Official Series Description


Lab Data Summary

Aggregate lab data for the MALBIS soil series. This aggregation is based on all pedons with a current taxon name of MALBIS, 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 MALBIS 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
133AS57_0291974-FL113-S57_029Malbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.7962589,-87.2775955
133AS57_0431976-FL113-S57_043Malbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.8963604,-86.9819641
133AS46_0171986-FL091-S46_017Malbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9183064,-86.7555008
133AS07AL-003-12007AL003001Malbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.5408333,-87.8819444
133A79P035479AL099021Malbis6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.3022213,-87.5566635
133A79P035679AL099023Malbis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.2691669,-87.6633301
133A79P035879AL099025Malbis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.2849998,-87.6102753
133A81P036281AL131001Malbis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0238876,-87.316391
133AS84AL-091-2384AL091023-pgmMalbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0583333,-87.625
133AS87AL-025-287AL025002-pgmMalbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.4208333,-87.7477778
133AS72AL-097-7S1972AL097007Malbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.13765,-88.1015833
133B40A4125S1957LA011005MALBIS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.7716675,-93.0563889
133B80P0508S1980LA069015MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.4227772,-93.1236115
133B80P0509S1980LA069016MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.395834,-93.1149979
133B80P0510S1980LA115001MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.1741676,-93.1261139
133B80P0511S1980LA115002MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.0069447,-93.0422211
135AS95AL-087-495AL087004-pgmMalbis3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3877778,-85.9255556
152B40A4124S1957LA011006MALBIS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.8030548,-93.2016678
152B80P0512S1980LA011001MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.7099991,-93.308609
152B80P0513S1980LA011002MALBIS7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.7686119,-93.4875031
152B80P0514S1980LA019002Malbis7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4024467,-93.6899109

Water Balance

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

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Click the image to view it full size.

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 MALBIS, 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. AL-2010-02-25-02 | Wilcox County - March 1999

    Generalized patterns of soils, geomorphology, and landscape relationships in the Urbo-Mooreville-Una, Annemaine-Izagora-Lenoir, Luverne-Halso, Arundel-Cantuche, and Bama-Malbis-Luverne general soil map units along the Alabama River in the central part of Wilcox County (Soil Survey of Wilcox County, Alabama; 1999).

