Soil Data Explorer - WINNESHIEK

Official Series Description

Lab Data Summary

Aggregate lab data for the WINNESHIEK soil series. This aggregation is based on all pedons with a current taxon name of WINNESHIEK, 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 WINNESHIEK 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
104	X45-714-1	1964IA089014	Winneshiek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.3427232,-92.1144538
104	85P0514	84IA1310021	Winneshiek	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2750015,-92.8666687
104	85P0515	84IA1310022	Winneshiek	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2750015,-92.8666687
104	86P0475	85IA1310031	Winneshiek	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2405548,-92.7897186
104	86P0476	85IA1310032	Winneshiek	5	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2405548,-92.7900009
104	X191714	S1959IA191009	Winneshiek	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.2896193,-92.0222181
104	X45-214S-1	S1965IA089914	Winneshiek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.42664,-92.17137
105	X65714N-4-1	S1962IA065016	Winneshiek	1	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.9714759,-91.6314629
105	X49-914-1	S1986IA097008	Winneshiek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1764957,-90.7142036
105	X49-914D2	S1988IA097051	Winneshiek	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.1047544,-90.6354579

Water Balance

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

Soil series sharing subgroup-level classification with WINNESHIEK, 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. IA-2010-09-09-28 | Winneshiek County - 2007

   Typical pattern of soils and parent material in the Winneshiek-Marlean association (Soil Survey of Winneshiek County, Iowa; 2007).

