Soil Data Explorer - TREMBLES

Official Series Description

Lab Data Summary

Aggregate lab data for the TREMBLES soil series. This aggregation is based on all pedons with a current taxon name of TREMBLES, 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 TREMBLES were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
54	97P0374	S1996ND053495	Trembles	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	47.9738884,-103.9574966
54	14N0307	S2013SD105001	Trembles	8	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	45.635515,-102.5348583

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TREMBLES 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 TREMBLES series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the TREMBLES 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 2023-10-09).

Geomorphic description summaries for the TREMBLES 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 2023-10-04).

Competing Series

Soil series competing with TREMBLES share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the TREMBLES 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 2023-10-09).

Geomorphic description summaries for the TREMBLES 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 2023-10-04).

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.

Soil series sharing subgroup-level classification with TREMBLES, 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 2023-10-02).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. ND-2010-09-27-08 | McKenzie County - 2006

   Typical pattern of soils and underlying material in the Havrelon-Lohler association (Soil Survey of McKenzie County, North Dakota; 2006).

2. SD-2012-03-16-05 | Ziebach County - March 1990

   Pattern of soils and parent material in the Trembles-Korchea-Banks and Lantry-Cabba-Rhoades associations (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing TREMBLES 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
Trembles loam, wet	92	1273	497048	jp6t	co685	1979	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	721A	3338	1487393	1lxrf	mt021	1971	1:24000
Cherry, Havrelon, and Trembles soils, 0 to 4 percent slopes, occasionally flooded	215B	1422	1487328	1lxpb	mt021	1971	1:24000
Trembles loam, 0 to 2 percent slopes, occasionally flooded	72A	513	1487391	1lxrc	mt021	1971	1:24000
Cherry-Havrelon-Trembles complex, 0 to 2 percent slopes	45	17326	344408	ckcy	mt055	1981	1:24000
Trembles fine sandy loam	139	5587	344337	ck9n	mt055	1981	1:24000
Trembles fine sandy loam, protected	140	710	344339	ck9q	mt055	1981	1:24000
Cherry, Havrelon, and Trembles soils, occasionally flooded	Ch	25793	345330	clbp	mt083	1973	1:24000
Trembles fine sandy loam	Tm	5652	3155865	clcx	mt083	1973	1:24000
Benz-Trembles complex, 0 to 8 percent slopes	BnC	2551	345325	clbj	mt083	1973	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	2369	345368	1vzw5	mt083	1973	1:24000
Trembles fine sandy loam	Tr	2510	348871	cq0x	mt091	1971	1:24000
Havrelon-Trembles complex, 0 to 2 percent slopes	28	18041	348231	cpc8	mt661	1982	1:24000
Havrelon-Trembles complex, protected, 0 to 2 percent slopes	29	15230	348232	cpc9	mt661	1982	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes	54	4946	348260	cpd6	mt661	1982	1:24000
Trembles fine sandy loam, protected, 0 to 2 percent slopes	55	2127	348261	cpd7	mt661	1982	1:24000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	126	2755664	1vzw8	nd001	1983	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	280	2707096	1vzw8	nd007	1998	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	1	2758436	1vzw5	nd007	1998	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	3077	2563624	1vzw5	nd011	1969	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	42	2563523	1vzw8	nd011	1969	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	294	2661732	2qz89	nd015	1967	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	3	2707250	1vzw8	nd025	1981	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	6040	2525891	2qz89	nd037	1985	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	1526	2525850	1vzw8	nd037	1985	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	902	2755690	1vzw8	nd041	1986	1:20000
Trembles fine sandy loam, slightly wet, 0 to 2 percent slopes, occasionally flooded	E4051A	1311	2699337	d1wq	nd053	2003	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	1197	2699350	1vzw5	nd053	2003	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	1339	2662466	1vzw5	nd055	1974	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	639	2662490	2qz89	nd055	1974	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	321	2699243	2qz89	nd057	1976	1:20000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	1034	2525996	1vzw5	nd065	1971	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	609	2525999	2qz89	nd065	1971	1:20000
Banks-Trembles fine sandy loams, 2 to 6 percent slopes, occasionally flooded	E4217B	303	2526000	2q640	nd065	1971	1:20000
Banks-Trembles fine sandy loams, 0 to 2 percent slopes, occasionally flooded	E4217A	2548	2759707	2qz89	nd085	1992	1:24000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	2017	2699070	1vzw8	nd085	1992	1:24000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	460	1716795	1vzw5	nd087	1974	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	214	2758523	1vzw8	nd087	1974	1:20000
Banks-Trembles-Fluvaquents fine sandy loams, channeled, 0 to 2 percent slopes, frequently flooded	E4221A	3660	2716019	1vzw8	nd089	1965	1:20000
Trembles fine sandy loam, 0 to 2 percent slopes, occasionally flooded	E4187A	2749	2716016	1vzw5	nd089	1965	1:20000
Trembles fine sandy loam, slightly wet, 0 to 2 percent slopes, occasionally flooded	E4051A	2749	2662547	d1wq	nd105	1993	1:24000
Trembles fine sandy loam, slightly wet, 0 to 1 percent slopes	1854	486	339028	ccsd	nd105	1993	1:24000
Trembles family, warm, dry, 0 to 10 percent slopes	14	1020	2934257	2wgjc	nm678		1:24000
Trembles fine sandy loam, channeled	Tm	15544	356221	cyp0	sd031	1986	1:24000
Trembles fine sandy loam, terrace	Tt	15172	356222	cyp1	sd031	1986	1:24000
Trembles fine sandy loam	Th	8738	356220	cynz	sd031	1986	1:24000
Trembles and Banks soils	Tr	10639	354248	cwmc	sd041	1972	1:24000
Trembles-Havrelon complex	Th	4595	354247	cwmb	sd041	1972	1:24000
Trembles fine sandy loam	Ta	29839	354664	cx1s	sd105	1977	1:24000
Cabba-Trembles complex, 2 to 30 percent slopes	CbD	19637	354620	cx0c	sd105	1977	1:24000
Bullock-Trembles-Slickspots complex, channeled	Ac	16821	354609	cx00	sd105	1977	1:24000
Trembles soils, channeled	Tb	8421	354665	cx1t	sd105	1977	1:24000
Lohler-Trembles complex	Sh	2938	354663	cx1r	sd105	1977	1:24000
Trembles fine sandy loam, channeled	Tr	4597	355901	cybp	sd137	1985	1:24000
Trembles fine sandy loam	Tm	4188	355900	cybn	sd137	1985	1:24000

Map of Series Extent

Approximate geographic distribution of the TREMBLES 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 2023-10-04).