Official Series Description


Lab Data Summary

Aggregate lab data for the OPAL soil series. This aggregation is based on all pedons with a current taxon name of OPAL, 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 OPAL 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
63A84P00481983SD085001Opal8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8936119,-99.9172211
63A85P00071984SD075002Opal8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9302788,-100.6600037
63A85P00081984SD075003Opal8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9302788,-100.6602783

Water Balance

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

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Competing Series

Soil series competing with OPAL 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 OPAL 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 OPAL 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.

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 OPAL, 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-2012-03-15-06 | Corson County - July 1995

    Pattern of soils and parent material in the Sansarc-Dupree-Opal association (Soil Survey of Corson County, SD; 1995).

  2. SD-2012-03-15-51 | Hyde County - 1998

    Typical pattern of soils and parent material in the Opal-Promise association (Soil Survey of Hyde County, SD; 1998).

  3. SD-2012-03-15-52 | Hyde County - 1998

    Typical pattern of soils and parent material in the Sansarc-Opal association (Soil Survey of Hyde County, SD; 1998).

  4. SD-2012-03-15-59 | Jones County - 1999

    Typical pattern of soils and parent material in the Bigbend-Hilmoe and Sansarc-Opal associations (Soil Survey of Jones County, SD; 1999).

  5. SD-2012-03-15-60 | Jones County - 1999

    Typical pattern of soils and parent material in the Promise-Kirley and Promise associations (Soil Survey of Jones County, SD; 1999).

  6. SD-2012-03-15-70 | Lyman County - May 1987

    Pattern of soils and parent material in the Millboro association (Soil Survey of Lyman County, SD; 1987).

  7. SD-2012-03-15-71 | Lyman County - May 1987

    Pattern of soils and parent material in the Sansarc-Opal and Munjor-Hilmoe-Bigbend associations (Soil Survey of Lyman County, SD; 1987).

