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Mineral Assemblages of the Sediments of the Ala Wai Canal and Its Drainage Basins, O'ahu, Hawai'i

机译:夏威夷瓦胡岛阿拉威运河及其流域沉积物的矿物组合

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摘要

To understand the origin of the mineralogy of the sediments in the Ala Wai Canal, 20 soil and stream sediment samples were collected from Manoa, Palolo, and Makiki Valleys. X-ray diffraction analysis was used to determine mineralogical composition. Four mineral assemblages are recognized: plagioclase from mechanical weathering present in Makiki Valley and pyroxene, olivine, plagioclase, and ilmenite in Manoa and Palolo Valleys; (2) maghemite, hematite, and kaolinite present in all three valleys from chemical weathering and gibbsite and goethite in Manoa Valley and goethite in Palolo Valley; (3) quartz in all three valleys from aeolian deposition; and (4) pyrite, calcite, and aragonite in the Ala Wai Canal, and kaolinite and gibbsite derived from the watershed studied.
机译:为了了解阿拉威运河沉积物的矿物学起源,从马诺阿,帕洛洛和马基基河流域收集了20个土壤和河流沉积物样本。 X射线衍射分析用于确定矿物学组成。公认有四种矿物组合:Makiki谷存在机械风化产生的斜长石,而Manoa和Palolo谷则存在辉石,橄榄石,斜长石和钛铁矿。 (2)在三个山谷中都存在磁赤铁矿,赤铁矿和高岭石,其化学风化和菱镁矿和针铁矿都存在于马诺阿河谷中,而帕洛洛谷地的针铁矿中; (3)三个风谷沉积形成的石英; (4)阿拉维运河中的黄铁矿,方解石和文石,以及从分水岭得到的高岭石和菱镁矿。

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