Official Series Description


Lab Data Summary

Aggregate lab data for the COURVILLE soil series. This aggregation is based on all pedons with a current taxon name of COURVILLE, 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 COURVILLE 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
43A02N057799MT029003Courville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9122772,-114.7339172

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COURVILLE 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 COURVILLE 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 COURVILLE 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 COURVILLE 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 hills figure.

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with COURVILLE 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 COURVILLE 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 COURVILLE 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.

Click the image to view it full size.

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 COURVILLE, 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 COURVILLE 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
Courville family-Andic Glossudalfs-Courville family, moderately deep, complex, glacially scoured mountain slopes74UA1488928091342trb5mt60319891:24000
Courville family-Andic Hapludalfs-McCay family, complex, glacially scoured mountain slopes74BA303028091332trb4mt60319891:24000
Courville gravelly ashy silt loam, 8 to 30 percent slopes35E451299559657blmt60319891:24000
Courville-Rumblecreek complex, 4 to 15 percent slopes39D1852995451mgb5mt60319891:24000
Courville-Pleasantvalley complex, 8 to 30 percent slopes35E-F172995456mj86mt60319891:24000
Winfall-Courville complex, dry, 8 to 30 percent slopes138E122995455mhlfmt60319891:24000
Courville-Pleasantvalley complex, 8 to 30 percent slopes35E11719581659mj86mt61820081:24000
Rockhill-Rock outcrop-Courville complex, 15 to 50 percent slopes634F7644581661mj88mt61820081:24000
Rumblecreek-Courville complex, dry, 4 to 15 percent slopes40D6385579796mgb3mt61820081:24000
Courville-Stevie-Winfall complex, 30 to 50 percent slopes35F4345581658mj85mt61820081:24000
Winfall-Courville complex, dry, 8 to 30 percent slopes138E2459581015mhlfmt61820081:24000
Pleasantvalley-Courville-Glaciercreek complex, 30 to 50 percent slopes225F2027581660mj87mt61820081:24000
Courville-Winfall complex, 4 to 15 percent slopes35D2018115140017n3ymt61820081:24000
Courville-Rumblecreek complex, 4 to 15 percent slopes39D1271579798mgb5mt61820081:24000
Rumblecreek-Courville complex, dry, 15 to 30 percent slopes40E759579797mgb4mt61820081:24000
Courville, dry-Rumblecreek, dry-Lozeau, deep complex, 30 to 60 percent slopes41F485512822k6mnmt61820081:24000
Courville-Rockhill-Rock outcrop complex, 30 to 50 percent slopes221F64186180720hc9mt61820081:24000
Pleasantvalley-Courville-Glaciercreek complex, 30 to 50 percent slopes225F36524099482lwr8mt61919881:24000
Courville-Pleasantvalley complex, 8 to 30 percent slopes35E31324099262lwqkmt61919881:24000
Courville-Winfall complex, 4 to 15 percent slopes35D20624099252lwqjmt61919881:24000
Winfall-Courville complex, dry, 8 to 30 percent slopes138E14424099452lwr5mt61919881:24000
Courville-Stevie-Winfall complex, 30 to 50 percent slopes35F5824099272lwqlmt61919881:24000
Courville gravelly silt loam, 15 to 30 percent slopes2973131451304w0mmt62919911:20000
Courville gravelly silt loam, 30 to 60 percent slopes3048931451334w0qmt62919911:20000
Courville gravelly silt loam, warm, 15 to 30 percent slopes3235981451354w0smt62919911:20000
Courville gravelly silt loam, 4 to 15 percent slopes2832681451274w0jmt62919911:20000
Courville gravelly silt loam, warm, 30 to 60 percent slopes3324191451364w0tmt62919911:20000
Courville-Rumblecreek complex, 8 to 30 percent slopes347401451424w10mt62919911:20000
Half Moon-Courville complex, 4 to 15 percent slopes704901452894w5rmt62919911:20000