Map Units

Map units containing OPAL 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
Sansarc-Opal clays, 9 to 25 percent slopes39E184473547092v670sd02119781:20000
Opal-Sansarc clays, 6 to 15% slopes40D75463547132v671sd02119781:20000
Opal clay, 6 to 9 percent slopes40C160126525092rmjcsd02119781:20000
Promise-Opal clays, 6 to 9 percent slopes41C750354716cx3gsd02119781:20000
Opal-Sansarc clays, cool, 6 to 15 percent slopesC942D68727979462rsr7sd02119781:20000
Opal clay, 3 to 6 percent slopes40B53026524982rmjbsd02119781:20000
Promise-Opal clays, cool, 6 to 9 percent slopesC940C49727979432rsr4sd02119781:20000
Opal clay, cool, 6 to 9 percent slopesC941C48827979452rsr6sd02119781:20000
Opal clay, cool, 3 to 6 percent slopesC941B37627979442rsr5sd02119781:20000
Sansarc-Opal clays, cool, 15 to 40 percent slopesC943E33727979472rsr8sd02119781:20000
Sansarc-Opal-Dupree clays, 9 to 25% slopesSdD306983562082v673sd03119861:24000
Sansarc-Opal clays, 9 to 25 percent slopesSbE246743562072v670sd03119861:24000
Opal-Dupree clays, 2 to 9 percent slopesOdC19797356183cymssd03119861:24000
Opal-Sansarc clays, 6 to 15% slopesOsC103153561852v671sd03119861:24000
Opal-Hurley complex, 0 to 9 percent slopesOhB61703561842v672sd03119861:24000
Opal clay, 3 to 6 percent slopesOaB454626524992rmjbsd03119861:24000
Opal clay, 6 to 9 percent slopesOaC403626525102rmjcsd03119861:24000
Sansarc-Opal clays, 9 to 25 percent slopesSbE35339027390072v670sd04119721:24000
Opal clay, 3 to 9 percent slopesOaB831253542142rmjfsd04119721:24000
Opal-Sansarc clays, 6 to 15% slopesOsC776303542172v671sd04119721:24000
Dupree-Opal clays, 2 to 9 percent slopesDoB64599354186cwkcsd04119721:24000
Opal-Hurley complex, 0 to 9 percent slopesOhB347283542152v672sd04119721:24000
Opal-Slickspots complex, 2 to 6 percent slopesOtB6213354218cwldsd04119721:24000
Opal-Promise clays, 3 to 6 percent slopesOpB33793542162v66rsd04119721:24000
Sansarc-Opal clays, 9 to 25 percent slopesS502E289826156412v670sd05319821:20000
Rock outcrop-Sansarc-Opal complex, 6 to 40 percent slopesRpE7026156422rmj2sd05319821:20000
Opal clay, 6 to 15 percent slopesOdD2023926525212rmjdsd05519921:24000
Sansarc-Opal clays, 9 to 25 percent slopesSoE1419527390092v670sd05519921:24000
Opal-Promise clays, 3 to 6 percent slopesOeB138123541272v66rsd05519921:24000
Opal-Promise clays, 6 to 9 percent slopesOeC120553541282ynv3sd05519921:24000
Opal clay, 6 to 9 percent slopesOdC1018126525122rmjcsd05519921:24000
Opal clay, 3 to 6 percent slopesOdB833326525002rmjbsd05519921:24000
Sansarc-Opal clays, 9 to 25 percent slopesLtD11053526432v670sd05919591:20000
Opal-Lakoma clays, 9 to 15 percent slopesOrD6103353315cvn8sd06519701:20000
Opal clay, 6 to 9 percent slopesOpC139926525132rmjcsd06519701:20000
Opal clay, 3 to 6 percent slopesOpB52726525012rmjbsd06519701:20000
Sansarc-Opal clays, 9 to 25 percent slopesSbF105903538472v670sd06919921:20000
Opal-Sansarc clays, 6 to 15% slopesOuD72573538312v671sd06919921:20000
Opal-Promise clays, 6 to 9 percent slopesOfC586626525142ynv3sd06919921:20000
Opal clay, 3 to 6 percent slopesOtB535526525022rmjbsd06919921:20000
Opal clay, 6 to 15 percent slopesOpD4283426525222rmjdsd07519911:24000
Opal clay, 6 to 9 percent slopesOpC2900326525152rmjcsd07519911:24000
Opal clay, 3 to 6 percent slopesOpB2554826525032rmjbsd07519911:24000
Sansarc-Opal clays, 9 to 25 percent slopesSoE2350527390102v670sd07519911:24000
Opal clay, 0 to 3 percent slopesOpA46726524952rmj9sd07519911:24000
Sansarc-Opal clays, 9 to 25 percent slopesSbE13575927390112v670sd08519841:20000
Opal-Sansarc clays, 6 to 15% slopesOnD1049833556032v671sd08519841:20000
Sansarc-Opal-Promise clays, 6 to 35 percent slopesSpE3685326156442rmj4sd08519841:20000
