Official Series Description


Lab Data Summary

Aggregate lab data for the JACKLAND soil series. This aggregation is based on all pedons with a current taxon name of JACKLAND, 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 JACKLAND were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JACKLAND 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 JACKLAND 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 JACKLAND 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 JACKLAND 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with JACKLAND 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 JACKLAND 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 JACKLAND 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 JACKLAND, 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. MD-2010-09-03-02 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

  2. MD-2012-02-03-03 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Legore association (Soil Survey of City of Baltimore, Maryland; 1998).

  3. 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).

  4. VA-2010-11-05-19 | Fauquier County -

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

Map Units

Map units containing JACKLAND 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
Jackland-Urban land complex, 0 to 8 percent slopesJuB47924048622lqg6md00520101:12000
Jackland silt loam, 3 to 8 percent slopesJaB29324048612lqg5md00520101:12000
Jackland silt loam, 3 to 8 percent slopesJaB211793008vm5xmd02720041:12000
Jackland silt loam, 3 to 8 percent slopes29B1085533619kx8jmd03119891:15840
Jackland-Urban land complex, 0 to 8 percent slopes12UB1813533891kxk9md51019931:12000
Jackland silt loam, 3 to 8 percent slopes12B213533890kxk8md51019931:12000
Jackland silt loam, 0 to 3 percent slopes12A14533889kxk7md51019931:12000
Jackland-Orange complex, 2 to 8 percent slopesJkB68529739202wx29nc03320161:24000
Jackland loam, 1 to 6 percent slopesJkB64924245442mcy3nc05919881:24000
Jackland fine sandy loam, 2 to 6 percent slopesJkB32524335252mp8tnc06719701:15840
Jackland fine sandy loam, 0 to 4 percent slopesJkB924331722mnxfnc08119751:20000
Jackland fine sandy loam, 2 to 8 percent slopesJkB110923890492l603nc15719831:24000
Jackland fine sandy loam, 8 to 15 percent slopesJkD65823890502l604nc15719831:24000
Jackland loam, 2 to 6 percent slopesJaB112823981872lhhwnc19719601:15840
Jackland loam, 6 to 10 percent slopesJaC66123981972lhj6nc19719601:15840
Jackland loam, 6 to 10 percent slopes, moderately erodedJaC247823981982lhj7nc19719601:15840
Jackland loam, 2 to 6 percent slopes, moderately erodedJaB222023981882lhhxnc19719601:15840
Jackland fine sandy loam, 2 to 7 percent slopes19B23871359422xx68va01919851:24000
Jackland fine sandy loam, 7 to 15 percent slopes19C18771359432xx69va01919851:24000
Jackland-Mirerock complex, 2 to 7 percent slopes22B1159024794152p714va02920101:24000
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
Jackland and Haymarket soils, 0 to 2 percent slopes, very bouldery39A28417263971vyg7va04720061:24000
Jackland-Mirerock complex, 2 to 7 percent slopes22B20915874211q8v4va04920051:24000
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
Jackland and Haymarket soils, 7 to 15 percent slopes63C10922504332fjrmva05920071:12000
Jackland silt loam, 0 to 2 percent slopes62A6622504292fjrhva05920071:12000
Hattontown-Jackland complex, 0 to 2 percent slopes53A2822503972fjqgva05920071:12000
Jackland and Haymarket soils, 15 to 25 percent slopes, very stony64D422504412fjrwva05920071:12000
Jackland and Haymarket soils, 2 to 7 percent slopes67B5960189536821m8xva06120061:12000
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-Mirerock-Redbrush complex, 8 to 15 percent slopes24C2027581999mjm5va06720041:24000
Jackland-Mirerock-Redbrush complex, 2 to 8 percent slopes24B429581998mjm4va06720041:24000
Jackland-Orange complex, 2 to 8 percent slopes26B313414728231lflfva08320041:24000
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 gravelly silt loam, 2 to 7 percent slopes27B14551369814ljrva12519921:24000
Jackland gravelly silt loam, 7 to 15 percent slopes27C7071369844ljvva12519921:24000
Orange-Jackland silt loams, 0 to 2 percent slopesOrA9661198972zhg1va13719661:15840
Orange-Jackland silt loams, 2 to 7 percent slopesOrB3651198982zhg2va13719661:15840
Orange-Jackland silt loams, 2 to 7 percent slopes, moderately erodedOrB21941198992zhg3va13719661:15840
Jackland silt loam, 2 to 7 percent slopes30B3435521178khb6va15319851:15840
Jackland-Haymarket complex, 2 to 7 percent slopes31B1850521179khb7va15319851:15840
Jackland-Haymarket complex, 7 to 15 percent slopes31C1327521180khb8va15319851:15840

Map of Series Extent

Approximate geographic distribution of the JACKLAND 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 .