Courville gravelly silt loam, warm, 4 to 15 percent slopes314431451344w0rmt62919911:20000
Courville gravelly silt loam, 15 to 30 percent slopes, lake effect19519217159341vlkqmt62919911:20000
Half Moon-Courville complex, 4 to 15 percent slopes, lake effect2027717159851vlmcmt62919911:20000
Courville-Pleasantvalley complex, 8 to 30 percent slopes35E6224099022lwpsmt62919911:20000
Courville-Winfall complex, 4 to 15 percent slopes35D1024099012lwprmt62919911:20000
Troybull-Courville-Tevis complex, 35 to 75 percent slopes2328F1445831648412yyw7mt63419881:24000
Courville-Troybull-Tevis complex, 35 to 75 percent slopes2355F978531648442yywbmt63419881:24000
Courville family-Andic Glossudalfs-Courville family, moderately deep, complex, glacially scoured mountain slopes74UA548031648652trb5mt63419881:24000
Sunroad-Courville complex, 20 to 60 percent slopes2329F350431648422yyw8mt63419881:24000
Cosely-Courville-Dewberry complex, 4 to 15 percent slopes2223D310131648472yyw4mt63419881:24000
Courville-Cosely-Troybull complex, 8 to 35 percent slopes2323E308831648402yyw6mt63419881:24000
Courville-Pleasantvalley complex, 8 to 30 percent slopes35E293224098612lwngmt63419881:24000
Rockhill-Rock outcrop-Courville complex, 15 to 50 percent slopes634F235224098712lwnsmt63419881:24000
Courville-Cosely complex, 2 to 8 percent slopes2106C217431648352yyvymt63419881:24000
Tevis-Courville complex, 15 to 60 percent slopes2302F174531648392yyw5mt63419881:24000
Courville-Winfall complex, 4 to 15 percent slopes35D130824098602lwnfmt63419881:24000
Courville-Stevie-Winfall complex, 30 to 50 percent slopes35F44724098622lwnhmt63419881:24000
Cosely-Courville complex, 4 to 15 percent slopes2221D26731648382yyw3mt63419881:24000
Pleasantvalley-Courville-Glaciercreek complex, 30 to 50 percent slopes225F21824098692lwnqmt63419881:24000
Courville family-Andic Hapludalfs-McCay family, complex, glacially scoured mountain slopes74BA14531648642trb4mt63419881:24000
Courville-Rockhill-Rock outcrop complex, 30 to 50 percent slopes221F4224098652lwnlmt63419881:24000
Courville gravelly silt loam, 8 to 30 percent slopes3122711454484wbwmt63819851:24000
Courville-Mitten gravelly silt loams, 30 to 60 percent slopes3220061454494wbxmt63819851:24000
Courville family-Andic Glossudalfs-Courville family, moderately deep, complex, glacially scoured mountain slopes74UA22830449772trb5mt63819851:24000
Courville family-Andic Glossudalfs-Courville family, moderately deep, complex, glacially scoured mountain slopes74UA50129953912trb5mt64419951:24000
Courville gravelly ashy silt loam, 8 to 30 percent slopes35E1747415601057blmt65119971:24000
Courville gravelly ashy silt loam, 30 to 50 percent slopes35F423515601157bmmt65119971:24000
Winfall-Courville complex, 8 to 30 percent slopes134E2106155819574fmt65119971:24000
Courville gravelly ashy silt loam, 2 to 8 percent slopes22C16251559065777mt65119971:24000
Courville-Rockhill-Rock outcrop complex, 30 to 50 percent slopes221F11461559025773mt65119971:24000
Winfall-Courville complex, dry, 8 to 30 percent slopes138E1016155821574hmt65119971:24000
Winfall-Courville complex, 30 to 60 percent slopes522F60215613657gnmt65119971:24000
Courville gravelly ashy silt loam, dry, 30 to 50 percent slopes222F4691559045775mt65119971:24000
Cosely-Courville-Dewberry complex, 4 to 15 percent slopes2223D13531648502yyw4mt65119971:24000
Courville family-Andic Glossudalfs-Courville family, moderately deep, complex, glacially scoured mountain slopes74UA12029954472trb5mt65119971:24000
Courville-Cosely-Troybull complex, 8 to 35 percent slopes2323E10531648512yyw6mt65119971:24000
Tevis-Courville complex, 15 to 60 percent slopes2302F7531648492yyw5mt65119971:24000
Courville-Troybull-Tevis complex, 35 to 75 percent slopes2355F931648522yywbmt65119971:24000

Map of Series Extent

Approximate geographic distribution of the COURVILLE 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 .