What Was The Soil Makeup Of Oso
Official Series Description
Lab Data Summary
Amass lab data for the BAYWOOD soil serial. This aggregation is based on all pedons with a current taxon name of BAYWOOD, and practical forth 1-cm thick depth slices. Solid lines are the slice-wise median, divisional on either side by the interval divers by the piece-wise 5th and 95th percentiles. The median is the value that splits the data in half. 5 percent of the information are less than the 5th percentile, and five pct of the data are greater than the 95th percentile. Values along the right hand side y-centrality 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 BAYWOOD 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:
| MLRA | Lab ID | Pedon ID | Taxonname | CI | NSSL / NASIS Reports | Link To SoilWeb GMap |
|---|---|---|---|---|---|---|
| 14 | 73C0028 | S1973CA087007 | BAYWOOD | 7 | Chief | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Backdrop | 36.9180565,-121.8511124 |
Water Residual
Monthly h2o remainder estimated using a leaky-bucket fashion model for the BAYWOOD 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 every bit 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 past 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-full water storage (sum[awc_r * horizon thickness]) for each soil serial. Note that this representation of "water storage" is based on the average ability of most plants to extract soil water betwixt 15 bar ("permanent wilting point") and 1/3 bar ("field capacity") matric potential. Soil moisture country can be roughly interpreted equally "dry out" when storage is depleted, "moist" when storage is betwixt 0mm and AWC, and "wet" when there is a surplus. Clearly there are a lot of assumptions broiled into this kind of monthly h2o 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 instance with the BAYWOOD serial. Sketches are arranged co-ordinate 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 BAYWOOD series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit of measurement geometry and 1981-2010, 800m PRISM information .
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Geomorphic description summaries for the BAYWOOD series and siblings. Serial are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. meridian to bottom). Well-nigh soil series (SSURGO components) are associated with a hillslope position and i 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. Pocket-sized Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .
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Competing Series
Soil serial competing with BAYWOOD share the aforementioned family unit level nomenclature in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .
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Select almanac climate data summaries for the BAYWOOD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM information .
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Geomorphic description summaries for the BAYWOOD series and competing. Serial are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. elevation to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Well-nigh soil series (SSURGO components) are associated with a hillslope position and one or more than 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 exist used to judge the reliability of trends. Shannon entropy values close to 0 stand for soil series with relatively consequent geomorphic association, while values close to 1 advise lack thereof. Source: SSURGO component records .
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There are bereft data to create the 3D hills figure.
In that location are insufficient data to create the 3D mountains figure.
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Block Diagrams
Click a link below to display the diagram. Notation that these diagrams may exist from multiple survey areas.
- CA-2012-05-09-sixteen | San Mateo Area - May 1961
Southwest to northeast cantankerous section, at Pigeon Indicate, showing human relationship of geologic formations, land forms, and soil series. Prepared by R. J. Arkley, Academy of California, Section of Soils and Establish Nutritions (Soil Survey of San Mateo Area, California; May 1961).
Map Units
Map units containing BAYWOOD as a major component. Limited to 250 records.
| Map Unit Proper noun | Symbol | Map Unit Area (air-conditioning) | Map Unit Key | National Map Unit Symbol | Soil Survey Area | Publication Date | Map Scale |
|---|---|---|---|---|---|---|---|
| Baywood sand, two to 15 percent slopes | BbC | 11300 | 455563 | h91l | ca053 | 1972 | 1:24000 |
| Baywood loamy sand, 2 to fifteen percentage slopes | 105 | 3027 | 455881 | h9cv | ca087 | 1976 | 1:24000 |
| Baywood loamy sand, 15 to xxx percent slopes | 106 | 2358 | 455882 | h9cw | ca087 | 1976 | 1:24000 |
| Baywood loamy sand, xxx to 50 per centum slopes | 107 | 1920 | 455883 | h9cx | ca087 | 1976 | 1:24000 |
| Baywood loamy sand, 0 to ii percent slopes | 104 | 1434 | 455880 | h9ct | ca087 | 1976 | 1:24000 |
| Baywood variant loamy sand | 108 | 447 | 455884 | h9cy | ca087 | 1976 | 1:24000 |
| Baywood loamy sand, 2 to 9 percentage slopes | BaC | 610 | 459670 | hfb2 | ca097 | 1968 | i:20000 |
| Baywood loamy sand, ix to xxx percent slopes | BaE | 205 | 459671 | hfb3 | ca097 | 1968 | one:20000 |
| Urban land-Baywood complex | 147 | 3843 | 456700 | hb78 | ca610 | 1975 | 1:24000 |
| Baywood variant, sand | 105 | 248 | 456658 | hb5x | ca610 | 1975 | 1:24000 |
| Baywood sandy loam, sloping, eroded | BaC2 | 147 | 456320 | h9v0 | ca637 | 1958 | i:15000 |
| Baywood sandy loam, gently slopping, eroded | BaB2 | 58 | 456319 | h9tz | ca637 | 1958 | 1:15000 |
| Baywood sandy loam, moderately steep, eroded | BaD2 | fourteen | 456321 | h9v1 | ca637 | 1958 | ane:15000 |
| Baywood fine sand, ii to ix pct slopes | 104 | 3545 | 457076 | hbmd | ca664 | 1977 | 1:24000 |
| Baywood fine sand, ix to 15 pct slopes | 105 | 1755 | 457077 | hbmf | ca664 | 1977 | 1:24000 |
| Baywood fine sand, xv to 30 percent slopes | 106 | 720 | 457078 | hbmg | ca664 | 1977 | one:24000 |
| Baywood loamy sand, 2 to 9 percent slopes | BcC | 1007 | 457566 | hc46 | ca673 | 1974 | 1:24000 |
| Caperton-Baywood families complex, 45 to eighty percent slopes | 43 | 3340 | 465351 | hm7b | ca776 | 1981 | 1:24000 |
Map of Series Extent
Approximate geographic distribution of the BAYWOOD soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, utilize the Series Extent Explorer (SEE) awarding. Source: generalization of SSURGO geometry .
Source: https://casoilresource.lawr.ucdavis.edu/sde/?series=baywood
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