Soil Data Explorer - LINDQUIST

Official Series Description

Lab Data Summary

Aggregate lab data for the LINDQUIST soil series. This aggregation is based on all pedons with a current taxon name of LINDQUIST, 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 LINDQUIST 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
n/a	10N1178	S2010WI069001	Lindquist	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	10N1179	S2010WI069002	Lindquist	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	10N1180	S2010WI085003	Lindquist	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	10N1181	S2010WI085004	Lindquist	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LINDQUIST 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 LINDQUIST 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 LINDQUIST 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 LINDQUIST 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 LINDQUIST 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 LINDQUIST 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 LINDQUIST 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 LINDQUIST, 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-2010-09-07-28 | Otsego County - 2004

   Typical pattern of soils and parent material in the Leelanau-Lindquist association. Depth is indicated in inches (Soil Survey of Otsego County, Michigan; 2004).

Map Units

Map units containing LINDQUIST 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
Lindquist sand, 0 to 6 percent slopes	147B	545	2440653	2mxpr	mi039	1993	1:15840
Linquist sand, 18 to 35 percent slopes	147E	227	2440654	2mxps	mi039	1993	1:15840
Lindquist sand, 6 to 18 percent slopes	385D	189	2440663	2mxq2	mi039	1993	1:15840
Lindquist sand, 0 to 6 percent slopes	147B	4235	190628	6dc9	mi079	1998	1:12000
Lindquist sand, 6 to 12 percent slopes	147C	1652	190682	6df1	mi079	1998	1:12000
Lindquist sand, 12 to 18 percent slopes	147D	1312	190687	6df6	mi079	1998	1:12000
Lindquist sand, 18 to 35 percent slopes	147E	624	190719	6dg7	mi079	1998	1:12000
Lindquist sand, 0 to 6 percent slopes	147B	2426	192192	6fzr	mi119	1997	1:12000
Lindquist sand, 6 to 18 percent slopes	385D	917	192267	6g25	mi119	1997	1:12000
Lindquist sand, 18 to 35 percent slopes	147E	468	192193	6fzs	mi119	1997	1:12000
Lindquist sand, 0 to 6 percent slopes	147B	19213	191447	6f6q	mi137	1998	1:12000
Lindquist sand, 8 to 50 percent slopes, dissected	401F	3622	191494	6f87	mi137	1998	1:12000
Lindquist sand, 6 to 12 percent slopes	147C	3282	191448	6f6r	mi137	1998	1:12000
Lindquist sand, 12 to 18 percent slopes	147D	2495	191449	6f6s	mi137	1998	1:12000
Lindquist sand, 18 to 35 percent slopes	147E	352	191450	6f6t	mi137	1998	1:12000
Lindquist sand, 6 to 18 percent slopes	385D	968	2440689	2mxqx	mi143	1999	1:12000
Sayner-Lindquist complex, 6 to 15 percent slopes	9012C	693	1444552	1kh5g	wi003	2006	1:12000
Sayner-Lindquist complex, 0 to 6 percent slopes	9012B	336	1444551	1kh5f	wi003	2006	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	269	1444455	1kh2b	wi003	2006	1:12000
Vilas-Lindquist complex, 0 to 6 percent slopes	594B	239	1444454	1kh29	wi003	2006	1:12000
Vilas-Lindquist complex, 15 to 30 percent slopes	594D	15	1444456	1kh2c	wi003	2006	1:12000
Sayner-Lindquist complex, 15 to 30 percent slopes	9012D	13	1444553	1kh5h	wi003	2006	1:12000
Sayner-Lindquist complex, 6 to 15 percent slopes	9012C	2354	1383944	1hg3c	wi007	2005	1:12000
Sayner-Lindquist complex, 15 to 30 percent slopes	9012D	2231	1383945	1hg3d	wi007	2005	1:12000
Sayner-Lindquist complex, 0 to 6 percent slopes	9012B	1868	1383943	1hg3b	wi007	2005	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	872	1147412	17hz9	wi007	2005	1:12000
Vilas-Lindquist complex, 15 to 30 percent slopes	594D	158	1147411	17hz8	wi007	2005	1:12000
Vilas-Lindquist complex, 0 to 6 percent slopes	594B	1652	1701243	1v38t	wi051	2006	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	517	1701244	1v38v	wi051	2006	1:12000
Vilas-Lindquist complex, 15 to 30 percent slopes	594D	83	1701245	1v38w	wi051	2006	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	3774	1598810	1qnpj	wi099	2006	1:12000
Vilas-Lindquist complex, 0 to 6 percent slopes	594B	2955	1292271	1dcq5	wi099	2006	1:12000
Sayner-Lindquist complex, 6 to 15 percent slopes	9012C	2018	1395743	1hvcz	wi099	2006	1:12000
Sayner-Lindquist complex, 0 to 6 percent slopes	9012B	1736	1395744	1hvd0	wi099	2006	1:12000
Vilas-Lindquist complex, 15 to 30 percent slopes	594D	838	1598811	1qnpk	wi099	2006	1:12000
Sayner-Lindquist complex, 15 to 30 percent slopes	9012D	232	1395742	1hvcy	wi099	2006	1:12000
Vilas-Lindquist complex, 0 to 6 percent slopes	594B	193	1145158	17fml	wi107	2006	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	88	1145160	17fmn	wi107	2006	1:12000
Vilas-Lindquist complex, 0 to 6 percent slopes	594B	7079	1017816	1353s	wi113	2006	1:12000
Vilas-Lindquist complex, 6 to 15 percent slopes	594C	7014	1017820	1353x	wi113	2006	1:12000
Vilas-Lindquist complex, 15 to 30 percent slopes	594D	2257	1017819	1353w	wi113	2006	1:12000
Sayner-Lindquist complex, 6 to 15 percent slopes	9012C	1662	1386111	1hjc8	wi113	2006	1:12000
Sayner-Lindquist complex, 15 to 30 percent slopes	9012D	653	1386110	1hjc7	wi113	2006	1:12000
Sayner-Lindquist complex, 0 to 6 percent slopes	9012B	207	1386112	1hjc9	wi113	2006	1:12000

Map of Series Extent

Approximate geographic distribution of the LINDQUIST 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).