Official Series Description


Lab Data Summary

Aggregate lab data for the RIVRA soil series. This aggregation is based on all pedons with a current taxon name of RIVRA, 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 RIVRA 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 RIVRA 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 RIVRA 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 RIVRA 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 RIVRA 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 RIVRA 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 RIVRA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the RIVRA 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 RIVRA, 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 RIVRA 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
Rivra complex, 0 to 2 percent slopes, occasionally flooded681A2002343646cjlcmt01719951:24000
Rivra complex, 0 to 2 percent slopes, frequently flooded851A2421342702chlxmt03320021:24000
Rivra complex, 0 to 2 percent slopes1073847344783cks1mt07919861:24000
Ryell-Rivra complex, 0 to 2 percent slopes571A576345224cl78mt10119921:24000
Banks soilsBs1888345389cldlmt10319611:20000
Havre-Rivra complex283329345543clkkmt10519761:24000
Ryell, rarely flooded-Rivra, frequently flooded complex, 0 to 4 percent slopes10B20731480904z33mt60420011:24000
Riverrun, occasionally flooded-Rivra complex, 0 to 2 percent slopes60A40516974841tzckmt60420011:24000
Rivra complex, 0 to 4 percent slopes, occassionally flooded111B3351482014z6pmt60420011:24000
Rivra, stony-Riverrun complex, 0 to 2 percent slopes161A11316974811tzcgmt60420011:24000
Ryell, rarely flooded-Rivra complex, cool, 0 to 2 percent slopes110A79609158nfw8mt60420011:24000
Rivra very gravelly sandy loam, cool, 2 to 4 percent slopes10522185964820f3nmt60520071:24000
Rivra complex, 0 to 4 percent slopes, occasionally flooded111B1185949220dymmt60520071:24000
Rivra gravelly loamRr35311475354yj6mt60919711:24000
Rivra-Mccabe-Bonebasin complex, 0 to 2 percent slopes701A1061476724ynmmt60919711:24000
Rivra-Ryell-Bonebasin complex, 0 to 2 percent slopes301A171476664ynfmt60919711:24000
Rivra gravelly sandy loam16510310341829cgprmt61319751:24000
Ryell-Rivra complex1724338341837cgq0mt61319751:24000
Straw-Rivra complex1852837341851cgqgmt61319751:24000
Rivra-Hanly complex, 0 to 2 percent slopes992953347015cn31mt61519921:24000
Rivra-Mccabe-Bonebasin complex, 0 to 2 percent slopes701A508315566856zkmt62219971:24000
Ryell-Rivra-Fairway complex, 0 to 2 percent slopes304A417315538756phmt62219971:24000
Fairway-Threeriv-Rivra complex, 0 to 2 percent slopes508A401415554756vnmt62219971:24000
Rivra, moist-Ryell-Bonebasin, 0 to 2 percent slopes401A359015545856rsmt62219971:24000
Meadowcreek-Rivra complex, 0 to 2 percent slopes603A210415561656xwmt62219971:24000
Fairway-Rivra complex, 0 to 2 percent slopes505A186115554456vkmt62219971:24000
Lamoose-Rivra-Bonebasin complex, 0 to 2 percent slopes541A158015558556wwmt62219971:24000
Meadowcreek, slightly saline-Rivra complex, 0 to 2 percent slopes503A151915554256vhmt62219971:24000
Greycliff-Rivra-Threeriv complex, 0 to 2 percent slopes526A117815557256wgmt62219971:24000
Rivra-Ryell-Bonebasin complex, 0 to 2 percent slopes301A87815538656pgmt62219971:24000
Rivra-Emyd-Greycliff complex, 0 to 2 percent slopes, protected801A736155733571nmt62219971:24000
Rivra cobbly sandy loam, 2 to 6 percent slopes201A22515531656m6mt62219971:24000
Glendive-Meadowcreek-Rivra complex, cool, 0 to 2 percent slopes, occasionally flooded105A316519125732265xmt62420211:24000
Glendive-Meadowcreek-Rivra complex, 0 to 2 percent slopes, occasionally flooded370A1749191257722661mt62420211:24000
Ryell-Rivra complex, 0 to 3 percent slopes117A32581476884yp4mt63019911:24000
Rivra-Ryell-Havre complex, cool, 0 to 2 percent slopes107189931463784x9wmt63619831:24000
Ryell-Rivra complex, cool, 0 to 2 percent slopes11068981463824xb0mt63619831:24000
Rivra very gravelly sandy loam, cool, 2 to 4 percent slopes10558171463764x9tmt63619831:24000
Ryell-Rivra sandy loams, cool, saline, 0 to 2 percent slopes1118271463834xb1mt63619831:24000
Riverrun-Rivra complex, 0 to 2 percent slopes2472016975011tzd3mt63619831:24000
Glendive-McCabe-Rivra complex, 0 to 2 percent slopes, occasionally flooded602A524813532p91nmt63920001:24000
Ryell-Rivra complex, 0 to 2 percent slopes, occasionally flooded111A7190348298cpffmt65719901:24000
Rivra, occasionally flooded-Riverwash complex, 0 to 4 percent slopes110B6608348297cpfdmt65719901:24000
Ryell-Rivra complex, 0 to 2 percent slopes, rarely flooded211A2664348439cpkzmt65719901:24000
Glendive-McCabe-Rivra complex, 0 to 2 percent slopes, occasionally flooded602A4422156943589pmt6691:24000
Riverwash-Rivra complex, 0 to 2 percent slopes1216A1108610335nh37mt6691:24000
Urban land-Glendive, occasionally flooded-Rivra , occasionally flooded complex, 0 to 2 percent slopes11A349886546yrj8mt6691:24000
Varney-Rivra complex, 0 to 4 percent slopes46A63714246251jtfnmt67020071:24000
Riverrun-Rivra complex, 0 to 2 percent slopes60A59014246391jtg3mt67020071:24000
Varney, stony-Anamac, very stony-Rivra, extremely stony complex, 2 to 8 percent slopes182C52914246891jthqmt67020071:24000
Rivra gravelly sandy loam, 0 to 4 percent slopes, moderately impacted38B497320252br7qmt67020071:24000
Rivra, stony-Riverrun complex, 0 to 2 percent slopes61A33014246381jtg2mt67020071:24000
Anamac-Varney-Rivra, rarely flooded complex, 0 to 6 percent slopes15B276320244br7gmt67020071:24000
Rivra-Urban land complex, 0 to 6 percent slopes252728502387jvs1wy62519851:24000
Rivra sandy clay loam, 0 to 3 percent slopes91230174362xbrrwy7371:24000

Map of Series Extent

Approximate geographic distribution of the RIVRA 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 .