Official Series Description


Lab Data Summary

Aggregate lab data for the MANDY soil series. This aggregation is based on all pedons with a current taxon name of MANDY, 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 MANDY 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
12796P008495WV083007Mandy5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9463882,-79.7030563
12796P008695WV093004Mandy5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9947205,-79.4283371
12796P008795WV093005Mandy5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9919434,-79.4294434
12712N8056S12WV071001Mandy6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7073222,-79.5732694
12712N8062S12WV083001Mandy6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8565639,-79.6554556
12796P0082S1995WV083005Mandy6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9838905,-79.6958313
14094P0233S1993NY009011Mandy6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2524986,-78.4822235
147VPI0162V1992-VA017-162Mandy2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2378611,-79.84225
147VPI0176V1992-WV075-176Mandy2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4152222,-79.7072778
147VPI0178V1992-WV075-178Mandy2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4039444,-79.7167222

Water Balance

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

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.

Competing Series

Soil series competing with MANDY 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 MANDY 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 MANDY 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 MANDY, 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

No block diagrams are available.

Map Units

Map units containing MANDY 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
Mandy channery silt loam, 25 to 35 percent slopes95E1584300032b26gny00320131:24000
Mandy channery silt loam, 35 to 70 percent slopes95F1420300033b26hny00320131:24000
Mandy channery silt loam, 8 to 15 percent slopes95C1356300030b26dny00320131:24000
Mandy channery silt loam, 3 to 8 percent slopes95B817300029b26cny00320131:24000
Mandy channery silt loam, 15 to 25 percent slopes95D506300031b26fny00320131:24000
Mandy channery silt loam, 25 to 35 percent slopes, extremely bouldery195E56299818b1zkny00320131:24000
Mandy channery silt loam, 15 to 25 percent slopes, extremely bouldery195D40299817b1zjny00320131:24000
Mandy channery silt loam, 8 to 15 percent slopes, extremely bouldery195C23299816b1zhny00320131:24000
Mandy channery silt loam, 35 to 70 percent slopes, extremely bouldery195F14299819b1zlny00320131:24000
Mandy channery silt loam, 35 to 50 percent slopes95F3985318178bp2tny00920021:24000
Mandy channery silt loam, 3 to 8 percent slopes95B32812897499qhrny00920021:24000
Mandy channery silt loam, 8 to 15 percent slopes95C32602897509qhsny00920021:24000
Mandy channery silt loam, 25 to 35 percent slopes95E3104318177bp2sny00920021:24000
Mandy channery silt loam, 15 to 25 percent slopes95D21772897519qhtny00920021:24000
Mandy channery silt loam, 3 to 15 percent slopes, extremely bouldery195C15682895509q9bny00920021:24000
Mandy channery silt loam, 15 to 25 percent slopes, extremely bouldery195D10162895519q9cny00920021:24000
Mandy-Rock outcrop complex, 3 to 15 percent slopes102C515318216bp41ny00920021:24000
Mandy channery silt loam, 25 to 50 percent slopes, extremely bouldery195E3882895529q9dny00920021:24000
Mandy channery silt loam, 25 to 35 percent slopesMaE19114523941krbfpa08319841:20000
Mandy channery silt loam, 3 to 15 percent slopes, extremely boulderyMbC12514523891krb8pa08319841:20000
Mandy channery silt loam, 15 to 25 percent slopes, extremely boulderyMbD11214523901krb9pa08319841:20000
Mandy channery silt loam, 3 to 8 percent slopesMaB2014523911krbbpa08319841:20000
Mandy channery silt loam, 8 to 15 percent slopesMaC1614523921krbcpa08319841:20000
Mandy channery silt loam, 35 to 55 percent slopes, very stony35E8014514911kqd9va01720051:24000
Mandy channery silt loam, 8 to 15 percent slopes, very stony35C5314514891kqd7va01720051:24000
Mandy channery silt loam, 15 to 35 percent slopes, very stony35D5014514901kqd8va01720051:24000
Mandy-Wildell complex, 15 to 35 percent slopes, very stony33wE152927362542sndjva09120101:24000
Mandy-Wildell complex, 35 to 55 percent slopes, very stony33wF93627362552sndkva09120101:24000
Mandy channery silt loam, 35 to 55 percent slopes, very stony33F51025120732q9hpva09120101:24000
