Official Series Description


Lab Data Summary

Aggregate lab data for the REYBOLD soil series. This aggregation is based on all pedons with a current taxon name of REYBOLD, 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 REYBOLD 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
149A95P0263S1994MD003013Reybold7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0536118,-76.6736145
153C40A416957DE001001Reybold5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2705002,-75.632225
153C93P027592DE003002Reybold6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5122223,-75.6327744
153C95P0545S95DE003004Reybold7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.434166,-75.7030563
n/a80P0130S1979VA001001Reybold6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the REYBOLD 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 REYBOLD 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 REYBOLD 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 REYBOLD 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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Competing Series

Soil series competing with REYBOLD 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 REYBOLD 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 REYBOLD 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 flats position figure.

Soil series sharing subgroup-level classification with REYBOLD, 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 REYBOLD 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
Reybold silt loam, 0 to 2 percent slopesReA89816086831qzz0de00120061:24000
Reybold silt loam, 2 to 5 percent slopesReB60816088541r04jde00120061:24000
Reybold-Queponco complex, 0 to 2 percent slopesRdA19116086851qzz2de00120061:24000
Reybold silt loam, 2 to 5 percent slopesReB2367924798212p7g7de00320091:24000
Reybold silt loam, 5 to 10 percent slopesReC502824798222p7g8de00320091:24000
Reybold-Queponco complex, 0 to 2 percent slopesRdA488224798192p7g5de00320091:24000
Reybold silt loam, 0 to 2 percent slopesReA326424798202p7g6de00320091:24000
Leipsic-Reybold complex, 2 to 5 percent slopesLfB267624797752p7drde00320091:24000
Leipsic-Reybold complex, 0 to 2 percent slopesLfA44124797742p7dqde00320091:24000
Reybold silt loam, 2 to 5 percent slopesReB27724406562mxpvmd01520091:12000
Reybold silt loam, 5 to 10 percent slopesReC7124406572mxpwmd01520091:12000
Reybold silt loam, 0 to 2 percent slopesReA6824406552mxptmd01520091:12000
Reybold silt loam, 2 to 5 percent slopesRsB105316086071qzwkmd01720071:12000
Reybold loam, gravelly subsoil, 0 to 2 percent slopesRgA72016086261qzx5md01720071:12000
Reybold silt loam, 0 to 2 percent slopesRsA59216086061qzwjmd01720071:12000
Reybold loam, gravelly subsoil, 2 to 5 percent slopesRgB54016086271qzx6md01720071:12000
Reybold silt loam, 5 to 10 percent slopesRsC35516086081qzwlmd01720071:12000
Reybold silt loam, 2 to 5 percent slopesReB2627026331r04jmd02919781:15840
Matapeake fine sandy loam, 2 to 5 percent slopes moderately erodedMmB2142512833149jqmd03719751:20000
Matapeake fine sandy loam, 0 to 2 percent slopesMmA101012833049jpmd03719751:20000
Matapeake fine sandy loam, 0 to 2 percent slopesMeA10241293354bl3md04719951:12000
Matapeake fine sandy loam, 2 to 5 percent slopesMeB6231293374bl5md04719951:12000

Map of Series Extent

Approximate geographic distribution of the REYBOLD 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 .