Official Series Description


Lab Data Summary

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

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
10485P055884IA0130011Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3116684,-92.3241653
10485P055984IA0130012Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3119431,-92.3233337
10485P037384IA1130012Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0275002,-91.5416641
10485P037584IA1130021Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9049988,-91.7566681
10485P037684IA1130022Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9036102,-91.7566681
10485P033185IA0550011Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5583344,-91.3166656
10485P033285IA0550012Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5583344,-91.3166656
10485P033385IA0550013Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5583344,-91.3166656
10485P034785IA0690021Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7999992,-93.2333298
10485P034885IA0690022Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7999992,-93.2361145
10485P035285IA0830021Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4122276,-93.0177002
10485P035385IA0830022Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4119492,-93.0182571
10486P018585IA113001Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8824997,-91.7324982
10486P018685IA113002Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8813896,-91.7322235
10486P018785IA113003Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8813896,-91.7316666
10487P032786IA0130013Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3113899,-92.3002777
10487P032886IA0130014Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3116684,-92.3019409
10487P035086IA1130041Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.913887,-91.628334
10487P035186IA1130042Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.913887,-91.6302795
10487P035286IA1130043Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.913887,-91.6305542
10488P061287IA113003Dinsdale6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0288887,-91.5541687
104UMN2031S1975MN1092031Dinsdale3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9082413,-92.6251907
104X53-377B-1S1982IA105016Dinsdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2778292,-91.1505214
104X53-377-2S1984IA105005Dinsdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9621227,-91.0856882
104UMN4451S1990MN1314451Dinsdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3114815,-93.0844345
10493P0136S1992MN131006Dinsdale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.310833,-93.0838852
10405N0262S2004IA017002Dinsdale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.67136,-92.537056
105X28-377B-1S1980IA055008Dinsdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5774263,-91.3287419
105X49-377B-1S1988IA097011Dinsdale2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.051163,-90.7439168
n/a86P032385IA0130041Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a86P032485IA0130042Dinsdale5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Competing Series

Soil series competing with DINSDALE 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 DINSDALE series and competing. 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 DINSDALE 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.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with DINSDALE, 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. IA-2010-09-02-04 | Black Hawk County - 2006

    Typical pattern of soils and parent material in the Dinsdale-Klinger-Maxfield association (Soil Survey of Black Hawk County, Iowa; 2006).

  2. IA-2010-09-09-06 | Bremer County - 2009

    Typical pattern of soils and parent material in the Klinger-Maxfield association (Soil Survey of Bremer County, Iowa; 2009).

  3. IA-2010-09-09-11 | Cedar County - 2009

    Typical pattern of soils and parent material in the Dinsdale-Klinger-Maxfield association (Soil Survey of Cedar County, Iowa; 2009).

  4. IA-2011-05-31-17 | Delaware County - 1986

    Pattern of soils and parent material in the Dinsdae-Sawmill-Tama association (Soil Survey of Delaware County, Iowa; 1986).

  5. IA-2011-05-31-27 | Floyd County - 1995

    Pattern of soils and parent material in the Maxfield-Klinger-Dinsdale association (Soil Survey of Floyd County, Iowa; 1995).

  6. IA-2011-05-31-47 | Hardin County - 1985

    Pattern of soils and parent material in the Dinsdale-Muscatine-Garwin association (Soil Survey of Hardin County, Iowa; 1985).

  7. IA-2011-06-01-02 | Jones County - 1991

    Typical pattern of soils and parent material in the Dinsdale-Waubeek-Downs association (Soil Survey of Jones County, Iowa; 1991).

  8. IA-2011-06-01-44 | Tama County - 1995

    Typical pattern of soils and parent material in the Dinsdale-Tama association (Soil Survey of Tama County, Iowa; 1995).

