Official Series Description


Lab Data Summary

Aggregate lab data for the WOODHURST soil series. This aggregation is based on all pedons with a current taxon name of WOODHURST, 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 WOODHURST 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
4713N57546S2012UT021001Woodhurst7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7475528,-112.7737139

Water Balance

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

Soil series competing with WOODHURST 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 WOODHURST 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 WOODHURST 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 WOODHURST, 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 WOODHURST 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
Woodhurst-Behanin deep families complex, 10 to 35 percent slopes.2752950470588hsp8ca70319831:24000
Woodhurst family-Cavemountain-Starley family, very stony surface, complex, 10 to 60 percent slopes9331231732752wv1lid71220081:24000
Woodhurst family-Ezbin complex, 25 to 65 percent slopes957131732772wv20id71220081:24000
Davtone-Sedgway-Woodhurst families, complex, 20 to 45 percent slopes10131027428994422w1fyid7131:24000
Woodhurst family-Parkay-Nielsen, very stony surface, complex, 30 to 70 percent slopes935577429638462wv1mid7131:24000
Woodhurst family-Ezbin complex, 25 to 65 percent slopes957389829638572wv20id7131:24000
Kingmine family, stony surface-Woodhurst family-Stringam, stony surface, complex, 30 to 65 percent slopes963349729682352wxbjid7131:24000
Davtone family-Moonlight-Woodhurst family, complex, 20 to 50 percent slopes990269029638752wv31id7131:24000
Woodhurst-Starley, stony surface, families, complex, 2 to 35 percent slopes945205829638522wv1vid7131:24000
Woodhurst family-Hourglass family-Ezbin complex, 30 to 65 percent slopes902158329638702wv2vid7131:24000
Woodhurst-Dailybasin families, complex, 3 to 30 percent slopes947139229638532wv1wid7131:24000
Woodhurst family-Cavemountain-Starley family, very stony surface, complex, 10 to 60 percent slopes933112629638452wv1lid7131:24000
Ediebench-Woodhurst families, complex, 20 to 60 percent slopes, extremely stony surface83914927334492slrlid7131:24000
Garlet-Dromedary-Woodhurst families, complex, 30 to 70 percent slopes2461382984238534gid7131:24000
Woodhurst-Dailybasin families, complex, 3 to 30 percent slopes94717231634772wv1wid7161:24000
Woodhurst-Swifton families, complex, mountain ridgetops102B548202403025y59id75819981:24000
Beeftrail-Marcetta-Woodhurst families, complex, gentle mountain slopes521E475202404325y5qid75819981:24000
Wander-Woodhurst-Philipsburg families, complex, gentle mountain slopes527C71202405025y5yid75819981:24000
Tiban-Raynesford-Woodhurst families, complex, gentle mountain slopes524E51202404425y5rid75819981:24000
Woodhurst stony loamWo36651474644yfxmt60219631:20000
Woodhurst-Spring creek stony complexWs25701474674yg0mt60219631:20000
Woodhurst-Alder stony complexWp25271474654yfymt60219631:20000
Woodhurst-Teton-Cheadle soilsWt10571474684yg1mt60219631:20000
Woodhurst-Loberg complexWr4691474664yfzmt60219631:20000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes38D20830395831hf4ymt60219631:20000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony38E7430395841hf54mt60219631:20000
Leavitt, stony-Poin, very stony-Woodhurst, extremely bouldery complex, 25 to 60 percent slopes240F3830395871r476mt60219631:20000
Tiban-Raynesford-Woodhurst families, complex, gentle mountain slopes524E280151486084zmtmt60520071:24000
Adel-Redchief-Woodhurst families, complex, gentle mountain slopes522E141481486024zmmmt60520071:24000
Adel-Wesdy-Woodhurst families, complex, landslide deposits704C90121487574zsmmt60520071:24000
Rooset-Woodhurst-Tiban families, complex, gentle mountain slopes523E48641492105087mt60520071:24000
Beeftrail-Marcetta-Woodhurst families, complex, gentle mountain slopes521E38851485974zmgmt60520071:24000
Woodhurst-Swifton families, complex, mountain ridgetops102B1843149001501hmt60520071:24000
