Official Series Description


Lab Data Summary

Aggregate lab data for the MAUCAV soil series. This aggregation is based on all pedons with a current taxon name of MAUCAV, 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 MAUCAV 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
43C00P1201S2000OR013004Maucav6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0220604,-120.3891525

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MAUCAV 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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Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MAUCAV series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the MAUCAV series and siblings. 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 MAUCAV 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 .

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.

Competing Series

Soil series competing with MAUCAV share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

There are insufficient data to create the competing sketch figure.

Select annual climate data summaries for the MAUCAV 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 MAUCAV 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 MAUCAV, 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 MAUCAV 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
Valpey, moist-Maucav-Valpey complex, 5 to 30 percent slopesP2101662434261431qkkkor6181:24000
Maule-Maucav-Ateron complex, 2 to 30 percent south slopes4331381434260632mlkor6181:24000
Maucav-Sintuf complex, 0 to 30 percent slopes3438AO82723426191130zror6181:24000
Maule-Maucav-Ateron complex, dry, 2 to 30 percent south slopes423715434261712mlpor6181:24000
Bingville-Hafmau-Maucav, dry complex, 15 to 40 percent slopesB400596834347482mplor6181:24000
Bigmow-Maucav-Kidnapspring complex, 0 to 30 percent slopes3450AO557934348141353qor6181:24000
Maule-Maucav complex, 30 to 60 percent south slopes434421634260702mljor6181:24000
Maucav-Ateron-Rock outcrop complex, 5 to 60 percent slopesX710269334261252mq1or6181:24000
Maucav-Canest-Norlo complex, 0 to 20 percent slopesP307266234261771qv5kor6181:24000
Ateron-Maucav-Hankins complex, 5 to 35 percent slopesT520264434350252mv1or6181:24000
Maule-Maucav complex, dry, 30 to 60 percent south slopes424263734350272mlnor6181:24000
Maucav-Yawkey-Sintuf complex, 30 to 60 percent slopes3440CO22653426146134ghor6181:24000
Tweener-Cleavage-Maucav complex, 0 to 10 percent slopesP545203534375931qkktor6181:24000
Maucav-Hafmau complex, 0 to 15 percent slopes3439AO17453426106130znor6181:24000
Maucav-Hafmau-Anatone complex, 15 to 30 percent slopes3447BO17293437528130zpor6181:24000
Normauk-Maule-Maucav complex, 5 to 35 percent north slopesX610142034261042mqzor6181:24000
Bigmow-Maucav-Kidnapspring complex, mass failure, 0 to 30 percent slopes3450AM125034374491356jor6181:24000
Maucav-Shotsprings-Hafmau complex, 30 to 60 percent slopes3448CO6663434897130zqor6181:24000
Ateron-Maucav dry, complex, 5 to 30 percent slopesB52060134261632mttor6181:24000
Hankins-Maucav-Hafmau complex, 15 to 30 percent slopes3439BO32034261492pgdcor6181:24000
Normauk, dry-Scarpal, dry-Maucav, moist complex, 30 to 60 percent north slopes271E126342607623dm6or6181:24000
Maucav-Anatone complex, 5 to 20 percent slopes275B25342609423dmdor6181:24000
Valpey, moist-Maucav-Valpey complex, 5 to 30 percent slopesP21020334251431qkkkor6271:24000
Maucav-Ateron-Rock outcrop complex, 5 to 60 percent slopesX7108334251192mq1or6271:24000
Maule-Maucav-Ateron complex, 2 to 30 percent south slopes433294434218042mlkor6771:24000
Maule-Maucav complex, 30 to 60 percent south slopes434226134218392mljor6771:24000
Normauk, dry-Scarpal, dry-Maucav, moist complex, 30 to 60 percent north slopes271E1841342186323dm6or6771:24000
Maucav-Anatone complex, 5 to 20 percent slopes275B870342199723dmdor6771:24000
Normauk-Maule-Maucav complex, 5 to 35 percent north slopesX61070534244542mqzor6771:24000
Maucav-Hafmau complex, 0 to 15 percent slopes3439AO6903424457130znor6771:24000
Maucav-Ateron-Rock outcrop complex, 5 to 60 percent slopesX71035234245852mq1or6771:24000
Hankins-Maucav-Hafmau complex, 15 to 30 percent slopes3439BO19034247182pgdcor6771:24000
Valpey, moist-Maucav-Valpey complex, 5 to 30 percent slopesP21017634246971qkkkor6771:24000
Ateron-Maucav dry, complex, 5 to 30 percent slopesB52010134247752mttor6771:24000
Maule-Maucav-Ateron complex, dry, 2 to 30 percent south slopes4236634248152mlpor6771:24000
Maucav-Canest-Norlo complex, 0 to 20 percent slopesP3075134248351qv5kor6771:24000
Maucav-Yawkey-Sintuf complex, 30 to 60 percent slopes3440CO313424701134ghor6771:24000
Maucav-Sintuf complex, 0 to 30 percent slopes3438AO13424872130zror6771:24000

Map of Series Extent

Approximate geographic distribution of the MAUCAV 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 .