Catroux G, Schnitzer M (1987) Chemical, spectroscopic, and biological characteristics of the organic matter in particle size fractions separated from an
Aquoll. Soil Science Society of America Journal 51, 1200-1207.
Catroux G, Schnitzer M (1987) Chemical, spectroscopic, and biological characteristics of the organic matter particle size fractions separated from an
Aquoll. Soil Science Society of America Journal 51, 1200-1207.
Chemical spectroscopic and biological characteristics of the organic matter in particle size fractions separated from an
Aquoll. Soil Science Society of America Journal 51, 1200-7.
Hydrosols have commonly been classified as Inceptisols, Alfisols, Entisols, and Mollisols with aquic conditions (Aquepts, Aqualfs, Aquents,
Aquolls).
Soils in wetlands of the study area are dominated by Aquepts and Aquents and to a lesser extent,
Aquolls and Aqualfs (USDA NRCS 1995; Lewis et al.
In the United States the dominant suborders of Mollisols appear as sequential bands across the country reflecting the moisture regimes in which each Mollisol developed: Albolls, Aquolls, Cryolls, Rendolls, Udolls, Ustolls, and Xerolls (Table 3-5; Figure 3-13).
* Aquolls are wet Mollisols, most of which have been drained for agricultural activity.
Histosols and
Aquolls comprise the soils of the north shore from site 9 to site 20 (Figure 1), whereas Riddles Loam is found along much of the southern shore.