Official Series Description


Lab Data Summary

Aggregate lab data for the MAYBESO soil series. This aggregation is based on all pedons with a current taxon name of MAYBESO, 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 MAYBESO 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
22086P016785AK280004Maybeso5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties56.9013901,-133.7611084
n/a84P014183AK130120Maybeso5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties55.9458351,-131.1416626
n/a83P0741S1983AK280001Maybeso5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the MAYBESO 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 MAYBESO 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 MAYBESO 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 terrace figure.

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Competing Series

Soil series competing with MAYBESO 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 MAYBESO 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 MAYBESO 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 MAYBESO, 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 MAYBESO 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
Kina-Maybeso association, 5 to 35 percent slopes220C111784496521nnpak64419941:31680
Maybeso-Kaikli complex, 5 to 60 percent slopes20CDX42544496481nnkak64419941:31680
Wadleigh-Maybeso complex, 5 to 35 percent slopes320C32204496871nptak64419941:31680
Maybeso peat, 5 to 60 percent slopes91CDX22260498311nvgak64419941:31680
Wadleigh-Maybeso complex, 5 to 60 percent slopes320CD21981496881npvak64419941:31680
Kogish-Maybeso complex, 2 to 10 percent slopes20115877496461nnhak64419941:31680
Wadleigh-Maybeso complex, 35 to 60 percent slopes320D11012496891npwak64419941:31680
Maybeso-Kina association, 5 to 35 percent slopes92C9177498331nvjak64419941:31680
Maybeso peat, 5 to 35 percent slopes91C5803498301nvfak64419941:31680
Maybeso-Kaikli complex, 5 to 35 percent slopes20C4754496471nnjak64419941:31680
Kina-Maybeso association, 35 to 60 percent slopes220D3783496531nnqak64419941:31680
Maybeso-Kaikli complex, 35 to 60 percent slopes20D2227496491nnlak64419941:31680
Maybeso peat, 35 to 60 percent slopes91D883498321nvhak64419941:31680
Kushneahin-Maybeso complex, 3 to 35 percent slopes64487709495631nktak64519921:31680
Maybeso peat, 5 to 35 percent slopes91B88025495811nldak64519921:31680
Maybeso peat, 35 to 60 percent slopes91D4410495821nlfak64519921:31680
Maybeso-Mosman complex, 35 to 75 percent slopes35D2898494961nhnak64519921:31680
Maybeso-Mosman complex, 5 to 35 percent slopes35B2145494951nhmak64519921:31680
Mosman-Maybeso complex, 50 to 100 percent slopes35F342494971nhpak64519921:31680

Map of Series Extent

Approximate geographic distribution of the MAYBESO 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 .