Official Series Description


Lab Data Summary

Aggregate lab data for the WIRT soil series. This aggregation is based on all pedons with a current taxon name of WIRT, 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 WIRT 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
108A88IL0450011988IL045001Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5440222,-87.6173139
108A83P0063S1982IL029026WIRT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4030571,-88.1597214
11380IL0490491980IL049049Wirt2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1894204,-88.5716603
11382IL0490031982IL049003Wirt2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1175769,-88.5834106
11382IL0490041982IL049004Wirt1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.151032,-88.5781438
11385IL1210261985IL121026Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.664825,-89.0247194
11386IL1210031986IL121003Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6852222,-89.0873333
114APM76931976IN133093Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.50525,-86.9220278
114A93P0499S1993IN119001Wirt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3527794,-86.9263916
114BDC77101977IN031010Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2290528,-85.5193167
114BRI78141978IN137014Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.168075,-85.0960778
114B90P004689IN143013Wirt5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7380562,-85.8455582
114B06N0332S2003IN079001Wirt6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0458336,-85.5280533
115AGN79331979IN055033Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9375639,-87.0835583
120BMT80141980IN101014Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.615325,-86.8469861
120BMT81021981IN101002Wirt3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.726525,-86.7704694

Water Balance

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

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Click the image to view it full size.

Competing Series

Soil series competing with WIRT 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 WIRT 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 WIRT 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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Click the image to view it full size.

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

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

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Soil series sharing subgroup-level classification with WIRT, 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. IL-2010-08-31-16 | Cumberland County - 2002

    Typical pattern of soils and parent material in the Holton-Wirt-Holly association (Soil Survey of Cumberland County, Illinois; 2002).

  2. IN-2010-09-24-13 | Owen County -

    Typical pattern of soils and parent materials in the Parke-Pike-Gallimore association (Soil Survey of Owen County, Indiana).

  3. IN-2010-09-24-14 | Owen County -

    Typical pattern of soils and parent materials in the Solsberry-Hickory-Ava association (Soil Survey of Owen County, Indiana).

  4. IN-2010-09-24-15 | Owen County -

    Typical pattern of soils and parent materials in the Zanesville-Tulip-Wellston and Crider-Haggatt associations (Soil Survey of Owen County, Indiana).

Map Units

Map units containing WIRT 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
Wirt silt loam, 0 to 2 percent slopes, frequently flooded3226A270523786722kv6cil00119971:12000
Wirt loam, 0 to 2 percent slopes, frequently flooded3226A296316074631qypnil02320061:12000
Wirt loam, sandy substratum, frequently flooded32262086210920628ssxil02519931:12000
Wirt silt loam, 0 to 2 percent slopes, frequently flooded3226A107614284171jyczil02920051:12000
Wirt silt loam, frequently flooded322618581748155vx6il03519921:15840
Wirt loam22640601734485th3il04919861:15840
Wirt silt loam, frequently flooded3226101733945tfcil05119911:15840
Wirt silt loam, 0 to 2 percent slopes, frequently flooded3226A915406051nq3yil08120051:12000
Wirt silt loam, 0 to 2 percent slopes, frequently flooded3226A20362027422261pqil12120081:12000
Wirt silt loam, 0 to 2 percent slopes, frequently flooded3226A31918407265jtil13319981:12000
Wirt silt loam, frequently flooded32263500179021608wil17319901:15840
Haymond-Wirt silt loams, 0 to 2 percent slopes, occasionally flooded, very brief durationHctAW106024645588g5in00520021:12000
Wirt loam, 0 to 2 percent slopes, frequently flooded, very brief durationWprAV305607358nd06in00520021:12000
Wirt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationWprAW26614543nmgzin00520021:12000
Wirt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationWprAW2613973nlwlin01920011:12000
Wirt loam, 0 to 2 percent slopes, frequently flooded, brief durationWprAH516525571sgm9in02519701:20000
Wirt loam, occasionally floodedWn22971623135fwxin04719841:15840
Wirt silt loam, sandy substratum, frequently floodedWr181601795cp2in05119861:15840
Wirt very fine sandy loam, frequently floodedWt14991615885f4jin05519841:15840
Wirt loam, 0 to 2 percent slopes, frequently flooded, very brief durationWprAV122201672dj89in07119851:15840
Wirt silt loam, occasionally floodedWt499196468911cv0in07719821:15840
Wirt silt loam, frequently floodedWz7497764011t9sin07719821:15840
Wirt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationWprAW676216514171sffjin07920101:12000
Wirt loam, 0 to 2 percent slopes, frequently flooded, very brief durationWprAV32624279312mhgcin07920101:12000
Wirt silt loam, 0 to 2 percent slopes, frequently flooded, brief durationWpuAH215186870620qjvin07920101:12000
Haymond-Wirt silt loams, 0 to 2 percent slopes, occasionally flooded, very brief durationHctAW5816527741sgv9in08119751:15840
Wirt loam, 0 to 2 percent slopes, frequently flooded, brief durationWprAH127316515131sfjmin09319821:15840
Wirt loam, 0 to 2 percent slopes, frequently flooded, brief durationWprAH233117081801vbhlin10119841:15840
Wirt silt loam, 0 to 2 percent slopes, frequently flooded, very brief durationWpuAV52331663765l3zin11919971:12000
Wirt-Pekin silt loams, 0 to 6 percent slopes, frequently flooded, very long durationWpyBJ7551663785l41in11919971:12000
Wirt silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationWpuAK5741663775l40in11919971:12000
Wirt loam, 0 to 2 percent slopes, rarely floodedWprAQ2911663755l3yin11919971:12000
Wirt loam, 0 to 2 percent slopes, frequently flooded, brief durationWprAH920535965kzq6in12319971:12000
Wirt silt loam, frequently floodedWt342014796551lnptin13719821:15840
Wirt loam, flaggy clay substratum, frequently floodedWr281514796541lnpsin13719821:15840
Wirt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationWprAW5561658425kkrin14319951:12000
Wirt silt loam, 0 to 2 percent slopes, frequently flooded, brief durationWpuAH2981658435kksin14319951:12000

Map of Series Extent

Approximate geographic distribution of the WIRT 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 .