Official Series Description


Lab Data Summary

Aggregate lab data for the LAHAINA soil series. This aggregation is based on all pedons with a current taxon name of LAHAINA, 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 LAHAINA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
15882P073582HI009001Lahaina7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties21.1227779,-157.2194519
15891P028189HI009005Lahaina6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties20.9244442,-156.6741638
15840A5595S1961HI003006LAHAINA3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties21.4215775,-157.999176

Water Balance

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the LAHAINA 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 LAHAINA series and siblings. 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 LAHAINA 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 LAHAINA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the LAHAINA 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 LAHAINA 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.

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 LAHAINA, 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 LAHAINA 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
Lahaina silty clay, 3 to 7 percent slopes, MLRA 158LaB20294681772w03bhi95019661:24000
Lahaina silty clay, 7 to 15 percent slopes, MLRA 158LaC15474681782w03chi95019661:24000
Lahaina silty clay, 7 to 15 percent slopes, severely eroded, MLRA 158LaC39524681792w03dhi95019661:24000
Lahaina silty clay, 0 to 3 percent slopes, MLRA 158LaA5484681762w037hi95019661:24000
Lahaina silty clay, 25 to 40 percent slopes, severely eroded, MLRA 158LaE34684681812w039hi95019661:24000
Lahaina silty clay, 15 to 25 percent slopes, severely eroded, MLRA 158LaD34254681802v0pthi95019661:24000
Lahaina silty clay, 3 to 7 percent slopes, MLRA 158LaB13984679462w03bhi97019661:24000
Lahaina silty clay, 7 to 15 percent slopes, MLRA 158LaC8264679482w03chi97019661:24000
Lahaina silty clay, 0 to 3 percent slopes, MLRA 158LaA7024679452w037hi97019661:24000
Lahaina silty clay, 7 to 15 percent slopes, severely eroded, MLRA 158LaC35824679492w03dhi97019661:24000
Lahaina silty clay, 3 to 7 percent slopes, severely eroded, MLRA 158LaB34284679472yybvhi97019661:24000
Lahaina silty clay, 15 to 25 percent slopes, severely eroded, MLRA 158LaD33684679502v0pthi97019661:24000
Lahaina silty clay, 25 to 40 percent slopes, severely eroded, MLRA 158LaE3644679512w039hi97019661:24000
Lahaina silty clay, 7 to 15 percent slopes, MLRA 158LaC14664683022w03chi98019681:24000
Lahaina silty clay, 3 to 7 percent slopes, MLRA 158LaB13294683012w03bhi98019681:24000
Lahaina silty clay, 15 to 25 percent slopesLaD562468303hq9khi98019681:24000
Lahaina silty clay, moist, 3 to 7 percent slopes, MLRA 167LaB40634684462wfhthi99019661:24000
Lahaina silty clay, 7 to 15 percent slopes, MLRA 158LaC27034684472w03chi99019661:24000
Lahaina silty clay, 7 to 15 percent slopes, severely eroded, MLRA 158LaC313024684482w03dhi99019661:24000
Lahaina silty clay, 0 to 3 percent slopes, MLRA 158LaA7014684452w037hi99019661:24000

Map of Series Extent

Approximate geographic distribution of the LAHAINA 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 .