Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with RIZZO 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 RIZZO 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 RIZZO 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 RIZZO, 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 RIZZO 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
Chemehuevi extremely gravelly loam-Rizzo occasionally flooded complex, 2 to 8 percent slopes4042763344153831hlzca68119681:24000
Rizzo complex, 2 to 8 percent slopes, frequently and very rarely flooded2408297344154031hm4ca68119681:24000
Rizzo-Rizzo, occasionally flooded complex, 2 to 8 percent slopes2403149022176082dflrca79420121:24000
Rizzo complex, 2 to 8 percent slopes2402146724844212pd7mca79420121:24000
Rizzo association, 4 to 15 percent slopes, rubbly1504116625081852pz5rca79420121:24000
Deprave-Rockhound-Rizzo complex, 2 to 4 percent slopes2090114024843832qb11ca79420121:24000
Rizzo-Chemwash-Carsitas complex, 4 to 8 percent slopes2409113024548232ndfvca79420121:24000
Rizzo complex, 2 to 8 percent slopes, channeled2404109024506082n81wca79420121:24000
Rizzo-Deprave complex, 2 to 8 percent slopes212072125174112qb1bca79420121:24000
Rizzo complex, 2 to 8 percent slopes, frequently and very rarely flooded2408297344165731hm4ca79420121:24000
Rizzo complex, 8 to 15 percent slopes244026925081872pz5qca79420121:24000
Rizzo very cobbly coarse sandy loam, 4 to 15 percent slopes, rubbly212120325081882pz5tca79420121:24000
Rizzo-Carsitas complex, 0 to 5 percent slopes1652454953441620307zdca8031:24000
Chemehuevi extremely gravelly loam-Rizzo occasionally flooded complex, 2 to 8 percent slopes40438377344165331hlzca8031:24000
Chemehuevi-Rizzo-Emptygun complex, 2 to 30 percent slopes201020318186073420g7pca8031:24000
Emptygun-Rizzo complex, 2 to 8 percent slopes20AA199823441623319ftca8031:24000
Rizzo-Carsitas complex, 2 to 8 percent slopes15FA1702634416132y0msca8031:24000
Snaggletooth-Rizzo association, 1 to 8 percent slopes202010762186073620g7rca8031:24000
Rizzo-Carsitas complex, 0 to 10 percent slopes165094633441619307zbca8031:24000
Rizzo association, 2 to 4 percent slopes, rarely flooded106821925355382qptqca8031:24000
Rizzo-Chemwash association, 2 to 8 percent slopes24005810186073920g7vca8031:24000
Havasulake-Rizzo association, 1 to 8 percent slopes2050580824315102mm5tca8031:24000
Rizzo-Lithic Torriorthents-Emptygun association, 8 to 75 percent slopes15025263186073020g7kca8031:24000
Rizzo-Rositas-Lagunita very rarely flooded complex, 0 to 15 percent slopes15DD508534416172ywzxca8031:24000
Rizzo-Carsitas complex, 1 to 4 percent slopes, rarely flooded, loamy substratum15FS435434416142ywztca8031:24000
Rizzo extremely gravelly fine sandy loam, 2 to 8 percent slopes15003163186072820g7hca8031:24000
Rizzo complex, 2 to 8 percent slopes, channeled2404313925354872n81wca8031:24000
Rizzo complex, 2 to 8 percent slopes, frequently and very rarely flooded24083126344165831hm4ca8031:24000
Rizzo complex, 2 to 8 percent slopes2402292625354862pd7mca8031:24000
Deprave-Rockhound-Rizzo complex, 2 to 4 percent slopes2090261925354772qb11ca8031:24000
Rizzo association, 4 to 15 percent slopes, rubbly1504232525354672pz5rca8031:24000
Rizzo association, dry, 2 to 4 percent slopes2415161524090852lvvfca8031:24000
Rizzo-Chemwash association, eroded, 2 to 8 percent slopes24011068186074020g7wca8031:24000
Rizzo-Chemwash-Carsitas complex, 4 to 8 percent slopes240998125081922ndfvca8031:24000
Rizzo association, 2 to 8 percent slopes1503915186073120g7lca8031:24000
Rizzo complex, 8 to 15 percent slopes244090525081932pz5qca8031:24000
Rizzo gravelly loamy sand, 30 to 75 percent slopes1501560186072920g7jca8031:24000
Rizzo very gravelly loam, 2 to 8 percent slopes241650424315042mm5mca8031:24000
Rizzo extremely gravelly loamy sand, 2 to 8 percent slopes150640525354602qpt0ca8031:24000
Rizzo-Deprave complex, 2 to 8 percent slopes212030425354822qb1bca8031:24000
Rizzo very cobbly coarse sandy loam, 4 to 15 percent slopes, rubbly212122425081942pz5tca8031:24000
Rizzo extremely gravelly sandy loam, 2 to 8 percent slopes24177924315072mm5qca8031:24000

Map of Series Extent

Approximate geographic distribution of the RIZZO 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 .