Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with MUNDALITE 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 MUNDALITE 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 MUNDALITE 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.

Click the image to view it full size.

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 MUNDALITE, 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 MUNDALITE 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
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D51942900842xj3yny01919951:24000
Mundalite-Rawsonville-Ampersand complex, 3 to 15 percent slopes, rocky, very bouldery931C15932900832xj3xny01919951:24000
Mundalite-Ampersand complex, 0 to 15 percent slopes, very bouldery933C14392900852xj3tny01919951:24000
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D486663197972xj3yny03120071:24000
Mundalite-Ampersand complex, 15 to 35 percent slopes, very bouldery932D1681014608372xj3vny03120071:24000
Mundalite-Ampersand complex, 0 to 15 percent slopes, very bouldery932C981514608362xj3tny03120071:24000
Mundalite-Rawsonville complex, 35 to 60 percent slopes, rocky, very bouldery931F5676319798bqs2ny03120071:24000
Mundalite-Rawsonville-Ampersand complex, 3 to 15 percent slopes, rocky, very bouldery930C561814602282xj3xny03120071:24000
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very boulderyMwD28703197352xj3sny03120071:24000
Mundalite fine sandy loam, 8 to 15 percent slopes, very boulderyMuC10513197272xj3qny03120071:24000
Mundalite fine sandy loam, 15 to 35 percent slopes, very boulderyMuD8763197282xj3pny03120071:24000
Mundalite-Rawsonville complex, 3 to 15 percent slopes, rocky, very boulderyMwC4473197342xj3rny03120071:24000
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D1980919129242xj3yny03320181:24000
Mundalite-Rawsonville-Ampersand complex, 3 to 15 percent slopes, rocky, very bouldery930C275319132652xj3xny03320181:24000
Mundalite-Rawsonville complex, 35 to 60 percent slopes, rocky, very bouldery931F25431913274226xjny03320181:24000
Mundalite fine sandy loam, 15 to 35 percent slopes, very bouldery936D101425216452xj3wny03320181:24000
Mundalite-Ampersand complex, 0 to 15 percent slopes, very bouldery932C87219132732xj3tny03320181:24000
Mundalite-Ampersand complex, 15 to 35 percent slopes, very bouldery932D13426794672xj3vny03320181:24000
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D1563199932xj3yny03520071:24000
Mundalite-Rawsonville complex, 35 to 60 percent slopes, rocky, very bouldery931F82319992bqzbny03520071:24000
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D553282919882xj3yny04119941:62500
Mundalite-Rawsonville-Ampersand complex, 3 to 15 percent slopes, rocky, very bouldery931C182222919872xj3xny04119941:62500
Mundalite-Ampersand complex, 0 to 15 percent slopes, very bouldery933C82102919902xj3tny04119941:62500
Mundalite-Rawsonville complex, 35 to 60 percent slopes, very bouldery931F68722919899sv0ny04119941:62500
Mundalite-Ampersand complex, 15 to 35 percent slopes, very bouldery933D58122919912xj3vny04119941:62500
Mundalite-Rawsonville complex, 15 to 35 percent slopes, rocky, very bouldery931D3165925182562xj3yny04320181:24000
Mundalite-Ampersand complex, 0 to 15 percent slopes, very bouldery932C1717825149732xj3tny04320181:24000
Mundalite-Rawsonville-Ampersand complex, 3 to 15 percent slopes, rocky, very bouldery930C1392125182572xj3xny04320181:24000
Mundalite fine sandy loam, 15 to 35 percent slopes, very bouldery936D53625216462xj3wny04320181:24000
Mundalite-Rawsonville complex, 35 to 60 percent slopes, rocky, very bouldery931F4432521633226xjny04320181:24000

Map of Series Extent

Approximate geographic distribution of the MUNDALITE 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 .