Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43B89P0769TSW12/89AFritz6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.761525,-110.5131972
43B89P0765TSW6/89DFritz7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7432028,-110.5257361

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FRITZ 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 FRITZ 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 FRITZ 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 FRITZ 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 FRITZ 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 FRITZ 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 FRITZ 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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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 FRITZ, 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 FRITZ 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
Fritz gravelly silt loam, 4 to 30 percent slopes113044323907551hdid7031:24000
PIFL2/LEKI2 Fritz-PSMEG/JUCO6 Juliette association, 40 to 70 percent slopes112923022322132dxswid75219991:24000
Juliette-Fritz association, 40 to 70 percent slopes11299908515039251hcid75819981:24000
Gany-Fritz association, 40 to 70 percent slopes11066787915038451h3id75819981:24000
Lagall-Povey-Fritz complex, 35 to 70 percent slopes12196433915041051hyid75819981:24000
Gany-Katpa-Fritz complex, 40 to 70 percent slopes11723222915040551hsid75819981:24000
Fritz gravelly silt loam, 4 to 30 percent slopes1130886415039351hdid75819981:24000
Blackhorse-Fritz-Latigo complex, 5 to 40 percent slopes12702107028093272mnqkid75819981:24000
Fritz, stony-Katpa-Sheege complex, 30 to 70 percent slopes1273856228093432mp6wid75819981:24000
Zeebar-Windicreek-Fritz complex, 1 to 40 percent slopes1274337928093452mp73id75819981:24000
Fritz-Zeale complex, 25 to 75 percent slopes1273121728093392mp6gid75819981:24000
Fritz-Adek complex, 20 to 60 percent slopes127355928093422mp6sid75819981:24000
Fritz, stony-Katpa-Sheege complex, 30 to 70 percent slopes12738265624334652mp6wid76120181:24000
Blackhorse-Fritz-Latigo complex, 5 to 40 percent slopes12702238924329902mnqkid76120181:24000
Fritz-Zeale complex, 25 to 75 percent slopes12731176624334522mp6gid76120181:24000
Zeebar-Windicreek-Fritz complex, 1 to 40 percent slopes12743101324334722mp73id76120181:24000
Fritz, stony-Rock outcrop complex, 2 to 20 percent slopes1274284724334692mp70id76120181:24000
Fritz-Windicreek complex, 1 to 4 percent slopes1272580624331172mnvnid76120181:24000
Fritz-Juliette association, 40 to 70 percent slopes112965728430312szlrid76120181:24000
Fritz-Adek complex, 20 to 60 percent slopes1273512224334622mp6sid76120181:24000
ABLA/ACGL Gany-ABLA/THOC Katpa-PSMEG/BERE,SYOR2 Fritz complex, 40 to 70 percent slopes1501299837192t3mid76219881:24000
Fritz gravelly silt loam, 4 to 30 percent slopes742123772542ksqmwy66619781:24000

Map of Series Extent

Approximate geographic distribution of the FRITZ 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 .