Official Series Description


Lab Data Summary

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

Soil series competing with TIERRA 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 TIERRA 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 TIERRA 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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Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with TIERRA, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2012-05-09-16 | San Mateo Area - May 1961

    Southwest to northeast cross section, at Pigeon Point, showing relationship of geologic formations, land forms, and soil series. Prepared by R. J. Arkley, University of California, Department of Soils and Plant Nutritions (Soil Survey of San Mateo Area, California; May 1961).

Map Units

Map units containing TIERRA 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
Tierra loam, 9 to 15 percent slopes, MLRA 14TaD49804558642tz0wca01319731:24000
Tierra loam, 2 to 9 percent slopes, MLRA 14TaC36664558632tz0rca01319731:24000
Tierra loam, 15 to 30 percent slopes, MLRA 14TaE25204558652tz0xca01319731:24000
Tierra-Watsonville complex, 15 to 30 percent slopes1743766455950h9g2ca08719761:24000
Tierra-Watsonville complex, 30 to 50 percent slopes1752158455951h9g3ca08719761:24000
Tierra loam, 2 to 9 percent slopes, MLRA 14TaCcc4566442tz0rca60919631:20000
Tierra loam, 2 to 9 percent slopes, MLRA 14TaCcc8251422tz0rca61019751:24000
Tierra loam, 15 to 30 percent slopes, MLRA 14TaEcc4567182tz0xca61019751:24000
Urban land-Tierra complex, 2 to 5 percent slopes1504832456703hb7cca61019751:24000
Urban land-Tierra complex, 5 to 15 percent slopes1512669456704hb7dca61019751:24000
Urban land-Tierra complex, 15 to 30 percent slopes1522158456705hb7fca61019751:24000
Tierra loam, 0 to 5 percent slopes145278456698hb76ca61019751:24000
Tierra loam, steep, erodedTeE222604565202yrffca63719581:15000
Tierra loam, moderately steep, erodedTeD216234565182yrfcca63719581:15000
Tierra loam, sloping, erodedTeC26384565172yrfdca63719581:15000
Tierra loam, steep, severely erodedTeE36224565212yrfgca63719581:15000
Tierra sandy loam, acid variant, gently slopingTsB535456524hb1lca63719581:15000
Tierra sandy loam, moderately steep, erodedTmD2360456523hb1kca63719581:15000
Tierra sandy loam, acid variant, sloping, erodedTsC2329456525hb1mca63719581:15000
Tierra sandy loam, sloping, erodedTmC2256456522hb1jca63719581:15000
Tierra loam, moderately steep, severely erodedTeD3109456519hb1fca63719581:15000
Tierra clay loam, sloping, erodedTcC21034565142yrfbca63719581:15000
Tierra clay loam, moderately steep, erodedTcD2764565152yrf9ca63719581:15000
Tierra sandy loam, acid variant, moderately steep, erodedTsD256456526hb1nca63719581:15000
Tierra loam, gently slopingTeB28456516hb1bca63719581:15000
Tierra sandy loam, acid variant, steep, severely erodedTsE322456527hb1pca63719581:15000
Briones-Tierra complex, 15 to 50 percent slopes1106950457082hbmlca66419771:24000
Pismo-Tierra complex, 9 to 15 percent slopes1913040457163hbq6ca66419771:24000
Tierra sandy loam, 2 to 9 percent slopes, MLRA 1421619604571882tz0qca66419771:24000
Tierra loam, 15 to 30 percent slopes, MLRA 142185904571902tz0xca66419771:24000
Tierra loam, 9 to 15 percent slopes, MLRA 142175854571892tz0wca66419771:24000
San Andreas-Tierra complex, 30 to 75 percent slopesSfG11119457487hc1nca67219661:20000
San Andreas-Tierra complex, 15 to 30 percent slopesSfE6729457485hc1lca67219661:20000
Tierra loam, 5 to 30 percent slopes, severely erodedTrE33078457539hc3bca67219661:20000
Tierra sandy loam, 15 to 30 percent slopes, erodedTnE22254457535hc36ca67219661:20000
Tierra loam, 2 to 9 percent slopes, MLRA 14TrC20174575362tz0rca67219661:20000
San Andreas-Tierra complex, 9 to 45 percent slopes, severely erodedSfF31745457486hc1mca67219661:20000
San Andreas-Tierra complex, 5 to 15 percent slopesSfD1517457484hc1kca67219661:20000
Tierra clay loam, 15 to 45 percent slopesTsF1477457540hc3cca67219661:20000
Tierra sandy loam, 2 to 9 percent slopes, MLRA 14TnC14464575332tz0qca67219661:20000
Tierra sandy loam, 9 to 15 percent slopes, erodedTnD21360457534hc35ca67219661:20000
Tierra loam, 9 to 15 percent slopes, MLRA 14TrD12704575372tz0wca67219661:20000
Tierra loamy sand, 9 to 30 percent slopesTmE1116457532hc33ca67219661:20000
Tierra loam, 15 to 30 percent slopes, erodedTrE21064457538hc39ca67219661:20000
Tierra loamy sand, 2 to 9 percent slopesTmC377457531hc32ca67219661:20000
San Andreas-Tierra complex , 15 to 30 percent slopes, erodedSaE2801457638hc6jca67319741:24000
San Andreas-Tierra complex, 30 to 50 percent slopes, erodedSaF2717457639hc6kca67319741:24000
Tierra-San Andreas complex , 15 to 30 percent slopes, severely erodedTaE2292457658hc75ca67319741:24000
San Andreas-Tierra complex, 9 to 15 percent slopes, erodedSaD2192457637hc6hca67319741:24000

Map of Series Extent

Approximate geographic distribution of the TIERRA 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 .