Official Series Description


Lab Data Summary

Aggregate lab data for the CHARD soil series. This aggregation is based on all pedons with a current taxon name of CHARD, 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 CHARD 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
886P006785WA075005Chard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7811127,-117.7930527
888P028187ID069001Chard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4134712,-116.9910355
892P031091ID069036Chard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4133339,-116.9897232
988P028287ID069002Chard5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4034691,-116.9543686
992P031191ID069037Chard7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3933334,-117.0247192

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CHARD 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 CHARD series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the CHARD 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 CHARD 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 .

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.

Competing Series

Soil series competing with CHARD 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 CHARD 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 CHARD 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.

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

Soil series sharing subgroup-level classification with CHARD, 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-2010-08-30-10 | Lewis and Nez Perce Counties - 2004

    Generalized distribution of the dominant soils in the immediate Lewiston area (Soil Survey of Lewis and Nez Perce Counties, Idaho; 2004).

Map Units

Map units containing CHARD 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
Chard sandy loam, 12 to 25 percent slopes2226203253811557kid60019891:24000
Chard sandy loam, 7 to 12 percent slopes2111593253816557jid60019891:24000
Chard sandy loam, 3 to 7 percent slopes207023253817557hid60019891:24000
Chard sandy loam, 25 to 40 percent slopes235233253818557lid60019891:24000
Chard variant loamy fine sand, 7 to 25 percent slopes25172686325557nid60919891:24000
Chard silt loam, 10 to 25 percent slopes265618796362nvxid61119941:24000
Chard silt loam, 25 to 45 percent slopes272144796372nvyid61119941:24000
Chard silt loam, 2 to 10 percent slopes252055796352nvwid61119941:24000
Chard complex, 30 to 50 percent slopes282024796382nvzid61119941:24000
Chard-Urban land complex, gently sloping301130796412nw2id61119941:24000
Tammany-Chard-Rock outcrop complex, 35 to 65 percent slopes127837795932ntjid61119941:24000
Chard-Tammany complex, 20 to 45 percent slopes29762796392nw0id61119941:24000
Chard sandy loam, 12 to 25 percent slopes221894153994557kid61719761:24000
Chard variant loamy fine sand, 2 to 7 percent slopes24691153996557mid61719761:24000
Chard sandy loam, 25 to 40 percent slopes23529153995557lid61719761:24000
Chard variant loamy fine sand, 7 to 25 percent slopes25434153997557nid61719761:24000
Chard sandy loam, 7 to 12 percent slopes21404153993557jid61719761:24000
Chard sandy loam, 3 to 7 percent slopes20384153992557hid61719761:24000
Chard very fine sandy loam, 15 to 30 percent slopes4096847632v69or67019991:24000
Chard silt loam, 0 to 5 percent slopesCHB30626815028xdwa00119651:20000
Chard silt loam, 5 to 30 percent slopesCHD17526815128xfwa00119651:20000
Chard very fine sandy loam, 5 to 15 percent slopes3327936880629lkwa02519791:24000
Chard silt loam, 0 to 15 percent slopes2338266861829dhwa04319781:24000
Chard silt loam, 15 to 25 percent slopes28895168522299dwa07519751:20000
Chard silt loam, 3 to 7 percent slopes26422968520299bwa07519751:20000
Chard silt loam, 7 to 15 percent slopes27346668521299cwa07519751:20000
Chard loam, 15 to 25 percent slopes142357694122b73wa60319841:24000
Chard loam, 2 to 5 percent slopes112149694032b6twa60319841:24000
Chard loam, 25 to 40 percent slopes151878694132b74wa60319841:24000
Chard loam, 10 to 15 percent slopes131303694112b72wa60319841:24000
Chard loam, 5 to 10 percent slopes121240694102b71wa60319841:24000
Chard loam, 40 to 60 percent slopes16527694142b75wa60319841:24000
Chard silt loam, 15 to 30 percent slopesChD3390696472bgpwa61319671:20000
Chard silt loam, 8 to 15 percent slopesChC2212696462bgnwa61319671:20000
Chard silt loam, 30 to 40 percent slopesChE1317696482bgqwa61319671:20000
Chard silt loam, 3 to 8 percent slopesChB281696452bgmwa61319671:20000
Chard silt loam, 25 to 40 percent slopesCdE12729697982bmkwa62319701:20000
Chard silt loam, 7 to 25 percent slopesCdD6529697972bmjwa62319701:20000
Chard silt loam, moderately shallow, 7 to 25 percent slopesCeD925697992bmlwa62319701:20000
Chard silt loam, 0 to 7 percent slopesCdB722697962bmhwa62319701:20000
Chard very fine sandy loam, 25 to 40 percent slopes, erodedChE2481698012bmnwa62319701:20000
Chard very fine sandy loam, 7 to 25 percent slopes, erodedChD2243698002bmmwa62319701:20000

Map of Series Extent

Approximate geographic distribution of the CHARD 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 .