Official Series Description


Lab Data Summary

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

Soil series competing with CALPAC 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 CALPAC 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 CALPAC 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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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 CALPAC, 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 CALPAC 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
Calpac-Ireland extremely bouldery surface-Ricrest complex, 10 to 45 percent slopes10202732389502mgkkid71019681:24000
Ireland-Calpac association, 30 to 60 percent slopes51-O6831732622v06zid71119831:24000
Hymas-Calpac-Ireland association, 30 to 70 percent slopes45-O5431733192v06yid71220081:24000
Hymas-Calpac-Ireland association, 30 to 70 percent slopes45-O140426198792v06yid7131:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes702053230938832x3mqid7131:24000
Ireland-Calpac association, 30 to 60 percent slopes5152326198802v06zid7131:24000
Ireland-Laschance-Calpac complex, 30 to 65 percent slopes702627429810742yvffid7131:24000
Calpac-Dranburn complex, 15 to 35 percent slopes89522329638682wv2sid7131:24000
Ireland-Calpac-Laschance complex, 15 to 45 percent slopes702519029810652yvfdid7131:24000
Dranburn-Dranyon-Calpac complex, 15 to 50 percent slopes706017730938842xxdmid7131:24000
Ireland-Calpac association, 30 to 60 percent slopes512261431635952v06zid71519941:24000
Hymas-Calpac-Ireland association, 30 to 70 percent slopes451115631635942v06yid71519941:24000
Hondoho-Calpac-Lizdale association, 30 to 70 percent slopes408457485634j9bmid71519941:24000
Calpac-Ridgecrest-Ireland association, 40 to 70 percent slopes178290485608j99sid71519941:24000
Povey-Ireland-Calpac association, 30 to 70 percent slopes927769485691j9dgid71519941:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes7020697429897282x3mqid7161:24000
Pavohroo-Ricafied-Calpac complex, 15 to 55 percent slopes2510565326404301im40id7161:24000
Ireland-Calpac-Laschance complex, 15 to 45 percent slopes7025437631568322yvfdid7161:24000
Dranburn-Dranyon-Calpac complex, 15 to 50 percent slopes7060412530740382xxdmid7161:24000
Calpac-Ireland extremely bouldery surface-Ricrest complex, 10 to 45 percent slopes1020308424270692mgkkid7161:24000
Hades-Calpac-Buist complex, 12 to 35 percent slopesBME2175599984n4bbid7161:24000
Dranburn-Calpac-Cedarhill complex, 15 to 50 percent slopes3250194324954752pt1tid7161:24000
Ireland-Calpac-Whitetop complex, 8 to 45 percent slopesJWC131231756352z43vid7161:24000
Ireland-Laschance-Calpac complex, 30 to 65 percent slopes702675331568332yvffid7161:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes7020134132389952x3mqid77019681:24000
Ireland-Calpac-Laschance complex, 15 to 45 percent slopes702572732389092yvfdid77019681:24000
Calpac-Lundy complex, 30 to 70 percent slopesCcF2331482477j61sut60819811:24000
Calpac-Agassiz complex, 30 to 70 percent slopesCbF1886482476j61rut60819811:24000

Map of Series Extent

Approximate geographic distribution of the CALPAC 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 .