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- W2078860551 abstract "Soils on a sequence of well drained Neoglacial moraines up to 240 years-old, plus an older soil, were sampled to investigate soil development through the initial stages of podzolization. Pebbles and cobbles in the moraines are about 75 to 80% granitic rock. Computations based on minerals observed optically and on chemical analyses indicate that plagioclase and quartz are the predominant minerals in the fine-earth. The climate is perhumid. Leaching of the moraines may have begun before they were free of glacial ice, but little organic matter accumulated under the initial vegetative cover of sparse dwarf fireweed (10-year site). As alder thicket developed, organic matter accumulated rapidly in Oi, Oe, and A horizons (38-year site). As spruce trees began to replace alder, organic matter was lost from the surface mineral soil to form an E horizon and an incipient Bs horizon formed below it, an Oa horizon formed, and the A horizon disappeared (70- and 90-year sites). Organic acid leaching continued, to form a spodic Bhs horizon in spruce forest (240-year site) and a spodic Bh horizon in spruce-hemlock forest (> 240-year site). Hornblende has been etched slightly within 240 years, apatite has been lost from E horizons and free-Fe, presumeably in ferrihydrite, has accumulated in B horizons. The younger moraine soils, both with and without incipient Bs horizons, are Typic Cryorthents and the 240-year-old and older soils with spodic Bhs and Bh horizons are Typic Haplocryods. They are expected to accumulate more organic matter and become Andic Humicryods, which is the most common subgroup of soils in the area." @default.
- W2078860551 created "2016-06-24" @default.
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- W2078860551 date "1996-07-01" @default.
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- W2078860551 title "Soil development on moraines of Mendenhall Glacier, southeast Alaska. 1. The moraines and soil morphology" @default.
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- W2078860551 doi "https://doi.org/10.1016/0016-7061(96)00021-3" @default.
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