Official Series Description


Lab Data Summary

Aggregate lab data for the MILACA soil series. This aggregation is based on all pedons with a current taxon name of MILACA, 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 MILACA 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
90AUMN1339S1971MN0171339Milaca2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6740265,-92.6475067
90AUMN3364S1980MN097048Milaca2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1544189,-93.8861008
90AUMN3704S1983MN065015Milaca3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.93293,-93.4795227
90A97P0276S1996MN095036Milaca6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1425018,-93.492775
90A97P0277S1996MN095039Milaca6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1361122,-93.4902802
90A04N0467S2003WI031006Milaca6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2860184,-92.2841873
90BUMN3701S1983MN097026Milaca3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9458351,-94.0727768
90BUMN3702S1983MN097027Milaca3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9230499,-94.0714035
91AUMN3270S1980MN097009 (3270)Milaca4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.074501,-94.3625031
91B99P0301S1998WI013011Milacan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0933342,-92.2024994
91B99P0302S1998WI013012Milacan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0922203,-92.2074966
n/a40A172963MN009003Milaca5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A173063MN095001Milaca6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with MILACA, 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 MILACA 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
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C2073731824782z19xmn00119961:20000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D1217931824862z19wmn00119961:20000
Milaca loam, 1 to 7 percent slopes, stonyC73C512131824362z19smn00119961:20000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C37431152272z19rmn00119961:20000
Milaca fine sandy loam, 3 to 8 percent slopes152B169432856gjf3mn00119961:20000
Milaca fine sandy loam, 15 to 25 percent slopes152E124432859gjf6mn00119961:20000
Milaca-Millward complex, 2 to 8 percent slopes738B28432964gjjlmn00119961:20000
Milaca fine sandy loam, 8 to 15 percent slopes152C16432857gjf4mn00119961:20000
Milaca-Millward complex, 8 to 15 percent slopes738C8432965gjjmmn00119961:20000
Milaca loam, 1 to 7 percent slopes, stonyC73C4163531824522z19smn00920071:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C556731824822z19xmn00920071:12000
Milaca, stony-St. Francis complex, 3 to 8 percent slopesC69B1491802990vykxmn00920071:12000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C146031824302z19rmn00920071:12000
Milaca fine sandy loam, 3 to 6 percent slopes, stonyC68B561802982vyknmn00920071:12000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D28531824902z19wmn00920071:12000
Milaca, stony-St. Francis complex, 8 to 15 percent slopesC69C272804203vzv1mn00920071:12000
Milaca fine sandy loam, 6 to 12 percent slopes, stonyC68C95802983vykpmn00920071:12000
Milaca fine sandy loam, 12 to 25 percent slopes, stonyC68E27802984vykqmn00920071:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C263431824792z19xmn01719731:20000
Milaca loam, 1 to 7 percent slopes, stonyC73C115431824402z19smn01719731:20000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D64231824872z19wmn01719731:20000
Milaca sandy loam, 2 to 6 percent slopes, very stony682B792396590f9p7mn02519901:15840
Milaca sandy loam, 12 to 18 percent slopes, very stony682D482396592f9p9mn02519901:15840
Milaca sandy loam, 6 to 12 percent slopes, very stony682C269396591f9p8mn02519901:15840
Milaca sandy loam, 18 to 25 percent slopes, very stony682E172396593f9pbmn02519901:15840
Milaca loam, 1 to 7 percent slopes, stonyC73C26531824442z19smn05919561:20000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D23731824882z19wmn05919561:20000
Milaca fine sandy loam, 12 to 18 percent slopesMr179398372fcjqmn05919561:20000
Milaca fine sandy loam, 7 to 12 percent slopesMn128398370fcjnmn05919561:20000
Milaca fine sandy loam, 12 to 25 percent slopes, severely erodedMs124398373fcjrmn05919561:20000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C5531152282z19rmn05919561:20000
Milaca fine sandy loam, 7 to 12 percent slopes, moderately erodedMd23398368fcjlmn05919561:20000
Milaca fine sandy loam, 2 to 7 percent slopesMf11398369fcjmmn05919561:20000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D2892631824922z19wmn06520061:12000
Milaca loam, 1 to 7 percent slopes, stonyC73C1378231824602z19smn06520061:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C726831824842z19xmn06520061:12000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C531431824322z19rmn06520061:12000
