Official Series Description


Lab Data Summary

Aggregate lab data for the WAYDEN soil series. This aggregation is based on all pedons with a current taxon name of WAYDEN, 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 WAYDEN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5461ND08900361ND089003Wayden2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7605556,-103.1863889
5461ND089003A61ND089003AWayden2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7605556,-103.1863889
5478P014977ND001004Wayden7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1413879,-102.8899994
5440A283677ND025001Wayden5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.083568572998,-102.92862701416
5440A283777ND025002Wayden5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0032920837402,-102.693901062012

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WAYDEN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the WAYDEN series and siblings. 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 WAYDEN 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 .

Click the image to view it full size.

Click the image to view it full size.

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.

Competing Series

Soil series competing with WAYDEN share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the WAYDEN 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 WAYDEN 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 .

Click the image to view it full size.

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 WAYDEN, 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 WAYDEN 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
Doney-Cabba-Wayden complex, 25 to 70 percent slopes831F3055343700cjn3mt01719951:24000
Wayden-Barkof complex, 4 to 15 percent slopes218D1975342155ch18mt02519911:24000
Cabba-Wayden complex, 8 to 45 percent slopes412E677342224ch3hmt02519911:24000
Doney-Wayden complex, 15 to 60 percent slopes6739402342569chgmmt02719791:24000
Doney-Winifred-Wayden complex, 15 to 45 percent slopes7019626342573chgrmt02719791:24000
Cabba-Doney-Wayden complex, 4 to 8 percent slopes3713639342536chfkmt02719791:24000
Cabba-Wayden-Rock outcrop complex, 45 to 60 percent slopes388151342537chflmt02719791:24000
Cabba-Wayden-Doney complex, 15 to 35 percent slopes684E68269466021m3mmt02719791:24000
Wayden-Whitecow complex, 4 to 35 percent slopes695E16269466421m3gmt02719791:24000
Cabba-Wayden-Doney complex, 4 to 15 percent slopes684D3269465921m2rmt02719791:24000
Cabba-Wayden-Rock outcrop complex, 15 to 60 percent slopes201F5727344150ck3mmt05119921:24000
Cabba-Wayden complex, 4 to 15 percent slopes201D2737344148ck3kmt05119921:24000
Wayden-Castner complex, 8 to 45 percent slopes261F745344533ckhzmt06519961:24000
Doney-Wayden complex, 15 to 60 percent slopes284F186344546ckjdmt06519961:24000
Wayden-Windham complex, 4 to 25 percent slopes262E96344534ckj0mt06519961:24000
Kuro-Wayden-Rock outcrop complex, 4 to 35 percent slopes260F79344532ckhymt06519961:24000
Wayden clay loam, hillyWb224651469684xxxmt60019691:24000
Wayden-Shale outcrop complex, steepWD129881469574xxkmt60019691:24000
Wayden clay loam, undulatingWa75011469674xxwmt60019691:24000
Tanna-Wayden clay loams, rollingTh42621469484xx8mt60019691:24000
Wayden-Absher complex, undulatingWc33091469694xxymt60019691:24000
Wyola-Wayden clay loams, rollingSf12821469314xwqmt60019691:24000
Midnot-Wayden complex, 4 to 15 percent slopes668D107269467421m2qmt60219631:20000
Wayden-Sagedale silty clay loams, 25 to 60 percent slopesWaF911474554yfmmt60219631:20000
Doney-Wayden complex, hillyDOe80902345923clytmt60719701:24000
Wayden-Regent silty clay loams, hillyWI29665346216cm88mt60719701:24000