Opal-Promise clays, 6 to 9 percent slopesOfC2534626525162ynv3sd08519841:20000
Rock outcrop-Sansarc-Opal complex, 6 to 40 percent slopesRpE2481826156462rmj2sd08519841:20000
Opal clay, 3 to 6 percent slopesOlB1970826525042rmjbsd08519841:20000
Opal-Chantier clays, 2 to 9 percent slopeOmC13275355602cy11sd08519841:20000
Sansarc-Opal-Schamber complex, 6 to 30 percent slopesSoE309626156432rmj5sd08519841:20000
Opal clay, 0 to 3 percent slopesOlA184126524962rmj9sd08519841:20000
Opal clay, 6 to 9 percent slopesOcC1677026525112rmjcsd09519711:20000
Opal clay, mounded, 5 to 9 percent slopesOgC13358353415cvrhsd09519711:20000
Opal-Kirley complex, 2 to 5 percent slopesOlB4123353416cvrjsd09519711:20000
Opal-Kirley complex, 5 to 9 percent slopesOlC3715353417cvrksd09519711:20000
Opal-Mosher complex, 2 to 6 percent slopesOmB3660353418cvrlsd09519711:20000
Opal-Woodly complex, 3 to 9 percent slopesOwC3500353422cvrqsd09519711:20000
Tuthill-Opal complex, 2 to 9 percent slopesToC3231353448cvsksd09519711:20000
Opal-Tuthill complex, 5 to 15 percent slopesOtD3029353421cvrpsd09519711:20000
Woodly-Opal complex, 2 to 5 percent slopesWoB2676353456cvstsd09519711:20000
Opal-Tuthill complex, 2 to 5 percent slopesOtB2069353420cvrnsd09519711:20000
Sansarc-Opal clays, 9 to 25 percent slopesS502E136226156482v670sd09519711:20000
Rock outcrop-Sansarc-Opal complex, 6 to 40 percent slopesRpE30826156492rmj2sd09519711:20000
Sansarc-Opal clays, 9 to 25 percent slopesSbE172913553722v670sd10719831:20000
Opal clay, 3 to 6 percent slopesOpB872426525052rmjbsd10719831:20000
Opal-Sansarc clays, 6 to 15% slopesOsD71543553572v671sd10719831:20000
Opal clay, 6 to 9 percent slopesOpC271626525172rmjcsd10719831:20000
Sansarc-Opal-Dupree, acid, clays, 6 to 25 percent slopesR510E15724824522v674sd10719831:20000
Sansarc-Opal clays, 9 to 25 percent slopesSoE17194227390132v670sd11719771:24000
Opal clay, 3 to 6 percent slopesOpB4613926525062rmjbsd11719771:24000
Opal clay, 6 to 9 percent slopesOpC4312926525182rmjcsd11719771:24000
Opal-Chantier clays, 2 to 6 percent slopesOtB14199353499cvv6sd11719771:24000
Opal-Chantier clays, 6 to 9 percent slopesOtC8711353500cvv7sd11719771:24000
Opal clay, 0 to 3 percent slopesOpA284426524972rmj9sd11719771:24000
Opal-Sansarc clays, 6 to 15% slopesOsD64310159632v671sd11719771:24000
Sansarc-Opal-Dupree, acid, clays, 6 to 25 percent slopesR510E1104727390202v674sd11919671:20000
Opal-Dupree clays, 6 to 21 percent slopesOuD977353111cvfpsd11919671:20000
Opal clay, 6 to 9 percent slopesOtC42626525192rmjcsd11919671:20000
Opal clay, 3 to 6 percent slopesOtB27826525072rmjbsd11919671:20000
Sansarc-Opal clays, 9 to 25 percent slopesS502E4082026156512v670sd12319751:20000
Opal-Sansarc clays, 6 to 15% slopesOsE65463544242v671sd12319751:20000
Rock outcrop-Sansarc-Opal complex, 6 to 40 percent slopesRpE141026156502rmj2sd12319751:20000
Opal clay, 3 to 9 percent slopesOpC11903544232rmjfsd12319751:20000
Sansarc-Opal clays, 9 to 25 percent slopesSaE175033545252v670sd12919751:20000
Opal-Sansarc clays, 6 to 15% slopesOsD146963545152v671sd12919751:20000
Opal clay, 3 to 9 percent slopesOpC89833545142rmjfsd12919751:20000
Opal clay, cool, 6 to 9 percent slopesC941C1928001512rsr6sd12919751:20000
Sansarc-Opal clays, 9 to 25 percent slopesR507E7474526492302v670sd13719851:24000
Sansarc-Opal clays, 9 to 25 percent slopesSaE5216727390162v670sd60319831:20000
Opal-Promise clays, 6 to 9 percent slopesOfC2409126525202ynv3sd60319831:20000
Opal clay, 3 to 6 percent slopesOmB1130426525082rmjbsd60319831:20000
Opal clay, saline, 1 to 6 percent slopesOpB766426525232rmjgsd60319831:20000

Map of Series Extent

Approximate geographic distribution of the OPAL 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 .