Adel-Libeg-Woodhurst families, complex, alluvial-colluvial deposits611E16891487204zrfmt60520071:24000
Woodhurst-Philipsburg-Prudy families, complex, gentle mountain slopes523X132814929750c1mt60520071:24000
Midfork-Wetopa-Woodhurst families, complex, cirque basins2510T123614931250cjmt60520071:24000
Tiban-Tibson-Woodhurst families, complex, ice-margin slopes464X121714929350bxmt60520071:24000
Wander-Woodhurst-Philipsburg families, complex, gentle mountain slopes527C11601486214zn7mt60520071:24000
Wander-Woodhurst-Philipsburg families, complex, gentle mountain slopes527C729111074zn7mt61020051:24000
Woodhurst-Bullrey, very stony-Nieman, extremely stony complex, 2 to 25 percent slopes560E320424246192md0jmt61220111:24000
Butchhill, very stony-Hairpin, very stony-Woodhurst complex, 15 to 50 percent slopes351F206324250252mdfmmt61220111:24000
Woodhurst, very stony-Bullrey, very stony-Shadow, stony complex, 15 to 45 percent slopes560F88424246022mczzmt61220111:24000
Woodhurst-Philipsburg-Prudy families, complex, gentle mountain slopes523X117259776850c1mt61220111:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes38D9530397042pg61mt61319751:24000
Beeftrail-Marcetta-Woodhurst families complex, gentle mountain slopes521E1517079871vb9cmt62319881:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony38E1031768481hf54mt62420211:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes38D379324862942pg61mt6321:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony38E284223927562l9vpmt6321:24000
Bundo, extremely bouldery-Woodhurst, very bouldery-Rock outcrop complex, 15 to 45 percent slopes950F106824862782pg5jmt6321:24000
Leavitt, stony-Poin, very stony-Woodhurst, extremely bouldery complex, 25 to 60 percent slopes240F83424935141r476mt6321:24000
Woodhall-Woodhurst, very stony-Bavdark complex, 8 to 15 percent slopes38D807213830321hf4ymt63720141:24000
Woodhall-Woodhurst complex, 15 to 35 percent slopes, stony38E795713830381hf54mt63720141:24000
Bundo, extremely bouldery-Woodhurst, very bouldery-Rock outcrop complex, 15 to 45 percent slopes950F5677185869220d3tmt63720141:24000
Leavitt, stony-Poin, very stony-Woodhurst, extremely bouldery complex, 25 to 60 percent slopes240F428216127811r476mt63720141:24000
Tophat-Woodhurst, cobbly-Decross, complex, 2 to 20 percent slopes5434E5348741479swkpmt6691:24000
Boneville, stony-Woodhurst-Arrowpeak, very stony, complex, 25 to 60 percent slopes5658F2837741528swm8mt6691:24000
Dalys-Gilispie-Woodhurst complex, 4 to 15 percent slopes5403E234915646857tcmt6691:24000
Woodhurst-Winnemucca-Passar families, association, 8 to 45 percent slopes218625264nzmtut6491:24000
Woodhurst-Forsey families, association, 20 to 70 percent slopes215625267nzmxut6491:24000
Woodhurst-Idmon, stony-Passar families, association, 20 to 50 percent slopes216625266nzmwut6491:24000
Forsey-Woodhurst-Namon families, association, 25 to 65 percent slopes158625229nzlput6491:24000
Woodhurst family-Van Wagoner family-Rock outcrop complex, 30 to 70 percent slopes217625265nzmvut6491:24000
Woodhurst family-Parkay-Nielsen, very stony surface, complex, 30 to 70 percent slopes9352130834802wv1mwy62319711:20000
Woodhurst family-Ezbin complex, 25 to 65 percent slopes957430834862wv20wy62319711:20000
Odark, extremely stony-Woodhurst, very stony complex, 40 to 70 percent slopes760331709682z1zzwy6291:24000
Garlet-Dromedary-Woodhurst families, complex, 30 to 70 percent slopes24624033151976534gwy66320121:24000
Midfork-Mulgon-Woodhurst families, complex, 40 to 90 percent slopes2753689151984534qwy66320121:24000
Frisco-Fulcher-Woodhurst families, complex, 30 to 60 percent slopes4253452152039536hwy66320121:24000
Woodhurst family-Parkay-Nielsen, very stony surface, complex, 30 to 70 percent slopes93567830834512wv1mwy66320121:24000
Woodhurst-Starley, stony surface, families, complex, 2 to 35 percent slopes945330834532wv1vwy66320121:24000
Garlet-Dromedary-Woodhurst families, complex, 30 to 70 percent slopes24602925211534gwy7231:24000

Map of Series Extent

Approximate geographic distribution of the WOODHURST 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 .