Official Series Description


Lab Data Summary

Aggregate lab data for the HEMCROSS soil series. This aggregation is based on all pedons with a current taxon name of HEMCROSS, 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 HEMCROSS 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
184P089284OR007003Hemcross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8925018,-123.4736099
191P093291OR067008Hemcross6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.573967,-123.3523254
192P0820S1992OR057100HEMCROSS6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2994461,-123.5372238
194P0063S1993OR057010HEMCROSS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2977791,-123.5444412
199P0177S1998OR003003Hemcross6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4583321,-123.5283356
199P0180S1998OR003006Hemcross6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4738884,-123.5022202
109N1166S2009OR071004Hemcross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3002167,-123.3832092
109N1171S2009OR071009Hemcross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2895126,-123.3581772
209N1168S2009OR071006Hemcross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3029594,-123.35186
209N1170S2009OR071008Hemcross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2990685,-123.3528519

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HEMCROSS 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 HEMCROSS 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 HEMCROSS 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 HEMCROSS 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 terrace figure.

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

Competing Series

Soil series competing with HEMCROSS 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 HEMCROSS 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 HEMCROSS 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.

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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.

Soil series sharing subgroup-level classification with HEMCROSS, 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 HEMCROSS 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
Hemcross-Klistan complex, 30 to 60 percent slopes845070852512vq1or00320041:24000
Formader-Hemcross complex, 3 to 35 percent slopes683212852592vq9or00320041:24000
Formader-Hemcross complex, 35 to 60 percent slopes692317852602vqbor00320041:24000
Klistan-Harslow-Hemcross complex, 5 to 30 percent slopes1031920852642vqgor00320041:24000
Hemcross-Klistan complex, 5 to 30 percent slopes831736852502vq0or00320041:24000
Formader-Klistan-Hemcross complex, 60 to 80 percent slopes70857852612vqcor00320041:24000
Hemcross-Klistan complex, 30 to 60 percent slopes26E112936086721bgor00719841:20000
Hemcross silt loam, 3 to 30 percent slopes25D61876086621bfor00719841:20000
Hemcross-Klistan complex, 30 to 60 percent slopes73E8426103221hsor00919831:20000
Hemcross silt loam, 3 to 30 percent slopes73D1256103121hror00919831:20000
Formader-Klistan-Hemcross complex, 60 to 80 percent slopes340G15514045931j4lgor05319771:20000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes43F831766720127xsor05720061:24000
Hemcross-Klistan complex, 30 to 60 percent slopes48E617526722127yfor05720061:24000
Hemcross-Klistan complex, 5 to 30 percent slopes48D128126721827ybor05720061:24000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes64G539617236491vvllor06719751:20000
Hemcross-Klistan complex, 30 to 60 percent slopes65F461317236511vvlnor06719751:20000
Hemcross-Klistan complex, 5 to 30 percent slopes65E243817236501vvlmor06719751:20000
Hemcross-Klistan complex, 30 to 60 percent slopes48E9523271119427yfor07119671:24000
Klistan-Harslow-Hemcross complex, 60 to 90 percent slopes43F5087271118927xsor07119671:24000
Hemcross-Klistan complex, 5 to 30 percent slopes48D3722271119327ybor07119671:24000
Hemcross-Klistan complex, 5 to 30 percent slopes370E114215111jq66or63719811:20000
Formader-Klistan-Hemcross complex, 60 to 80 percent slopes21H2407064628257sor63819901:20000
Formader-Hemcross complex, 35 to 60 percent slopes20G1116064627257ror63819901:20000
Formader-Hemcross complex, 3 to 35 percent slopes20E575564626257qor63819901:20000
Hemcross-Klistan complex, 3 to 30 percent slopes94E4546710427tnor64919941:24000
Klistan-Hemcross complex, 30 to 60 percent slopes127F15766319270bor64919941:24000

Map of Series Extent

Approximate geographic distribution of the HEMCROSS 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 .