Official Series Description


Lab Data Summary

Aggregate lab data for the JACWIN soil series. This aggregation is based on all pedons with a current taxon name of JACWIN, 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 JACWIN 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
104X45-444S-1S1965IA089926Jacwin2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.42607,-92.21485
105X65444-1-1S1962IA065032Jacwin1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9850719,-91.6443641

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JACWIN 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 JACWIN 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 JACWIN 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 JACWIN 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 mountains figure.

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Competing Series

Soil series competing with JACWIN 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 JACWIN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the JACWIN 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 JACWIN, 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-2011-05-31-29 | Floyd County - 1995

    A cross section showing the parent material of some of the soils in Floyd County (Soil Survey of Floyd County, Iowa; 1995).

Map Units

Map units containing JACWIN 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
Jacwin loam, 3 to 9 percent slopes444C1512550269fjdmia01519771:15840
Jacwin silty clay loam, 1 to 3 percent slopes444816403842fk75ia03319781:15840
Jacwin variant loam, 2 to 5 percent slopes614B622403865fk7xia03319781:15840
Jacwin variant silty clay loam, 5 to 9 percent slopes, severely eroded614C3212403866fk7yia03319781:15840
Jacwin silty clay loam, 1 to 5 percent slopes444B1624745932p20lia03319781:15840
Jacwin loam, 2 to 5 percent slopes444B1034404260fknnia04319791:15840
Jacwin loam, 5 to 9 percent slopes444C530404261fknpia04319791:15840
Jacwin loam, 9 to 14 percent slopes444D244404262fknqia04319791:15840
Fayette-Dubuque-Jacwin complex, 14 to 25 percent slopes497F3947405790fm80ia06519751:15840
Fayette-Dubuque-Jacwin complex, 25 to 40 percent slopes497G1276405791fm81ia06519751:15840
Jacwin loam, 5 to 9 percent slopes444C693405778fm7mia06519751:15840
Jacwin loam, 2 to 5 percent slopes444B301405777fm7lia06519751:15840
Jacwin loam, 9 to 14 percent slopes444D233405779fm7nia06519751:15840
Jacwin silty clay loam, 1 to 5 percent slopes444B903405934fmdnia06719891:15840
Jacwin variant silty clay loam, 5 to 9 percent slopes, severly eroded614C3224792792p6wria06719891:15840
Jacwin loam, 1 to 5 percent slopes444B1141404917flbvia06919771:15840
Jacwin loam, 5 to 9 percent slopes, moderately eroded444C2203404918flbwia06919771:15840
Jacwin silty clay loam, 0 to 2 percent slopes444315406957fngnia08919691:15840
Copaston-jacwin complex, 1 to 3 percent slopes345137816548wdp8ia18720061:12000
Jacwin-Urban land complex, 1 to 3 percent slopes444410416011561qr46ia18720061:12000
Jacwin loam, 2 to 5 percent slopes444B2524450541h3tlia19120051:12000
Jacwin loam, 5 to 9 percent slopes444C667450542h3tmia19120051:12000
Calamine-Jacwin complex, 0 to 3 percent slopes2551493766669tqs8ia19120051:12000
Jacwin loam, 0 to 2 percent slopes444404450540h3tkia19120051:12000

Map of Series Extent

Approximate geographic distribution of the JACWIN 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 .