Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
107B40A1498S1970IA133004MODALE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1049995,-96.2324982
115BM91041051991MO041005Modale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM98051011998MO051128Modale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6171728,-92.2115514
115BM03219072003MO219007Modale4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6021917,-90.9987361

Water Balance

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

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Sibling Summary

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

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

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Geomorphic description summaries for the MODALE 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 .

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

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

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Click the image to view it full size.

Competing Series

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

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

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Geomorphic description summaries for the MODALE 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 .

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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.

Click the image to view it full size.

Soil series sharing subgroup-level classification with MODALE, 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. MO-2010-09-08-03 | Holt County - 1997

    Typical pattern of soils and parent material in the Leta-Grable-Haynie association (Soil Survey of Holt County, Missouri; 1997).

  2. NE-2012-02-10-04 | Cedar County - October 1985

    Typical pattern of soils in the Sarpy-Blake-Albaton association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

Map Units

Map units containing MODALE 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
Modale silt loam1491752406100fml0ia07119681:20000
Modale silt loam1491710406736fn7jia08519711:15840
Modale very fine sandy loam549267406778fn8wia08519711:15840
Modale silt loam, 0 to 2 percent slopes1491198409539fr4yia12919791:15840
Modale silt loam, 0 to 2 percent slopes, rarely flooded1491918447349h0hmia13319941:12000
Modale silty clay loam, 0 to 2 percent slopes, rarely flooded1471077447348h0hlia13319941:12000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded1150225447408h0kjia13319941:12000
Modale silty clay loam, 0 to 2 percent slopes, occasionally flooded114781447406h0kgia13319941:12000
Modale silt loam, dark subsoil variant, 0 to 2 percent slopes149272410322frz6ia14919721:20000
Modale silt loam, 0 to 2 percent slopes1491722410446fs36ia15519861:15840
Modale complex, 0 to 2 percent slopes, rarely flooded35494543741620swq7ia19320031:12000
Modale complex, 0 to 2 percent slopes, occasionally flooded549115741619swq6ia19320031:12000
Modale silt loam, 0 to 2 percent slopes, rarely flooded13553276525284212qmtxmo02119841:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded13552195225284142qmtwmo04119921:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded13552123525284172qmtwmo04719821:24000
Modale silt loam, 0 to 2 percent slopes, rarely flooded13553345325284202qmtxmo08719921:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded13552123125284152qmtwmo09519821:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded1355281725284162qmtwmo10719701:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded1355240825284182qmtwmo13919751:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded13552434425284192qmtwmo17719791:24000
Modale silt loam, 0 to 2 percent slopes, occasionally flooded1355296225284132qmtwmo21919751:24000
Modale silt loam, occasionally flooded77581527427839gc68ne02119781:20000
Modale silt loam, rarely flooded7759952427116gbfyne02719821:20000
Modale silt loam, occasionally flooded7758770426745gb1zne04319721:20000
Modale very fine sandy loam, rarely flooded7757497426677g9zsne05119751:20000
Modale silt loam, 0 to 2 percent slopesMo591445592gynysd02719951:24000
Modale silt loamMb6033453708h73rsd12719741:20000

Map of Series Extent

Approximate geographic distribution of the MODALE 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 .