Wayden-Rock outcrop complex, rollingWL25159346218cm8bmt60719701:24000
Wayden silty clay loam, hillyWE17846346212cm84mt60719701:24000
Wyola-Wayden silty clay loams, 4 to 15 percent slopesSef11022346155cm69mt60719701:24000
Wayden-Rock outcrop complex, hillyWM10224346219cm8cmt60719701:24000
Wayden complex, hillyWO7568346221cm8fmt60719701:24000
Wayden silty clay loam, rollingWD6652346211cm83mt60719701:24000
Wayden-Arnegard complex, hillyWF6284346213cm85mt60719701:24000
Wayden-Grail complex, hillyWG6200346214cm86mt60719701:24000
Windham-Wayden complex, 15 to 35 percent slopesWW5717346225cm8kmt60719701:24000
Wayden-Judith silty clay loams, hillyWH4462346215cm87mt60719701:24000
Doney-Rock outcrop complex, very steepDOd4374345922clysmt60719701:24000
Wayden-Shale outcrop complex, very steepWN4357346220cm8dmt60719701:24000
Wayden-Wyola silty clay loams, rollingWK2667346217cm89mt60719701:24000
Wayden-Castner association, steepWD24579347183cn8gmt61119711:24000
Wayden-Cabba association, steepWC16449347182cn8fmt61119711:24000
Wayden-Cabba association, hillyWA7304347181cn8dmt61119711:24000
Wayden-Sagedale silty clay loams, 25 to 60 percent slopes621F13895346862cmy3mt61519921:24000
Sagedale-Wayden silty clay loams, 8 to 25 percent slopes621E6560346861cmy2mt61519921:24000
Zahill-Sagedale-Wayden complex, 15 to 45 percent slopes722F5119346899cmz9mt61519921:24000
Cabba-Wayden-Rock outcrop complex, 25 to 70 percent slopes201F2594346624cmpfmt61519921:24000
Cabba-Wayden-Doney complex, 4 to 15 percent slopes684D1894189517721m2rmt62420211:24000
Midnot-Wayden complex, 4 to 15 percent slopes668D1585189517621m2qmt62420211:24000
Wayden-Whitecow complex, 4 to 35 percent slopes695E911189519921m3gmt62420211:24000
Wayden silty clay loam, 4 to 25 percent slopes667E502189676321nqxmt62420211:24000
Cabba-Wayden-Doney complex, 15 to 35 percent slopes684E331189520421m3mmt62420211:24000
Winspect-Cabba-Wayden complex, 8 to 35 percent slopes443E97281478204ytdmt63019911:24000
Wayden-Cabba-Regent complex, 15 to 45 percent slopes679E82351478844ywgmt63019911:24000
Regent-Wayden-Cabba complex, 15 to 45 percent slopes479E52301478254ytkmt63019911:24000
Regent-Wayden complex, 8 to 35 percent slopes879E36841479274yxvmt63019911:24000
Wayden-Cabba-Rock outcrop complex, 15 to 60 percent slopes579E34161478604yvpmt63019911:24000
Castner-Wayden complex, moist, 15 to 60 percent slopes283F1964614985350xzmt63920001:24000
Wayden-Castner complex, 15 to 60 percent slopes331F1290814988550z0mt63920001:24000
Wayden-Castner-Cabba complex, 2 to 15 percent slopes262D1015714982550x2mt63920001:24000
Sinnigam-Wayden complex, moist, 15 to 45 percent slopes336E238014989350z8mt63920001:24000
Absarokee-Wayden complex, 2 to 8 percent slopes261C146814982450x1mt63920001:24000
Wayden-Castner-Rock outcrop complex, 25 to 60 percent slopes362F13091499205104mt63920001:24000
Wayden-Rock outcrop complex, 15 to 60 percent slopes286F80614985750y3mt63920001:24000
Wayden-Doney complex, 2 to 8 percent slopes260C43114982350x0mt63920001:24000
Wayden-Amherst-Winifred complex, 8 to 45 percent slopes432E362149997512mmt63920001:24000
Wayden clay, 2 to 15 percent slopes259D23014982250wzmt63920001:24000
Wayden-Castner complex, 15 to 60 percent slopes, bouldery438F88150003512tmt63920001:24000
Sagedale-Cabba-Wayden complex, 8 to 25 percent slopes1588791347984cp39mt64919851:24000
Cabba-Wayden-Sagedale complex, 25 to 70 percent slopes534215348085cp6kmt64919851:24000
Cabba-Wayden-Rock outcrop complex, 25 to 70 percent slopes523089348084cp6jmt64919851:24000
Wayden-Castner association, steep6340599348197cpb5mt65519751:24000
Wayden-Castner-Cabba complex, 2 to 15 percent slopes262D1060361448d43mmt65519751:24000
