Official Series Description


Lab Data Summary

Aggregate lab data for the PORT BYRON soil series. This aggregation is based on all pedons with a current taxon name of PORT BYRON, 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 PORT BYRON 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
104X23-662-2S1972IA045003Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8661685,-90.879711
105X65977S1962IA065010Port Byron1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0657336,-91.8359847
105X45-620-1S1969IA089005Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4766671,-92.1666608
105UMN1129S1970MN0491129Port Byron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3553352,-93.008667
105UMN1220S1970MN0491220Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5031395,-92.6158447
105UMN1221S1970MN0491221Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5031395,-92.6159286
105UMN1736S1974MN1091736Port Byron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8654099,-92.321373
105UMN2075S1975MN055054Port Byron3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6613613,-91.5276281
105X3-620B-1S1984IA005008Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4942696,-91.3863839
108A84IL0110281984IL011028Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.553775,-89.5461667
108A84IL0110331984IL011033Port Byron2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5027278,-89.5300222
108B39IL1310021939IL131002Port Byron4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1084329,-90.8217087
108B83IL1310021983IL131002Port Byron1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0758333,-90.7986111
115C71IL1610031971IL161003Port Byron1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6131594,-90.192133
115C71IL1610061971IL161006Port Byron1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.440927,-90.7814024
115C83IL1310011983IL131001Port Byron1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0977778,-90.8433333

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PORT BYRON 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 PORT BYRON 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 PORT BYRON 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 PORT BYRON 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 PORT BYRON 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 PORT BYRON 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 PORT BYRON 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with PORT BYRON, 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-2011-06-01-09 | Bureau County - 1992

    Typical pattern of soils and parent material in the Waukegan-Sparta-Orio association (Soil Survey of Bureau County, Illinois; 1992).

  2. IL-2011-08-04-22 | Henry County - 1984

    Pattern of soils in the Seaton-Port Byron association (Soil Survey of Henry County, Illinois; 1984).

  3. IL-2011-08-04-25 | Henry County - 1984

    Pattern of soils in the Niota-Coyne-Denrock association (Soil Survey of Henry County, Illinois; 1984).

  4. IL-2011-08-04-72 | Mercer County - 1991

    Typical pattern of soils and parent material in the Seaton-Port Byron-Joy Association (Soil Survey of Mercer County, Illinois; 1991).

Map Units

Map units containing PORT BYRON 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
Port Byron silt loam, 2 to 5 percent slopes620B78115861771q7k0ia01720081:12000
Port Byron silt loam, 5 to 9 percent slopes, moderately eroded620C276815861781q7k1ia01720081:12000
Port Byron silt loam, 2 to 5 percent slopes620B1324747772p26jia02319781:15840
Port Byron silt loam, 5 to 9 percent slopes, moderately eroded620C21430404940flclia06919771:15840
Port Byron silt loam, 9 to 14 percent slopes, moderately eroded620D21110404941flcmia06919771:15840
Port Byron silt loam, 14 to 20 percent slopes, moderately erode620E2304404942flcnia06919771:15840
Port Byron silt loam, 5 to 9 percent slopes620C244404939flckia06919771:15840
Port Byron silt loam, 2 to 5 percent slopes620B19824747692p268ia06919771:15840
Port Byron silt loam, 9 to 18 percent slopes, severely eroded620E399406315fmsyia07519731:15840
Port Byron silt loam, 5 to 9 percent slopes, moderately eroded620C276406314fmsxia07519731:15840
Port Byron silt loam, 9 to 14 percent slopes, moderately eroded620D21646407673fp6ria09919751:15840
Port Byron silt loam, 14 to 18 percent slopes, moderately eroded620E21040407674fp6sia09919751:15840
Port Byron silt loam, 5 to 9 percent slopes, moderately eroded620C2658407672fp6qia09919751:15840
Port Byron silt loam, 18 to 25 percent slopes, moderately eroded620F2293407675fp6tia09919751:15840
Port Byron silt loam, 2 to 5 percent slopes277B2727849308xhs1il01520051:12000
Port Byron silt loam, 5 to 10 percent slopes277C1737849309xhs2il01520051:12000
Port Byron silt loam, 5 to 10 percent slopes, eroded277C2690849310xhs3il01520051:12000
Port Byron silt loam, 2 to 5 percent slopes277B59314016351j1j1il07120051:12000
Port Byron silt loam, 5 to 10 percent slopes, eroded277C213514050941j53mil07120051:12000
Port Byron silt loam, 5 to 10 percent slopes, eroded277C294824468586m2il07320011:12000
Port Byron silt loam, 2 to 5 percent slopes277B94924497886xjil13120001:12000
Port Byron silt loam, 5 to 10 percent slopes277C5924497986xkil13120001:12000
Port Byron silt loam, 2 to 5 percent slopes277B8244793055vm7fil19520031:12000
Port Byron silt loam, 5 to 10 percent slopes277C318793056vm7gil19520031:12000
Port Byron silt loam, 2 to 6 percent slopes285B2154396825f9xtmn03719801:15840
Port Byron silt loam, 0 to 2 percent slopes285A332396824f9xsmn03719801:15840
Port Byron silt loam, 6 to 12 percent slopes285C213396826f9xvmn03719801:15840
Port Byron silt loam, 2 to 6 percent slopesN591B872117116182wtrcmn04920071:12000
Port Byron-Dinsmore complex, 2 to 6 percent slopesN643B414417130721vhldmn04920071:12000
Port Byron silt loam, 6 to 12 percent slopes, moderately erodedN591C2109117116172wtrdmn04920071:12000
Port Byron silt loam, 0 to 2 percent slopesN591A91616701202wtrbmn04920071:12000
Port Byron-Dinsmore complex, 6 to 12 percent slopes, moderately erodedN643C246517130731vhlfmn04920071:12000
Port Byron silt loam, 2 to 6 percent slopes285B9304296382wtrcmn13119961:12000
Port Byron silt loam, 0 to 2 percent slopes285A1424296372wtrbmn13119961:12000
Port Byron silt loam, 6 to 12 percent slopesPrC5485753563t94hwi02519721:15840
Port Byron silt loam, chert substratum, 2 to 6 percent slopes, moderately eroded261B22225615282m8g9wi05719871:12000
Port Byron silt loam, 6 to 12 percent slopes, moderately eroded270C267025177832wtrdwi10320021:12000
Port Byron silt loam, 2 to 6 percent slopes270B241225177942wtrcwi10320021:12000
Port Byron silt loam, 2 to 6 percent slopesPoB774422176g59lwi10919751:15840
Port Byron silt loam, 12 to 20 percent slopesPoD365422178g59nwi10919751:15840
Port Byron silt loam, 6 to 12 percent slopesPoC319422177g59mwi10919751:15840
Port Byron silt loam, 6 to 12 percent slopes, moderately eroded270C288926395572wtrdwi12119691:12000
Port Byron silt loam, chert substratum, 2 to 6 percent slopes, moderately eroded261B236024212022m8g9wi12319651:12000
Port Byron silt loam, 0 to 2 percent slopes270A7524212162wtrbwi12319651:12000

Map of Series Extent

Approximate geographic distribution of the PORT BYRON 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 .