Official Series Description


Lab Data Summary

Aggregate lab data for the MEDARY soil series. This aggregation is based on all pedons with a current taxon name of MEDARY, 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 MEDARY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
103UMN2185S1975MN0372185Medary2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7762794,-93.181488
105X3-951G-2S1988IA005020Medary2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3416984,-91.2108644
105X3-951G-1S1988IA005025Medary2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3304856,-91.2201822
10593P0176S1992IA005002Medary7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1561127,-91.1972198
10593P0174S1992IA061002Medary7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5672226,-90.7147217
n/aX49-951-1S1988IA097028Medary2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aX49-000-1S1988IA097928Medary2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MEDARY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the MEDARY series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the MEDARY 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 .

Click the image to view it full size.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

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

Competing Series

Soil series competing with MEDARY share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the MEDARY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the MEDARY 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 .

Click the image to view it full size.

Click the image to view it full size.

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 MEDARY, 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 .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. IL-2010-09-01-32 | Jo Daviess County - 1996

    Typical pattern of soils and parent material in the Zwingle-Medary association (Soil Survey of Jo Daviess County, Illinois; 1996).

  2. IL-2011-08-04-36 | Jo Daviess County - 1996

    Typical pattern of soils and parent material in the Zwingle-Medary association (Soil Survey of Jo Daviess County, Illinois; 1996).

Map Units

Map units containing MEDARY 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
Medary silt loam, 15 to 45 percent slopes951G5554026192xnbmia00519921:15840
Medary silt loam, 15 to 45 percent slopes951F2754043242xnbmia04319791:15840
Medary silt loam, 15 to 45 percent slopes951F2374044752xnbmia04519781:15840
Medary silt loam, 15 to 45 percent slopes951F2534054882xnbmia06119831:15840
Medary silt loam, 15 to 45 percent slopes941G4104075812xnbmia09719881:15840
Medary silt loam, 15 to 45 percent slopes569F250014783332xnbmil01520051:12000
Medary silt loam, 15 to 45 percent slopes569F295719495822xnbmil08519901:12000
Medary silty clay loam, 6 to 12 percent slopes, moderately eroded569C277619495812xnblil08519901:12000
Medary silt loam, 0 to 6 percent slopes, moderately erodedMbB245822163942xnbkmn15720081:12000
Medary silt loam, 0 to 6 percent slopes, moderately eroded262B5864290232xnbkmn16919871:20000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B214825617812xnbkwi01119601:12000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B259125040122xnbkwi02319601:12000
Medary silty clay loam, 6 to 12 percent slopes, moderately eroded326C210425040172xnblwi02319601:12000
Medary silt loam, 15 to 45 percent slopes326F95127747582xnbmwi04319591:20000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B25054242952xnbkwi04319591:20000
Medary silty clay loam, 6 to 12 percent slopes, moderately eroded326C21424242962xnblwi04319591:20000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B223525040132xnbkwi06320011:12000
Medary silt loam, 15 to 45 percent slopes326F11025040182xnbmwi06320011:12000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B29625040142xnbkwi09119981:12000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B215525040152xnbkwi10320021:12000
Medary silt loam, 0 to 6 percent slopes, moderately eroded326B234725040162xnbkwi12319651:12000
Medary silt loam, 15 to 45 percent slopes326F32825040192xnbmwi12319651:12000

Map of Series Extent

Approximate geographic distribution of the MEDARY 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 .