Map Units

Map units containing DINSDALE 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
Dinsdale silty clay loam, 2 to 5 percent slopes377B797134028782t3f9ia01119771:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C311724028792t3fcia01119771:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C293884028802t3fdia01119771:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B176764132462t3f9ia01320011:12000
Dinsdale silty clay loam, 5 to 9 percent slopes377C10674132472t3fcia01320011:12000
Dinsdale-Urban land complex, 2 to 5 percent slopes4377B641413347fw3sia01320011:12000
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C25834132482t3fdia01320011:12000
Dinsdale-Urban land complex, 5 to 9 percent slopes4377C21413346fw3ria01320011:12000
Dinsdale silty clay loam, 2 to 5 percent slopes377B96315859932t3f9ia01720081:12000
Dinsdale silty clay loam, 5 to 9 percent slopes377C4415859942t3fcia01720081:12000
Dinsdale silt loam, 2 to 5 percent slopes377B10004032302t3f5ia01919781:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B138124033932t3f9ia02319781:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C211074033942t3fdia02319781:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B1254513971112t3f9ia03120081:12000
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C2171413971132t3fdia03120081:12000
Dinsdale silty clay loam, 5 to 9 percent slopes377C100413971122t3fcia03120081:12000
Dinsdale silty clay loam, 0 to 2 percent slopes37719804038312t3f8ia03319781:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B15034038322t3f9ia03319781:15840
Dinsdale silt loam, 2 to 5 percent slopes377B89544044132t3f5ia04519781:15840
Dinsdale silt loam, 5 to 9 percent slopes377C14424044142t3f6ia04519781:15840
Dinsdale silt loam, 2 to 5 percent slopes377B82164050362t3f5ia05519841:15840
Dinsdale silt loam, 5 to 9 percent slopes377C5824050372t3f6ia05519841:15840
Dinsdale silt loam, 5 to 9 percent slopes, eroded377C24274050382t3f7ia05519841:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B32574059102t3f9ia06719891:15840
Dinsdale silty clay loam, 0 to 2 percent slopes37727404059092t3f8ia06719891:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B284774049032t3f9ia06919771:15840
Dinsdale silty clay loam, 0 to 2 percent slopes37729284049022t3f8ia06919771:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C218694049052t3fdia06919771:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C8804049042t3fcia06919771:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B225774062972t3f9ia07519731:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C238364062992t3fdia07519731:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C26594062982t3fcia07519731:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, eroded377D23094063002t3ffia07519731:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C227244066592t3fdia08319821:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B21754066582t3f9ia08319821:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, eroded377D25394066602t3ffia08319821:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B8977579552t3f9ia09520051:12000
Dinsdale silty clay loam, 5 to 9 percent slopes377C5427579562t3fcia09520051:12000
Dinsdale silt loam, 2 to 5 percent slopes377B263407497fp12ia09719881:15840
Dinsdale silt loam, 2 to 5 percent slopes, moderately eroded377B2253407498fp13ia09719881:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B39724080052t3f9ia10319791:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C23124080062t3fdia10319791:15840
Dinsdale silt loam, 2 to 5 percent slopes377B101344081452t3f5ia10519881:15840
Dinsdale silt loam, 5 to 9 percent slopes377C19054081462t3f6ia10519881:15840
Dinsdale silt loam, 5 to 9 percent slopes, eroded377C27474081472t3f7ia10519881:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B233984086192t3f9ia11319701:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C32514086202t3fcia11319701:15840
Dinsdale-Urban land complex, 2 to 5 percent slopes4377B20942606463fw3sia11319701:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C218464086212t3fdia11319701:15840
Dinsdale-Urban land complex, 5 to 9 percent slopes4377C7582606464fw3ria11319701:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C223884094672t3fdia12719781:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, eroded377D219914094682t3ffia12719781:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C3924094662t3fcia12719781:15840
Dinsdale silty clay loam, 0 to 2 percent slopes377166454096652t3f8ia13119711:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B95964096662t3f9ia13119711:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, eroded377D24654105832t3ffia15719781:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C22374105822t3fdia15719781:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B21114109692t3f9ia16319891:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C213974109712t3fdia16319891:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C9754109702t3fcia16319891:15840
Dinsdale silty clay loam, 5 to 9 percent slopes, eroded377C2277334114602t3fdia17119891:15840
Dinsdale silty clay loam, 2 to 5 percent slopes377B120824114572t3f9ia17119891:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, eroded377D253944114622t3ffia17119891:15840
Dinsdale silty clay loam, 5 to 9 percent slopes377C41264114592t3fcia17119891:15840
Dinsdale silty clay loam, 2 to 5 percent slopes, eroded377B217534114582t3fbia17119891:15840
Dinsdale silty clay loam, 9 to 14 percent slopes, severely eroded377D38354114632t3fgia17119891:15840
Dinsdale silt loam, 2 to 5 percent slopes377B340925814412t3f5ia19520121:12000
Dinsdale silt loam, 0 to 2 percent slopes37777125814402t3f4ia19520121:12000

Map of Series Extent

Approximate geographic distribution of the DINSDALE 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 .