Map Units

Map units containing WINNESHIEK 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
Winneshiek loam, 30 to 40 inches to limestone, till plain, 2 to 5 percent slopes	713B	319	403427	2xl3b	ia023	1978	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 2 to 5 percent slopes	714B	318	403428	2xl35	ia023	1978	1:15840
Winneshiek loam, 30 to 40 inches to limestone, till plain, 2 to 5 percent slopes	713B	214	404060	2xl3b	ia037	1989	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 2 to 5 percent slopes	714B	156	404061	2xl35	ia037	1989	1:15840
Winneshiek loam, 2 to 5 percent slopes	914B	147	2479325	2p6y7	ia037	1989	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 2 to 5 percent slopes	714B	921	404301	fkpz	ia043	1979	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 5 to 9 percent slopes	714C	393	404302	fkq0	ia043	1979	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 3 to 9 percent slopes	714C	742	405474	flxt	ia061	1983	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 2 to 5 percent slopes	714B	1845	405803	fm8f	ia065	1975	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 5 to 9 percent slopes	714C	492	405804	fm8g	ia065	1975	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 0 to 2 percent slopes	714	259	405802	fm8d	ia065	1975	1:15840
Winneshiek loam, 20 to 30 inches to limestone, 9 to 14 percent slopes	714D	194	405805	fm8h	ia065	1975	1:15840
Winneshiek silt loam, 20 to 30 inches to limestone, till plain, 2 to 5 percent slopes	714B	880	405999	2xl3k	ia067	1989	1:15840
Winneshiek silt loam, 30 to 40 inches to limestone, till plain, 2 to 5 percent slopes	713B	783	405996	2xl3n	ia067	1989	1:15840
Winneshiek silt loam, 20 to 30 inches to limestone, till plain, 5 to 9 percent slopes	714C	521	406000	2xl3l	ia067	1989	1:15840
Winneshiek silt loam, 30 to 40 inches to limestone, till plain, 0 to 2 percent slopes	713	332	405995	2xl3m	ia067	1989	1:15840
Winneshiek loam, moderately deep, 2 to 5 percent slopes	714B	1972	406977	fnh9	ia089	1969	1:15840
Winneshiek loam, deep, 2 to 5 percent slopes	713B	1685	406974	fnh6	ia089	1969	1:15840
Winneshiek loam, moderately deep, 5 to 9 percent slopes	714C	923	406978	fnhb	ia089	1969	1:15840
Winneshiek loam, deep, 0 to 2 percent slopes	713A	809	406973	fnh5	ia089	1969	1:15840
Winneshiek loam, moderately deep, 9 to 14 percent slopes	714D	353	406980	fnhd	ia089	1969	1:15840
Winneshiek loam, deep, 5 to 9 percent slopes	713C	292	406975	fnh7	ia089	1969	1:15840
Winneshiek loam, moderately deep, 0 to 2 percent slopes	714A	201	406976	fnh8	ia089	1969	1:15840
Winneshiek loam, shaly subsoil variant, 0 to 2 percent slopes	148A	196	407012	fnjf	ia089	1969	1:15840
Winneshiek loam, moderately deep, 5 to 9 percent slopes, moderately eroded	714C2	196	406979	fnhc	ia089	1969	1:15840
Winneshiek loam, 5 to 9 percent slopes, moderately eroded	914C2	894	407568	fp3c	ia097	1988	1:15840
Winneshiek loam, 9 to 14 percent slopes, moderately eroded	914D2	735	407569	fp3d	ia097	1988	1:15840
Winneshiek loam, 2 to 9 percent slopes	914C	1047	408220	fpsd	ia105	1988	1:15840
Winneshiek loam, 9 to 18 percent slopes	914E	501	408221	fpsf	ia105	1988	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 2 to 5 percent slopes	714B	1894	409690	2xl35	ia131	1971	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 5 to 9 percent slopes	714C	1437	409691	2xl36	ia131	1971	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 0 to 2 percent slopes	714	283	409689	2xl33	ia131	1971	1:15840
Winneshiek loam, 20 to 30 inches to limestone, till plain, 9 to 14 percent slopes	714D	282	409692	2xl38	ia131	1971	1:15840
Winneshiek loam, 2 to 5 percent slopes	914B	10044	451061	h4cc	ia191	2005	1:12000
Winneshiek loam, 5 to 9 percent slopes	914C	2736	451062	h4cd	ia191	2005	1:12000
Winneshiek loam, 9 to 14 percent slopes	914D	516	451064	h4cg	ia191	2005	1:12000
Winneshiek loam, 14 to 18 percent slopes	914E	358	451066	h4cj	ia191	2005	1:12000
Winneshiek silt loam, 0 to 3 percent slopes	WnA	727	186261	67tf	mi045	1974	1:15840
Nasset-Winneshiek complex, 12 to 18 percent slopes, moderately eroded	M527D2	838	1384979	1hh5r	mn039	2005	1:12000
Winneshiek silt loam, 2 to 6 percent slopes	M526B	792	1384980	1hh5s	mn039	2005	1:12000
Winneshiek silt loam, 6 to 12 percent slopes, moderately eroded	M526C2	570	1384983	1hh5w	mn039	2005	1:12000
Schapville-Winneshiek complex, 2 to 6 percent slopes	N552B	154	1385012	1hh6t	mn039	2005	1:12000
Winneshiek-Waucoma complex, 18 to 35 percent slopes	N598E	2362	1670241	1t20r	mn049	2007	1:12000
Winneshiek-Waucoma complex, 12 to 18 percent slopes, moderately eroded	N598D2	2240	1670242	1t20s	mn049	2007	1:12000
Waucoma-Winneshiek complex, 6 to 12 percent slopes, moderately eroded	N597C2	1302	1670237	1t20m	mn049	2007	1:12000
Winneshiek silt loam, 2 to 6 percent slopes	M526B	760	1481632	1lqrl	mn049	2007	1:12000
Winneshiek silt loam, 6 to 12 percent slopes, moderately eroded	M526C2	467	1481630	1lqrj	mn049	2007	1:12000
Winneshiek loam, sinkhole karst, 2 to 6 percent slopes	N599B	225	1670681	1t2gy	mn049	2007	1:12000
Winneshiek loam, sinkhole karst, 6 to 12 percent slopes, moderately eroded	N599C2	92	1670680	1t2gx	mn049	2007	1:12000
Nasset-Winneshiek complex, 12 to 18 percent slopes, moderately eroded	M527D2	68	1670743	1t2jy	mn049	2007	1:12000
Schapville-Winneshiek complex, 2 to 6 percent slopes	N552B	2	1711647	1vg3f	mn049	2007	1:12000
Winneshiek fine sandy loam, 2 to 6 percent slopes	WnB	1333	423381	g6kg	wi021	1972	1:15840
Winneshiek fine sandy loam, 6 to 12 percent slopes, eroded	WnC2	853	423382	g6kh	wi021	1972	1:15840

Map of Series Extent

Approximate geographic distribution of the WINNESHIEK 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).