Official Series Description


Lab Data Summary

Aggregate lab data for the ZIMMERMAN soil series. This aggregation is based on all pedons with a current taxon name of ZIMMERMAN, 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 ZIMMERMAN 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
57UMN2640S1978MN137079 (2640)Zimmerman3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.659729,-92.9840164
88UMN2453S1900MN0612453Zimmerman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6096115,-94.3142166
88UMN2454S1900MN0612454Zimmerman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6023712,-94.3088837
88UMN2811S1978MN0612811Zimmerman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2047049,-93.4748949
88UMN2812S1978MN0612812Zimmerman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.210331,-93.474823
90BUMN1578S1972MN1631578Zimmerman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1100273,-92.9328613
91B40A1698S1960MN141001Zimmerman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5227699,-93.6974564
91B40A1690S1960MN141002Zimmerman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5311012,-93.9121857
91B40A1691S1960MN141003Zimmerman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5269356,-93.9432983
91BUMN1079S1965MN0031079Zimmerman3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.340641,-93.1079636
91B94P0691S1994MN003002Zimmerman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3893623,-93.0757217

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ZIMMERMAN 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 ZIMMERMAN 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 ZIMMERMAN 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 ZIMMERMAN 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 ZIMMERMAN 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 ZIMMERMAN 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 ZIMMERMAN 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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Click the image to view it full size.

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 ZIMMERMAN, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MN-2010-09-08-06 | Cass County - 1997

    Typical pattern of soils and parent material in the Menahga-Markey-Friendship general soil map unit (Soil Survey of Cass County, Minnesota; 1997).

