Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZIGWEID 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 ZIGWEID 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 ZIGWEID 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 ZIGWEID 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 ZIGWEID 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 ZIGWEID 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 ZIGWEID 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 mountains figure.

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Soil series sharing subgroup-level classification with ZIGWEID, 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. SD-2012-03-15-11 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils, topography, and underlying material in the Nunn-Satanta association (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

  2. WY-2012-03-23-11 | Natrona County Area - 1997

    Diagram of the Cambria-Zigweid association, dry, sloping, on plateaus dissected by many drainageways. Chipenhill gravelly clay loam, 5 to 40 percent slopes, is on plateau breaks, and the Effington-Uffens complex, 0 to 6 percent slopes, is on terraces (Soil Survey of Natrona County Area, WY; 1997).

Map Units

Map units containing ZIGWEID 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
Zigweid-Nihill complex, 6 to 15 percent slopesZnE56563551652t34dsd04719801:24000
Zigweid-Nihill complex, 6 to 15 percent slopesZaD455093543612t34dsd60019741:24000
Zigweid-Nihill complex, 6 to 15 percent slopesZnD3957225809912t34dsd60620111:24000
Zigweid-Canyon complex, 2 to 15 percent slopesZcC4752586461cyftsd60720111:24000
Nihill-Zigweid complex, 15 to 50 percent slopesNfE4552586457cydfsd60720111:24000
Zigweid-Nihill complex, 6 to 15 percent slopesZnD16825865642t34dsd60720111:24000
Kim-Zigweid loams, 3 to 10 percent slopes902435349370cqk0wy01119781:24000
Cushman-Shingle loams, 10 to 30 percent slopes541761349334cqhvwy01119781:24000
Zigweid loam, 2 to 6 percent slopes2131087349301cqgswy01119781:24000
Cushman-Shingle loams, 6 to 10 percent slopes53886349333cqhtwy01119781:24000
Cambria-Kishona-Zigweid loams, 0 to 6 percent slopes2562267802522v09twy01119781:24000
Shingle-Badland-Zigweid complex, 4 to 20 percent slopes5C0333566882zb03wy04319761:24000
Zigweid-Bowbac-Bunkwater-like complex, 1 to 25 percent slopes5C13335669130zsvwy04319761:24000
Kishona-Theedle-Zigweid loams, 2 to 10 percent slopes5622550349461cqmywy04519841:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes1488314239462ztzfwy04519841:24000
Hiland-like-Zigweid-Ulm complex 0 to 4 percent slopes111531709232w7hmwy6031:24000
Cambria-Kishona-Zigweid loams, 0 to 6 percent slopes116281723498012v09twy60519951:24000
Zigweid-Bahl association, 0 to 6 percent slopes272308816697601t1j7wy60920061:24000
Zigweid-Cambria complex, 0 to 6 percent slopes273201916697612yv7jwy60920061:24000
Zigweid-Theedle loams, 3 to 15 percent slopes27458116697622v09rwy60920061:24000
Cambria-Zigweid complex, 2 to 15 percent slopes1176316696652v09swy60920061:24000
Zigweid loam, 2 to 9 percent slopes271916697632wlrxwy60920061:24000
Zigweid-Huntsman-like-Stonebarn-like complex, 1 to 6 percent slopes, frequently flooded110833582792ypnswy6171:24000
Zigweid-Bowbac-Bunkwater-like complex, 1 to 25 percent slopes5C13335826130zsvwy6171:24000
Zigweid loam, 6 to 15 percent slopes67C330287453tmwy6171:24000
Zigweid loam, 0 to 3 percent slopes67A335831153tjwy6171:24000
Shingle-Badland-Zigweid complex, 4 to 20 percent slopes5C0331970362zb03wy6171:24000
Zigweid loam, 3 to 6 percent slopes67B335831253tlwy6171:24000
Shingle-Kishona-Zigweid loams, 6 to 30 percent slopesSNc154273509302yv74wy61919711:24000
Cambria-Zigweid complex, 0 to 6 percent slopesSTg125513509432yv7hwy61919711:24000
