Official Series Description


Lab Data Summary

Aggregate lab data for the MONTREAL soil series. This aggregation is based on all pedons with a current taxon name of MONTREAL, 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 MONTREAL 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
93B01P0154S2000MI083002Montreal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.4345818,-87.9929199
93B07N0001U05MI083-001Montreal7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9142494,-89.1489716
93B06N0526U05MI083-001Montreal6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9142494,-89.1489716

Water Balance

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

Competing Series

Soil series competing with MONTREAL 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 MONTREAL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the MONTREAL 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 .

There are insufficient data to create the 2D hillslope position figure.

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.

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

Soil series sharing subgroup-level classification with MONTREAL, 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. MI-2010-09-10-09 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Arcadian-Michigamme-Rock outcrop association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  2. MI-2010-09-10-10 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Montreal-Paavola-Arcadian association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  3. MI-2010-09-10-12 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Arcadian-Nipissing-Rock outcrop association (Soil Survey of Keweenaw County Area, Michigan; 2006).

Map Units

Map units containing MONTREAL 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
Montreal-Paavola-Waiska complex, 1 to 8 percent slopes139B11210416078fyywmi06119891:20000
Montreal-Net complex, 0 to 8 percent slopes103B7682416036fyxjmi06119891:20000
Montreal-Paavola complex, 1 to 8 percent slopes89B5092416170fz1vmi06119891:20000
Montreal-Paavola-Michigamme complex, dissected, 1 to 12 percent slopes, rocky116B4899416053fyy2mi06119891:20000
Montreal cobbly fine sandy loam, 1 to 8 percent slopes86B4265416167fz1rmi06119891:20000
Montreal-Paavola-Waiska complex, dissected, 1 to 12 percent slopes140B3691416081fyyzmi06119891:20000
Montreal-Paavola complex, dissected, 1 to 12 percent slopes115B3453416050fyxzmi06119891:20000
Montreal cobbly fine sandy loam, 8 to 15 percent slopes86D1839416168fz1smi06119891:20000
Montreal-Paavola-Waiska complex, 8 to 15 percent slopes139D1232416079fyyxmi06119891:20000
Montreal-Paavola complex, 8 to 15 percent slopes89D924416171fz1wmi06119891:20000
Montreal-Paavola-Dishno complex, dissected, 8 to 35 percent slopes, very rocky, very bouldery173E19313435403gm28mi60520041:24000
Montreal-Paavola-Waiska complex, dissected, 8 to 35 percent slopes, rocky, very bouldery155E17974801612vx4gmi60520041:24000
Montreal-Paavola-Waiska complex, dissected, 1 to 12 percent slopes, rocky, very bouldery155C8832435388gm1smi60520041:24000
Montreal-Paavola-Dishno complex, dissected, 1 to 12 percent slopes, very rocky, very bouldery173C8787801609vx4cmi60520041:24000
Monteal-Dishno-Gratiot complex, 0 to 8 percent slopes, rocky, very bouldery174B5086801608vx4bmi60520041:24000
Montreal-Michigamme complex, 3 to 17 percent slopes, rocky, very stony63D351123782572ktrzmi6061:12000
Montreal-Nevens complex, 1 to 9 percent slopes, very stony49C314623782122ktqjmi6061:12000
Chippewa Harbor-Montreal complex, 0 to 19 percent slopes, very rocky, very stony53D190623782282ktr1mi6061:12000
Montreal loam, 2 to 8 percent slopes, rocky, very stony15C151117179111vnmhmi6061:12000
Montreal-Paavola complex, 4 to 16 percent slopes, rocky, very stony16C113717179121vnmjmi6061:12000

Map of Series Extent

Approximate geographic distribution of the MONTREAL 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 .