Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with AGASSIZ 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 AGASSIZ 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 AGASSIZ 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 terrace figure.

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Soil series sharing subgroup-level classification with AGASSIZ, 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 AGASSIZ 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
Rodie-Shalcleav-Agassiz association4204275475030hy9knv76519861:24000
Agassiz-Croesus-Rubble land association10103945474862hy44nv76519861:24000
Amene-Ekim-Agassiz assocation5612620475056hybdnv76519861:24000
Agassiz-Skutum-Lizzant complex, 25 to 70 percent slopesDRG1979528102622trdnut0131:24000
Senchert-Calfhollow-Agassiz complex, 5 to 35 percent slopesQuC549525037352pw0cut0131:24000
Starvation-Isbell-Agassiz complex, 15 to 60 percent slopes, very stonySNF278814280951jy1lut0131:24000
Agassiz-Rock outcrop-Sheep Creek association, 25 to 75 percent slopes, extremely stonySRG68714260641jvy2ut0131:24000
Agassiz-Picayune association, very steepAGG4887481316j4vbut60219691:20000
Elzinga-Agassiz association, steepEMF855481345j4w8ut60219691:20000
AGASSIZ-DATEMAN ASSOCIATION, ERODEDADG214318482657j67lut60319681:20000
AGASSIZ-BRADSHAW ASSOCIATION, ERODEDABG29508482656j67kut60319681:20000
BICKMORE-SHEEP CREEK ASSOCIATION, ERODEDBLG28423482675j685ut60319681:20000
SHEEP CREEK-AGASSIZ ASSOCIATION, ERODEDSOG26259482826j6f1ut60319681:20000
BRADSHAW-AGASSIZ ASSOCIATION, ERODEDBSG25012482676j686ut60319681:20000
MULT-AGASSIZ ASSOCIATIONMNE3717482772j6c9ut60319681:20000
AGASSIZ VERY COBBLY SILT LOAM, 6 TO 30 PERCENT SLOPESAAE2927482654j67hut60319681:20000
AGASSIZ-ELWOOD ASSOCIATION, ERODEDAEG22717482658j67mut60319681:20000
PICAYUNE-AGASSIZ ASSOCIATION, ERODEDPOG22554482794j6d0ut60319681:20000
AGASSIZ VERY COBBLY SILT LOAM, 30 TO 70 PERCENT SLOPES,ERODEDAAG21817482655j67jut60319681:20000
POLELINE-AGASSIZ ASSOCIATION, ERODEDPSG21671482796j6d2ut60319681:20000
AGASSIZ-GORING ASSOCIATIONAGE1548482659j67nut60319681:20000
HOSKIN-ELZINGA ASSOCIATION, ERODEDHMG21510482731j69zut60319681:20000
AGASSIZ-GORING ASSOCIATION, ERODEDAGG21444482660j67put60319681:20000
BICKMORE-AGASSIZ ASSOCIATION, ERODEDBKG21338482674j684ut60319681:20000
LUCKY STAR-RED SPUR COMPLEX, 6 TO 30 PERCENT SLOPESLWE1123482764j6c1ut60319681:20000
MULT-AGASSIZ ASSOCIATION, ERODEDMNG21081482773j6cbut60319681:20000
ELWOOD-AGASSIZ ASSOCIATIONEGE999482712j69cut60319681:20000
MULT-LUCKY STAR ASSOCIATIONMSE668482774j6ccut60319681:20000
Agassiz-Rock outcrop complex, 25 to 60 percent slopesACF8030503800jx7mut60419801:24000
Mult-Agassiz complex, 10 to 25 percent slopesMCD2340503876jxb2ut60419801:24000
Agassiz-Mult complex, 10 to 25 percent slopesAAD2030503797jx7jut60419801:24000
Agassiz-Richville complex, 10 to 60 percent slopesABF1250503799jx7lut60419801:24000
Agassiz-Mult complex, 25 to 60 percent slopesAAF1230503798jx7kut60419801:24000
Richens-Agassiz complex, 25 to 60 percent slopesRGF550503895jxbput60419801:24000
Agassiz-Rock outcrop complex, 30 to 70 percent slopesAbF19575482445j60rut60819811:24000
Agassiz very stony loam, 30 to 70 percent slopesAaF2057482444j60qut60819811:24000
Calpac-Agassiz complex, 30 to 70 percent slopesCbF1886482476j61rut60819811:24000
Agassiz-Rock outcrop complex, 40 to 70 percent slopesAaG12030506504k01vut60919741:24000
Geertsen-Agassiz complex, 30 to 70 percent slopesGcG5005506549k039ut60919741:24000
Agassiz-Rock outcrop complex, shallow, 40 to 70 percent slopesAbG2320506505k01wut60919741:24000
Agassiz-Geertsen-Rock outcrop association, very steepAGG1555506503k01tut60919741:24000
Bradshaw-Agassiz association, steepBEG9795482868j6gdut61219671:20000
Agassiz association, very steepAGG2573482865j6g9ut61219671:20000
Horrocks-Agassiz very cobbly loams, 30 to 70 percent slopes14316114508187k1t4ut61319991:24000
Hades-Agassiz-Rock outcrop complex, 30 to 70 percent slopes13611611508180k1sxut61319991:24000
Agassiz-Rock outcrop complex, 30 to 70 percent slopes1016240508227k1vfut61319991:24000
Agassiz-Wallsburg association, very steepAWF608504175jxmqut62219671:24000
Burgi-Agassiz association, very steepBXF576504202jxnlut62219671:24000
Agassiz very cobbly loam, 25 to 60 percent slopesAGF446504174jxmput62219671:24000
Agassiz channery silt loam, 10 to 40 percent slopes752266756857tdkrut6471:24000
Agassiz-Bezzant family, very stony-Rock outcrop complex, 30 to 70 percent slopes1032049757982tfr1ut6471:24000
Agassiz channery silt loam, 40 to 70 percent slopes781957757481tf6wut6471:24000
Agassiz-Abes-Rock outcrop complex, 15 to 70 percent slopes1041733757981tfr0ut6471:24000
Agassiz, extremely stony-Onkeyo, rubbly-Bradshaw families association, 30 to 70 percent slopesR35562623909ny73ut6471:24000
Bezzant family, very stony-Agassiz association, 30 to 70 percent slopes40-78265757990tfr9ut6471:24000
Agassiz-Abes association, 15 to 70 percent slopes70-78146757482tf6xut6471:24000
Agassiz-Hourglass families-Rock outcrop complex, 30 to 70 percent slopes103625182nzk5ut6491:24000
Agassiz family-Rock outcrop complex, 15 to 50 percent slopes104581646mj7sut6491:24000
Forsey-Forsey, moderately deep-Agassiz families, association, 30 to 70 percent slopes155581651mj7yut6491:24000
Pernty family-Agassiz family-Rock outcrop complex, 40 to 75 percent slopes182581653mj80ut6491:24000
Pernty family-Agassiz family-Rock outcrop complex, 5 to 40 percent slopes181581655mj82ut6491:24000
Agassiz-Forsey families-Rock outcrop complex, 30 to 70 percent slopes102625183nzk6ut6491:24000
Jebo, extremely stony-Agassiz, rubbly families, complex, 25 to 60 percent slopes634581812397w8ccut6511:24000

Map of Series Extent

Approximate geographic distribution of the AGASSIZ 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 .