Official Series Description


Lab Data Summary

Aggregate lab data for the GIESE soil series. This aggregation is based on all pedons with a current taxon name of GIESE, 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 GIESE 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
90A40A1673S1957MN095002Giese6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.770546,-93.5871735
90A40A1674S1957MN095005Giese6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8686028,-93.6849594
90AUMN4688S1992MN0014688Giese3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3383026,-93.0544128
90AUMN4697S1992MN0014697Giese3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1795158,-93.2207336

Water Balance

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

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

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Competing Series

Soil series competing with GIESE 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 GIESE 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 GIESE 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 hills figure.

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 GIESE, 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 GIESE 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
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A2842931824702z19zmn00119961:20000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A189231152142z19qmn00119961:20000
Twig and Giese soils990110432985gjk8mn00119961:20000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A1169631152172z19qmn00920071:12000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A883231824742z19zmn00920071:12000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A288131824712z19zmn01719731:20000
Ahmeek-Mesaba, stony-Giese, rubbly complex, 0 to 18 percent slopes, very rockyA2-41D321827746012rn04mn03120131:24000
Greysolon-Normanna-Giese, rubbly complex, 0 to 8 percent slopes, very rockyA2-40B214627745782rn03mn03120131:24000
Mesaba, stony-Giese, rubbly-Barto, stony complex, 0 to 18 percent slopes, very rockyA2-30D185927746682rn02mn03120131:24000
Twig-Tacoosh-Giese complex, 0 to 1 percent slopes, depressionalA3-11A132527746282rmzhmn03120131:24000
Greysolon-Giese, rubbly-Barto, stony complex, 0 to 8 percent slopes, very rockyA2-30B120927746372rn01mn03120131:24000
Hermantown-Canosia-Giese, depressional complex, 0 to 3 percent slopesA3-40A92429437392rmzsmn03120131:24000
Normanna-Giese, depressional complex, 0 to 8 percent slopes, pittedA3-41B38427747212rmztmn03120131:24000
Giese, rubbly-Tacoosh-Rifle complex, 0 to 2 percent slopesA3-10A26627747002rn05mn03120131:24000
Giese muck, 0 to 2 percent slopes, rubblyA3-13A4927745552rmzkmn03120131:24000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A18931152152z19qmn05919561:20000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A1469231152192z19qmn06520061:12000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A1087031824762z19zmn06520061:12000
Cathro, Twig, and Giese, stony, soils, depressional, 0 to 1 percent slopesC96A22116735171t5ffmn06520061:12000
Twig-Tacoosh-Giese complex, 0 to 1 percent slopes, depressionalA3-11A1017527421192rmzhmn07520131:24000
Normanna-Giese, depressional complex, 0 to 8 percent slopesA3-41B720927421302zw3vmn07520131:24000
Hermantown-Canosia-Giese, depressional complex, 0 to 3 percent slopesA3-40A418327421282zw3tmn07520131:24000
Ahmeek-Mesaba, stony-Giese, rubbly complex, 0 to 18 percent slopes, very rockyA2-41D336527421382rn04mn07520131:24000
Giese muck, depressional, 0 to 1 percent slopesA3-12A287927421202rmzjmn07520131:24000
Mesaba, stony-Giese, rubbly-Barto, stony complex, 0 to 18 percent slopes, very rockyA2-30D272427421362rn02mn07520131:24000
Greysolon-Normanna-Giese, rubbly complex, 0 to 8 percent slopes, very rockyA2-40B220127421372rn03mn07520131:24000
Giese muck, 0 to 2 percent slopes, rubblyA3-13A211627421212rmzkmn07520131:24000
Giese, rubbly-Tacoosh-Rifle complex, 0 to 2 percent slopesA3-10A198527421392rn05mn07520131:24000
Greysolon-Giese, rubbly-Barto, stony complex, 0 to 8 percent slopes, very rockyA2-30B11127421352rn01mn07520131:24000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A2699731152202z19qmn09520061:12000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A493231824772z19zmn09520061:12000
Cathro, Twig, and Giese, stony, soils, depressional, 0 to 1 percent slopesC96A31816764181t8g0mn09520061:12000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A976531824722z19zmn09719871:20000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A823831152162z19qmn09719871:20000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A834731824752z19zmn11520091:24000
Giese, stony-Cathro complex, 0 to 1 percent slopes, frequently pondedC47A64853314102308xvmn11520091:24000
Cebana-Giese, frequently ponded-Freer complex, 0 to 3 percent slopes, stonyC126A312931152182z19qmn11520091:24000
Cebana-Giese, frequently ponded-Ronneby complex, 0 to 3 percent slopes, stonyC4A46331824732z19zmn14119941:15840
Hermantown-Canosia-Giese, depressional, complex, 0 to 3 percent slopesF135A23825449572h2tbmn61520071:24000
Normanna-Giese, depressional, complex, pitted, 0 to 8 percent slopesF140B9848449577h2thmn61520071:24000
Giese muck, depressional, 0 to 1 percent slopesF134A8751449571h2t9mn61520071:24000
Twig-Tacoosh-Giese complex, depressional, 0 to 1 percent slopesF150A730764968tp0dmn61520071:24000
Giese muck, 0 to 2 percent slopes, rubblyF146A21764972tp0jmn61520071:24000
Hermantown-Canosia-Giese, depressional, complex, 0 to 3 percent slopesF135A1183017158491vlgzmn61920091:24000
Normanna-Giese, depressional, complex, pitted, 0 to 8 percent slopesF140B366117158541vlh4mn61920091:24000
Giese muck, depressional, 0 to 1 percent slopeF134A297217158481vlgymn61920091:24000
Giese muck, 0 to 2 percent slopes, rubblyF146A143517158601vlhbmn61920091:24000
Twig-Tacoosh-Giese complex, depressional, 0 to 1 percent slopesF150A39017158641vlhgmn61920091:24000
Giese muck, 0 to 1 percent slopes, very stony631A235656106q0qqwi01320041:12000
Giese, stony-Cathro complex, 0 to 1 percent slopes, frequently pondedC47A703314115308xvwi01320041:12000
Milaca-Mora-Giese complex, 0 to 15 percent slopes, very stony1053C2694781548v787wi03120051:12000
Giese, stony-Cathro complex, 0 to 1 percent slopes, frequently pondedC47A21443314128308xvwi03120051:12000
Giese muck, 0 to 1 percent slopes, very stony631A1091781397v73cwi03120051:12000

Map of Series Extent

Approximate geographic distribution of the GIESE 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 .