Mandy-Wildell complex, 8 to 15 percent slopes, very stony33wC42627362532sndfva09120101:24000
Mandy channery silt loam, 15 to 35 percent slopes, very stony33E35425120722q9hnva09120101:24000
Mandy channery silt loam, 8 to 15 percent slopes, very stony33C8425120742q9hqva09120101:24000
Mandy-Paddyknob-Rock outcrop complex, 8 to 35 percent slopes, very stony37D57216711431t2yvva16720061:24000
Mandy channery silt loam, 35 to 55 percent slopes, very stonyMkF25860553067lkhwwv02520021:24000
Mandy channery silt loam, 15 to 35 percent slopes, very stonyMkE13057553066lkhvwv02520021:24000
Mandy channery silt loam, 3 to 15 percent slopes, very stonyMkC9652553087lkjjwv02520021:24000
Mandy channery silt loam, 55 to 80 percent slopes, very stonyMkG266553068lkhxwv02520021:24000
Mandy-Wildell complex, 35 to 55 percent slopes, very stonyMfwF172127362562sndkwv07119881:20000
Mandy-Wildell complex, 15 to 35 percent slopes, very stonyMfwE103827362522sndjwv07119881:20000
Mandy channery silt loam, 8 to 15 percent slopesMaC629514184k81lwv07119881:20000
Mandy-Wildell complex, 8 to 15 percent slopesMfdC56127362482snddwv07119881:20000
Mandy channery silt loam, 15 to 35 percent slopes, stonyMdE350514186k81nwv07119881:20000
Mandy-Wildell complex, 8 to 15 percent slopes, very stonyMfwC33827362492sndfwv07119881:20000
Mandy-Wildell complex, 15 to 25 percent slopesMfdD29427362502sndgwv07119881:20000
Mandy channery silt loam, 35 to 55 percent slopes, stonyMdF266514187k81pwv07119881:20000
Mandy-Wildell complex, 25 to 35 percent slopesMfdE23727362512sndhwv07119881:20000
Mandy channery silt loam, 15 to 25 percent slopesMaD6514185k81mwv07119881:20000
Mandy-Wildell complex, 35 to 55 percent slopes, very stonyMfwF3523927362432sndkwv07519921:24000
Mandy channery silt loam, 35 to 55 percent slopes, very stonyMfF28755515426k9bnwv07519921:24000
Mandy channery silt loam, 15 to 35 percent slopes, very stonyMfE14113515425k9bmwv07519921:24000
Mandy-Wildell complex, 15 to 35 percent slopes, very stonyMfwE1077027362412sndjwv07519921:24000
Mandy channery silt loam, 3 to 15 percent slopes, very stonyMfC8376515424k9blwv07519921:24000
Mandy-Wildell complex, 25 to 35 percent slopesMfdE378527362422sndhwv07519921:24000
Mandy-Wildell complex, 8 to 15 percent slopes, very stonyMfwC357727362392sndfwv07519921:24000
Mandy-Wildell complex, 15 to 25 percent slopesMfdD268727362402sndgwv07519921:24000
Mandy-Wildell complex, 55 to 80 percent slopes, very stonyMfwG261827362442sndlwv07519921:24000
Gauley-Mandy complex, moist, 3 to 15 percent slopes, very stonyGumC137930549182x4xmwv07519921:24000
Mandy-Wildell complex, 8 to 15 percent slopesMfdC135927362382snddwv07519921:24000
Mandy channery silt loam, 55 to 80 percent slopes, very stonyMfG661515427k9bpwv07519921:24000
Gauley-Mandy complex, moist, 15 to 35 percent slopes, very stonyGumE41830549202xhvnwv07519921:24000
Mandy channery silt loam, 8 to 15 percent slopesMdC87515422k9bjwv07519921:24000
Mandy channery silt loam, 15 to 25 percent slopesMdD11515423k9bkwv07519921:24000
Mandy channery silt loam, 35 to 55 percent slopes, extremely stonyMaF8806515140k91fwv10119921:24000
Mandy channery silt loam, 15 to 35 percent slopes, extremely stonyMaE4797515139k91dwv10119921:24000
Mandy channery silt loam, 3 to 15 percent slopes, extremely stonyMaC4627515138k91cwv10119921:24000
Mandy channery silt loam, 55 to 70 percent slopes, extremely stonyMaG898515141k91gwv10119921:24000
Mandy-Wildell complex, 35 to 55 percent slopes, very stonyMfwF1198827362352sndkwv60319781:20000
Mandy-Wildell complex, 15 to 35 percent slopes, very stonyMfwE914227362342sndjwv60319781:20000
Gauley-Mandy complex, moist, 3 to 15 percent slopes, very stonyGumC587629990622x4xmwv60319781:20000
Mandy-Wildell complex, 25 to 35 percent slopesMfdE338127362332sndhwv60319781:20000
Mandy-Wildell complex, 8 to 15 percent slopes, very stonyMfwC264827362312sndfwv60319781:20000
Mandy-Wildell complex, 8 to 15 percent slopesMfdC207927362302snddwv60319781:20000
Mandy-Wildell complex, 15 to 25 percent slopesMfdD200427362322sndgwv60319781:20000
Gauley-Mandy complex, moist, 15 to 35 percent slopes, very stonyGumE93530378312xhvnwv60319781:20000
Mandy channery silt loam, 15 to 35 percent slopes, extremely stonyMaE22425934372qdpywv76720111:20000
Mandy channery silt loam, 3 to 15 percent slopes, extremely stonyMaC15325934362qdpxwv76720111:20000

Map of Series Extent

Approximate geographic distribution of the MANDY 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 .