Map Units

Map units containing ZIMMERMAN 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
Zimmerman-Annalake complex, 6 to 18 percent slopes85D59021903766d35mi00119931:20000
Zimmerman-Annalake complex, 0 to 6 percent slopes85B27281903756d34mi00119931:20000
Zimmerman loamy fine sand, 6 to 12 percent slopes84C15371903736d32mi00119931:20000
Zimmerman loamy fine sand, 0 to 6 percent slopes84B14101903726d31mi00119931:20000
Zimmerman-Alcona complex, 25 to 60 percent slopes80F13231903666d2vmi00119931:20000
Zimmerman loamy fine sand, 12 to 18 percent slopes84D6711903746d33mi00119931:20000
Zimmerman-Annalake complex, 6 to 18 percent slopes85D9471913086f27mi00719981:12000
Zimmerman loamy fine sand, 0 to 6 percent slopes84B7011913076f26mi00719981:12000
Zimmerman loamy fine sand, 18 to 35 percent slopes84E3111913226f2pmi00719981:12000
Zimmerman loamy fine sand, 6 to 12 percent slopes84C1321913296f2xmi00719981:12000
Zimmerman fine sand, 0 to 8 percent slopes21B27601905486d8qmi03119881:15840
Zimmerman fine sand, 6 to 18 percent slopes60D8240415233fy2mmi04319851:20000
Zimmerman fine sand, 0 to 6 percent slopes60B8093415232fy2lmi04319851:20000
Zimmerman fine sand, 18 to 35 percent slopes60F1183415234fy2nmi04319851:20000
Zimmerman-Rock outcrop complex, 18 to 35 percent slopes66F912415240fy2vmi04319851:20000
Zimmerman-Rock outcrop complex, 6 to 18 percent slopes66D897415239fy2tmi04319851:20000
Zimmerman loamy fine sand, 0 to 6 percent slopes84B101919586fr6mi06919951:15840
Zimmerman fine sand, 2 to 8 percent slopes90B8821909646dq4mi14119891:15840
Zimmerman fine sand, 1 to 6 percent slopesZmB473043959742q12wmn00319721:15840
Zimmerman fine sand, 6 to 12 percent slopesZmC60433959752wl5zmn00319721:15840
Zimmerman fine sand, 0 to 2 percent slopesZmA41133959732wl5ymn00319721:15840
Urban land-Zimmerman complex, 0 to 8 percent slopesUzB3659885510yqfvmn00319721:15840
Zimmerman fine sand, 12 to 24 percent slopesZmD1171395976f91fmn00319721:15840
Zimmerman loamy fine sand, 1 to 8 percent slopesA60B761830265162x14fmn00719911:24000
Zimmerman-Snellman complex, 15 to 30 percent slopes2020E608825204662qkj7mn00719911:24000
Zimmerman-Snellman complex, 1 to 8 percent slopes2020B516125204642qkj5mn00719911:24000
Zimmerman-Andrusia complex, 1 to 8 percent slopes2017B401925204632qkj4mn00719911:24000
Snellman-Zimmerman complex, 1 to 8 percent slopes, pitted2024B348925204722qkjgmn00719911:24000
Zimmerman fine sand, 0 to 6 percent slopes2034B303025204542qkhxmn00719911:24000
Zimmerman loamy fine sand, 3 to 15 percent slopesA60C172030265172x14hmn00719911:24000
Zimmerman-Andrusia complex, 8 to 15 percent slopes2017C101025204772qkjpmn00719911:24000
Zimmerman-Snellman complex, 8 to 15 percent slopes2020C61825204652qkj6mn00719911:24000
Zimmerman-Andrusia complex, 15 to 30 percent slopes2017E21925204782qkjqmn00719911:24000
Zimmerman-Hiwood complex, 1 to 8 percent slopesA92B13330265182x14jmn00719911:24000
Zimmerman fine sand, banded substratum, 1 to 6 percent slopesD55B2085753285t8vjmn00920071:12000
Zimmerman fine sand, 1 to 6 percent slopesD64B110719140592q12wmn00920071:12000
Zimmerman fine sand, banded substratum, 12 to 35 percent slopesD55E574753282t8vfmn00920071:12000
Anoka and Zimmerman soils, terrace, 2 to 6 percent slopesD1B413729079sgnpmn00920071:12000
Zimmerman fine sand, banded substratum, 6 to 12 percent slopesD55C296753284t8vhmn00920071:12000
Zimmerman fine sand, 6 to 12 percent slopesD64C16219140602wl5zmn00920071:12000
Zimmerman fine sand, 0 to 2 percent slopesD64A14719140352wl5ymn00920071:12000
Anoka and Zimmerman soils, terrace, 6 to 12 percent slopesD1C59729080sgnqmn00920071:12000
Zimmerman fine sand, 12 to 30 percent slopesD64E301914064227r0mn00920071:12000
Guida-Zimmerman-Redby complex, 0 to 8 percent slopesB253B2480231151412z32lmn02119931:20000
Zimmerman loamy fine sand, 1 to 8 percent slopesA60B1800830265212x14fmn02119931:20000
Zimmerman-Hiwood complex, 1 to 8 percent slopesA92B1002030265232x14jmn02119931:20000
Zimmerman-Guida complex, 1 to 18 percent slopesB254D783931151432z32kmn02119931:20000
Zimmerman loamy fine sand, 3 to 15 percent slopesA60C338530265222x14hmn02119931:20000
Zimmerman fine sand, moraine, 1 to 8 percent slopes158B297397706fbv7mn02119931:20000
Zimmerman fine sand, 1 to 6 percent slopes158B190603965462q12wmn02519901:15840
Zimmerman fine sand, 6 to 12 percent slopes158C18123965472wl5zmn02519901:15840
Zimmerman-Andrusia complex, 1 to 8 percent slopes2017B94026036422qkj4mn02919931:20000
Zimmerman-Andrusia complex, 8 to 15 percent slopes2017C38226036442qkjpmn02919931:20000
Zimmerman-Snellman complex, 15 to 30 percent slopes2020E34426036392qkj7mn02919931:20000
