Official Series Description


Lab Data Summary

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

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TRIMAD, 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 TRIMAD 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
Trimad-Blazon, thin solum-Rock outcrop complex, 20 to 45 percent slopes132401497631jptmco64419801:24000
Poposhia-Trimad complex, 3 to 15 percent slopes129348497628jptjco64419801:24000
Ipson-Trimad complex, 15 to 45 percent slopes12791497626jptgco64419801:24000
Trimad gravelly loam, 2 to 8 percent slopes39C2451609140nfvpmt60420011:24000
Bronec-Trimad-Kalsted complex, 15 to 45 percent slopes927E17941482074z6wmt60420011:24000
Sieben-Trimad complex, 4 to 15 percent slopes, rubbly152D54624509732n8fnmt60520071:24000
Trimad very stony loam, 2 to 8 percent slopes141119185966420f45mt60520071:24000
Trimad loam, 0 to 4 percent slopes42B211476594yn6mt60919711:24000
Amesha-Trimad complex, 15 to 45 percent slopes32E1614765756pwmt60919711:24000
Cabbart-Amesha-Trimad complex, 15 to 45 percent slopes710E141476734ynnmt60919711:24000
Trimad-Bronec complex, 4 to 15 percent slopes100D1072723795142kw2jmt61220111:24000
Bronec, very stony-Trimad, stony complex, 8 to 35 percent slopes100E819823755692kqz8mt61220111:24000
Trimad-Scravo complex, 0 to 2 percent slopes200A206624824842pb74mt61220111:24000
Trimad gravelly loam, 2 to 8 percent slopes39C135613854361hhnhmt61220111:24000
Bronec, stony-Tibson, stony-Trimad, very stony association, 2 to 35 percent slopes186E111122203382djftmt61220111:24000
Trimad, extremely stony-Coyoteflats, rubbly-Trimad complex, 4 to 15 percent slopes200D106623830782kzshmt61220111:24000
Sieben-Trimad complex, 4 to 15 percent slopes, rubbly152D54424304142ml1gmt61220111:24000
Trimad gravelly loam, 2 to 8 percent slopes39C3532520825nfvpmt61420121:24000
Trimad, extremely stony-Coyoteflats, rubbly-Trimad complex, 4 to 15 percent slopes200D14131628342kzshmt61420121:24000
Cabbart-Amesha-Trimad complex, 15 to 45 percent slopes710E759815567256zpmt62219971:24000
Amesha-Trimad complex, 15 to 45 percent slopes32E599915539956pwmt62219971:24000
Anceney-Trimad-Meagher complex, 15 to 60 percent slopes755F4924155711570ymt62219971:24000
Trimad cobbly loam, 15 to 35 percent slopes242E320415534256n1mt62219971:24000
Trimad cobbly loam, 0 to 4 percent slopes242B102915533956mymt62219971:24000
Trimad loam, calcareous surface, 0 to 4 percent slopes442B63115548456smmt62219971:24000
Trimad cobbly loam, 8 to 15 percent slopes242D57315534156n0mt62219971:24000
Cabbart, moist-Amesha-Trimad complex, 15 to 45 percent slopes810E555155734571pmt62219971:24000
Trimad loam, 0 to 4 percent slopes42B40315546956s4mt62219971:24000
Trimad cobbly loam, 4 to 8 percent slopes242C38215534056mzmt62219971:24000
Trimad cobbly loam, moist, 35 to 60 percent slopes742F278155705570rmt62219971:24000
Trimad cobbly loam, 15 to 45 percent slopes140247851464154xc2mt63619831:24000
Trimad-Kalsted complex, 8 to 45 percent slopes142168511464174xc4mt63619831:24000
Trimad cobbly loam, 2 to 8 percent slopes13982291464134xc0mt63619831:24000
Trimad very stony loam, 2 to 8 percent slopes14154841464164xc3mt63619831:24000
Bronec-Trimad-Kalsted complex, 15 to 45 percent slopes2349641466124xkfmt63619831:24000
Anceney-Trimad-Meagher complex, 15 to 60 percent slopes166301465654xhxmt63619831:24000
Trimad, stony-Beaverell, very stony-Chinook complex, 4 to 25 percent slopes2404D259615651457vvmt6691:24000
Trimad-Binna complex, 2 to 8 percent slopes23C18461568065858mt6691:24000
Trimad-Trimad stony complex, 0 to 8 percent slopes2207C1074696125rccnmt6691:24000
Trimad, very stony-Frenchcreek, very stony-Rubble land complex, 25 to 60 percent slopes742F126814247961jtm5mt67020071:24000
Trimad-Blazon-Rock outcrop complex, 3 to 40 percent slopes24827771046023hv8wy03119981:24000
Trimad-Weed-Blazon association, 0 to 15 percent slopes2501031044403hp1wy03119981:24000
Blazon-Trimad complex, 15 to 45 percent slopes111261044243hnjwy03119981:24000
Trimad-Evanston complex, 3 to 30 percent slopes249231044393hp0wy03119981:24000
Evanston-Weed-Trimad loams, 3 to 15 percent slopes148191044303hnqwy03119981:24000
Trimad-Evanston-Delpoint complex, 25 to 50 percent slopes553831368732ypp9wy6291:24000
Trimad-Yampa-Bondoe complex, 15 to 40 percent slopes250432066342zc4kwy6291:24000
Trimad-Evanston complex, 6 to 20 percent slopes230531368462ypngwy6291:24000
Amalia-like-Shooter-Trimad complex, 8 to 25 slopes231732066302zc4gwy6291:24000
Trimad-Trivar complex, 0 to 25 percent slopes28610914361037d3pcwy63319871:24000
Trimad-Doney-Wayden complex, 15 to 45 percent slopes2854509361038d3pdwy63319871:24000
Trimad-Twin Creek association, 0 to 6 percent slopes287450361036d3pbwy63319871:24000
Blazon-Trimad complex, 15 to 45 percent slopes46414148151jh76wy71519741:20000
Bronec-Trimad complex, 6 to 30 percent slopes984226715292191nb8nwy71920131:24000
Varney-Trimad sandy loams, 6 to 45 percent slopes968114615292061nb87wy71920131:24000
Trimad-Trivar complex, 0 to 25 percent slopes9638215414391nqzvwy71920131:24000
Poposhia-Trimad complex, 3 to 15 percent slopes162527501049633j6xwy72119941:24000
Blazon-Trimad complex, 15 to 45 percent slopes111325891049123j58wy72119941:24000
Trimad-Weed-Blazon association, 0 to 15 percent slopes180197911049813j7hwy72119941:24000
Trimad-Blazon, thin solum-Rock outcrop complex, 20 to 45 percent slopes177195791049783j7dwy72119941:24000
Evanston-Weed-Trimad loams, 3 to 15 percent slopes133165781049343j5zwy72119941:24000
Trimad-Blazon complex, 15 to 45 percent slopes176164281049773j7cwy72119941:24000
Ipson-Trimad complex, 15 to 45 percent slopes14178111049423j67wy72119941:24000
Urban land-Poposhia-Trimad complex, 3 to 15 percent slopes18959341049903j7swy72119941:24000
Trimad-Poposhia complex, dry, 6 to 15 percent slopes17958881049803j7gwy72119941:24000
Trimad-Evanston complex, 3 to 30 percent slopes17818921049793j7fwy72119941:24000

Map of Series Extent

Approximate geographic distribution of the TRIMAD 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 .