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JAEA Reports

None

; *; Tokizawa, Takayuki; *

JNC TY6400 2000-013, 102 Pages, 2000/02

JNC-TY6400-2000-013.pdf:2.45MB

None

Journal Articles

Weathering of chlorite in a quartz-chlorite schist,I; Mineralogical and chemical changes

Murakami, Takashi*; Isobe, Hiroshi; Sato, Tsutomu; Onuki, Toshihiko

Clays and Clay Minerals, 44(2), p.244 - 256, 1996/00

 Times Cited Count:55 Percentile:84.43(Chemistry, Physical)

no abstracts in English

JAEA Reports

None

PNC TJ1626 95-001, 92 Pages, 1995/04

PNC-TJ1626-95-001.pdf:3.04MB

None

JAEA Reports

Investigation of leaching rate on minerals for development of groundwater quality evolution model

*

PNC TJ1211 95-007, 117 Pages, 1995/02

PNC-TJ1211-95-007.pdf:5.29MB

1. Survey on leaching rate of pyrite, chlorite, epidote and siderite. (1) Pyrite Reaction rate (K) is depended on dissolve O$$_{2}$$ concentration in Lin's literature. 1 - (1-x) $$^{1/3}$$ = k [O$$_{2}$$] $$^{ 1/2}$$ ・t (x: Mole number of dissolved FeS$$_{2}$$ , [O$$_{2}$$]: Dissolve O$$_{2}$$ concentration. T:Time) Reaction rate is changed by temperature. k = 2.2 $$times$$ 10$$^{9}$$ exp(-9140/T) (2) chlorite Reaction rate is measured 2.7 $$sim$$ 6.7 $$times$$ 10$$^{-12}$$ mol/m$$^{2}$$/s(pH3 $$sim$$ 4.5) by Swoboda-Colberg et al. Reaction rate is controlled by inner diffusion. (3) Epidote Reaction rate is measured 10$$^{-14}$$ $$sim$$ 10$$^{-13}$$ mol/cm$$^{2}$$/s in pH1 $$sim$$ 11 by Rose. (4) Siderite Reaction rate is measured 9.93 $$times$$ 10$$^{-6}$$ mol/m$$^{2}$$/s in O$$_{2}$$-free solution by Greenberg et al. 2. Experimental study on leaching rate of minerals. (1) Measurement of leaching rate of minerals. Leaching rate of pyrite was measured in distilled waster under redox condition. Reaction rate (K) was estimated 10$$^{-4}$$ $$sim$$ 10$$^{-3}$$ (cm$$^{3}$$・mol$$^{-1}$$) 1/2・h$$^{-1}$$ by Lin's rate equation. At 56 days in the experiments. Alterated layer could not be found in SEM and EDX observation. (2) Measurement of leaching rate of chlorite Leaching rate of chlorite was measured in distilled waster under air condition. Disolution process of chloric was parabolic Stage, and reaction rate (K) was estimated order of 10$$^{-15}$$ $$sim$$ 10$$^{-14}$$ by Ross's rate equation. $$alpha$$$$^{2}$$ = kt [ $$alpha$$ : disoleved mineral amount / intial mineral amount, t : time(sec) ] At 56 days in the experiments, alterated layer could not be found in SEM and EDX observation.

JAEA Reports

None

*

PNC TJ1211 95-006, 72 Pages, 1995/02

PNC-TJ1211-95-006.pdf:1.14MB

None

Journal Articles

Migration behavior of uranium series nuclides in altered quartz-chlorite schist

Onuki, Toshihiko; Murakami, Takashi; Sekine, Keiichi; Yanase, Nobuyuki; Isobe, Hiroshi; Kobayashi, Yoshii

Materials Research Society Symposium Proceedings, Vol. 176, p.607 - 614, 1990/00

no abstracts in English

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