Soil Data Explorer - LONIGAN

Official Series Description

Lab Data Summary

Aggregate lab data for the LONIGAN soil series. This aggregation is based on all pedons with a current taxon name of LONIGAN, 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 LONIGAN 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
28A	81P0577	81ID071001	Lonigan	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.0305557,-112.1180573

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LONIGAN 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 LONIGAN 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 LONIGAN 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 LONIGAN 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 flats position figure.

Competing Series

Soil series competing with LONIGAN 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 LONIGAN 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 LONIGAN 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 terrace figure.

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

Soil series sharing subgroup-level classification with LONIGAN, 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. ID-2010-08-30-09 | Franklin County Area - 2008

   Typical pattern of soils and underlying material in general soil map unit 11 (Wormcreek-Lonigan-Manila) (Soil Survey of Franklin County Area, Idaho; 2008).

Map Units

Map units containing LONIGAN 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
Coalbank-Lonigan-Trailcreek complex, 20 to 50 percent slopes	40	1424	3163533	2v05s	id711	1983	1:24000
Coalbank-Trailcreek-Lonigan complex, 12 to 20 percent slopes	39	1241	82910	2s8j	id711	1983	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76-O	485	3173263	2v073	id711	1983	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24-O	273	3173261	2v06s	id711	1983	1:24000
Lonigan family-Copenhagen-Coalbank family, complex, 15 to 60 percent slopes	469	95	3173253	2q7wj	id711	1983	1:24000
Coalbank family-Lonigan family-Copenhagen complex, 10 to 50 percent slopes	467	25	3173251	2rg0d	id711	1983	1:24000
Lonigan family-Sanyon-Stines complex, 20 to 50 percent slopes	465	3570	2619873	2rg05	id713		1:24000
Lonigan family-Copenhagen-Coalbank family, complex, 15 to 60 percent slopes	469	2992	2508634	2q7wj	id713		1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24	2705	2619844	2v06s	id713		1:24000
Coalbank family-Lonigan family-Copenhagen complex, 10 to 50 percent slopes	467	2527	2619918	2rg0d	id713		1:24000
Pavohroo-Stines-Lonigan association, 10 to 40 percent slopes	89-O	2329	2619853	2v076	id713		1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76	2068	2619882	2v073	id713		1:24000
Lonigan-Lizdale association, 6 to 40 percent slopes	71	256	2619881	2v070	id713		1:24000
Lonigan-Lizdale, very stony surface, association, 6 to 40 percent slopes	85-F	144	2619893	2v07w	id713		1:24000
Coalbank-Lonigan-Trailcreek complex, 20 to 50 percent slopes	40	52	2619917	2v05s	id713		1:24000
Nyman-Lonigan-Copenhagen complex, 30 to 60 percent slopes	103	2327	485191	j8wb	id714	1997	1:24000
Wormcreek-Lonigan complex, 15 to 55 percent slopes	157	2302	485250	j8y7	id714	1997	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	40	1789	485285	j8zc	id714	1997	1:24000
Iphil-Lonigan complex, 8 to 20 percent slopes	62	1724	485309	j904	id714	1997	1:24000
Lonigan-Ricrest association, 50 to 80 percent slopes	86	1401	485335	j90z	id714	1997	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	93	555	485344	j918	id714	1997	1:24000
Lonigan-Lizdale, very stony surface, association, 6 to 40 percent slopes	85	419	3163572	2v07w	id714	1997	1:24000
Lonigan family-Sanyon-Stines complex, 20 to 50 percent slopes	465	245	3173346	2rg05	id714	1997	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76-O	171	3173329	2v073	id714	1997	1:24000
Camelback, very deep-Lonigan complex, 20 to 50 percent slopes	32	48	485276	j8z2	id714	1997	1:24000
Lonigan-Lizdale association, 6 to 40 percent slopes	71-O	3	3173327	2v070	id714	1997	1:24000
Copenhagen-Lonigan-Manila association, 12 to 50 percent slopes	24	9871	3163589	2v06s	id715	1994	1:24000
Pavohroo-Stines-Lonigan association, 10 to 40 percent slopes	89	3126	3163603	2v076	id715	1994	1:24000
Manila-Lonigan complex, 6 to 40 percent slopes	76	3008	3163599	2v073	id715	1994	1:24000
Lonigan family-Sanyon-Stines complex, 20 to 50 percent slopes	465	1536	3173377	2rg05	id715	1994	1:24000
Lonigan-Lizdale association, 6 to 40 percent slopes	71	946	3163596	2v070	id715	1994	1:24000
Lonigan family-Copenhagen-Coalbank family, complex, 15 to 60 percent slopes	469	487	3173366	2q7wj	id715	1994	1:24000
Coalbank family-Lonigan family-Copenhagen complex, 10 to 50 percent slopes	467	404	3173380	2rg0d	id715	1994	1:24000

Map of Series Extent

Approximate geographic distribution of the LONIGAN 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).