Official Series Description


Lab Data Summary

Aggregate lab data for the HEMBRE soil series. This aggregation is based on all pedons with a current taxon name of HEMBRE, 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 HEMBRE 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
184P089684OR041002Hembre7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7236,-123.7055
110N0527S10OR071001Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2834816,-123.3676682
110N0528S10OR071002Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.282383,-123.3746643
110N0531S10OR071005Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2822762,-123.3740845
110N0532S10OR071006Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2829094,-123.3811264
110N0533S10OR071007Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2832527,-123.3806229
110N0534S10OR071008Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2832527,-123.3806229
110N0535S10OR071009Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2921982,-123.37883
110N0536S10OR071010Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2879601,-123.3756714
110N0537S10OR071011Hembre6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2841911,-123.372467

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HEMBRE 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 HEMBRE 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 HEMBRE 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 HEMBRE 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 hills figure.

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

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

Competing Series

Soil series competing with HEMBRE 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 HEMBRE 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 HEMBRE 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 hills figure.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with HEMBRE, 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. OR-2012-05-10-23 | Yamhill County - January 1974

    Pattern of typical soils of association 10 that are on the Coast Range (Soil Survey of Yamhill County, Oregon; January 1974).

Map Units

Map units containing HEMBRE 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
Hembre-Klickitat complex, 30 to 60 percent slopes25E12386096521fmor00919831:20000
Hembre-Klickitat complex, 3 to 30 percent slopes25D2926096421flor00919831:20000
Hembre gravelly silt loam, 3 to 25 percent slopes32D22416233822vxor05319771:20000
Hembre gravelly silt loam, 25 to 50 percent slopes32E11606233922vyor05319771:20000
Hembre gravelly silt loam, 50 to 75 percent slopes32F2856234022vzor05319771:20000
Hembre medial silt loam, 30 to 60 percent slopes420E26717227wvor05720061:24000
Hembre medial silt loam, 60 to 90 percent slopes420F26717127wtor05720061:24000
Hembre silt loam, 30 to 60 percent slopes20F83236144521y3or06719751:20000
Hembre silt loam, 3 to 30 percent slopes20E50646144421y2or06719751:20000
Hembre silt loam, 60 to 90 percent slopes20G15096144621y4or06719751:20000
Hembre silt loam, 30 to 60 percent slopesHBF107322711242230zor07119671:24000
Hembre silt loam, 3 to 30 percent slopesHBE81342711235230yor07119671:24000
Hembre silt loam, 60 to 90 percent slopesHBG248527112092310or07119671:24000
Hembre clay loam, 5 to 25 percent slopesHlD48414259911jvvqor60119681:20000
Formader-Hembre-Klickitat complex, 50 to 80 percent slopes50G26710626902378or63719811:20000
Hembre-Klickitat complex, 30 to 60 percent slopes55G349162698237jor63719811:20000
Hembre-Klickitat complex, 3 to 30 percent slopes55E253662697237hor63719811:20000
Hembre silt loam, 25 to 60 percent slopes54G163162696237gor63719811:20000
Hembre silt loam, 5 to 25 percent slopes54D134662695237for63719811:20000
Hembre silt loam, 3 to 35 percent slopes26E1025646412586or63819901:20000
Hembre silt loam, 35 to 60 percent slopes26G745646422587or63819901:20000

Map of Series Extent

Approximate geographic distribution of the HEMBRE 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 .