Official Series Description


Lab Data Summary

Aggregate lab data for the RASALO soil series. This aggregation is based on all pedons with a current taxon name of RASALO, 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 RASALO 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 RASALO 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 RASALO 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 RASALO 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 RASALO 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.

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

Competing Series

Soil series competing with RASALO 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 RASALO 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 RASALO 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 RASALO, 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 RASALO 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
Rasalo-Enott complex, 15 to 25 percent slopesReD2005929739302wx2mnc03320161:24000
Rasalo-Enott complex, 8 to 15 percent slopesReC1193929739322wx2pnc03320161:24000
Rasalo-Enott complex, 2 to 8 percent slopesReB612029739312wx2nnc03320161:24000
Rasalo-Zion complex, 2 to 6 percent slopesRaB7424313262mlzwnc03519691:15840
Rasalo fine sandy loam, 2 to 8 percent slopesRaB1250824245542mcyfnc05919881:24000
Rasalo fine sandy loam, 8 to 15 percent slopesRaC128524245552mcygnc05919881:24000
Rasalo fine sandy loam, 2 to 15 percent slopes, very stonyRcC35824245562mcyhnc05919881:24000
Rasalo fine sandy loam, 6 to 10 percent slopesRaC251024335232mp8rnc06719701:15840
Rasalo fine sandy loam, 10 to 15 percent slopesRaD176024335242mp8snc06719701:15840
Rasalo fine sandy loam, 2 to 6 percent slopesRaB76724335202mp8nnc06719701:15840
Rasalo fine sandy loam, 2 to 6 percent slopesRaB35724330982mnv1nc08119751:20000
Rasalo fine sandy loam, 6 to 10 percent slopesRaC29124331002mnv3nc08119751:20000
Rasalo fine sandy loam, 10 to 15 percent slopesRaD15524331022mnv5nc08119751:20000
Rasalo clay loam, 6 to 10 percent slopes, moderately erodedRsC22624331132mnvjnc08119751:20000
Rasalo clay loam, 10 to 15 percent slopes, moderately erodedRsD22424330122mnr8nc08119751:20000
Rasalo-Udorthents complex, 6 to 15 percent slopes, gulliedRuD41224331092mnvdnc08119751:20000
Rasalo-Zion complex, 6 to 10 percent slopesRaC2924246832md2lnc09720111:12000
Rasalo-Zion complex, 2 to 6 percent slopesRaB1924246822md2knc09720111:12000
Rasalo fine sandy loam, 2 to 6 percent slopesRaB387924392882mw8qnc14519871:24000
Rasalo fine sandy loam, 6 to 10 percent slopesRaC169624392892mw8rnc14519871:24000
Rasalo-Halifax complex, 2 to 7 percent slopes33B79415874411q8vsva04920051:24000
Rasalo-Halifax complex, 7 to 15 percent slopes33C45815874421q8vtva04920051:24000
Rasalo-Spriggs complex, 15 to 45 percent slopes, very stony34E38315874431q8vvva04920051:24000
Spriggs-Rasalo complex, 8 to 15 percent slopes43C2663114728501lfm9va08320041:24000
Rasalo-Orange complex, 2 to 8 percent slopes40B1205514728441lfm3va08320041:24000
Spriggs-Rasalo complex, 15 to 25 percent slopes43D932014728511lfmbva08320041:24000
Spriggs-Rasalo complex, 2 to 8 percent slopes43B252614728491lfm8va08320041:24000

Map of Series Extent

Approximate geographic distribution of the RASALO 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 .