课题基金 / 基金详情

A set up of an atmosphere-controlled furnace with stirring device, and effect of stirring on the crystallization behavior of basaltic melts.

A set up of an atmosphere-controlled furnace with stirring device, and effect of stirring on the crystallization behavior of basaltic melts.
带搅拌装置的气氛控制炉的设置以及搅拌对玄武岩熔体结晶行为的影响。
批准号:
01840030
负责人:
SATO Hiroaki
金额:
$2.37万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Developmental Scientific Research
财政年份:
1989
资助国家:
日本
项目状态:
已结题
起止时间:
1989 至 1991

项目摘要

项目成果

SATO Hiroaki的其他基金

相关文献

中文摘要
翻译
构造了带搅拌装置的气控加热炉。加热器为Siliconit DSP-26(螺旋SiC加热器),半径56mm,长度300mm。该炉的特点是样品内部温度梯度小(30ml铂熔胶,上直径36mm)。炉内气氛由H2和CO2混合气体控制,温度由采用Pt-PtRh热电偶的自动晶闸管炉控制器控制。炉内温度控制在2ºC以内,样品现场氧逸度精度在0.5 log单位棒以内。搅拌Pt管直径为11mm,连接在陶瓷棒上,以5- 57rpm的速度旋转。从炉顶观察和取样可熔料中的熔体。样品是用陶瓷棒手工制作的,并在空气中淬火。我们用的是1778A。日本伊豆大岛的熔岩,作为起始材料。以前用静态线环法研究了结晶行为和元素分配关系。先在1250℃(高于液温约50℃)下不搅拌熔融10小时,然后在搅拌下恒速冷却。过热的基性熔体延迟斜长石成核已经有很好的记录(例如Gibb, 1974 Min)。杂志)。在本实验中,当旋转速率为57 rpm,冷却速率为10‰/小时时,斜长石的成核需要约35‰的过冷。在1150℃的样品中,不搅拌时斜长石的密度为4*10^4cm^<-3>,转速为57rpm时斜长石的密度为7*10^5cm^<-3>,表明搅拌对基性熔体中斜长石的成核有影响。
英文摘要
An atmosphere-controlled furnace with stirring device was constructed. The heater is a Siliconit DSP-26 (spiral SiC heater) with radius of 56mm and length of 300mm. The furnace is characterized by small temperature gradient within the sample (30ml platinum crusible, with upper diameter of 36mm). The furnace atmosphere is controlled by mixed gas of H2 and CO2, and the temperature is controlled by an automatic thyristor furnace controller using a Pt-PtRh thermocouple. The furnace temperature is controlled within 2゚C and oxygen fugacity is accurate within 0.5 log unit of bars at the sample site. The stirring Pt pipe is 11mm in diameter and is attached to ceramic rod, which is rotated at a rate of 5-57 rpm. The melt in the crusible is observed and sampled from the top of the furnace. The sampling was made manually by a ceramic rod, and quenched in air.We used a 1778A. D. lava of Izu-Oshima, Japan, as a starting material. The crystallization behavior and element partition relation was investigated by static wire-loop method previously. The sample is first melted at 1250゚C (about 50゚C above the liquidus temperature) for 10 hours without stirring, and then cooled at constant rate with stirring. Delay of plagioclase nucleation from overheated basaitic melts has been well documented (e. g. Gibb, 1974 Min. Mag.). In the present experiment, ca. 35゚C undercooling was requirred for plagioclase nucleation for rotation rate of 57 rpm at a cooling rate of 10゚C/hr. Plagioclase population density at 1150゚C sample is 4*10^4cm^<-3> for a run without stirring, and 7*10^5cm^<-3> for a run with rotation rate of 57rpm, indicating an effect of stirring on the nucleation of plagioclase in a basaitic melt.
期刊论文(26)
专著(0)
科研奖励(0)
会议论文
Sato, H.: "Eruption processes and rock textures. (in Japanese)" The Earth Monthly. 13. 372-379 (1991)
Sato, H.:“喷发过程和岩石纹理。(日语)”《地球月刊》。
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Hiroaki Sato: "MgーFe partitioning between plagioclase and liquid in basatts of Hole 504B,ODP Leg 111:A study of metting at 1 afm." Proceeding of Ocean Drilling Program,Sci.Resutts.111. 17-26 (1989)
Hiroaki Sato:“504B 孔的斜长石和液体之间的 Mg-Fe 分配,ODP Leg 111:1 afm 下的会议记录”,Sci.Resutts.111(1989)。
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