Official Series Description


Lab Data Summary

Aggregate lab data for the CARRIZO soil series. This aggregation is based on all pedons with a current taxon name of CARRIZO, 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 CARRIZO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
3181P038081CA071004Carrizo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.2738876,-114.3572235
4080P016980AZ013010Carrizo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.9783325,-112.660553
4084P048184AZ021008Carrizo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8416672,-112.1333313

Water Balance

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

Click the image to view it full size.



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 CARRIZO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

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

Click the image to view it full size.

Select annual climate data summaries for the CARRIZO 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 CARRIZO 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with CARRIZO, 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. AZ-2011-05-27-02 | Aguila-Carefree Area, Parts of Maricopa and Pinal Counties - 1986

    Diagram of Agua Fria River-Lake Pleasant Area (Soil Survey of Aguila-Carefree Area, Parts of Maricopa and Pinal Counties, Arizona; 1986).

  2. AZ-2011-05-27-10 | Gila Bend-Ajo Area - 1997

    Typical pattern of soil associations in the survey area (Soil Survey of Gila Bend-Ajo Area, Arizona; 1997).

  3. AZ-2011-05-27-11 | Gila Bend-Ajo Area - 1997

    A typical area of Gunsight-Chuckawalla complex, 1 to 15 percent slopes (Soil Survey of Gila Bend-Ajo Area, Arizona; 1997).

  4. AZ-2011-05-27-12 | Gila Bend-Ajo Area - 1997

    An idealized soil-landscape profile of the Maricopa Mountains (Soil Survey of Gila Bend-Ajo Area, Arizona; 1997).

  5. AZ-2011-05-27-13 | Gila Bend-Ajo Area - 1997

    Cross section of the Valley of the Ajo, from Black Mountain across Rio Cornez (Soil Survey of Gila Bend-Ajo Area, Arizona; 1997).