Wayden-Castner complex, 15 to 60 percent slopes331F372361444d43hmt65519751:24000
Castner-Wayden complex, moist, 15 to 60 percent slopes283F73361447d43lmt65519751:24000
Cabba-Wayden-Castner complex, 4 to 35 percent slopes574E4530348725cpw6mt65719901:24000
Winifred-Wayden-Cabba complex, 2 to 15 percent slopes285C2664348535cpp2mt65719901:24000
Wayden-Cabba-Winifred complex, 15 to 45 percent slopes187F1931348411cpk2mt65719901:24000
Wayden-Windham complex, 4 to 25 percent slopes262E21915316551ndt7mt66620081:24000
Wayden-Castner complex, 8 to 45 percent slopes261F10315316571ndt9mt66620081:24000
Wayden-Castner-Rock Outcrop complex, 25 to 60 percent slopes362F61620222ntd5mt6691:24000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C207225257281vzsgnd00119831:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C6027556401vzsdnd00119831:20000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C59126990481vzsgnd00719981:24000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C143825635871vzsdnd01119691:20000
Cabba and Wayden stony soils, 3 to 35 percent slopesCe126499280112b2vnd01119691:20000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C114327070321vzsgnd01119691:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesMwC12099287112b53nd01119691:20000
Wayden silty clay, 9 to 25 percent slopesE0939E700127071892q648nd02519811:20000
Barkof-Wayden-Dogtooth complex, 3 to 9 percent slopesE0725C444727072752r4gnnd03319851:24000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C2727596351vzsdnd03719851:20000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C195525257851vzsgnd04119861:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C8717185861vzsdnd04119861:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C194027150451vzsdnd05320031:24000
Moreau-Wayden silty clays, 9 to 15 percent slopesE0913D465926992931vzsfnd05719761:20000
Moreau-Wayden silty clays, 9 to 15 percent slopesE0913D599617183401vzsfnd05919981:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C226126991931vzsdnd05919981:20000
Regent-Wayden silty clay loams, 6 to 15 percent slopesE0923D4127597002r4fxnd08519921:24000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C135527073881vzsgnd08719741:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C517167771vzsdnd08719741:20000
Moreau-Wayden silty clays, 6 to 9 percent slopesE0913C343417134861vzsdnd08919651:20000
Moreau-Wayden-Rock outcrop complex, 6 to 15 percent slopesE8097D184127160411w025nd08919651:20000
Moreau-Wayden silty clays, 9 to 15 percent slopesE0913D110017134871vzsfnd08919651:20000
Wayden-Moreau silty clays, 3 to 9 percent slopesE0931C1817134881vzsgnd08919651:20000
Wayden-Cabba complex, 9 to 40 percent slopesWcE25222356227cyp6sd03119861:24000
Regent-Wayden silty clay loams, 6 to 15 percent slopesRpC19948356200cynbsd03119861:24000
Wayden and Cabba soils, 6 to 40 percent slopes, extremely stonyWdE2993356228cyp7sd03119861:24000
Wayden-Moreau silty clays, 25 to 40 percent slopesWaF36494354251cwmgsd04119721:24000
Moreau-Wayden silty clays, 9 to 25 percent slopesMbD23759354207cwl1sd04119721:24000
Regent-Wayden silty clay loams, 6 to 15 percent slopesRhD11541354653cx1fsd10519771:24000
Cabba and Wayden stony soils, 2 to 25 percent slopesCcD7569354621cx0dsd10519771:24000
Wayden silty clay loam, 15 to 40 percent slopesWdE10545355907cybwsd13719851:24000
Trimad-Doney-Wayden complex, 15 to 45 percent slopes2854509361038d3pdwy63319871:24000
Wayden silty clay, 0 to 35 percent slopes298464361025d3nzwy63319871:24000

Map of Series Extent

Approximate geographic distribution of the WAYDEN 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 .