Official Series Description


Lab Data Summary

Aggregate lab data for the PETRIE soil series. This aggregation is based on all pedons with a current taxon name of PETRIE, 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 PETRIE 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
58B83P063483WY025009Petrie8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5969429,-106.5669479

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PETRIE 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 PETRIE 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 PETRIE 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 PETRIE 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 PETRIE 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 PETRIE 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 PETRIE 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 mountains figure.

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Soil series sharing subgroup-level classification with PETRIE, 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 PETRIE 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
Petrie clay loam, 0 to 3 percent slopes1365303349216cqd1wy01119781:24000
Bahl-Petrie complex, 0 to 3 percent slopes107119523495272wcbpwy02719931:24000
Petrie clay loam, 0 to 3 percent slopes7617158349483cqnnwy04519841:24000
Petrie-Ustic Torriorthents complex, saline, 0 to 6 percent slopes7715142349484cqnpwy04519841:24000
Bahl-Petrie complex, 0 to 3 percent slopes1533116148382wcbpwy04519841:24000
Petrie-Bone-Absted complex, 0 to 6 percent slopesPE133693509012yv7qwy61919711:24000
Petrie silty clayPc1216350909cs4nwy61919711:24000
Silhouette-Petrie clay loams, 1 to 6 percent slopes2782298169222wlrtwy61919711:24000
Petrie-Zigweid complex, wet, 0 to 3 percent slopes23526816847wdzxwy61919711:24000
Petrie-Arvada complex, 0 to 6 percent slopes236188168482wlrpwy61919711:24000
Orella, dry-Cadoma-Petrie clay loams, 3 to 30 percent slopes227399335023442xtvlwy62519851:24000
Petrie-Arvada complex, 0 to 6 percent slopes236294765023622wlrpwy62519851:24000
Petrie clay loam, 0 to 3 percent slopes234226715023582yrxzwy62519851:24000
Silhouette-Petrie clay loams, 1 to 6 percent slopes278189725024142wlrtwy62519851:24000
Petrie-Zigweid complex, wet, 0 to 3 percent slopes2353825502360jvr5wy62519851:24000

Map of Series Extent

Approximate geographic distribution of the PETRIE 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 .