Official Series Description


Lab Data Summary

Aggregate lab data for the BREMER soil series. This aggregation is based on all pedons with a current taxon name of BREMER, 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 BREMER 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
107BM87195221987MO195022mBremer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.07,-93.4475
107B09N0790S09IA029008Bremer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3597221,-95.0601425
109M89175021989MO175002Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9162472,-93.9829222
115BM88073131988MO073013Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88073141988MO073014Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88121101988MO121010Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88121451988MO121045Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM88121511988MO121051Bremer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89001061989MO001006Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89045021989MO045002Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM89053381989MO053038Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9255556,-92.9798056
115BM90019351990MO019035Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90041031990MO041003Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90041121990MO041012Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90041131990MO041013Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM90151191990MO151019Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4562611,-91.0013083
115BM91041091991MO041009Bremer1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM91151141991MO151014Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM92197141992MO197014Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM94099181993MO099222Bremer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.404219,-90.5231639
116AM90053701990MO053070BREMER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7846667,-92.87175

Water Balance

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BREMER, 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. IA-2010-09-09-18 | Iowa County - 2007

    Typical pattern of soils and parent material in the Colo-Nevin-Nodaway association (Soil Survey of Iowa County, Iowa; 2007).

  2. IA-2011-06-01-21 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Nodaway-Colo-Zook association (Soil Survey of Montgomery County, Iowa; 1989).

  3. IA-2011-06-01-46 | Tama County - 1995

    Typical pattern of soils and parent material in the Colo-Bremer-Nodaway association (Soil Survey of Tama County, Iowa; 1995).

Map Units

Map units containing BREMER 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
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4364214048402y69jia00320081:12000
Bremer silty clay loam, sandy substratum, 0 to 2 percent slopes, rarely flooded104320404028062y8qwia01119771:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4317918597472y8qzia01720081:12000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4319044034132y8qzia02319781:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded43118918679902y69jia02920101:12000
Bremer silty clay loam, 0 to 2 percent slopes30034624243582y69gia02920101:12000
Bremer silty clay loam, 0 to 2 percent slopes43537404803fl75ia05319861:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded431024792832y8qzia06719891:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4316604063102y8qzia07519731:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4343904528572y8qzia09520051:12000
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded4326664076622y8qyia09919751:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4321184080152y8qzia10319791:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded439464091662y69hia12119681:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded4315744093282y8qyia12319711:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4313134127782y69jia12519761:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4311404094802y8qzia12719781:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded4322054095672y69hia12919791:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded4313874098662y69hia13719871:15840
Bremer silty clay loam, sandy substratum, 0 to 2 percent slopes, rarely flooded104313504099052y8qwia13919861:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4312464102162y69jia14519751:20000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded438574129322y69jia15319931:12000
Bremer silty clay loam, 0 to 2 percent slopes, rarely floodedL436253101998fvpdia15319931:12000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4322224104892y69jia15519861:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded433084105902y8qzia15719781:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded43135504114892y8qyia17119891:15840
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded4320104119382y69hia18119751:15840
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded4336484120552y8qzia18319831:15840
Bremer silty clay loam, rarely flooded72111961186235820hy2ks10319731:24000
Bremer silty clay loam, rarely flooded7211758186224620htgks20919731:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507115025320522y69jmo00319861:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded135072724325283342qmtbmo03319881:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007190825320442qnvbmo03319881:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507712525283362qmtbmo03719811:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607432125798842qs1tmo03719811:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded360071725320422qnvbmo03719811:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007617125320502qnvbmo04719821:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607461825445292qs1tmo04719821:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507255125283332qmtbmo04919811:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded360073025320452qnvbmo04919811:24000
Bremer silty clay loam, 1 to 3 percent slopes, rarely flooded135292925444322qs0rmo04919811:24000
Bremer silt loam, 0 to 2 percent slopes, rarely flooded36008183425320532qnvcmo06119521:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507317025283322qmtbmo07519821:24000
Bremer silty clay loam, 1 to 3 percent slopes, rarely flooded1352928525444312qs0rmo07519821:24000
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded26000625285042y69hmo07519821:24000
Bremer silt loam, 0 to 2 percent slopes, rarely flooded36008471925320542qnvcmo08919751:24000
Bremer silt loam, 1 to 3 percent slopes, rarely flooded67025437825755842r0dxmo08919751:24000
Bremer silt loam, 0 to 2 percent slopes, frequently flooded6751087025754982r0d7mo08919751:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607426825755522qs1tmo08919751:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007564225320462qnvbmo09519821:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607465525798912qs1tmo09519821:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507414625283352qmtbmo10119771:24000
Bremer silty clay loam, 1 to 3 percent slopes, rarely flooded1352955325798972qs0rmo10119771:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded360072125320432qnvbmo10119771:24000
Bremer silt loam, 1 to 5 percent slopes125003989888029yt23mo10719701:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007925320472qnvbmo10719701:24000
Bremer silt loam, 0 to 2 percent slopes, rarely flooded36008363025320552qnvcmo12119911:24000
Bremer loam, 0 to 2 percent slopes, overwash, occasionally flooded660641377888592ytn8mo12119911:24000
Bremer silty clay loam, 0 to 2 percent slopes, occasionally flooded26000321325285032y69hmo14719831:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded135072625320562y69jmo14719831:24000
Bremer silty clay loam, 0 to 2 percent slopes, rarely flooded13507106425283312qmtbmo16319911:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007196825320482qnvbmo16519821:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded360745925445282qs1tmo16519821:24000
Bremer silt loam, 0 to 2 percent slopes, rarely flooded36008249725320512qnvcmo17519861:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607424126076872qs1tmo17519861:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007793525320412qnvbmo17719791:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded3607446825445272qs1tmo17719791:24000
Bremer silt loam, 0 to 2 percent slopes, occasionally flooded36007302425320492qnvbmo19519891:24000
Bremer silt loam, 1 to 3 percent slopes, occasionally flooded360743625445302qs1tmo19519891:24000

Map of Series Extent

Approximate geographic distribution of the BREMER 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 .