Official Series Description


Lab Data Summary

Aggregate lab data for the REYWAT soil series. This aggregation is based on all pedons with a current taxon name of REYWAT, 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 REYWAT 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
1099P0250S1998OR069015Reywat6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6294441,-120.2741699
n/a78P0448S1978UT023001Reywat5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the REYWAT 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 REYWAT 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 REYWAT 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 REYWAT 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 flats position figure.

Competing Series

Soil series competing with REYWAT 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 REYWAT 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 REYWAT 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.

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 REYWAT, 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. ID-2010-08-30-01 | Adams-Washington Area - 2001

    Typical pattern of soils and underlying material in general soil map units 5, 10, 16, and 17 (Soil Survey of Adams-Washington Area, Idaho; 2001).

  2. UT-2010-11-05-04 | Tooele County Area - 2000

    Typical pattern of soils and parent material in the Borvant-Abela-Kapod general soil map unit (adjacent to the Lodar-Reywat-Lundy general soil map unit) (Soil Survey of Tooele County Area, Utah; 2000).

  3. UT-2010-11-05-05 | Tooele County Area - 2000

    Typical pattern of soils and parent material in the Lakewin-Erda-Kapod general soil map unit (adjacent to the Lodar-Reywat-Lundy general soil map unit) (Soil Survey of Tooele County Area, Utah; 2000).

  4. UT-2012-03-22-15 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Borvant-Abela-Kapod general soil map units (adjacent to the Lodar-Reywat-Lundy general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

  5. UT-2012-03-22-16 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Lakewin-Erda-Kapod general soil map units (adjacent to the Lodar-Reywat-Lundy general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

  6. UT-2012-03-22-17 | Tooele Area - 2000

    Typical pattern of soils and parent material in the Lodar-Reywat-Lundy and Dateman-Podmor-Rock outcrop general soil map units (adjacent to the Borvant-Abela-Kapod general soil map unit). (Soil Survey of Tooele Area, Utah; Tooele County and Parts of Box Elder, Davis, and Juab Counties, Utah, and Parts of White Pine and Elko Counties, Nevada; 2000).

