Official Series Description


Lab Data Summary

Aggregate lab data for the YALMER soil series. This aggregation is based on all pedons with a current taxon name of YALMER, 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 YALMER 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
9279P0079S1978WI003001Yalmer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0711098,-90.4166641
9279P0080S1978WI003002Yalmer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0702782,-90.414444
9279P0082S1978WI003004Yalmer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0758324,-90.4233322
93B40A1967S1966MI061002Yalmer5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0422211,-88.5717163
94A40A1968S1966MI085001Yalmer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.109169,-85.5910568

Water Balance

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

Competing Series

Soil series competing with YALMER 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 YALMER 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 YALMER 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 YALMER, 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-2010-09-07-19 | Marquette County - 2007

    Typical pattern of soils and parent material in the Skanee-Munising-Gay association (Soil Survey of Marquette County, Michigan; 2007).

  2. MI-2010-09-10-11 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Skanee-Munising-Gay association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  3. MI-2010-09-10-13 | Keweenaw County Area - 2006

    Typical pattern of soils and parent material in the Munising-Yalmer-Garlic association (Soil Survey of Keweenaw County Area, Michigan; 2006).

  4. MI-2012-02-06-18 | Houghton County Area - October 1991

    Diagrammatic cross section of Houghton County showing the topography, elevation, general soil texture, landforms, and dominant soils and their drainage class (Soil Survey of Houghton County Area, Michigan; October 1991).

  5. MI-2012-02-06-19 | Houghton County Area - October 1991

    Typical pattern of soils and parent material in the Munising-Yalmer association (Soil Survey of Houghton County Area, Michigan; October 1991).

Map Units

Map units containing YALMER 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
Munising-Yalmer-Frohling complex, calcareous substratum, 1 to 6 percent slopes35B874914552631kv9zmi00320071:24000
Munising-Yalmer complex, 1 to 12 percent slopes, dissected, very stony145C325014553191kvcsmi00320071:24000
Munising-Yalmer-Frohling complex, calcareous substratum, 1 to 12 percent slopes, dissected272C136714554121kvgsmi00320071:24000
Munising-Yalmer complex, 1 to 6 percent slopes25B135814552571kv9smi00320071:24000
Munising-Yalmer complex, 6 to 18 percent slopes25D38614552581kv9tmi00320071:24000
Munising-Yalmer loamy sands, 1 to 8 percent slopes23B22492414958fxsrmi01319841:20000
Munising-Yalmer loamy sands, dissected, 1 to 8 percent slopes88B7960415033fxw5mi01319841:20000
Yalmer-Assinins complex, 0 to 6 percent slopes111B5811414932fxrxmi01319841:20000
Munising-Yalmer loamy sands, 8 to 15 percent slopes23D4923414959fxssmi01319841:20000
Munising-Yalmer loamy sands, dissected, 8 to 35 percent slopes88D4777415034fxw6mi01319841:20000
Yalmer loamy sand, 1 to 8 percent slopes47B2333414985fxtmmi01319841:20000
Yalmer-Munising loamy sands, 15 to 35 percent slopes69E1568415011fxvgmi01319841:20000
Yalmer loamy sand, rocky, 1 to 8 percent slopes106B281414925fxrpmi01319841:20000
Yalmer sand, 0 to 6 percent slopesYaB72915881291q9kzmi04119691:24000
Yalmer sand, 6 to 18 percent slopesYaD5515881301q9l0mi04119691:24000
Munising-Yalmer complex, dissected, 1 to 12 percent slopes98B15027416182fz27mi06119891:20000
Munising-Yalmer complex, 1 to 8 percent slopes33B13954416119fz06mi06119891:20000
Munising-Yalmer complex, dissected, 8 to 35 percent slopes98D7676416183fz28mi06119891:20000
Frohling-Yalmer complex, dissected, 15 to 60 percent slopes98E5861416184fz29mi06119891:20000
Yalmer-Assinins sands, 0 to 8 percent slopes79B5497416162fz1lmi06119891:20000
Munising-Yalmer complex, 8 to 15 percent slopes33D768416120fz07mi06119891:20000
Munising-Yalmer complex, 1 to 12 percent slopes, dissected, very stony145C5954395078f83gmi10319991:24000
Munising-Onota-Yalmer complex, 1 to 12 percent slopes, dissected, stony158C2452395102f847mi10319991:24000
Munising-Yalmer complex, 1 to 6 percent slopes25B2109395175f86lmi10319991:24000
Yalmer-Kalkaska complex, 1 to 6 percent slopes119B1077394999f80xmi10319991:24000
Yalmer fine sand, 1 to 6 percent slopes29B1074395183f86vmi10319991:24000
Munising-Yalmer complex, 6 to 18 percent slopes25D918395176f86mmi10319991:24000
Yalmer-Rubicon-Urban land complex, 4 to 18 percent slopes174D817395125f84zmi10319991:24000
Yalmer-Kalkaska complex, 6 to 18 percent slopes119D672395000f80ymi10319991:24000
Yalmer fine sand, 6 to 18 percent slopes29D556395184f86wmi10319991:24000
Munising-Yalmer-Frohling complex, calcareous substratum, 1 to 6 percent slopes294B16114570391kx58mi15320071:24000
Munising-Yalmer complex, dissected, 1 to 12 percent slopes184C5241801604vx46mi60520041:24000
Munising-Abbaye-Yalmer complex, dissected, 8 to 35 percent slopes, stony183E2901801605vx47mi60520041:24000
Munising-Abbaye-Yalmer complex, dissected, 1 to 12 percent slopes, stony183C2535801606vx48mi60520041:24000
Munising-Yalmer complex, dissected, 8 to 35 percent slopes184E2336801603vx45mi60520041:24000

Map of Series Extent

Approximate geographic distribution of the YALMER 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 .