Milaca fine sandy loam, 8 to 15 percent slopes, stonyC5C40016734451t5c3mn06520061:12000
Milaca fine sandy loam, 15 to 30 percent slopes, stonyC5E25216734461t5c4mn06520061:12000
Milaca, stony-Chetek complex, 8 to 15 percent slopesC91C13616735111t5f7mn06520061:12000
Milaca, stony-Chetek complex, 3 to 8 percent slopesC91B9216735101t5f6mn06520061:12000
Milaca, stony-Mora, stony-Cathro complex, pitted, 0 to 8 percent slopesC123B6816735491t5ggmn06520061:12000
Milaca, stony-Chetek complex, 15 to 30 percent slopesC91E1216735121t5f8mn06520061:12000
Milaca loam, 1 to 7 percent slopes, stonyC73C1313231824642z19smn09520061:12000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D1186331824932z19wmn09520061:12000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C624931824332z19rmn09520061:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C179431824852z19xmn09520061:12000
Milaca, stony-St. Francis complex, 3 to 8 percent slopesC69B6716764001t8ffmn09520061:12000
Milaca, stony-Chetek complex, 15 to 30 percent slopesC91E516764131t8fvmn09520061:12000
Milaca, stony-St. Francis complex, 8 to 15 percent slopesC69C316764011t8fgmn09520061:12000
Milaca, stony-Mora, stony-Cathro complex, pitted, 0 to 8 percent slopesC123B216764501t8h1mn09520061:12000
Milaca loam, 1 to 7 percent slopes, stonyC73C2588231824482z19smn09719871:20000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D646331824892z19wmn09719871:20000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C387531824802z19xmn09719871:20000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C115031152292z19rmn09719871:20000
Milaca fine sandy loam, 8 to 15 percent slopes152C471400346ffldmn09719871:20000
Milaca fine sandy loam, 4 to 8 percent slopes152B356400345fflcmn09719871:20000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C1446231824832z19xmn11520091:24000
Milaca-Millward complex, 2 to 20 percent slopes, stonyC72D966031824912z19wmn11520091:24000
Milaca-Mora-Greysolon complex, 2 to 20 percent slopes, stonyC11D51423314090308xfmn11520091:24000
Milaca loam, 1 to 7 percent slopes, stonyC73C348631824562z19smn11520091:24000
Milaca silt loam, 5 to 30 percent slopes, stonyC52E15413314095308xmmn11520091:24000
Milaca-Brennyville complex, 1 to 7 percent slopes, stonyC1C150931824312z19rmn11520091:24000
Milaca loam, 1 to 7 percent slopes, stonyC73C113231824682z19smn14119941:15840
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C28931824812z19xmn14119941:15840
Milaca fine sandy loam, moderately wet, 3 to 6 percent slopes1270B209431451ggysmn14119941:15840
Milaca fine sandy loam, 6 to 12 percent slopes152C60431453ggyvmn14119941:15840
Milaca fine sandy loam, 12 to 25 percent slopes152E41431454ggywmn14119941:15840
Bigisland-Milaca complex, 15 to 45 percent slopes, very stony469E1330448505h1pxwi01320041:12000
Milaca sandy loam, 2 to 6 percent slopes, very stony742B1198449330h2kjwi01320041:12000
Milaca-Mora-Greysolon complex, 2 to 20 percent slopes, stonyC11D3553314105308xfwi01320041:12000
Milaca sandy loam, 6 to 12 percent slopes, very stony742C214449331h2kkwi01320041:12000
Milaca sandy loam, 12 to 20 percent slopes, very stony742D71449332h2klwi01320041:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C3533141142z19xwi01320041:12000
Milaca-Mora-Greysolon complex, 2 to 20 percent slopes, stonyC11D290603314117308xfwi03120051:12000
Milaca-Mora complex, 1 to 7 percent slopes, stonyC71C281133141272z19xwi03120051:12000
Milaca-Mora-Giese complex, 0 to 15 percent slopes, very stony1053C2694781548v787wi03120051:12000
Milaca sandy loam, 2 to 6 percent slopes, very stony742B2227781461v75fwi03120051:12000
Milaca sandy loam, 6 to 12 percent slopes, very stony742C1272781462v75gwi03120051:12000
Milaca silt loam, 6 to 12 percent slopes, very stony717C328781450v752wi03120051:12000
Bigisland-Milaca complex, 15 to 45 percent slopes, very stony469E251781272v6zbwi03120051:12000
Milaca sandy loam, 12 to 20 percent slopes, very stony742D241781463v75hwi03120051:12000
Brennyville-Milaca complex, 1 to 6 percent slopes, very stony718B164781451v753wi03120051:12000
Milaca silt loam, 3 to 6 percent slopes, very stony717B138781449v751wi03120051:12000
Milaca-Mora-Haustrup complex, 0 to 15 percent slopes, very stony, rocky928C8514826911lrvrwi03120051:12000
Milaca silt loam, 12 to 20 percent slopes, very stony717D69784560vbddwi03120051:12000
Milaca silt loam, 5 to 30 percent slopes, stonyC52E173314122308xmwi03120051:12000
Bigisland-Milaca complex, 15 to 45 percent slopes, very stony469E2124276902mh6lwi09519781:15840

Map of Series Extent

Approximate geographic distribution of the MILACA 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 .