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• W2003261661 abstract "Abstract Gravelly floodplain deposits and six terrace treads in the Waimea Plains, northeast Southland, New Zealand, range in age from ca. 1000 years old to 350,000 yr old. Deposits are progressively more weathered with increasing parent material age. Soils developed in them are classified as Recent Soils, Brown Soils and Ultic Soils in the New Zealand Soil Classification and Udifluvents, Dystrochrepts, Haplohumults, Hapludults and Paleudults in the USDA Soil Classification (Soil Taxonomy). The youngest soils are slightly acid. Those developed in deposits 35,000–70,000 yr old are strongly acid. In soils in deposits 160,000 yr old and older, that have weathered in two or three interglacial periods, including the present one, pH and total exchangeable bases values are higher than in soils in younger deposits. The higher pH of the soils in older deposits is attributed to release of cations by stone weathering. Soils developed in deposits up to 70,000 yr old have clays dominated by mica and chlorite. Stones in these soils are at most weakly weathered, and the Two phases of weathering are distinguished: a phase of approximate duration 100,000 yr in which most weathering and leaching occurs in the matrix, which becomes increasingly acidified; and a phase from 100,000 to 350,000 yr which is dominated by cation release from stones, reversal of the acidification trend, and breakdown of stone fabric." @default.
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• W2003261661 date "1996-02-01" @default.
• W2003261661 modified "2023-10-02" @default.
• W2003261661 title "Weathering trends in terrace deposits up to 350,000 years old in northeast Southland, New Zealand" @default.
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• W2003261661 doi "https://doi.org/10.1016/0341-8162(96)00032-x" @default.
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