Official Series Description


Lab Data Summary

Aggregate lab data for the MODJESKA soil series. This aggregation is based on all pedons with a current taxon name of MODJESKA, 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 MODJESKA 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
1971C0074S1971CA059011Modjeska7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.6413879,-117.5986099
1971C0075S1971CA059012MODJESKA6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.6338882,-117.6080551
n/a71C0073S1971CA059002MODJESKA7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MODJESKA 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 MODJESKA 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 MODJESKA 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 MODJESKA 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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Competing Series

Soil series competing with MODJESKA 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 MODJESKA 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 MODJESKA 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 terrace figure.

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

Soil series sharing subgroup-level classification with MODJESKA, 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

No block diagrams are available.

Map Units

Map units containing MODJESKA 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
Modjeska gravelly loam, 2 to 9 percent slopes1692395458070hcngca67819741:24000
Modjeska gravelly loam, 0 to 2 percent slopes1682380458069hcnfca67819741:24000
Modjeska gravelly loam, 15 to 30 percent slopes171785458072hcnjca67819741:24000
Modjeska gravelly loam, 9 to 15 percent slopes170635458071hcnhca67819741:24000
Modjeska gravelly loam, 2 to 9 percent slopes16929729101sgpdca67919671:15840
Modjeska gravelly loam, 9 to 15 percent slopes1706729099sgpbca67919671:15840
Trigo, granitic substratum-Modjeska families association, 5 to 60 percent slopes300af4852670241hm6tca69620161:24000
Yorba-Modjeska-Morical families association, 30 to 60 percent slopes5246253465321hm6cca77219811:24000
Agua Dulce-Los Robles-Modjeska families association, 10 to 60 percent slopes343147465296hm5kca77219811:24000
Millerton-Reliz-Modjeska families association, 40 to 70 percent slopes2835926465294hm5hca77219811:24000
Lodo-Modjeska-Botella families association, 10 to 70 percent slopes1827696465283hm54ca77219811:24000
Millerton-Modjeska familes association, 30 to 80 percent slopes2712154465293hm5gca77219811:24000
Modjeska-Modesto families association, 30 to 60 percent slopes3410724465301hm5qca77219811:24000
Modjeska-Lodo families association, 40 to 80 percent slopes338892465300hm5pca77219811:24000
Trigo, granitic substratum-Modjeska families association, 5 to 60 percent slopes3005170465335hm6tca77619811:24000
Lodo-Modjeska-Botella families association, 10 to 70 percent slopes18159991370128lpca77619811:24000

Map of Series Extent

Approximate geographic distribution of the MODJESKA 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 .