Official Series Description


Lab Data Summary

Aggregate lab data for the MAURERTOWN soil series. This aggregation is based on all pedons with a current taxon name of MAURERTOWN, 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 MAURERTOWN 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
n/a98P028197VA017001MAURERTOWN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P028297VA017002MAURERTOWN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P028498VA163035MAURERTOWN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P028398VA163036MAURERTOWN6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MAURERTOWN 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 MAURERTOWN 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 MAURERTOWN 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 MAURERTOWN 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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Competing Series

Soil series competing with MAURERTOWN 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 MAURERTOWN 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 MAURERTOWN 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 MAURERTOWN, 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. VA-2010-11-05-02 | Bland County -

    Diagram of a sequence of landforms along Walker Creek in Bland County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Bland County, Virginia).

  2. VA-2010-11-05-03 | Bland County -

    Diagram of a sequence of landforms along Wolf Creek in Bland County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Bland County, Virginia).

  3. VA-2010-11-05-29 | Rockbridge County -

    Generalized diagram of a sequence of landforms along a river system underlain by shale bedrock in the western part of Rockbridge County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Rockbridge County, Virginia).

  4. VA-2010-11-05-33 | Scott County - 2006

    Diagram of a sequence of landforms along the Clinch River in Scott County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Scott County, Virginia; 2006).

Map Units

Map units containing MAURERTOWN 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
Maurertown silt loamMb1831545164l98ypa05519991:24000
Maurertown silty clay loam, 0 to 3 percent slopes, rarely flooded36A56714514711kqcnva01720051:24000
Maurertown silt loam, 0 to 3 percent slopes, rarely flooded22A88014027081j2mnva02120051:24000
Maurertown silt loam, 0 to 3 percent slopes, rarely flooded24A52824810822p8rxva04520101:24000
Maurertown silty clay loam, 0 to 3 percent slopes, rarely flooded34A77625120752q9hrva09120101:24000
Maurertown silt loam, 0 to 2 percent slopes32A256517244kc79va13919951:20000
Maurertown-Toms complex, 0 to 3 percent slopes, rarely flooded40A122425148202qdbtva16320101:24000
Maurertown silt loam, 0 to 3 percent slopes, rarely flooded29A378778072v3n3va16920031:24000
Toms silt loam, 0 to 2 percent slopes55A1279520787kgxlva17119881:15840
Maurertown silty clay loam, 0 to 2 percent slopes42A605520767kgwyva17119881:15840
Maurertown silt loam, 0 to 2 percent slopes, occasionally flooded25A229518685kdqsva17319951:24000
Maurertown silt loam, 0 to 2 percent slopes, rarely flooded32A320519350kff7va19119981:15840
Maurertown silt loam, 0 to 3 percent slopes, rarely flooded51A31325085812q7qyva19520101:24000
Maurertown silt loam, 0 to 3 percent slopesMaA22617167131vmcvwv06319621:24000
Maurertown silt loam, drained, 0 to 3 percent slopesMtA6132446952zf7pwv62819801:20000

Map of Series Extent

Approximate geographic distribution of the MAURERTOWN 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 .