Official Series Description


Lab Data Summary

Aggregate lab data for the CURLEW soil series. This aggregation is based on all pedons with a current taxon name of CURLEW, 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 CURLEW 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
n/a69C0065S1969ID071033Curlew3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CURLEW 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 CURLEW 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 CURLEW 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 CURLEW 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 CURLEW 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 CURLEW series and competing. 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 CURLEW 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.

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Soil series sharing subgroup-level classification with CURLEW, 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 CURLEW 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
Curlew-Riverrun complex, 0 to 2 percent slopes146A99924226122m9xsmt63819851:24000
Riverrun-Gash-Curlew complex, 0 to 2 percent slopes160A42324226212m9y2mt63819851:24000
Histic Endoaquolls-Curlew-Water complex, 0 to 2 percent slopes147A22324226132m9xtmt63819851:24000
Chereete-Curlew complex, 0 to 45 percent slopes14F14824225972m9x9mt63819851:24000
Chereete-Riverrun-Curlew complex, 0 to 8 percent slopes17C6824227572mb2gmt63819851:24000
Curlew-Riverrun complex, 0 to 2 percent slopes, rarely flooded146A343815856059zvmt64520131:12000
Riverrun, rarely flooded-Gash, occasionally flooded-Curlew, rarely flooded complex, 0 to 2 percent slopes160A32551585745b09mt64520131:12000
Chereete-Riverrun, rarely flooded-Curlew, rarely flooded complex, 0 to 8 percent slopes17C3243633397p835mt64520131:12000
Riverrun-Curlew complex, 0 to 2 percent slopes, rarely flooded12A2283757590tfbdmt64520131:12000
Chereete-Curlew, rarely flooded complex, 0 to 45 percent slopes14F1418633376p82hmt64520131:12000
Curlew, rarely flooded-Victor complex, 0 to 4 percent slopes315B1283633664p8csmt64520131:12000
Curlew, rarely flooded-Groff loams, 0 to 4 percent slopes316B1226633665p8ctmt64520131:12000
Bandy, occasionally flooded-Curlew, rarely flooded-Water complex, 0 to 2 percent slopes147A971633608p89zmt64520131:12000
Crow-Haugan-Curlew families, complex, fan remnants17B33916633754p8gpmt64520131:12000
Yreka-Repkie-Curlew families, complex, moraines44B3262324238132mc5jmt64520131:12000
Curlew silt loam, 0 to 4 percent slopes, rarely flooded350B604633690p8dmmt64520131:12000
Riverside-Tiechute-Curlew, rarely flooded complex, 0 to 40 percent slopes16E547633396p834mt64520131:12000
Chargold-Haulings-Curlew complex, 0 to 2 percent slopes, rarely flooded21A50823913702l8dzmt64520131:12000
Blossberg-Curlew, rarely flooded complex, 0 to 4 percent slopes318B447633668p8cxmt64520131:12000
Overwhich-Curlew, rarely flooded complex, 2 to 8 percent slopes350C393633691p8dnmt64520131:12000
Chereete-Curlew, rarely flooded-Poverty complex, 0 to 35 percent slopes323E29522293682dtv3mt64520131:12000
Repkie-Losthorse-Curlew families, complex, trough bottoms47B13237633784p8hnmt64520131:12000
Crow-Haugan-Curlew families, complex, fan remnants17B336398150221519vmt64720071:24000
Yreka-Repkie-Curlew families, complex, moraines, extremely bouldery44B32422015037851gxmt64720071:24000
Repkie-Losthorse-Curlew families, complex, trough bottoms, extremely bouldery47B13139815032851f9mt64720071:24000
Chereete-Riverrun-Curlew complex, 0 to 8 percent slopes17C3319078222217nmt64720071:24000
Curlew-Groff loams, 0 to 4 percent slopes316B1124871692ph38mt64720071:24000
Chereete-Curlew complex, 0 to 45 percent slopes14F824871582ph2xmt64720071:24000
Riverrun-Curlew complex, 0 to 2 percent slopes12A324871552ph2tmt64720071:24000
Overwhich-Curlew complex, 2 to 8 percent slopes350C324871772ph3jmt64720071:24000
Curlew-Riverrun complex, 0 to 2 percent slopes146A124871572ph2wmt64720071:24000

Map of Series Extent

Approximate geographic distribution of the CURLEW 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 .