Official Series Description


Lab Data Summary

Aggregate lab data for the WHALAN soil series. This aggregation is based on all pedons with a current taxon name of WHALAN, 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 WHALAN 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
104X45-207-11964IA089006Whalan1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.329875,-92.1079389
104UMN2161S1976MN1092161Whalan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8459702,-92.5695877
105X191205-4-1S1959IA191021Whalan1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4138845,-92.0095679
90BUMN1991S1974MN1631991Whalan3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8627014,-92.7917938

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WHALAN 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 WHALAN 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 WHALAN 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 WHALAN 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 WHALAN 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 WHALAN 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 WHALAN 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.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with WHALAN, 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 WHALAN 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
Whalan loam, 20 to 30 inches to limestone, till plain, 2 to 9 percent slopes207C1904028592xl2hia01119771:15840
Whalan silt loam, 20 to 30 inches to limestone, till plain, 2 to 5 percent slopes207B4704032192xl2wia01919781:15840
Whalan silt loam, 30 to 40 inches to limestone, till plain, 2 to 5 percent slopes205B4314032182xl2yia01919781:15840
Whalan loam, 20 to 30 inches to limestone, 2 to 5 percent slope207B653405021flg6ia05519841:15840
Whalan loam, 30 to 40 inches to limestone, 2 to 5 percent slope205B468405020flg5ia05519841:15840
Whalan loam, 20 to 30 inches to limestone, 5 to 9 percent slope207C394405022flg7ia05519841:15840
Whalan silt loam, till plain, 2 to 5 percent slopes806B2004060422xl2ria06719891:15840
Whalan loam, moderately deep, 2 to 5 percent slopes207B205407036fnk6ia08919691:15840
Whalan loam, moderately deep, 5 to 9 percent slopes207C180406921fnfhia08919691:15840
Whalan loam, 20 to 30 inches to limestone, till plain, 5 to 9 percent slopes, eroded207C21494085802xl2mia11319701:15840
Whalan loam, 30 to 40 inches to limestone, till plain, 2 to 5 percent slopes205B5444096452xl2dia13119711:15840
Whalan loam, 30 to 40 inches to limestone, till plain, 5 to 9 percent slopes205C3984096462xl2jia13119711:15840
Whalan silt loam, 2 to 5 percent slopes806B1086766676tqshia19120051:12000
Whalan silt loam, 5 to 9 percent slopes, moderately eroded806C2864766677tqsjia19120051:12000
Whalan silt loam, 9 to 14 percent slopes806D385766678tqskia19120051:12000
Whalan and NewGlarus silt loams, 5 to 10 percent slopes, eroded561C26614832121lsdkil00720061:12000
Whalan and NewGlarus silt loams, 10 to 15 percent slopes, eroded561D26214832131lsdlil00720061:12000
Whalan and NewGlarus silt loams, 2 to 5 percent slopes561B261998606pz3il00720061:12000
Whalan silt loam, 2 to 4 percent slopes509B8929888841260hil09120031:12000
Whalan silt loam, 0 to 2 percent slopes509A6489888831260gil09120031:12000
Whalan loam, 10 to 18 percent slopes509D83194212510mc4il10320041:12000
Whalan loam, 18 to 35 percent slopes509F27994212910mc8il10320041:12000
Whalan loam, 2 to 5 percent slopes509B26094212410mc3il10320041:12000
Whalan loam, 5 to 10 percent slopes, eroded509C24702208643703fil14120051:12000
Whalan loam, 10 to 18 percent slopes, eroded509D2214513989501hyqfil14120051:12000
Whalan loam, 18 to 25 percent slopes, eroded509E2131913989511hyqgil14120051:12000
Whalan loam, 2 to 5 percent slopes509B574208642703dil14120051:12000
Whalan loam, 10 to 18 percent slopes509D214788521lmvxil14120051:12000
Whalan loam, 2 to 5 percent slopes509B590793076vm83il19520031:12000
Whalan and NewGlarus silt loams, 5 to 10 percent slopes, eroded561C229221741275v60il20119971:12000
Whalan and NewGlarus silt loams, 10 to 15 percent slopes, eroded561D220221741285v61il20119971:12000
Whalan and NewGlarus silt loams, 2 to 5 percent slopes561B4851741265v5zil20119971:12000
Whalan loam, 1 to 6 percent slopes67B5051888036bgfmi07519791:15840
Dubuque and Whalan silt loams, 18 to 45 percent slopesDx2264422167272ddpbmn04520081:12000
Dubuque and Whalan silt loams, 12 to 17 percent slopes, moderately erodedDv1017022167322ddphmn04520081:12000