Map Units

Map units containing MALBIS 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
Malbis fine sandy loam, 0 to 2 percent slopesMaA298983281752w8xval00319611:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB1894733348662w8xxal00319611:20000
Malbis fine sandy loam, 5 to 12 percent slopesMaD1110333348672w8xyal00319611:20000
Malbis fine sandy loam, 1 to 3 percent slopesMbB42703284662tl1jal01319961:20000
Malbis fine sandy loam, 5 to 8 percent slopesMbC14603284672wty9al01319961:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB115531164022zkvnal02119671:20000
Malbis fine sandy loam, 5 to 8 percent slopesMaC16631164052wty9al02119671:20000
Malbis fine sandy loam, 0 to 2 percent slopesMaA15631164012zkvmal02119671:20000
Malbis fine sandy loam, 1 to 5 percent slopesMaB83306000702s69val02520041:24000
Gritney-Malbis-Fuquay complex, 1 to 8 percent slopesGyC31929328729c125al03519851:20000
Malbis sandy loam, 1 to 6 percent slopesMaB23156328734c12bal03519851:20000
Dothan and Malbis sandy loams, 1 to 5 percent slopesDmB719923287592ttl3al03919851:20000
Dothan and Malbis sandy loams, 0 to 1 percent slopesDmA2574328758c133al03919851:20000
Malbis fine sandy loam, 1 to 3 percent slopesMbB31803305142tl1jal04120051:24000
Malbis fine sandy loam, 5 to 8 percent slopesMbC8903305152wty9al04120051:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA779731164082zkvmal05119481:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB291731164092zkvnal05119481:20000
Malbis fine sandy loam, 5 to 8 percent slopesMaC88031164142wty9al05119481:20000
Malbis fine sandy loam, 0 to 2 percent slopesMaA73673293462w8xval05319691:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB22983293472w8xxal05319691:20000
Orangeburg-Greenville-Malbis complex, 3 to 12 percent slopes, erodedOvC2897329351c1q7al05319691:20000
Malbis fine sandy loam, 1 to 3 percent slopesMbB479725149192tl1jal08520111:24000
Malbis fine sandy loam, 3 to 8 percent slopesMbC109425149202qdh8al08520111:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA2625330473c2wfal08719971:24000
Malbis fine sandy loam, 2 to 5 percent slopesMaB801129949892w8xxal09720181:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA795329949882w8xval09720181:24000
Malbis fine sandy loam, 5 to 12 percent slopesMaD748529949902w8xyal09720181:24000
Malbis-Urban land complex, 0 to 8 percent slopesMbC214829950652x5r2al09720181:24000
Malbis fine sandy loam, 1 to 5 percent slopesMaB469003308512s69val09919841:20000
Malbis loam, 0 to 1 percent slopesMaA19100330850c38lal09919841:20000
Malbis fine sandy loam, 5 to 8 percent slopesMaC83003308522wty9al09919841:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB25531164212zkvnal10119581:20000
Malbis fine sandy loam, 0 to 2 percent slopesMaA9531164172zkvmal10119581:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB2251626421062w8xxal12920131:24000
Malbis fine sandy loam, 5 to 12 percent slopesMaD2167526421072w8xyal12920131:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA405226421052w8xval12920131:24000
Malbis fine sandy loam, 2 to 5 percent slopesMbB12800331664c43val13119971:24000
Malbis silt loam, 0 to 2 percent slopesMaA4590331663c43tal13119971:24000
Malbis fine sandy loam, 5 to 8 percent slopesMbC23603316652wty9al13119971:24000
Malbis sandy loam, 0 to 2 percent slopes41148014253471jv5yfl03319981:24000
Malbis sandy loam, 2 to 5 percent slopes4250014253481jv5zfl03319981:24000
Malbis fine sandy loam, 2 to 5 percent slopes60155903240332w8xxfl13119851:20000
Malbis fine sandy loam, 5 to 8 percent slopes612100324034bw5qfl13119851:20000
Malbis fine sandy loam, 0 to 2 percent slopes599703240312w8xvfl13119851:20000
Malbis fine sandy loam, 1 to 5 percent slopesMa2678615861112wdl3la00319781:24000
Malbis fine sandy loam, 3 to 5 percent slopesMbC2659517257161vxr8la01119931:24000
Malbis fine sandy loam, 1 to 3 percent slopesMbB2486617257151vxr7la01119931:24000
Malbis fine sandy loam, 5 to 8 percent slopesMbD300117257171vxr9la01119931:24000
Malbis fine sandy loam, 1 to 3 percent slopesMgB1501217245931vwl1la01319921:24000
Malbis fine sandy loam, 3 to 8 percent slopesMgD1383617245941vwl2la01319921:24000
Malbis fine sandy loam, 1 to 5 percent slopesMa3008815274672wdl3la04319821:24000
Malbis fine sandy loam, 1 to 5 percent slopesMb327516001792wdl3la05919861:24000
Malbis fine sandy loam, 1 to 5 percent slopesMa2689219031132wdl3la06919831:24000
Malbis fine sandy loam, 1 to 5 percent slopesMaC567735699682wdl3la07919731:24000
Malbis-Beauregard association, gently slopingMAB1698817206741vrhmla08119731:24000
Hallsummit-Malbis association, 3 to 8 percent slopesMLC1086217206752zb6sla08119731:24000
Malbis fine sandy loam, 3 to 8 percent slopesMgD45524013782llttla08119731:24000
Malbis fine sandy loam, 1 to 3 percent slopesMgB2924013762lltrla08119731:24000
Malbis fine sandy loam, 3 to 8 percent slopesMa614215365151nkw0la10519851:24000
Malbis fine sandy loam, 1 to 5 percent slopesMn2230617253522wdl3la11119921:24000
Malbis fine sandy loam, 1 to 3 percent slopesMaB8505217255611vxl8la11519921:24000
Malbis fine sandy loam, 3 to 5 percent slopesMaC7136317255621vxl9la11519921:24000
Malbis fine sandy loam, 1 to 3 percent slopesMp30632570357m4hmla11919891:24000
Malbis fine sandy loam, 3 to 8 percent slopesMs14638570358m4hnla11919891:24000
Malbis fine sandy loam, 1 to 5 percent slopesMc24519038392wdl3la12719911:24000
Malbis loam, 2 to 5 percent slopesMaB1852332225c4pyms03519761:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB2001926422122w8xxms04120121:24000
Malbis fine sandy loam, 5 to 12 percent slopesMaD443826422132w8xyms04120121:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA247526422112w8xvms04120121:24000
Malbis fine sandy loam, 2 to 5 percent slopesMaB33423323972w8xxms04519791:20000
Malbis fine sandy loam, 5 to 8 percent slopesMaC15103323982w9vyms04519791:20000
Malbis fine sandy loam, 0 to 2 percent slopesMaA2333323962w8xvms04519791:20000
Malbis fine sandy loam, 2 to 5 percent slopes45112343325822w8xxms05919971:24000
Malbis fine sandy loam, 0 to 2 percent slopes4457723325812w8xvms05919971:24000
Malbis fine sandy loam, 5 to 8 percent slopes43C418863327312w9vyms06719841:20000
Malbis fine sandy loam, 2 to 5 percent slopes43B185623327302w8xxms06719841:20000
Malbis-Urban land complex42583332726c573ms06719841:20000
Malbis fine sandy loam, undulating8221345332741c57lms06719841:20000
Malbis-Susquehanna-Saucier association slopingME55625333544c62hms10919801:20000
Malbis fine sandy loam, 2 to 5 percent slopesMaB328933335472w8xxms10919801:20000
Malbis-Saucier association, slopingMD19396333543c62gms10919801:20000
Malbis fine sandy loam, 5 to 8 percent slopesMaC162913335482w9vyms10919801:20000
Malbis fine sandy loam, 0 to 2 percent slopesMaA62793335462w8xvms10919801:20000
Malbis fine sandy loam, undulating194481334094c6n7ms13119971:24000
Malbis fine sandy loam, 2 to 5 percent slopes174833340902w8xxms13119971:24000
Malbis fine sandy loam, 5 to 8 percent slopes181123340932w9vyms13119971:24000
Malbis fine sandy loam, 2 to 5 percent slopesMaB2218124034622w8xxms15320081:24000
Malbis fine sandy loam, 5 to 8 percent slopesMaC456224034632w9vyms15320081:24000
Malbis fine sandy loam, 0 to 2 percent slopesMaA63024034612w8xvms15320081:24000

Map of Series Extent

Approximate geographic distribution of the MALBIS 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 .