Official Series Description


Lab Data Summary

Aggregate lab data for the MONDAMIN soil series. This aggregation is based on all pedons with a current taxon name of MONDAMIN, 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 MONDAMIN 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
53B91P02081990ND105265Mondamin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.4382934570312,-102.997261047363
53B84ND06108684ND061086Mondamin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0255556,-101.9436111
53B84ND06110184ND061101Mondamin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0027778,-101.9583333
55A40A012058ND013001Mondamin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.5480556,-102.2347222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MONDAMIN 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 MONDAMIN 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 MONDAMIN 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 MONDAMIN 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 mountains figure.

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

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Competing Series

Soil series competing with MONDAMIN 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 MONDAMIN 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 MONDAMIN 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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Soil series sharing subgroup-level classification with MONDAMIN, 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 MONDAMIN 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
Mondamin silty clay loam, 0 to 2 percent slopesC420A35231150602w436nd01319911:24000
Mondamin silty clay loam, 0 to 2 percent slopesC420A772931150612w436nd01519671:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B172031150672w437nd01519671:20000
Mondamin silty clay loam, 6 to 9 percent slopesC420C36031150752yxj4nd01519671:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A7631150622w436nd04319851:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B1031150692w437nd04719921:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B126331150702w437nd05119921:24000
Mondamin silty clay loam, 0 to 2 percent slopesC420A52431150632w436nd05119921:24000
Mondamin silty clay loam, 2 to 6 percent slopesC420B23731150712w437nd05519741:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A131150642w436nd05519741:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A329531150652w436nd06119881:24000
Mondamin silty clay loam, 2 to 6 percent slopesC420B22031150722w437nd06119881:24000
Mondamin silty clay loam, 2 to 6 percent slopesC420B1831150732w437nd08319901:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A129031150662w436nd10519931:24000
Mondamin silty clay loam, 0 to 2 percent slopes2355231339066cctmnd10519931:24000
Mondamin silty clay loam, 2 to 6 percent slopesC420B1031150742w437nd10519931:24000
Mondamin silty clay loam, 0 to 2 percent slopesC420A764727986002w436sd04519731:20000
Mondamin-Heil complex, 0 to 2 percent slopesC430A330727985942rrqdsd04519731:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B315227986012w437sd04519731:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A140027986702w436sd04919811:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B50627986712w437sd04919811:20000
Mondamin silty clay loam, 0 to 2 percent slopesMoA392355182cxlhsd04919811:20000
Mondamin silty clay loam, 2 to 6 percent slopesMoB278355183cxljsd04919811:20000
Mondamin silty clay loam, gently slopingMyB569352653ctyxsd05919591:20000
Mondamin silty clay loam, 0 to 2 percent slopesC420A48127987692w436sd08919801:20000
Mondamin silty clay loam, 2 to 6 percent slopesC420B7527987702w437sd08919801:20000

Map of Series Extent

Approximate geographic distribution of the MONDAMIN 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 .