Soil Data Explorer - IPHIL

Official Series Description

Lab Data Summary

Aggregate lab data for the IPHIL soil series. This aggregation is based on all pedons with a current taxon name of IPHIL, 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 IPHIL were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
13	89P0103	89ID029005	Iphil	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	42.8422203,-111.9086075
13	13N17666	S2012ID065001	Iphil	6	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	43.76455,-111.791

Water Balance

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

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the IPHIL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the IPHIL series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the IPHIL 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 (updated 2024-10-23).

Competing Series

Soil series competing with IPHIL share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the IPHIL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the IPHIL 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 (updated 2024-10-23).

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 flats position figure.

Soil series sharing subgroup-level classification with IPHIL, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing IPHIL 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
Iphil-Lostine-Ririe complex, 0 to 12 percent slopes	13514	9735	2426024	2mfgv	id650	2011	1:24000
Iphil-Lostine-Tetonia complex, 2 to 20 percent slopes	13515	4076	1529390	1nbg5	id650	2011	1:24000
Iphil-Ririe complex, 4 to 20 percent slopes	13456	2426	2427839	2mhcd	id650	2011	1:24000
Iphil, very deep-Feeder complex, 4 to 20 percent slopes	405F	151	3238956	5bn9	id710	1968	1:24000
Iphil silt loam, very deep, 4 to 12 percent slopes	405A	54	3238955	5bn4	id710	1968	1:24000
Iphil, very deep-Feeder complex, 1 to 4 percent slopes	405I	6	3238957	5bw5	id710	1968	1:24000
Iphil-Watercanyon complex, 2 to 20 percent slopes	110	3386	154301	55kg	id712	2008	1:24000
Bearhollow-Brifox-Iphil complex, 12 to 35 percent slopes	20	2616	154376	55mw	id712	2008	1:24000
Rexburg-Iphil complex, 4 to 8 percent slopes	172	2580	154350	55m1	id712	2008	1:24000
Iphil silt loam, 4 to 12 percent slopes	107	2023	154297	55kb	id712	2008	1:24000
Rexburg-Iphil complex, 1 to 4 percent slopes	171	1581	154353	55m4	id712	2008	1:24000
Iphil silt loam, 1 to 4 percent slopes	106	1397	154300	55kf	id712	2008	1:24000
Bearhollow-Brifox-Iphil complex, 4 to 12 percent slopes	19	892	154377	55mx	id712	2008	1:24000
Iphil silt loam, 12 to 20 percent slopes	108	533	154298	55kc	id712	2008	1:24000
Iphil-Lanoak-Watercanyon complex, 12 to 25 percent slopes	109	500	154303	55kj	id712	2008	1:24000
Iphil-Watercanyon complex, dry, 4 to 12 percent slopes	111	346	791549	vknv	id712	2008	1:24000
Ririe-Iphil complex, 1 to 4 percent slopes	183	132	154360	55mc	id712	2008	1:24000
Iphil, very deep-Feeder complex, cool, 4 to 12 percent slopes	405FF	11	3238976	2fgwt	id712	2008	1:24000
Ririe-Iphil-Rexburg complex, 4 to 12 percent slopes	115-O	3	2619911	2v07g	id713		1:24000
Iphil, very deep-Feeder complex, cool, 4 to 12 percent slopes	405FF	2	3238894	2fgwt	id713		1:24000
Iphil-Lonigan complex, 8 to 20 percent slopes	62	1724	485309	j904	id714	1997	1:24000
Bearhollow-Brifox-Iphil complex, 20 to 35 percent slopes	17	67	485259	j8yj	id714	1997	1:24000
Bearhollow-Brifox-Iphil, very deep, complex, 20 to 40 percent slopes	910A	27	3173392	5bqq	id714	1997	1:24000
Ririe-Iphil-Rexburg complex, 4 to 12 percent slopes	115	6242	3163611	2v07g	id715	1994	1:24000
Ririe-Iphil-Kucera complex, 2 to 8 percent slopes	114	3711	485582	j98y	id715	1994	1:24000
Rexburg-Iphil-Watercanyon complex, 12 to 30 percent slopes	99	1479	485698	j9dp	id715	1994	1:24000
Jensen-Iphil-Wursten complex, 4 to 12 percent slopes	54	1103	485649	j9c3	id715	1994	1:24000
Iphil-Ririe-Watercanyon complex, 8 to 20 percent slopes	50	490	485645	j9bz	id715	1994	1:24000
Ririe-Iphil complex, very deep, 1 to 4 percent slopes	710I	5447	159248	5bq1	id716		1:24000
Iphil silt loam, very deep, 1 to 4 percent slopes	405D	3257	159192	5bn7	id716		1:24000
Rexburg, very deep-Iphil, deep-Kucera complex, 1 to 4 percent slopes	700G	1527	159421	5bwm	id716		1:24000
Iphil, very deep-Feeder complex, 4 to 20 percent slopes	405F	1266	159194	5bn9	id716		1:24000
Iphil, very deep-Lanoak-Feeder complex, 4 to 12 percent slopes	405H	1229	159408	5bw6	id716		1:24000
Iphil silt loam, very deep, 12 to 30 percent slopes	405B	1188	159190	5bn5	id716		1:24000
Iphil silt loam, very deep, 4 to 12 percent slopes	405A	1091	159189	5bn4	id716		1:24000
Rexburg-Iphil complex, very deep, 4 to 15 percent slopes	700M	840	159238	5bpq	id716		1:24000
Bearhollow-Brifox-Iphil, very deep, complex, 20 to 40 percent slopes	910A	821	159269	5bqq	id716		1:24000
Iphil, very deep-Feeder complex, 1 to 4 percent slopes	405I	666	159407	5bw5	id716		1:24000
Bearhollow-Brifox-Iphil, very deep, complex, 12 to 20 percent slopes	910C	505	1860273	20frt	id716		1:24000
Bearhollow-Iphil, very deep-Rock outcrop complex, 1 to 6 percent slopes	910E	434	159437	5bx4	id716		1:24000
Iphil, very deep-Lanoak-Feeder complex, 12 to 25 percent slopes	405G	422	159195	5bnb	id716		1:24000
Bearhollow-Brifox-Iphil, very deep, complex, 4 to 12 percent slopes	910B	286	159270	5bqr	id716		1:24000
Iphil, very deep-Feeder complex, cool, 4 to 12 percent slopes	405FF	237	2248641	2fgwt	id716		1:24000
Rexburg-Iphil complex, very deep, 1 to 4 percent slopes	700RR	210	2370700	2kkx6	id716		1:24000
Ririe-Iphil complex, very deep, cool, 1 to 4 percent slopes	710II	180	2370706	2kkxd	id716		1:24000
Iphil silt loam, very deep, cool, 1 to 4 percent slopes	405DD	117	2248432	2fgp2	id716		1:24000
Rexburg-Iphil complex, very deep, cool, 4 to 8 percent slopes	700MM	115	2370697	2kkx3	id716		1:24000
Iphil silt loam, very deep, cool, 4 to 12 percent slopes	405AA	102	2248202	2fgfn	id716		1:24000
Iphil silt loam, very deep, cool, 12 to 30 percent slopes	405BB	71	2248431	2fgp1	id716		1:24000
Iphil-Lostine-Ririe complex, 0 to 12 percent slopes	13514	460	2515232	2qf4d	id766	1978	1:24000
Iphil-Truscreek-Downey complex, 0 to 10 percent slopes	1091	2382	2848294	2v5vw	mt634	1988	1:24000

Map of Series Extent

Approximate geographic distribution of the IPHIL 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 (updated 2024-10-30).