652	398302	fcgg	mn055	1981	1:15840
Lamoille-Dorerton silt loams, 30 to 45 percent slopes	584F	17282	429076	gdh5	mn169	1987	1:20000
Lamoille-Elbaville silt loams, 20 to 30 percent slopes	592E	12178	429082	gdhc	mn169	1987	1:20000
Lamoille silt loam, 6 to 12 percent slopes, moderately eroded	134C2	32	2503796	2v3g5	wi023	1960	1:12000
Lamoille silt loam, 12 to 20 percent slopes, moderately eroded	134D2	1788	2504336	2v3g4	wi063	2001	1:12000
Lamoille silt loam, 6 to 12 percent slopes, moderately eroded	134C2	667	2503797	2v3g5	wi063	2001	1:12000
Lamoille silt loam, 12 to 20 percent slopes, moderately eroded	134D2	5773	2685193	2v3g4	wi081	1981	1:15840
Lamoille silt loam, 20 to 30 percent slopes, moderately eroded	134E2	1853	2685199	2s051	wi081	1981	1:15840
Lamoille silt loam, 6 to 12 percent slopes, moderately eroded	134C2	7735	2503798	2v3g5	wi103	2002	1:12000
Lamoille silt loam, 2 to 6 percent slopes, moderately eroded	134B2	1125	2504334	2v3g6	wi103	2002	1:12000
Lamoille silt loam, 6 to 12 percent slopes, moderately eroded	134C2	44	2503799	2v3g5	wi123	1965	1:12000
Lamoille silt loam, 12 to 20 percent slopes, moderately eroded	134D2	8	2504337	2v3g4	wi123	1965	1:12000
Lamoille silt loam, 2 to 6 percent slopes, moderately eroded	134B2	1	2504335	2v3g6	wi123	1965	1:12000

Map of Series Extent

Approximate geographic distribution of the LAMOILLE 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).