Official Series Description


Lab Data Summary

Aggregate lab data for the RICREST soil series. This aggregation is based on all pedons with a current taxon name of RICREST, 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 RICREST 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 RICREST 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 RICREST 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 RICREST 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 RICREST 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 flats position figure.

Competing Series

Soil series competing with RICREST 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 RICREST 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 RICREST 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 RICREST, 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. ID-2011-06-01-07 | Bingham Area - 1973

    Representative pattern of soils in association 7 (Soil Survey of Bingham Area, Idaho; 1973).

Map Units

Map units containing RICREST 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
Ireland-Ricrest association, 30 to 50 percent slopes834014825592rx6id70819871:24000
Searla-Ricrest complex, 30 to 75 percent slopes1331996824502rspid70819871:24000
Ricrest-Searla complex, 12 to 20 percent slopes118484824332rs4id70819871:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes812781931635102v06did70919761:24000
Dranyon-Ricrest association, steep171875825902ry6id70919761:24000
Ricrest-Ridgecrest cobbly loams, steepRDG1189828062s55id71019681:24000
Ricrest-Ridgecrest gravelly loams, hillyRCF971828052s54id71019681:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes310048632389532pt1qid71019681:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes814731732302v06did71019681:24000
Calpac-Ireland extremely bouldery surface-Ricrest complex, 10 to 45 percent slopes10202732389502mgkkid71019681:24000
Huffman-Ricrest-Cedarhill complex, 10 to 25 percent slopesRFF63238961n4cgid71019681:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes33996131635282v05xid71119831:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes33-B6531732652v05xid71220081:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes33336725145782v05xid7131:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes702053230938832x3mqid7131:24000
Ricrest-Ridgecrest, stony surface, complex, 20 to 60 percent slopes8128726198332v06did7131:24000
Ricrest-Pontuge-Buist complex, 8 to 40 percent slopes70003430938862xxdhid7131:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes54-F3429170622sltlid7131:24000
Lonigan-Ricrest association, 50 to 80 percent slopes861401485335j90zid71419971:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes54114331635692sltlid71419971:24000
Ricrest gravelly silt loam, 4 to 12 percent slopes127418485217j8x5id71419971:24000
Cedarhill-Hades-Ricrest complex, 20 to 50 percent slopes3548485279j8z5id71419971:24000
Cedarhill, high precipitation-Hades-Ricrest complex, 20 to 50 percent slopes33-B7431733592v05xid71519941:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes3100774024954722pt1qid7161:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes7020697429897282x3mqid7161:24000
Cedarhill-Ricrest complex, 15 to 45 percent slopes3150657424954732pt1rid7161:24000
Ireland-Ricrest-Lanoak complex, 12 to 40 percent slopes7034342031756312z43qid7161:24000
Calpac-Ireland extremely bouldery surface-Ricrest complex, 10 to 45 percent slopes1020308424270692mgkkid7161:24000
Ricrest-Cedarhill complex, 10 to 50 percent slopes7065283830740392xxdnid7161:24000
Ricrest-Pontuge-Buist complex, 8 to 40 percent slopes7000170830740342xxdhid7161:24000
Bothwell-Hades-Ricrest complex, 10 to 30 percent slopes224077824846852pdj4id7161:24000
Huffman-Ricrest-Cedarhill complex, 10 to 25 percent slopesRFF576600019n4cgid7161:24000
Hondoho, stony surface-Ricrest complex, 4 to 40 percent slopes5440029841392sltlid7161:24000
Ricrest loam, steep, stonyRHG4416800022p7qid77019681:24000
Ricrest-Wahtigup complex, steep, stonyRLG2718800052p7tid77019681:24000
Calpac-Ricrest-Ireland, extremely bouldery surface, complex, 12 to 50 percent slopes7020134132389952x3mqid77019681:24000
Ricrest loam, hilly, stonyRHF988800012p7pid77019681:24000
Ricrest-Wahtigup complex, hilly, stonyRLF965800042p7sid77019681:24000
Ricrest loam, very steep, extremely stonyRIG422800032p7rid77019681:24000

Map of Series Extent

Approximate geographic distribution of the RICREST 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 .