Kim-Zigweid association, gently slopingKZB5399350869cs3cwy61919711:24000
Zigweid-Keyner complex, hillyZKD3104350969cs6lwy61919711:24000
Kim-Zigweid association, moderately steepKZD2045350870cs3dwy61919711:24000
Zigweid loam, 3 to 6 percent slopesZgB1927350971cs6nwy61919711:24000
Zigweid loam, 0 to 3 percent slopesZgA10773509702v09nwy61919711:24000
Cambria-Zigweid complex, 2 to 15 percent slopes142448165972v09swy61919711:24000
Cambria-Kishona-Zigweid loams, 0 to 6 percent slopes116288168622v09twy61919711:24000
Petrie-Zigweid complex, wet, 0 to 3 percent slopes23526816847wdzxwy61919711:24000
Forkwood-Zigweid complex, 3 to 15 percent slopes188501465022762wlrgwy62519851:24000
Zigweid-Theedle loams, 3 to 15 percent slopes311363065024592v09rwy62519851:24000
Cambria-Zigweid complex, 2 to 15 percent slopes142332905022212v09swy62519851:24000
Zigweid loam, 2 to 9 percent slopes310245675024572wlrxwy62519851:24000
Cambria-Zigweid association, dry, sloping1437179502223jvlrwy62519851:24000
Petrie-Zigweid complex, wet, 0 to 3 percent slopes2353825502360jvr5wy62519851:24000
Zigweid-Urban land complex, 2 to 8 percent slopes312335502461jvvfwy62519851:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes31917514213552ztzfwy62519851:24000
Zigweid-Cambria complex, 0 to 6 percent slopes3291414260872yv7jwy62519851:24000
Zigweid-Thedalund-Shingle association, 6 to 35 percent slopes -- Draft35124834882pc8jwy6291:24000
Taluce, very bouldery-Zigweid complex, 15 to 50 percent slopes582032031392zy9xwy6291:24000
Larim-like-Zigweid-Taluce-like complex, 15 to 60 percent slopes554432030382zbqxwy6291:24000
Zigweid-Huntsman-like-Stonebarn-like complex, 1 to 6 percent slopes, frequently flooded110831368562ypnswy6291:24000
Vonalee-like-Keeline-like, frequently flooded-Zigweid complex, 0 to 4 percent slopes112131332712ynmzwy6291:24000
Zigweid-Shingle-Begay complex, 4 to 20 percent slopes532329119702y4yswy6291:24000
Cambria-Zigweid complex, 1 to 6 percent slopes213129118922w7j0wy6291:24000
Hiland-like-Zigweid-Ulm complex 0 to 4 percent slopes111529118782w7hmwy6291:24000
Zigweid-Cushman complex, 8 to 35 percent slopes540829118732w7hhwy6291:24000
Vonid-Cascajo-Zigweid complex, 1 to 4 percent slopes113232066322zc4hwy6291:24000
Zigweid loam, 6 to 15 percent slopes67C15263253tmwy6291:24000
Zigweid loam, 3 to 6 percent slopes67B15263153tlwy6291:24000
Zigweid loam, 0 to 3 percent slopes67A15262953tjwy6291:24000
Kishona-Zigweid-Cambria loams, moist, 6 to 9 percent slopes320276593593212yrydwy63319871:24000
Kishona-Zigweid-Cambria complex, 6 to 15 percent slopes317177103610062wls0wy63319871:24000
Kishona-Zigweid-Cambria complex, moist, 3 to 6 percent slopes319112613610042yrybwy63319871:24000
Kishona-Zigweid-Cambria complex, moist, 0 to 3 percent slopes31878853610052yry9wy63319871:24000
Zigweid-Cambria loams, 0 to 6 percent slopes3166429361007d3ndwy63319871:24000
Zigweid loam, 0 to 3 percent slopes3159053610082v09nwy63319871:24000
Zigweid loam, 6 to 15 percent slopes67C325333453tmwy65620081:24000
Kishona-Zigweid-Cambria complex, 6 to 15 percent slopes33913198176182wls0wy70520031:24000
Zigweid-Cambria loams, 0 to 6 percent slopes338775817617wfsrwy70520031:24000
Zigweid-Cambria complex, 0 to 6 percent slopes151124873515292yv7jwy70919831:24000
Zigweid-Cambria-Theedle complex, 6 to 15 percent slopes152117533515302ztzfwy70919831:24000
Zigweid-Bahl association, 0 to 6 percent slopes1506525351528cssmwy70919831:24000
Forkwood-Zigweid complex, 3 to 15 percent slopes24611814279032wlrgwy70919831:24000
Zigweid-Theedle loams, 3 to 15 percent slopes2492914279062v09rwy70919831:24000
Kishona-Zigweid loams, 3 to 15 percent slopes, gullied734181214738801lgpjwy71920131:24000

Map of Series Extent

Approximate geographic distribution of the ZIGWEID 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 .