Official Series Description


Lab Data Summary

Aggregate lab data for the REINACH soil series. This aggregation is based on all pedons with a current taxon name of REINACH, 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 REINACH 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
80A88P045888OK047003Reinach4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5522232,-97.8741684
80A88P045988OK047004Reinach4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.55229,-97.87408

Water Balance

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

There are insufficient data to create the 2D hillslope position figure.

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

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

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with REINACH 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 REINACH series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the REINACH 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 REINACH, 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. OK-2012-02-16-32 | Garfield County - October 1967

    Typical pattern of soils in the Grant-Pond Creek association, and Port, Reinach, and Pulaski soils of soil association 2 on the bordering flood plains (Soil Survey of Garfield County, Oklahoma; October 1967).

  2. OK-2012-02-16-50 | Hughes County - December 1968

    Typical pattern of soils in associations 4 and 5 (Soil Survey of Hughes County, Oklahoma; December 1968).

  3. OK-2012-02-17-05 | Logan County - June 1960

    Soils of central and western Logan County on recent alluvium and on loams and sands of Quaternary age. Red beds are exposed in the upper right corner (Soil Survey of Logan County, Oklahoma; June 1960).

  4. OK-2012-02-17-12 | Major County - October 1968

    Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  5. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

Map Units

Map units containing REINACH 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
Dale and Reinach silt loams, rarely flooded6236152114440031kglrks17319761:24000
Dale and Reinach silt loams, rarely flooded62363107914446401kh89ks19119741:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedRa161823814412tp6jok00319711:24000
Reinach silt loam, 0 to 1 percent slopes, rarely floodedRhA119333819192tp6kok01519671:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedRa63763819752tp6jok01719721:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedRa22313822942tp6jok03719521:24000
Reinach silt loam, 0 to 1 percent slopes, rarely flooded4384413826642tp6kok05119751:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely flooded47114983827372tp6jok05319831:24000
Reinach loam, 0 to 1 percent slopes, rarely floodedRcA15486383361dvxhok07119651:24000
Reinach loam, 0 to 1 percent slopes, rarely floodedRe840383474dw14ok07519731:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedRa52603838542tp6jok09319651:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedReiA2493841082tp6jok10319941:24000
Reinach silt loam, 0 to 1 percent slopes, rarely flooded4273863850282tp6kok14919761:24000
Reinach very fine sandy loam, 0 to 1 percent slopes, rarely floodedReiA27873852272tp6jok15119951:24000

Map of Series Extent

Approximate geographic distribution of the REINACH 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 .