Official Series Description


Lab Data Summary

Aggregate lab data for the HAYMARKET soil series. This aggregation is based on all pedons with a current taxon name of HAYMARKET, 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 HAYMARKET 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
14800P1102S2000VA047003Haymarket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.540156,-77.865039
14800P1106S2000VA047017Haymarket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.403261,-77.978581
14800P1117S2000VA047023Haymarket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.366506,-77.960906
14800P1072S2000VA107009Haymarket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.094886,-77.559586
14800P1076S2000VA107017Haymarket3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.993511,-77.502831

Water Balance

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

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 HAYMARKET 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 HAYMARKET 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 HAYMARKET 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with HAYMARKET, 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-2010-11-05-10 | Culpeper County -

    Relationship of soils and landscape in the Culpeper Triassic Basin Diabase and Hornfel (Soil Survey of Culpeper County, Virginia).

Map Units

Map units containing HAYMARKET 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
Haymarket-Mirerock complex, 2 to 7 percent slopes20B4481367274l8kva00920041:24000
Haymarket-Mirerock complex, 7 to 15 percent slopes20C2091367284l8lva00920041:24000
Jackland and Haymarket soils, 2 to 7 percent slopes38B853917263961vyg6va04720061:24000
Jackland and Haymarket soils, 2 to 7 percent slopes, very bouldery39B431717263981vyg8va04720061:24000
Jackland and Haymarket soils, 0 to 2 percent slopes38A215017263951vyg5va04720061:24000
Haymarket-Jackland complex, 7 to 15 percent slopes, bouldery35C52717263901vyg0va04720061:24000
Haymarket silt loam, 15 to 25 percent slopes, very bouldery36D36417263911vyg1va04720061:24000
Jackland and Haymarket soils, 0 to 2 percent slopes, very bouldery39A28417263971vyg7va04720061:24000
Haymarket silt loam, 25 to 45 percent slopes, extremely bouldery37E23817263921vyg2va04720061:24000
Jackland and Haymarket soils, 7 to 15 percent slopes, very stony64C168722504392fjrtva05920071:12000
Jackland and Haymarket soils, 2 to 7 percent slopes63B105222504322fjrlva05920071:12000
Hattontown-Jackland-Haymarket complex, 2 to 7 percent slopes54B105122504012fjqlva05920071:12000
Hattontown-Jackland-Haymarket complex, 7 to 15 percent slopes54C78122504032fjqnva05920071:12000
Jackland and Haymarket soils, 2 to 7 percent slopes, very stony64B32922504372fjrrva05920071:12000
Haymarket silt loam, 7 to 15 percent slopes59C12322504192fjr5va05920071:12000
Haymarket silt loam, 2 to 7 percent slopes59B11122504172fjr3va05920071:12000
Jackland and Haymarket soils, 7 to 15 percent slopes63C10922504332fjrmva05920071:12000
Hattontown-Haymarket complex, 7 to 15 percent slopes52C8922503962fjqfva05920071:12000
Hattontown-Haymarket complex, 2 to 7 percent slopes52B4022503942fjqcva05920071:12000
Jackland and Haymarket soils, 15 to 25 percent slopes, very stony64D422504412fjrwva05920071:12000
Jackland and Haymarket soils, 2 to 7 percent slopes67B5960189536821m8xva06120061:12000
Haymarket silt loam, 2 to 7 percent slopes167B1142189542821mbvva06120061:12000
Montalto and Haymarket soils, 7 to 15 percent slopes167C985189542921mbwva06120061:12000
Jackland and Haymarket soils, 7 to 15 percent slopes67C952189536921m8yva06120061:12000
Jackland and Haymarket soils, 2 to 7 percent slopes, very stony68B859189537021m8zva06120061:12000
Jackland and Haymarket soils, 7 to 15 percent slopes, very stony68C767189537121m90va06120061:12000
Jackland and Haymarket soils, 2 to 7 percent slopes67B6039642094pk4qva10720061:12000
Jackland and Haymarket soils, 2 to 7 percent slopes, very stony68B2478642098pk4vva10720061:12000
Jackland and Haymarket soils, 7 to 15 percent slopes, very stony68C969642099pk4wva10720061:12000
Jackland and Haymarket soils, 7 to 15 percent slopes67C668642096pk4sva10720061:12000
Jackland-Haymarket complex, 2 to 7 percent slopes31B1850521179khb7va15319851:15840
Jackland-Haymarket complex, 7 to 15 percent slopes31C1327521180khb8va15319851:15840
Haymarket silt loam, 2 to 7 percent slopes28B493521171kh9zva15319851:15840
Haymarket silt loam, 7 to 15 percent slopes28C437521172khb0va15319851:15840
Hattontown-Haymarket complex, 2 to 7 percent slopes52B1230505342xn6qva60020071:12000

Map of Series Extent

Approximate geographic distribution of the HAYMARKET 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 .