Official Series Description


Lab Data Summary

Aggregate lab data for the KUREB soil series. This aggregation is based on all pedons with a current taxon name of KUREB, 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 KUREB 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
152AS57_0471976-FL113-S57_047Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3982506,-87.0221939
152AS03_0051979-FL005-S03_005Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.2080173,-85.8442917
152AS66_0081979-FL131-S66_008Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3399754,-86.2012939
152AS46_0011985-FL091-S46_001Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3852501,-86.4167023
152AS19_0011986-FL037-S19_001Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.8503838,-84.6528168
152AS23_0131989-FL045-S23_013Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.6826916,-85.3681488
153AS16_0041974-FL031-S16_004Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3785324,-81.485527
153BS45_0191985-FL089-S45_019Kureb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.6498089,-81.4451447

Water Balance

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

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

Soil series sharing subgroup-level classification with KUREB, 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. FL-2011-05-31-12 | Nassau County - 1991

    Typical pattern of soils and parent material in an area of the Kureb-Fripp-Newhan and Mandarin-Echaw map units (Soil Survey of Nassau County, Florida; 1991).

  2. NC-2012-02-07-04 | Carteret County - September 1987

    Landscape position and seasonal high water table relationships are illustrated in uplands where the soils are sandy (Soil Survey of Carteret County, North Carolina; September 1987).

Map Units

Map units containing KUREB 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
Kureb sand, 0 to 5 percent slopes454983320833brvgfl00519821:20000
Otela limestone substratum-Chiefland-Kureb complex, 0 to 5 percent slopes91661614211411jpt8fl02919981:24000
Kureb sand, 2 to 5 percent slopes6296914211371jpt4fl02919981:24000
Kureb fine sand, 2 to 8 percent slopes29880738841sstlfl03119961:24000
Kureb fine sand, rolling, 8 to 20 percent slopes31420738843sstnfl03119961:24000
Kureb sand, 0 to 8 percent slopes773014253152ttl6fl03319981:24000
Kureb sand, 8 to 12 percent slopes177014253251jv57fl03319981:24000
Kureb fine sand, 3 to 8 percent slopes1943514770701ll0ffl03719901:20000
Kureb-Corolla complex, rolling48201414727681lfjnfl04519971:24000
Kureb-Resota fine sands, rolling3012151329184g9pfl08919891:15840
Kureb fine sand, 0 to 5 percent slopes86751329504gbqfl08919891:15840
Kureb sand, 0 to 8 percent slopes10361014446922ttl6fl09119891:20000
Kureb sand, 0 to 8 percent slopes2032808237672ttl6fl11319781:24000
Kureb sand, 0 to 8 percent slopes1640703239852ttl6fl13119851:20000
Kureb sand, hilly56190324028bw5jfl13119851:20000
Kureb sand, 1 to 8 percent slopesKuB160324591bwrpga03319821:20000
Kureb sand, 5 to 12 percent slopesKuC2850324770bwygga10719931:20000
Kureb sand, 5 to 12 percent slopesKuD2365325532bxr1ga61719761:20000
Kureb sand, 1 to 8 percent slopesKuB11811154963w5pnc01719831:24000
Kureb fine sand, 1 to 8 percent slopesKrB157691155423w75nc01919831:24000
Kureb sand, 0 to 6 percent slopesKuB47781155983w8znc03119841:24000
Kureb sand, 1 to 8 percent slopesKuB5411156503wbnnc04719861:24000
Kureb sand, 0 to 6 percent slopesKuB9161157533wfznc04919841:24000
Kureb sand, 1 to 8 percent slopesKuB954811113w70ync05119811:24000
Kureb sand, 1 to 8 percent slopesKr90851160403wr7nc12919741:15840
Kureb-Urban land complex, 1 to 8 percent slopesKu8881160413wr8nc12919741:15840
Kureb fine sand, 1 to 6 percent slopesKuB79821160823wslnc13319841:24000
Kureb fine sand, 2 to 6 percent slopesKuB35841161743wwknc14119861:24000

Map of Series Extent

Approximate geographic distribution of the KUREB 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 .