Dubuque and Whalan silt loams, 7 to 11 percent slopes, moderately erodedDu566022167302ddpfmn04520081:12000
Dubuque and Whalan silt loams, 2 to 6 percent slopesDs314422167282ddpcmn04520081:12000
Whalan loam, 1 to 6 percent slopes340B3805400765fg0xmn10919771:15840
Whalan loam, 6 to 12 percent slopes340C2052400766fg0ymn10919771:15840
Whalan silt loam, shallow, 12 to 18 percent slopes, moderately erodedWsD268822164512dddfmn15720081:12000
Whalan silt loam, shallow, 6 to 12 percent slopes, moderately erodedWsC243722164562dddlmn15720081:12000
Whalan silt loam, 6 to 12 percent slopes, moderately erodedWhC236122164492dddcmn15720081:12000
Whalan silt loam, 12 to 18 percent slopes, moderately erodedWhD234022164472ddd9mn15720081:12000
Whalan silt loam, 18 to 25 percent slopesWsE24922164522dddgmn15720081:12000
Whalan silt loam, 25 to 35 percent slopesWsF21822164542dddjmn15720081:12000
Whalan silt loam, 2 to 6 percent slopesWhB16522164482dddbmn15720081:12000
Whalan silt loam, shallow, 2 to 6 percent slopesWsB9022164532dddhmn15720081:12000
Whalan silt loam, 1 to 6 percent slopes340B93016771001t950mn16319781:15840
Whalan silt loam, 6 to 12 percent slopes340C85616771011t951mn16319781:15840
Whalan silt loam, 6 to 12 percent slopes, erodedWxC23273753607t95xwi02519721:15840
Whalan silt loam, 12 to 20 percent slopes, erodedWxD22682753608t95ywi02519721:15840
Whalan silt loam, 2 to 6 percent slopesWxB2046753606t95wwi02519721:15840
Whalan loam, 20 to 30 percent slopes, erodedWwE2990753605t95vwi02519721:15840
Whalan silt loam, 6 to 12 percent slopes, moderately erodedWlC25862425394g8ndwi04519691:12000
Whalan silt loam, 2 to 6 percent slopes, moderately erodedWlB22448425393g8ncwi04519691:12000
Whalan silt loam, 12 to 20 percent slopes, moderately erodedWlD21011425395g8nfwi04519691:12000
Whalan loam, 6 to 12 percent slopes, moderately erodedWhC2542425392g8nbwi04519691:12000
Whalan loam, 2 to 6 percent slopes, moderately erodedWhB2472425391g8n9wi04519691:12000
Whalan loam, 2 to 6 percent slopesWxB2169423846g71gwi05519761:15840
Whalan loam, 6 to 12 percent slopes, erodedWxC2740423847g71hwi05519761:15840
Whalan variant silt loam, 0 to 3 percent slopesWyA291423848g71jwi05519761:15840
Dorerton, very stony-Boone-Whalan complex, 20 to 60 percent slopes1105F581816986131v0jzwi09320061:12000
Whalan silt loam, 6 to 12 percent slopes, moderately eroded823C2417616931611ttw3wi09320061:12000
Whalan silt loam, 12 to 20 percent slopes, moderately eroded823D2398716931581ttw0wi09320061:12000
Whalan silt loam, 2 to 6 percent slopes, moderately eroded823B2307816931591ttw1wi09320061:12000
Whalan silt loam, 20 to 30 percent slopes823E297716931601ttw2wi09320061:12000
Whalan silt loam, strath terrace, 6 to 12 percent slopes, moderately eroded803C2177916932061ttxkwi09320061:12000
Whalan silt loam, strath terrace, 12 to 20 percent slopes, moderately eroded803D272216932041ttxhwi09320061:12000
Whalan silt loam, strath terrace, 20 to 30 percent slopes803E14516932051ttxjwi09320061:12000
Whalan fine sandy loam, 2 to 6 percent slopes800B9517012351v38kwi09320061:12000
Whalan fine sandy loam, 6 to 12 percent slopes800C9217012361v38lwi09320061:12000
Whalan loam, 6 to 12 percent slopes, erodedWlC24505426412g9q7wi10519701:20000
Whalan loam, 2 to 6 percent slopes, erodedWlB24129426411g9q6wi10519701:20000
Whalan sandy loam, 2 to 6 percent slopes, erodedWhB21380426408g9q3wi10519701:20000
Whalan loam, 12 to 20 percent slopes, erodedWlD2555426413g9q8wi10519701:20000
Whalan sandy loam, 6 to 12 percent slopes, erodedWhC2546426409g9q4wi10519701:20000
Whalan loam, 0 to 2 percent slopesWlA275426410g9q5wi10519701:20000
Whalan silt loam, 2 to 6 percent slopesWhB2734422208g5bmwi10919751:15840
Whalan silt loam, 6 to 12 percent slopes, erodedWhC22426422209g5bnwi10919751:15840
Whalan silt loam, 12 to 25 percent slopes, erodedWhD21319422210g5bpwi10919751:15840
Whalan loam, 2 to 6 percent slopesWhB655422761g5xgwi13519821:15840
Whalan variant loamy fine sand, 2 to 6 percent slopesWvB383422763g5xjwi13519821:15840
Whalan loam, 6 to 12 percent slopes, erodedWhC2345422762g5xhwi13519821:15840
Whalan silt loam, 2 to 6 percent slopesWhB1951422834g5ztwi13919771:20000
Whalan loamy fine sand, 2 to 8 percent slopesWfB353422833g5zswi13919771:20000
Whalan silt loam, 6 to 12 percent slopes, erodedWhC2216422835g5zvwi13919771:20000
Whalan silt loam, 2 to 6 percent slopesWpB2783422911g629wi60019761:15840

Map of Series Extent

Approximate geographic distribution of the WHALAN 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 .