Map Units

Map units containing REYWAT 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
Devada-Reywat-Bitner association37216135103466413qn8ca68520061:24000
Devada-Reywat association3716813103469713qpbca68520061:24000
Reywat-Marepas association539670413871431hkfkca68520061:24000
Devada-Reywat-Rubble land association3746243103469613qp9ca68520061:24000
Reywat-Devada association5375508103465713qn1ca68520061:24000
Devada-Reywat-Rock outcrop association3733605103469513qp8ca68520061:24000
Reywat-Rock outcrop-Marepas association540348613871441hkflca68520061:24000
Bucklake-Reywat association3283243103465613qn0ca68520061:24000
Old Camp-Reywat-Rubble land association5002986103473813qqnca68520061:24000
Steerlake-Reywat association5721998103467713qnpca68520061:24000
Bucklake-Bombadil-Reywat association3251420103472713qq9ca68520061:24000
Reywat cobbly loam, 4 to 15 percent slopes535762103471313qpvca68520061:24000
Reywat very stony loam, 8 to 30 percent slopes536449103476713qrlca68520061:24000
Reywat-Fernpoint association538139103476813qrmca68520061:24000
Gem-Reywat complex, 2 to 30 percent slopes7361448812702qkmid65619921:24000
Gem-Reywat complex, 30 to 65 percent slopes7449983812712qknid65619921:24000
Bakeoven-Reywat complex, 2 to 30 percent slopes1348312811292qf2id65619921:24000
Bakeoven-Reywat-Rock outcrop complex, 30 to 60 percent slopes1441369811402qffid65619921:24000
Cranecreek-Reywat complex, 2 to 25 percent slopes3715576812302qjbid65619921:24000
Reywat-Bakeoven complex, 30 to 60 percent slopesRBF6376813852qpbid65919711:20000
Reywat-Bakeoven complex, 2 to 30 percent slopesRBE3333813842qp9id65919711:20000
Reywat gravelly loam, 0 to 30 percent slopes537608823882rqpid70719761:24000
Devada-Old Camp-Reywat association7165326026194352rbrtnv62519811:24000
Reywat-Ister-Rock outcrop association7740228126194342ttw5nv62519811:24000
Ister-Reywat-Koontz association2444864741122w4fcnv62519811:24000
Yuko-Reywat-Rock outcrop association3426153474271hxj2nv62819801:24000
Tristan-Arzo-Reywat association12724292474163hxdlnv62819801:24000
Reywat-Rock outcrop complex, 15 to 50 percent slopes8633844474392hxmznv62819801:24000
Reywat extremely stony loam, 15 to 30 percent slopes8611387474390hxmxnv62819801:24000
Reywat-Ister-Rock outcrop association674012364744512ttw5nv62819801:24000
Reywat-Rock outcrop complex, cool, 15 to 50 percent slopes8641176474441hxpknv62819801:24000
Reywat very cobbly sandy loam, 8 to 15 percent slopes862655474391hxmynv62819801:24000
Ister-Reywat-Koontz association84163024627932w4fcnv62919751:24000
Devada-Reywat association116718090474504hxrlnv75919951:24000
Old Camp-Reywat-Rubble land association10658910474474hxqmnv75919951:24000
Reywat-Fernpoint association13288260474568hxtnnv75919951:24000
Reywat-Devada association13293530474569hxtpnv75919951:24000
Reywat very stony loam, 8 to 30 percent slopes13263490474566hxtlnv75919951:24000
Reywat-Westbutte-Hapgood association13273110474567hxtmnv75919951:24000
Reywat-Devada-Hart Camp association13252590474565hxtknv75919951:24000
Hart Camp-Reywat-Westbutte association1276310474548hxt0nv75919951:24000
Terca-Reywat-Wylo association37440590477477j0vhnv77119901:24000
Jaybee-Old Camp-Reywat association3129721477457j0tvnv77119901:24000
Bombadil-Old Camp-Reywat association2809515477450j0tmnv77119901:24000
Old Camp-Reywat-Jaybee association2508990477426j0svnv77119901:24000
Old Camp-Reywat-Theon association2587148477433j0t2nv77119901:24000
Bucklake-Reywat association5135766477499j0w6nv77119901:24000
Bucklake-Bombadil-Reywat association5105319477496j0w3nv77119901:24000
Reywat-Ister association3444915477470j0v8nv77119901:24000
Bucklake-Reywat-Devada association5154624477500j0w7nv77119901:24000
Devada-Reywat-Tunnison association1384277477356j0qlnv77119901:24000
Jaybee-Reywat association3183974477463j0v1nv77119901:24000
Wylo-Reywat-Rock outcrop association2792736477449j0tlnv77119901:24000
Reywat-Rock outcrop complex, 15 to 50 percent slopes340450477466j0v4nv77119901:24000
Reywat-Ister-Rock outcrop association7401151026194502ttw5nv77219851:24000
Devada-Reywat-Duco association163945024527022nb7fnv77219851:24000
Reywat-Devada-Rock outcrop association741475024527332nb8fnv77219851:24000
Reywat-Tristan-Devada association743364024527352nb8hnv77219851:24000
Reywat-Devada-Ister association742256024527342nb8gnv77219851:24000
Devada-Old Camp-Reywat association16510024527042nb7hnv77219851:24000
Old Camp-Reywat association699495644589pmr6nv77319811:24000
Ruclick-Reywat-Rock outcrop complex, 20 to 50 percent south slopes5021430827222822sf3jor6451:24000
Sumine-Reywat-Rock outcrop complex, 10 to 30 percent slopesSsE25231482626j66lut60819811:24000
Reywat-Rock outcrop complex, 30 to 60 percent slopesReF12102482594j65kut60819811:24000
Sumine-Reywat-Rock outcrop complex, 30 to 60 percent slopesSsF11705482627j66mut60819811:24000
Borvant-Reywat complex, 8 to 30 percent slopesBhD6764482466j61fut60819811:24000
Reywat-Rock outcrop complex, 10 to 30 percent slopesReE5613482593j65jut60819811:24000
Borvant-Reywat complex, 30 to 60 percent slopesBhF5129482467j61gut60819811:24000
Reywat-Reebok-Rock outcrop complex, 10 to 30 percent slopesRdE3149482592j65hut60819811:24000
Reywat-Broad-Rock outcrop association, 30 to 60 percent slopes4894349482155j5qdut61119921:24000
Broad, moist-Reywat, moist-Rock outcrop association, 30 to 60 percent slopes1016076482112j5p0ut61119921:24000
Reywat-Broad families-Rock outcrop association, 15 to 80 percent slopes642620031838912x4gnut6171:24000
Reywat-Red Butte families complex, 5 to 50 percent slopes62949331838892x4glut6171:24000
Reywat family-Rock outcrop complex, 15 to 80 percent slopes63440131838902x4gmut6171:24000
Red Butte-Kanarra-Reywat families, association, 5 to 40 percent slopes188625244nzm5ut6491:24000
Reywat-Pharo-Amtoft families, complex, 25 to 65 percent slopes190581656mj83ut6491:24000

Map of Series Extent

Approximate geographic distribution of the REYWAT 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 .