Official Series Description


Lab Data Summary

Aggregate lab data for the COLLEGEDALE soil series. This aggregation is based on all pedons with a current taxon name of COLLEGEDALE, 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 COLLEGEDALE 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 COLLEGEDALE 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 COLLEGEDALE 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 COLLEGEDALE 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 COLLEGEDALE 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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Competing Series

Soil series competing with COLLEGEDALE 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 COLLEGEDALE 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 COLLEGEDALE 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 COLLEGEDALE, 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 COLLEGEDALE 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
Collegedale-Rock outcrop complex, 20 to 35 percent slopesCkE3873188737721bz4tn00119781:15840
Collegedale silt loam, 5 to 12 percent slopesCgC3400188737321bz0tn00119781:15840
Collegedale clay, 5 to 12 percent slopes, severely erodedChC32067188737421bz1tn00119781:15840
Collegedale silt loam, 12 to 20 percent slopesCgD1663188737521bz2tn00119781:15840
Collegedale clay, 12 to 20 percent slopes, severely erodedChD3812188737621bz3tn00119781:15840
Collegedale silt loam, 2 to 5 percent slopesCgB249188737221byztn00119781:15840
Collegedale-Rock outcrop complex, 5 to 20 percent slopes, erodedCrD23724524252kljctn01319931:24000
Collegedale silt loam, 5 to 12 percent slopes, erodedCoC23660524250klj9tn01319931:24000
Collegedale silt loam, 5 to 12 percent slopesCoC1446524249klj8tn01319931:24000
Collegedale silt loam, 12 to 25 percent slopes, erodedCoD2425524251kljbtn01319931:24000
Collegedale silt loam, 2 to 5 percent slopesCoB366524248klj7tn01319931:24000
Collegedale-Rock outcrop complex, 20 to 35 percent slopes, erodedCrE2332524253kljdtn01319931:24000
Dewey-Collegedale complex, 6 to 15 percent slopes, severely erodeduDcC32115932050832zvlttn05919541:15840
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD3758032050842zvlvtn05919541:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, moderately erodeduDcC2539033952872zvljtn05919541:15840
Dewey-Collegedale gravelly silt loams, 6 to 15 percent slopesDdC307652509030tkltn05919541:15840
Dewey-Collegedale gravelly silt loams, 15 to 25 percent slopesDdD238352508930tkmtn05919541:15840
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD2209133952822zvlktn05919541:15840
Dewey-Collegedale gravelly silty clay loams, 15 to 25 percent slopes, moderately erodedDdD2178752509230tkqtn05919541:15840
Dewey-Collegedale gravelly silty clay loams, 25 to 50 percent slopes, moderately erodedDdE2145052509730tkrtn05919541:15840
Dewey-Collegedale gravelly silt loams, 25 to 50 percent slopesDdE132652509130tkptn05919541:15840
Dewey-Collegedale gravelly silty clay loams, 6 to 15 percent slopes, moderately erodedDdC260652509330tkntn05919541:15840
Dewey-Collegedale complex, 25 to 40 percent slopes, moderately erodeduDcE244033952782zvlltn05919541:15840
Dewey-Collegedale complex, 25 to 40 percent slopes, severely erodeduDcE332332050852zvlwtn05919541:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, moderately erodeduDcC2101705253192zvljtn06320071:24000
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD262415253212zvlktn06320071:24000
Dewey-Collegedale complex, 25 to 40 percent slopes, moderately erodeduDcE211155253232zvlltn06320071:24000
Collegedale silt loam, 2 to 12 percent slopesCoC131410178401354ktn06519801:15840
Collegedale silt loam, 12 to 25 percent slopesCoD77510178411354ltn06519801:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, moderately erodeduDcC21284732560312zvljtn08919911:24000
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD3872232050872zvlvtn08919911:24000
Collegedale-Talbott-Rock outcrop complex, 5 to 20 percent slopes, erodedCtD28110525448kmrytn08919911:24000
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD2631832560322zvlktn08919911:24000
Collegedale-Talbott-Rock outcrop complex, 20 to 35 percent slopes, erodedCtE25395525449kmrztn08919911:24000
Dewey-Collegedale complex, 6 to 15 percent slopes, severely erodeduDcC3403632050862zvlttn08919911:24000
Collegedale silt loam, 5 to 12 percent slopes, erodedCoC22387525445kmrvtn08919911:24000
Dewey-Collegedale complex, 25 to 40 percent slopes, severely erodeduDcE3219632050882zvlwtn08919911:24000
Dewey-Collegedale complex, 25 to 40 percent slopes, moderately erodeduDcE2188132560332zvlltn08919911:24000
Dewey-Collegedale complex, 2 to 6 percent slopes, moderately erodeduDcB291332560302zvlhtn08919911:24000
