Soil Data Explorer - GLADWIN

Official Series Description

Lab Data Summary

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

No block diagrams are available.

Map Units

Map units containing GLADWIN 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
Gladwin-Allendale association, undulating	GnB	1952	189165	6bv3	mi011	1964	1:20000
Gladwin loamy sand	Gm	456	189164	6bv2	mi011	1964	1:20000
Gladwin loamy sand, 0 to 6 percent slopes	GlB	1844	190449	6d5j	mi029	1970	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	GaA	3839	189613	6c9k	mi035	1977	1:15840
Gladwin loamy sand, loamy substratum, 0 to 2 percent slopes	GlA	58	2673504	6ch0	mi035	1977	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	GhA	7237	189781	6cgz	mi051	1966	1:15840
Gladwin loamy sand, loamy substratum, 0 to 2 percent slopes	GlA	2833	189782	6ch0	mi051	1966	1:15840
Gladwin-Epoufette-Croswell association, undulating	GPB	2806	189783	6ch1	mi051	1966	1:15840
Gladwin-Epoufette association	GE	747	189780	6cgy	mi051	1966	1:15840
Gladwin-Epoufette-Covert association, undulating	GFB	139	2673499	2qz6d	mi051	1966	1:15840
Gladwin-Richter gravelly sandy loams, 0 to 2 percent slopes	GrA	457	189436	6c3v	mi055	1963	1:15840
Gladwin-Richter gravelly sandy loams, 2 to 6 percent slopes	GrB	135	189437	6c3w	mi055	1963	1:15840
Gladwin-Richter gravelly sandy loams, 6 to 12 percent slopes	GrC	57	189438	6c3x	mi055	1963	1:15840
Gladwin sandy loam, 0 to 2 percent slopes	GlA	393	187970	69lk	mi067	1965	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	GhA	293	187968	69lh	mi067	1965	1:15840
Gladwin sandy loam, 2 to 6 percent slopes	GlB	173	187971	69ll	mi067	1965	1:15840
Gladwin loamy sand, 2 to 6 percent slopes	GhB	114	187969	69lj	mi067	1965	1:15840
Gladwin loamy sand, 0 to 3 percent slopes	197A	412	191726	6fhq	mi069	1995	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	104A	7	2673519	6c9k	mi073	1983	1:15840
Gladwin loamy sand, 0 to 3 percent slopes	197A	285	190726	6dgg	mi079	1998	1:12000
Gladwin loamy sand, 0 to 3 percent slopes	15A	2317	415453	fy9q	mi109	1985	1:20000
Gladwin loamy sand, 0 to 2 percent slopes	GhA	38	2673544	6cgz	mi111	1976	1:15840
Gladwin loamy sand, 0 to 3 percent slopes	34A	471	192427	6g7b	mi113	1983	1:15840
Gladwin loamy sand and Palo sandy loam, 0 to 2 percent slopes	Ga	10758	187281	68wb	mi117	1956	1:20000
Gladwin loamy sand and Palo sandy loam, 2 to 6 percent slopes	Gb	495	187282	68wc	mi117	1956	1:20000
Gladwin sand, 0 to 3 percent slopes	47A	5337	189924	6cml	mi129	1987	1:15840
Gladwin sandy loam, 0 to 2 percent slopes	GdA	537	190030	6cr0	mi133	1966	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	GaA	156	190028	6cqy	mi133	1966	1:15840
Gladwin loamy sand, 2 to 6 percent slopes	GaB	109	190029	6cqz	mi133	1966	1:15840
Gladwin sandy loam, 2 to 6 percent slopes	GdB	108	190031	6cr1	mi133	1966	1:15840
Gladwin loamy sand, 0 to 3 percent slopes	197A	425	191551	6fb2	mi137	1998	1:12000
Gladwin sandy loam, 0 to 2 percent slopes	GeA	2716	192664	6ggz	mi139	1967	1:15840
Gladwin sandy loam, 2 to 6 percent slopes	GeB	850	192665	6gh0	mi139	1967	1:15840
Gladwin loamy sand, 0 to 3 percent slopes	37A	1780	190886	6dmm	mi141	1989	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	111A	16	2423168	2mbhq	mi145	1991	1:15840
Gladwin and Palo sandy loams, 0 to 2 percent slopes	GbA0	3609	188261	69wy	mi151	1955	1:15840
Gladwin and Palo sandy loams, 2 to 7 percent slopes, slightly eroded	GbB1	1364	188262	69wz	mi151	1955	1:15840
Gladwin loamy sand, 0 to 2 percent slopes	GmA	843	187799	69f1	mi155	1967	1:12000

Map of Series Extent

Approximate geographic distribution of the GLADWIN 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).