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contributor authorMaria Chrysochoou
contributor authorDennis G. Grubb
contributor authorKelly L. Drengler
contributor authorNicholas E. Malasavage
date accessioned2017-05-08T21:46:47Z
date available2017-05-08T21:46:47Z
date copyrightAugust 2010
date issued2010
identifier other%28asce%29gt%2E1943-5606%2E0000308.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/62067
description abstractThe prior two papers in this series reported on the geoenvironmental and geomechanical properties of 20 stabilized dredged material (SDM) blends using dredged material (DM) from the U.S. Army Corps of Engineers Craney Island confined disposal facility. The pozzolans included lime, cement kiln dust (CKD), class F fly ash, and two cements (portland and slag cement). This paper reports on the mineralogical evolution of the SDM blends over a 6-month curing period using techniques new to mainstream geotechnical engineering: X-ray diffraction (XRD) with Rietveld quantification analysis which allows direct quantitative mineralogical comparisons between soil samples. Despite being classified as a high plasticity clay-organic clay (CH/OH soil), XRD showed that the DM contained no montmorillonite, illite or kaolinite, and was thus mineralogically unreactive. The quartz, feldspar, and mica contents were numerically tracked and were shown to remain stable 6 months after blending. The chlorite (in DM) content decreased over time and with the fly ash served as the sources of soluble silica and alumina for pozzolanic reactions especially in the lime-based SDM blends. Lime in the lime-based blends persisted in significant quantities (3%) as unreacted portlandite
publisherAmerican Society of Civil Engineers
titleStabilized Dredged Material. III: Mineralogical Perspective
typeJournal Paper
journal volume136
journal issue8
journal titleJournal of Geotechnical and Geoenvironmental Engineering
identifier doi10.1061/(ASCE)GT.1943-5606.0000292
treeJournal of Geotechnical and Geoenvironmental Engineering:;2010:;Volume ( 136 ):;issue: 008
contenttypeFulltext


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