Official Series Description


Lab Data Summary

Aggregate lab data for the MALABAR soil series. This aggregation is based on all pedons with a current taxon name of MALABAR, 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 MALABAR 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
155S05_0151967-FL009-S05_015Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties28.3639393,-80.7961502
155S64_0231975-FL127-S64_023Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties28.8302898,-81.049736
155S56_0291977-FL111-S56_029Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.3807411,-80.3634338
155S08_0041978-FL015-S08_004Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.927887,-81.9504852
155S26_0151983-FL051-S26_015Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.6343327,-81.5183563
155S14_0101984-FL027-S14_010Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.131258,-81.5874252
155S28_0111984-FL055-S28_011Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.189003,-81.180954
155S22_0021988-FL043-S22_002Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.0641251,-81.0374527
155S26_009S1982FL051009Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties26.5609436,-81.3686295
156BS56_0171975-FL111-S56_017Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.4905224,-80.6057816
156BS43_021S1977FL085021Malabar3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties27.1482754,-80.4574432

Water Balance

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

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Competing Series

Soil series competing with MALABAR 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 MALABAR series and competing. 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 MALABAR 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with MALABAR, 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 MALABAR 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
Malabar, Holopaw, and Pineda soils311154514733171lg3cfl00919901:24000
Malabar sand, high29669914733151lg39fl00919901:24000
Malabar sand, 0 to 2 percent slopes30568914733162sm5kfl00919901:24000
Malabar fine sand, high, 0 to 2 percent slopes632547914534732svz4fl01519821:20000
Malabar fine sand, 0 to 2 percent slopes341057914534502svz3fl01519821:20000
Malabar fine sand, frequently ponded, 0 to 1 percent slopes44263114534602svz5fl01519821:20000
Malabar fine sand-Urban land complex, 0 to 2 percent slopes119236930458532x9cdfl01519821:20000
Malabar fine sand, high-Urban land complex, 0 to 2 percent slopes12199630458552x9cffl01519821:20000
Malabar fine sand, ponded-Urban land complex, 0 to 1 percent slopes1205730458542x9cgfl01519821:20000
Malabar fine sand, 0 to 2 percent slopes6219953210972svz3fl01719851:20000
Malabar fine sand, 0 to 2 percent slopes212156013869152svz3fl02719861:24000
Malabar fine sand, high, 0 to 2 percent slopes22954013869162svz4fl02719861:24000
Malabar fine sand, frequently ponded, 0 to 1 percent slopes23390013869172svz5fl02719861:24000
Malabar fine sand, 0 to 2 percent slopes16770015294182svz3fl03519911:15840
Malabar fine sand, 0 to 2 percent slopes61977014535652svz3fl04319911:24000
Malabar fine sand, high, 0 to 2 percent slopes361394014535892svz4fl04319911:24000
Malabar sand, 0 to 2 percent slopes81869011514102sm5kfl05119861:24000
Malabar fine sand, high, 0 to 2 percent slopes51772011514402svz4fl05119861:24000
Malabar sand, frequently ponded, 0 to 1 percent slopes61182011514472svz6fl05119861:24000
Malabar fine sand, 0 to 2 percent slopes17769914135172svz3fl05519821:24000
Malabar sand, frequently ponded, 0 to 1 percent slopes37165214135362svz6fl05519821:24000
Malabar fine sand, 0 to 2 percent slopes273066514069772svz3fl05719861:20000
Malabar fine sand393986756760tdgmfl06119841:20000
Malabar fine sand-Urban land complex, 0 to 2 percent slopes1191245631028732x9cdfl07119821:20000
Malabar fine sand, 0 to 2 percent slopes341165214834282svz3fl07119821:20000
Malabar fine sand, high-Urban land complex, 0 to 2 percent slopes121407431028752x9cffl07119821:20000
Malabar fine sand, frequently ponded, 0 to 1 percent slopes44305914834392svz5fl07119821:20000
Malabar fine sand, high, 0 to 2 percent slopes63280214834542svz4fl07119821:20000
Malabar fine sand, ponded-Urban land complex, 0 to 1 percent slopes120175731028742x9cgfl07119821:20000
Malabar fine sand, high, 0 to 2 percent slopes521357614215982svz4fl08519791:20000
Malabar fine sand2320658323136bv7rfl09519861:20000
Malabar fine sand, 0 to 2 percent slopes192759614838592svz3fl09719761:20000
Malabar-Pineda complex21625014838611lt2hfl09719761:20000
Malabar fine sand, frequently ponded, 0 to 1 percent slopes20489831029262svz5fl09719761:20000
Malabar fine sand, 0 to 2 percent slopes101176914250022svz3fl10519871:20000
Malabar fine sand353340323400bvj8fl10719851:15840
Malabar fine sand, 0 to 2 percent slopes23688914211802svz3fl11119901:24000
Malabar fine sand-Urban land complex, 0 to 2 percent slopes65153231030222x9cdfl11519881:24000
Malabar fine sand, 0 to 2 percent slopes25124314600992svz3fl11519881:24000
Malabar fine sand, 0 to 2 percent slopes18152614787022svz3fl11719861:20000
Malabar fine sand, frequently flooded482090323656bvsjfl11919851:24000
Malabar fine sand311309015441331ntsrfl12719771:20000
Malabar fine sand-Urban land complex, 0 to 2 percent slopes120876331029762x9cdfl62119891:24000
Malabar fine sand, 0 to 2 percent slopes3875714134562svz3fl62119891:24000
Ft. Drum-Malabar, high association, 0 to 2 percent slopes20510930459262x9fwfl62119891:24000
Ft. Drum-Malabar, high, fine sands-Urban land association, 0 to 2 percent slopes109155130458912x9fmfl62119891:24000

Map of Series Extent

Approximate geographic distribution of the MALABAR 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 .