Map Units

Map units containing CARRIZO 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
Carrizo complex, 1 to 5 percent slopes151189522491rcgaz62319941:24000
Carrizo family very gravelly loamy sand, 1 to 3 percent slopes193609315078821mm2caz62720051:24000
Carrizo-Riverwash complex, 3 to 8 percent slopes MLRA 30211514015078842ss19az62720051:24000
Carrizo-Riverwash complex, 1 to 3 percent slopes22593915078851mm2gaz62720051:24000
Carrizo family-Riverwash complex, 1 to 3 percent slopes20514215078831mm2daz62720051:24000
Toquop-Carrizo complexTx41615454921nw6laz64119651:31680
Denure-Momoli-Carrizo complex, low precipitation3032370530491s68az64519821:24000
Momoli-Carrizo complex, low precipitation9223899531681sb3az64519821:24000
Antho-Carrizo-Maripo complex317286530471s66az64519821:24000
Momoli-Carrizo complex9114589531551s9paz64519821:24000
Brios-Carrizo complex, low precipitation, 1 to 5 percent slopes1113070529701s3qaz64519821:24000
Brios-Carrizo complex, 1 to 5 percent slopes1013050529571s39az64519821:24000
Denure-Momoli-Carrizo complex299360530411s60az64519821:24000
Carrizo-Gunsight complex, 1 to 5 percent slopes159020529971s4laz64519821:24000
Antho-Carrizo-Maripo complex, low precipitation44390530701s6yaz64519821:24000
Carrizo very gravelly sand142950529951s4jaz64519821:24000
Carrizo very gravelly sand342787532781sfnaz64919781:24000
Antho-Carrizo complex, 0 to 3 percentAGB29356532921sg3az65119721:20000
Carrizo and Brios soilsCF17457533141sgtaz65119721:20000
Carrizo gravelly sandy loamCb4703533171sgxaz65119721:20000
Antho-Carrizo complex, 0 to 1 percent slopesAfA3861533031sggaz65119721:20000
Carrizo-Ebon complex, 3 to 12 percent slopesCeD1928533181sgyaz65119721:20000
Antho-Carrizo complex, 1 to 3 percent slopesAfB1106533041sghaz65119721:20000
Vint-Carrizo complexVr686534161sl3az65119721:20000
Gunsight-Rillito-Carrizo complex, 1 to 15 percent slopes37105585534561smdaz65319851:24000
Carrizo-Momoli complex, 0 to 3 percent slopes637770534811sn6az65319851:24000
Why-Carrizo complex, 0 to 3 percent slopes6722022534891sngaz65319851:24000
Quilotosa-Momoli-Carrizo complex, 1 to 15 percent slopes5319590534741smzaz65319851:24000
Carrizo-Dateland complex, 0 to 3 percent slopes517463534701smvaz65319851:24000
Momoli-Carrizo extremely gravelly sandy loams, 1 to 10 percent slopes4914370534691smtaz65319851:24000
Momoli-Carrizo, bench, very gravelly sandy loams, 1 to 3 percent slopes504317534711smwaz65319851:24000
Denure-Carrizo, bench, gravelly fine sandy loams182239534351slqaz65319851:24000
Carrizo fine sandy loamCb905535011snvaz65519691:20000
Carrizo gravelly loamy sandCa304535001sntaz65519691:20000
Carrizo extremely gravelly coarse sand, 0 to 3 percent slopes511790547991v0qaz65619831:20000
Gunsight-Chuckawalla-Carrizo association, 1 to 45 percent slopes172406547811v04az65619831:20000
Momoli-Carrizo family complex, 1 to 5 percent slopes22021992524205502m7s8az6571:24000
Carrizo family-Riverbend family-Riverwash complex, dry, 0 to 3 percent slopes39018084824402942mxb5az6571:24000
Gilman-Carrizo family complex, dry, 0 to 3 percent slopes4002287324402932mxb4az6571:24000
Oxyaquic Torrifluvents-Carrizo family-Typic Fluvaquents complex, dry, 0 to 5 percent slopes670271431096362ybs3az6571:24000
Carrizo family very gravelly sandy loam, dry, 0 to 3 percent slopes38513224402952mxb6az6571:24000
Cavelt-Carrizo-Gunsight complex, 1 to 10 percent slopes98245543381tjvaz65819911:24000
Carrizo-Momoli complex, 1 to 3 percent slopes34725542991thlaz65819911:24000
Carrizo very gravelly coarse sand, 0 to 1 percent slopes52815543301tjlaz65819911:24000
Carrizo-Pinamt complex, 1 to 5 percent slopes41595543201tj8az65819911:24000
Momoli-Carrizo complex, 1 to 8 percent slopes3418736535601sqraz65919841:24000
Carrizo family-Brios-Riverwash complex, 0 to 5 percent slopes1190526010320jtaz66120091:24000
Ebon-Carrizo family complex, 0 to 10 percent slopes3620606009020jdaz66120091:24000
Momoli-Carrizo family complex, 1 to 8 percent slopes6815506009720jmaz66120091:24000
Carrizo complex, 1 to 5 percent slopes1542539798363vsrnaz69720051:24000
Huevi-Carrizo complex, 1 to 25 percent slopes6326729798424vstmaz69720051:24000
Carrizo-Riverwash complex, 3 to 8 percent slopes MLRA 3017267087983652ss19az69720051:24000
Carrizo-Riverwash complex, 0 to 1 percent slopes169446798364vsrpaz69720051:24000
Carrizo complex, 1 to 5 percent slopes181257615810nnsvaz70120011:24000
Carrizo-Carrizo-Riverbend association1949615811nnswaz70120011:24000
Carrizo very gravelly sand, 0 to 9 percent slopesCeC28288456768hb9gca63819671:24000
