Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5UCD725300972-CA-53-009xPARDALOE3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7003403,-122.9190598
579P027879CA045002Pardaloe6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0120926,-123.4247055
584P015983CA105007PARDALOE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8063889,-123.0813904
584P008783CA105012Pardaloe7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7755547,-123.0886078
584P054084CA105002PARDALOE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8038902,-123.078331

Water Balance

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

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 PARDALOE 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 PARDALOE 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 PARDALOE 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 PARDALOE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2011-05-27-03 | Mendocino County, Eastern Part, and Trinity County, Southwestern Part - 1991

    Pattern of active, metastable, and stable slopes (Soil Survey of Mendocino County, Eastern Part, and Trinity County, Southwestern Part, California; 1991).

Map Units

Map units containing PARDALOE 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
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd191wm16074622xkbnca09719681:20000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd41836226004452y4jjca60120111:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd416334701532xkbpca60120111:24000
PARDALOE-GOULDING COMPLEX, 50 TO 75 PERCENT SLOPES1864164466086hn01ca60619901:24000
PARDALOE-DEDRICK ASSOCIATION, 50 TO 75 PERCENT SLOPES1852378466085hn00ca60619901:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes, low ffd11101697331152832y4jgca68719851:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd17401563031152972y4jjca68719851:24000
Wohly-Casabonne-Pardaloe complex, 50 to 75 percent slopes2137133461098hgt4ca68719851:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes, high ffd11164024609962y4jcca68719851:24000
Pardaloe-Kekawaka-Casabonne complex, 50 to 75 percent slopes1723547461057hgrtca68719851:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd1730306731152962xkbpca68719851:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd17314254610582xkbnca68719851:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, high ffd17411744610592xk9wca68719851:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes, high ffd1219956631153092y4jcca69419931:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, high ffd19164444657682xkbnca69419931:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, high ffd19060684657662xk9wca69419931:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes, low ffd1210305031153082y4jgca69419931:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd1900239831153222y4jjca69419931:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes12112644656762xkbkca69419931:24000
Pardaloe-Woodin-Casabonne complex, 30 to 50 percent slopes, low ffd191080831153232xkbpca69419931:24000
Casabonne-Wohly-Pardaloe complex, 50 to 75 percent slopes, low ffd1110em20517011332y4jgca70119841:24000
Pardaloe-Goulding complex, 50 to 75 percent slopes186tw3378186883020qnvca70719831:24000
Pardaloe-Dedrick association, 50 to 75 percent slopes185tw608186882820qnsca70719831:24000
Pardaloe-Woodin complex, 50 to 75 percent slopes, low ffd1740me3127478492y4jjca70920101:24000

Map of Series Extent

Approximate geographic distribution of the PARDALOE 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 .