Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with FRANCISCAN 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 FRANCISCAN 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 FRANCISCAN 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 FRANCISCAN, 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 FRANCISCAN 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
Franciscan gravelly sandy loam, 30 to 50 percent slopes704fw6216126221r422ca03119801:24000
Hentine-Franciscan-Rock outcrop complex, 30 to 65 percent slopes774fw9042562653hp2cca06919651:20000
Franciscan sandy loam, 50 to 70 percent slopes, MLRA 15187wm3032519312wp4vca06919651:20000
Gonzaga-Honker-Franciscan complex, 30 to 50 percent slopes, MLRA 1516481304620562wv8jca07719901:24000
Gonzaga-Honker-Franciscan complex, 50 to 75 percent slopes, MLRA 1516537654620572wv8kca07719901:24000
Gonzaga-Franciscan complex, 30 to 50 percent slopes1633655462055hht0ca07719901:24000
Gonzaga-Honker-Franciscan complex, 50 to 75 percent slopes, MLRA 15165414566422wv8kca60919631:20000
Gonzaga-Franciscan complex, 30 to 50 percent slopes16336456643hb5fca60919631:20000
Gonzaga-Honker-Franciscan complex, 50 to 75 percent slopes, MLRA 15601276954669832wv8kca64219981:24000
Gonzaga-Honker-Franciscan complex, 30 to 50 percent slopes, MLRA 15600140654669822wv8jca64219981:24000
Franciscan-Quinto-Honker complex, 50 to 75 percent slopes, MLRA 15625104404669912tz11ca64219981:24000
Franciscan sandy loam, 50 to 70 percent slopes, MLRA 1562023404669902wp4vca64219981:24000
Hytop-Franciscan-Vallecitos complex, 50 to 75 percent slopes7001485467007hnyrca64219981:24000
Gonzaga-Honker-Franciscan complex, 50 to 75 percent slopes, MLRA 15601ws2916996432wv8kca64619671:24000
Gonzaga-Honker-Franciscan complex, 30 to 50 percent slopes, MLRA 15600ws1096994242wv8jca64619671:24000
Franciscan-Quinto-Honker complex, 50 to 75 percent slopes, MLRA 15625ws846996512tz11ca64619671:24000
Franciscan sandy loam, 50 to 70 percent slopes, MLRA 15187wm188170762wp4vca64619671:24000
Franciscan-Quinto-Honker complex, 50 to 75 percent slopes, MLRA 15188107604628402tz11ca64719841:24000
Franciscan-Rock outcrop complex, 30 to 50 percent slopes1893300462841hjmcca64719841:24000
Franciscan sandy loam, 50 to 70 percent slopes, MLRA 1518728504628392wp4vca64719841:24000
Hentine-Franciscan-Rock outcrop complex, 30 to 65 percent slopes7743578467119hp2cca65320001:24000
Franciscan gravelly sandy loam, 30 to 50 percent slopes704916467136hp2xca65320001:24000

Map of Series Extent

Approximate geographic distribution of the FRANCISCAN 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 .