Carrizo stony sand, 2 to 9 percent slopesCcC18104464007hktzca68019741:24000
Carrizo complex, 4 to 15 percent slopes1542170624840962n81vca68019741:24000
Carrizo gravelly sandCe9680464064hkwtca68119681:24000
Carrizo association, 2 to 8 percent slopes154372825355092qpt6ca6951:24000
Carrizo-Orita-Rositas association, 0 to 8 percent slopes5516975466717hnndca69720001:24000
Carrizo-Clegorpass-Carrizo frequently flooded association, 2 to 8 percent slopes5503742466716hnncca69720001:24000
Rositas-Carrizo-Bunkerhill association, 2 to 30 percent slopes141507466590hnj9ca69720001:24000
Carrizo complex, 2 to 8 percent slopes313613243229647hnqsca6991:24000
Bristolake-Carrizo association, 0 to 4 percent slopes252151283229626hnq3ca6991:24000
Carrizo-Clegorpass association, 2 to 8 percent slopes315138263229645hnqqca6991:24000
Carrizo complex, 2 to 8 percent slopes, rubbly31454683229646hnqrca6991:24000
Carrizo-Carrizo, warm, association, 2 to 4 percent slopes, frequently flooded3169313229677hnrrca6991:24000
Carrizo association, 2 to 4 percent slopes, frequently flooded3107023229644hnqpca6991:24000
Carrizo stony sand, 2 to 9 percent slopesCcC10848237xgnhca77719811:24000
Pintobasin-Carrizo complex, 2 to 8 percent slopes15151495524380472mtzpca79420121:24000
Oldale-Carrizo complex, 2 to 8 percent slopes207611215470122hs67ca79420121:24000
Carrizo-Rubylee complex, 1 to 4 percent slopes151310311470123hs68ca79420121:24000
Carrizo very gravelly sandy loam, 2 to 4 percent slopes15108028470118hs63ca79420121:24000
Carrizo complex, 2 to 8 percent slopes, flooded151154792027364261mvca79420121:24000
Carrizo extremely gravelly sandy loam, 2 to 8 percent slopes15125090470120hs65ca79420121:24000
Carrizo-Russiroks complex, 2 to 8 percent slopes1540348925051982pz54ca79420121:24000
Carrizo-Pintobasin-Rubylee complex, 0 to 4 percent slopes1514342224844202pd7lca79420121:24000
Carrizo complex, 4 to 15 percent slopes1542310924506072n81vca79420121:24000
Oldale-Carrizo association, 0 to 8 percent slopes2077210525174102qb19ca79420121:24000
Carrizo complex, 0 to 4 percent slopes24051654470109hs5tca79420121:24000
Pintobasin-Carrizo association, 2 to 8 percent slopes, flooded24061404470128hs6fca79420121:24000
Pintobasin-Carrizo association, 2 to 4 percent slopes240737225174062qb15ca79420121:24000
Carrizo-Cambidic Haplodurids association, 4 to 15 percent slopes15418925174052qb14ca79420121:24000
Carrizo gravelly fine sandy loam, 2 to 8 percent slopes4113250526938502s10gca79520231:24000
Carrizo-Typic Haplocalcids association, 1 to 4 percent slopes4321226928910312vjqkca79520231:24000
Carrizo complex, 2 to 8 percent slopes, extremely stony11292933940772ss22ca79520231:24000
Carrizo-Russiroks complex, 2 to 8 percent slopes1540303525354702pz54ca8031:24000
Carrizo stony sand, 2 to 9 percent slopesCcC10972535524hktzca8031:24000
Oldale-Carrizo association, 0 to 8 percent slopes207749625354762qb19ca8031:24000
Carrizo complex, 0 to 4 percent slopes24053622535488hs5tca8031:24000
Carrizo-Cambidic Haplodurids association, 4 to 15 percent slopes154114425354712qb14ca8031:24000
Sweetspring-Carrizo associationSWC375817124261vgxknv60819671:24000
Carrizo-Carrizo-Riverbend associationCRD16217124511vgycnv60819671:24000
Carrizo associationCAC217124501vgybnv60819671:24000
Carrizo-Carrizo-Riverbend association57119133468911hqy5nv75520061:24000
Carrizo association57016675468910hqy4nv75520061:24000
Riverbend-Cheme-Carrizo association59312359469000hr11nv75520061:24000
Cheme-Riverbend-Carrizo association55010608468907hqy1nv75520061:24000
Gypwash-Callville-Carrizo association23510323468984hr0jnv75520061:24000
Riverbend-Carrizo association5908651468915hqy9nv75520061:24000
Heleweiser-Carrizo-Teebar association2856492468987hr0mnv75520061:24000
Varwash-Carrizo association7416280469006hr17nv75520061:24000
Heleweiser-Carrizo association2862866469016hr1knv75520061:24000
Cheme-Carrizo-Huevi association5512673468908hqy2nv75520061:24000
Carrizo-Riverbend association5732233468998hr0znv75520061:24000
Carrizo-Sunrock association5742038469022hr1rnv75520061:24000
Sweetspring-Carrizo association121131516782881tbdbnv75520061:24000
Riverbend-Carrizo, frequently flooded association592972468999hr10nv75520061:24000
Carrizo complex, 1 to 5 percent slopes57546316119681r3cznv75520061:24000
Carrizo very cobbly coarse sand, 2 to 8 percent slopes572437468912hqy6nv75520061:24000
Gypwash-Callville-Carrizo association23554016810011tf6vnv78819821:24000

Map of Series Extent

Approximate geographic distribution of the CARRIZO 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 .