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Mineralogy of a Holocene Chronosequence on Andesitic Beach Sediments in Costa Rica
Author(s) -
Nieuwenhuyse A.,
Jongmans A. G.,
Breemen N.
Publication year - 1994
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1994.03615995005800020034x
Subject(s) - allophane , andesite , geology , weathering , geochemistry , clay minerals , plagioclase , andosol , parent rock , gibbsite , volcanic glass , kaolinite , soil water , mineralogy , volcanic rock , quartz , volcano , soil science , paleontology
We investigated weathering and neoformation of minerals in a Holocene (<5000 yr) soil chronosequence on sandy, andesitic, ocean beach ridges in humid tropical Costa Rica using micromorphological, mineralogical, and chemical analyses. Troposamments are present on the younger beach ridges and Hapludands are on the older ones. The parent materials of all soils are sands with similar mineralogical composition: andesitic rock fragments, plagioclase, and pyroxene dominate, with minor amounts of opaque minerals. None of the parent materials contained >13% (v/v) volcanic glass. Weathering and neoformation of minerals with increasing soil age is characterized by (i) increasing pellicular and linear alteration of sand grains and (ii) decrease of the sand fraction and concomitant increase of finer material. Andesitic rock fragments weather more rapidly than plagioclase and pyroxene mineral grains. The alteration rates of the latter two are similar. Clay content in the ≈ 2000‐yr‐old soil is several times higher than in soils developed in rhyolitic parent materials of similar age in New Zealand. Formation of allophane with Al/Si ratios ranging from 1.9 to 3.8 takes place mainly in the B horizons. Aluminum‐humus complexes, allophane, and Al oxides and hydroxides are mainly formed in the A horizons. Small amounts of gibbsite were noticed in soils older than 2000 yr. Small amounts of 2:1 and 1:1 clay minerals present in the clay fraction of all soils are thought to be inherited from the parent material, which contains sand‐sized bodies of clay and andesitic rock fragments with clay pseudomorphs, both consisting of 2:1 and 1:1 clay minerals.