Snellman-Zimmerman complex, 1 to 8 percent slopes, pitted2024B19326036502qkjgmn02919931:20000
Zimmerman-Snellman complex, 8 to 15 percent slopes2020C19026036382qkj6mn02919931:20000
Zimmerman-Snellman complex, 1 to 8 percent slopes2020B15226036372qkj5mn02919931:20000
Zimmerman-Andrusia complex, 15 to 30 percent slopes2017E9526036432qkjqmn02919931:20000
Zimmerman loamy fine sand, 1 to 6 percent slopesD62B1871025104021vvlfmn03520091:24000
Zimmerman loamy fine sand, 0 to 2 percent slopesD62A1523125104031vvlgmn03520091:24000
Zimmerman-Urban land complex, 0 to 6 percent slopesD69B266325104102lvb3mn03520091:24000
Zimmerman loamy fine sand, 6 to 15 percent slopesD62C205425104092lvb0mn03520091:24000
Zimmerman loamy fine sand, 0 to 3 percent slopes, pittedD63A113625104001vvlcmn03520091:24000
Anoka and Zimmerman soils, terrace, 2 to 6 percent slopesD1B1122451658h4zmmn05320011:12000
Anoka and Zimmerman soils, terrace, 6 to 12 percent slopesD1C295451657h4zlmn05320011:12000
Zimmerman loamy fine sand, 1 to 8 percent slopesA60B16574365592x14fmn05719981:24000
Zimmerman loamy fine sand, 3 to 15 percent slopesA60C604365602x14hmn05719981:24000
Zimmerman fine sand, 1 to 6 percent slopesZu550653984152q12wmn05919561:20000
Zimmerman loamy fine sand and fine sand, 7 to 12 percent slopesZp7011398412fcl0mn05919561:20000
Zimmerman fine sand, 6 to 12 percent slopesZn48603984112wl5zmn05919561:20000
Zimmerman fine sand, 0 to 2 percent slopesZf14833984082wl5ymn05919561:20000
Zimmerman loamy fine sand and fine sand, 12 to 18 percent slopesZr500398413fcl1mn05919561:20000
Zimmerman fine sand, 12 to 18 percent slopes, moderately erodedZx459398417fcl5mn05919561:20000
Zimmerman fine sand, 12 to 18 percent slopesZh238398410fckymn05919561:20000
Zimmerman fine sand, 7 to 12 percent slopes, severely erodedZs57398414fcl2mn05919561:20000
Zimmerman loamy fine sand, 1 to 8 percent slopesA60B3574830265322x14fmn06119821:24000
Guida-Zimmerman-Redby complex, 0 to 8 percent slopesB253B2054831151442z32lmn06119821:24000
Zimmerman-Guida complex, 1 to 18 percent slopesB254D816731151462z32kmn06119821:24000
Zimmerman loamy fine sand, 3 to 15 percent slopesA60C21831846422x14hmn06119821:24000
Zimmerman fine sand, 1 to 6 percent slopesD60B576616764812q12wmn09520061:12000
Zimmerman fine sand, 0 to 2 percent slopesD60A96316764802wl5ymn09520061:12000
Zimmerman fine sand, 6 to 12 percent slopesD60C62416764822wl5zmn09520061:12000
Zimmerman fine sand, 12 to 30 percent slopesD60E22416764831t8j3mn09520061:12000
Zimmerman loamy fine sand, 1 to 4 percent slopes158B5668400349fflhmn09719871:20000
Urban land-Zimmerman complex, 1 to 8 percent slopes859B736016772811t9bvmn12319781:15840
Zimmerman fine sand, 1 to 6 percent slopes158B332816772032q12wmn12319781:15840
Zimmerman fine sand, 6 to 12 percent slopes158C86316772042wl5zmn12319781:15840
Zimmerman loamy fine sand, 12 to 25 percent slopes158D62116772051t98dmn12319781:15840
Zimmerman fine sand, 1 to 6 percent slopes158B3797394819f7v3mn13519991:24000
Zimmerman fine sand, 1 to 6 percent slopes158B310534314562q12wmn14119941:15840
Zimmerman fine sand, 0 to 2 percent slopes158A209674314552wl5ymn14119941:15840
Zimmerman fine sand, 6 to 12 percent slopes158C63634314572wl5zmn14119941:15840
Zimmerman fine sand, thick solum, 1 to 6 percent slopes1258B2966431445ggylmn14119941:15840
Zimmerman fine sand, thick solum, 6 to 12 percent slopes1258C2523431446ggymmn14119941:15840
Zimmerman fine sand, 12 to 25 percent slopes158E1481431458ggz0mn14119941:15840
Zimmerman fine sand, thick solum, 12 to 35 percent slopes1258E1054431447ggynmn14119941:15840
Zimmerman loamy fine sand, 1 to 6 percent slopes158B939428503gcwpmn15319851:20000
Zimmerman loamy fine sand, 6 to 15 percent slopes158C185428504gcwqmn15319851:20000
Zimmerman fine sand, 1 to 6 percent slopes158B282116770682q12wmn16319781:15840
Urban land-Zimmerman complex, 1 to 8 percent slopes859B161116771461t96hmn16319781:15840
Zimmerman fine sand, 6 to 12 percent slopes158C144116770692wl5zmn16319781:15840
Zimmerman loamy fine sand, 12 to 25 percent slopes158D69116770701t941mn16319781:15840
Zimmerman fine sand, 3 to 6 percent slopes158B166433670gk8cmn17119981:12000
Zimmerman fine sand, 0 to 3 percent slopes158A110433673gk8gmn17119981:12000
Zimmerman fine sand, 6 to 12 percent slopes158C36433691gk91mn17119981:12000
Zimmerman fine sand, 12 to 25 percent slopes158E34433690gk90mn17119981:12000
Zimmmerman-Soderville complex, 2 to 8 percent slopesB251B61629437972dv56mn62520151:24000

Map of Series Extent

Approximate geographic distribution of the ZIMMERMAN 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 .