Collegedale silty clay loam, 5 to 15 percent slopes, severely erodedCoC3717525446kmrwtn08919911:24000
Collegedale silt loam, 2 to 5 percent slopes, erodedCoB2502525444kmrttn08919911:24000
Collegedale silt loam, 12 to 20 percent slopes, erodedCoD2467525447kmrxtn08919911:24000
Collegedale-Talbott complex, 5 to 12 percent slopes, rockyCkC3011632905p7l9tn09320051:12000
Collegedale-Talbott complex, 12 to 25 percent slopes, rockyCkD1334632906p7lbtn09320051:12000
Collegedale silty clay loam, 5 to 12 percent slopes, severely erodedCeC3327632908p7ldtn09320051:12000
Collegedale silty clay loam, 2 to 5 percent slopes, severely erodedCeB3291632907p7lctn09320051:12000
Collegedale-Loyston-Rock outcrop complex, 2 to 5 percent slopesCgB285632904p7l8tn09320051:12000
Collegedale silty clay loam, 12 to 25 percent slopes, severely erodedCeD3176632909p7lftn09320051:12000
Collegedale silt loam, 5 to 12 percent slopes, erodedCoC218526114kngftn10719991:24000
Collegedale-Talbott complex, 5 to 12 percent slopes, eroded, rockyCtC2186015475041ny9htn12119681:15840
Collegedale-Talbott complex, 12 to 20 percent slopes, eroded, rockyCtD2129715475051ny9jtn12119681:15840
Collegedale-Talbott complex, 2 to 5 percent slopes, eroded, rockyCtB292015475031ny9gtn12119681:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, moderately erodeduDcC2763432560342zvljtn12319741:20000
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD3174032050902zvlvtn12319741:20000
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD2136032560352zvlktn12319741:20000
Dewey-Collegedale complex, 25 to 40 percent slopes, moderately erodeduDcE212305278802zvlltn12319741:20000
Dewey-Collegedale complex, 6 to 15 percent slopes, severely erodeduDcC3102332050892zvlttn12319741:20000
Dewey-Collegedale complex, 2 to 6 percent slopes, moderately erodeduDcB28295278772zvlhtn12319741:20000
Collegedale silt loam, 5 to 12 percent slopes, erodedCoC23165523739kkzttn13919971:24000
Collegedale silt loam, 12 to 25 percent slopes, erodedCoD2373523740kkzvtn13919971:24000
Collegedale silt loam, 2 to 12 percent slopesCgC1082728853sgfdtn14320031:24000
Collegedale silt loam, 12 to 25 percent slopesCgD403728854sgfftn14320031:24000
Collegedale silt loam, 5 to 12 percent slopesCoC32131475634301h3tn14520051:24000
Collegedale silt loam, 12 to 20 percent slopesCoD10501475635301h4tn14520051:24000
Collegedale silt loam, 2 to 5 percent slopesCoB1863349770301hztn14520051:24000
Collegedale-Etowah complex, 12 to 20 percent slopes, severely erodedCeD3372865300592wplttn16319911:20000
Collegedale-Etowah complex, 5 to 12 percent slopes, erodedCeC2370895300582wplstn16319911:20000
Collegedale-Etowah complex, 20 to 35 percent slopes, severely erodedCeE3118235300602wplvtn16319911:20000
Collegedale-Urban land complex, 5 to 20 percent slopesCuD7955530061kskrtn16319911:20000
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD23105284082zvlktn17119801:24000
Dewey-Collegedale complex, 6 to 15 percent slopes, severely erodeduDcC33970132050912zvlttn17919551:15840
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD32874732050922zvlvtn17919551:15840
Dewey-Collegedale complex, 25 to 40 percent slopes, severely erodeduDcE3281532050932zvlwtn17919551:15840
Collegedale-Etowah complex, 12 to 20 percent slopes, severely erodedCeD3130216896362wplttn17919551:15840
Collegedale-Etowah complex, 5 to 12 percent slopes, erodedCeC2109816896352wplstn17919551:15840
Collegedale-Etowah complex, 20 to 35 percent slopes, severely erodedCeE327516896372wplvtn17919551:15840
Dewey-Collegedale complex, 15 to 25 percent slopes, moderately erodeduDcD2128185285472zvlktn60219731:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, moderately erodeduDcC2106685285462zvljtn60219731:15840
Dewey-Collegedale complex, 25 to 40 percent slopes, moderately erodeduDcE242935285482zvlltn60219731:15840
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD350132050942zvlvtn60219731:15840
Dewey-Collegedale complex, 6 to 15 percent slopes, severely erodeduDcC3803532050952zvlttn60919551:20000
Dewey-Collegedale complex, 15 to 25 percent slopes, severely erodeduDcD3366032050962zvlvtn60919551:20000
Dewey-Collegedale gravelly silt loams, 6 to 15 percent slopesDdC1933189948530tkltn60919551:20000
Dewey-Collegedale gravelly silt loams, 15 to 25 percent slopesDdD1640189948630tkmtn60919551:20000
Dewey-Collegedale complex, 2 to 6 percent slopes, severely erodeduDcB3149532050982zvlstn60919551:20000
Dewey-Collegedale complex, 25 to 40 percent slopes, severely erodeduDcE323132050972zvlwtn60919551:20000
Dewey-Collegedale gravelly silt loams, 25 to 50 percent slopesDdE153189948730tkptn60919551:20000

Map of Series Extent

Approximate geographic distribution of the COLLEGEDALE 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 .