Official Series Description


Lab Data Summary

Aggregate lab data for the MERTZ soil series. This aggregation is based on all pedons with a current taxon name of MERTZ, 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 MERTZ 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
14769PA1090111969PA109011Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7930556,-77.2122222
14770PA0670031970PA067003Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5894444,-77.3316667
14770PA0670101970PA067010Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6813889,-77.1413889
14770PA0670111970PA067011Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6808333,-77.1397222
14770PA0990101970PA099010Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3672222,-77.4855556
14770PA0990111970PA099011Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3686111,-77.2183333
14770PA0990121970PA099012Mertz5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3552778,-77.2738889
n/aAS-0111962-OH005-011Mertz3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aLC-0281979-OH089-028Mertz4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MERTZ 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 MERTZ 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 MERTZ 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 MERTZ 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 terrace figure.

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

Competing Series

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

Click the image to view it full size.

Geomorphic description summaries for the MERTZ 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.

Click the image to view it full size.

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 MERTZ, 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. PA-2012-03-13-42 | Juniata and Mifflin Counties - April 1981

    Typical pattern of soils and underlying material of the Morrison association (Soil Survey of Juniata and Mifflin Counties, PA; 1981).

Map Units

Map units containing MERTZ 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
Mertz very cherty silt loam, 18 to 35 percent slopes, very stonyMrE6051710575qzzoh08919861:15840
Frankstown variant-Mertz complex, 2 to 6 percent slopes, very stonyFrB4851710295qz2oh08919861:15840
Mertz very cherty silt loam, 15 to 35 percent slopesMpD2415407721nq9boh08919861:15840
Mertz very cherty silt loam, 15 to 35 percent slopesMkD678537918l1r6oh11919891:15840
Frankstown variant-Mertz complex, 3 to 8 percent slopesFkB272537887l1q6oh11919891:15840
Mertz channery silt loam, 8 to 15 percent slopesMhC1792541828l5tbpa00919891:24000
Mertz channery silt loam, 3 to 8 percent slopesMnB818542385l6d9pa01319781:20000
Mertz channery silt loam, 8 to 15 percent slopesMnC724542386l6dbpa01319781:20000
Mertz channery silt loam, 15 to 25 percent slopesMnD409542387l6dcpa01319781:20000
Mertz cherty silt loam, 8 to 15 percent slopesMeC8320545514l9n7pa60519751:20000
Mertz cherty silt loam, 3 to 8 percent slopesMeB4278545513l9n6pa60519751:20000
Mertz cherty silt loam, 15 to 25 percent slopesMeD3984545515l9n8pa60519751:20000
Mertz channery silt loam, 8 to 15 percent slopes, very stonyMzC1925553069lkhywv02520021:24000
Mertz channery silt loam, 15 to 35 percent slopes, very stonyMzE1795553070lkhzwv02520021:24000
Mertz channery silt loam, 8 to 15 percent slopes, very stonyMzC2004515430k9bswv07519921:24000
Mertz channery silt loam, 15 to 35 percent slopes, very stonyMzE1377515431k9btwv07519921:24000
Mertz channery silt loam, 3 to 8 percent slopesMrB573515429k9brwv07519921:24000
Mertz cherty loam, 8 to 15 percent slopesMfC431515939k9w6wv62819801:20000
Mertz cherty loam, 15 to 25 percent slopesMfD294515940k9w7wv62819801:20000

Map of Series Extent

Approximate geographic distribution of the MERTZ 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 .