Official Series Description


Lab Data Summary

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

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.

Competing Series

Soil series competing with PINECREEK 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 PINECREEK 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 PINECREEK 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 PINECREEK, 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-2010-08-31-08 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 1 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  2. ID-2010-08-31-09 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 2 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  3. ID-2011-06-01-16 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 1 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  4. ID-2011-06-01-17 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 2 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

Map Units

Map units containing PINECREEK 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
Pinecreek-Noil complex, 20 to 60 percent slopesPn1760814016wb1lid05720131:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes2v71h6226629522v71hid60619761:24000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes7706026630022v71gid60619761:24000
Pinecreek gravelly ashy silt loam, moist, 20 to 65 percent slopes7753726630041hnkmid60619761:24000
Pinecreek gravelly ashy silt loam, moist, 35 to 65 percent slopes97753530990092dvrbid60619761:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes5316581534642v71hid60819941:24000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes7751021534942v71gid60819941:24000
Pinecreek-Lotuspoint, stony complex, strongly acid, 35 to 65 percent slopes, eroded78301415349554qgid60819941:24000
Pinecreek gravelly ashy silt loam, moist, 20 to 65 percent slopes1hnkm3927430721hnkmid60819941:24000
Pinecreek-Noil complex, 20 to 60 percent slopesPn172743030wb1lid60819941:24000
Pinecreek ashy silt loam, moist, 35 to 65 percent slopes774193313901501hnkkid62020131:24000
Pinecreek, moist-Lotuspoint complex, 35 to 65 percent slopes7841697186180920hccid62020131:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes903114213897632v71hid62020131:24000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes77088513901412v71gid62020131:24000
Pinecreek gravelly ashy silt loam, moist, 20 to 65 percent slopes77543013901521hnkmid62020131:24000
Ahrs-Pinecreek association, 25 to 75 percent slopes2v71h142128509832v71hid6701:24000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes2v71g12828510012v71gid6701:24000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes977041822302422v71gwa06320121:24000
Pinecreek gravelly ashy silt loam, moist, 20 to 65 percent slopes977527522302431hnkmwa06320121:24000
Pinecreek gravelly ashy silt loam, moist, 20 to 65 percent slopes97751426513891hnkmwa07519751:20000
Pinecreek gravelly ashy silt loam, 30 to 75 percent slopes9770326513882v71gwa07519751:20000

Map of Series Extent

Approximate geographic distribution of the PINECREEK 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 .