Soil Data Explorer - LALLIE

Official Series Description

Lab Data Summary

Aggregate lab data for the LALLIE soil series. This aggregation is based on all pedons with a current taxon name of LALLIE, 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 LALLIE 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
52	40A3497	S1950MT085005	Lallie	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	48.057724,-105.8012466

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the LALLIE 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 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 LALLIE, 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. ND-2010-09-27-08 | McKenzie County - 2006

   Typical pattern of soils and underlying material in the Havrelon-Lohler association (Soil Survey of McKenzie County, North Dakota; 2006).

2. ND-2012-02-08-43 | Nelson County Area - June 1989

   Typical pattern of soils and parent material in the Wamduska-Lallie-Mauvais association (Soil Survey of Nelson County Area, North Dakota; June 1989).

3. ND-2012-02-08-46 | Ramsey County - August 1986

   Typical pattern of soils and underlying material in the Lallie-Mauvais-Wamduska association (Soil Survey of Ramsey County, North Dakota; August 1986).

Map Units

Map units containing LALLIE 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
Cashel-Lallie-Wahpeton silty clays, 0 to 15 percent slopes, flooded	I136F	7065	2798881	21wt3	mn069	2007	1:12000
Lallie mucky silt loam, map 18-22, 0 to 1 percent slopes	1405	6168	394816	f7v0	mn135	1999	1:24000
Lallie silty clay, 0 to 2 percent slopes	473A	1135	343482	cjf2	mt017	1995	1:24000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	713	345350	1vzvq	mt083	1973	1:24000
Lallie silty clay	32	3687	345548	clkq	mt105	1976	1:24000
Alluvial land	Au	7185	347034	cn3n	mt611	1971	1:24000
Lallie silty clay loam	119	4368	341778	cgn3	mt613	1975	1:24000
Lallie-Swampcreek complex, 0 to 2 percent slopes, rarely flooded	408A	808	1914399	2282t	mt624	2021	1:24000
Lallie silty clay, 0 to 2 percent slopes	650A	203	1948662	23dr2	mt624	2021	1:24000
Lallie family, silty clay, 0 to 2 percent slopes	250A	1359	149810	50wl	mt639	2000	1:24000
Soapcreek-Lallie family complex, 0 to 8 percent slopes	396C	140	149956	5119	mt639	2000	1:24000
Lallie clay loam, 0 to 1 percent slopes	901A	3846	347792	cnx3	mt641	1994	1:24000
Lallie silty clay, saline, 0 to 2 percent slopes	34	21545	348238	cpch	mt661	1982	1:24000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	27	2755656	1vzvp	nd001	1983	1:20000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	9	2755657	1vzvq	nd001	1983	1:20000
Lallie silty clay loam, ponded, 0 to 1 percent slopes	F416A	15180	2587749	2q552	nd005		1:12000
Lallie silty clay loam, 0 to 1 percent slopes	F414A	11400	2587734	2q551	nd005		1:12000
Lallie silty clay loam, saline, 0 to 1 percent slopes	F450A	3557	2587772	2q55j	nd005		1:12000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	336	2563569	1vzvq	nd011	1969	1:20000
Harriet-Lallie complex, 0 to 2 percent slopes, occasionally flooded	E4007A	254	2563560	1vzvn	nd011	1969	1:20000
Lallie clay loam, 0 to 1 percent slopes	Ke	207	992843	12b46	nd011	1969	1:20000
Lallie silty clay, low precipitation, 0 to 1 percent slopes, occasionally flooded	L4033A	201	2563494	2q38b	nd011	1969	1:20000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	1475	2661701	1vzvq	nd015	1967	1:20000
Lallie silty clay loam, 0 to 1 percent slopes	G414A	272	2576306	2q5cg	nd027		1:12000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	440	2661787	1vzvq	nd029	1979	1:20000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopes	G446A	714	2576449	2q5n3	nd031	1990	1:20000
Lallie silty clay loam, 0 to 1 percent slopes, ponded	I154A	3036	2642586	2mbl9	nd035	1980	1:20000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	81	2525888	1vzvp	nd037	1985	1:20000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	63	2759652	1vzvq	nd037	1985	1:20000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopes	G446A	181	2576630	2q5n3	nd039	1991	1:24000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	3	2759721	1vzvq	nd053	2003	1:24000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	1016	2662463	1vzvq	nd055	1974	1:20000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	200	2662462	1vzvp	nd055	1974	1:20000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	971	2699174	1vzvp	nd059	1998	1:20000
Lallie silty clay loam, saline, 0 to 1 percent slopes	F450A	3019	2587384	2q55j	nd063		1:12000
Lallie silty clay loam, ponded, 0 to 1 percent slopes	F416A	97	2587374	2q552	nd063		1:12000
Lallie, saline-Minnewaukan complex, 0 to 2 percent slopes	G446A	95	2577332	2q5n3	nd063		1:12000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	1154	2525988	1vzvq	nd065	1971	1:20000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	405	2525987	1vzvp	nd065	1971	1:20000
Lallie silty clay loam, 0 to 1 percent slopes	F414A	15	2587270	2q551	nd069	1975	1:20000
Lallie silty clay loam, 0 to 1 percent slopes	F414A	3536	2587126	2q551	nd071	1984	1:12000
Lallie silty clay loam, saline, 0 to 1 percent slopes	F450A	1366	2587134	2q55j	nd071	1984	1:12000
Lallie silty clay loam, ponded, 0 to 1 percent slopes	F416A	995	2587127	2q552	nd071	1984	1:12000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	94	2759702	1vzvp	nd085	1992	1:24000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	87	2759703	1vzvq	nd085	1992	1:24000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	1081	2715857	1vzvq	nd087	1974	1:20000
Lallie silty clay, low precipitation, 0 to 1 percent slopes, occasionally flooded	L4033A	493	2715946	2q38b	nd087	1974	1:20000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	E4033A	1314	2716003	1vzvq	nd089	1965	1:20000
Lallie silty clay, very poorly drained, 0 to 1 percent slopes, frequently flooded	E4031A	266	2716002	1vzvp	nd089	1965	1:20000
Harriet-Lallie complex, 0 to 2 percent slopes, occasionally flooded	E4007A	124	2716001	1vzvn	nd089	1965	1:20000
Lallie silty clay, 0 to 1 percent slopes, occasionally flooded	La	4921	356177	1vzvq	sd031	1986	1:24000
Lallie silty clay loam	Le	579	355762	cy66	sd063	1984	1:24000

Map of Series Extent

Approximate geographic distribution of the LALLIE 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).