Official Series Description


Lab Data Summary

Aggregate lab data for the MALAGA soil series. This aggregation is based on all pedons with a current taxon name of MALAGA, 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 MALAGA 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 MALAGA 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 MALAGA 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 MALAGA 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 MALAGA 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with MALAGA 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 MALAGA 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 MALAGA 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 MALAGA, 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 MALAGA 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
Malaga gravelly fine sandy loam, 0 to 8 percent slopes2311667699505rgwpwa01719981:12000
Malaga cobbly fine sandy loam, 0 to 8 percent slopes232667699506rgwqwa01719981:12000
Malaga cobbly sandy loam, 0 to 15 percent slopes5525717992dq3wa02119941:20000
Malaga stony sandy loam, 0 to 15 percent slopes77529006885429n3wa02519791:24000
Malaga gravelly sandy loam, 0 to 5 percent slopes73318776885029mzwa02519791:24000
Malaga very stony sandy loam, 0 to 35 percent slopes78317686885529n4wa02519791:24000
Malaga cobbly sandy loam, 0 to 15 percent slopes75237736885229n1wa02519791:24000
Malaga-Ephrata complex, 0 to 15 percent slopes79166746885629n5wa02519791:24000
Ephrata-Malaga complex, 0 to 5 percent slopes4581986881929lzwa02519791:24000
Ephrata-Malaga complex, 5 to 15 percent slopes4622876882029m0wa02519791:24000
Malaga gravelly sandy loam, 5 to 15 percent slopes7413486885129n0wa02519791:24000
Malaga cobbly sandy loam, 15 to 35 percent slopes769156885329n2wa02519791:24000
Malaga gravelly fine sandy loam, 3 to 15 percent slopesMaC542733592gbfwa60719691:20000
Malaga gravelly fine sandy loam, 0 to 3 percent slopesMaA234733582gbdwa60719691:20000
Malaga stony sandy loam, 3 to 15 percent slopes9243510773042lfpwa63720081:24000
Winchester-Burbank-Malaga complex, 30 to 60 percent slopes960441773512lh6wa63720081:24000
Sagehill-Burbank-Malaga complex, 30 to 60 percent slopes911356772912lf8wa63720081:24000
Malaga gravelly sandy loam, 2 to 5 percent slopes748196771352l87wa63720081:24000
Malaga cobbly sandy loam, 15 to 30 percent slopes71375771172l7nwa63720081:24000
Malaga cobbly sandy loam, 3 to 15 percent slopes71229771162l7mwa63720081:24000
Malaga gravelly fine sandy loam, 0 to 15 percent slopes200405762112k9fwa63920031:24000
Malaga cobbly sandy loam, 3 to 15 percent slopes931797712532d4hwa68119941:24000
Malaga gravelly sandy loam, 5 to 10 percent slopes921055712502d4dwa68119941:24000
Sagehill-Burbank-Malaga complex, 30 to 60 percent slopes139363708052cp1wa68119941:24000
Malaga complex, 3 to 15 percent slopes20045707592cmkwa68119941:24000

Map of Series Extent

Approximate geographic distribution of the MALAGA 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 .