The Role of Cementation and Electrolyte Concentration in Marine Clay Behavior
胶结作用和电解质浓度在海洋粘土行为中的作用
基本信息
- 批准号:63560232
- 负责人:
- 金额:$ 1.86万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for General Scientific Research (C)
- 财政年份:1988
- 资助国家:日本
- 起止时间:1988 至 1990
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
1. The samples of Ariake clay sediment contain smectite, vermiculite, kaolinite, illite, and chrolite as clay minerals, and the smectite content varies from 50% at the surface zone to 20% at the depth of 17m. The chlorine concentration of the clay sediment increased from 0.07N at the surface zone to 0.3N at the depth of 4m and then decreased to 0.01N at further depth. The variation of the ratio of undrained shear strength against overburden pressure was explained in terms of the clay content and salt concentration, and another factor of pH was added to explain the variation of the liquid and plastic limits.2. A negative correlation was observed between the mean particlediameter of flocks in the suspensions and the zeta potential. The sediment volume of the clay suspensions of pH7 was found to be positively correlated with mean particle-diameter of flocks. The void ratio of the sediment exhibited a rapid decrease with increasing depth at the surface zone and a subsequent slow decrease at greater depth.3. Addition of the iron oxides to the illite increased the yield stress over a pH range of 3 to 10. With increasing pH the yield stress decreased for for the complexes with iron oxides of 2 and 5% while the complexes with iron oxides of 7, 10, and 20% exhibited the maximum yield stresses at the pH values of 6 to 8. The yield stress for the complexes was correlated with their zeta potential, and the higher yield stress was explained to be due to smaller interparticle repulsion.
1、有明粘土沉积物样品中含有蒙脱石、蛭石、高岭石、伊利石、铬绿石等粘土矿物,蒙脱石含量从表层的50%到17m深度的20%不等。粘土沉积物的氯浓度从表层的0.07N增加到4m深度的0.3N,然后在更深处降低到0.01N。用粘土含量和盐浓度解释了不排水剪切强度与上覆压力之比的变化,并加入了另一个pH因素来解释液限和塑限的变化。 2.悬浮液中絮团的平均粒径与 zeta 电位之间观察到负相关。研究发现,pH7 的粘土悬浮液的沉积体积与絮团的平均粒径呈正相关。沉积物孔隙比在表层随深度增加而快速减小,随深度增加而缓慢减小。 3.在 3 至 10 的 pH 范围内,向伊利石中添加氧化铁会增加屈服应力。随着 pH 值的增加,对于氧化铁含量为 2 和 5% 的络合物,屈服应力降低,而对于氧化铁含量为 7、10 的络合物,屈服应力降低。 ,20% 在 pH 值 6 至 8 时表现出最大屈服应力。复合物的屈服应力与其 zeta 电位相关,较高的屈服应力被解释为由于较小的颗粒间排斥力。
项目成果
期刊论文数量(12)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
江頭和彦,宣保清一: Applied Clay Science. 3. 253-263 (1988)
Kazuhiko Egashira,Seiichi Nobuyasu:应用粘土科学 3. 253-263 (1988)。
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- 影响因子:0
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- 通讯作者:
大坪政美 OHTSUBO MASAMI: "Interaction of iron oxides with clays" Clay Science. 7. 227-242 (1989)
OHTSUBO Masami:“氧化铁与粘土的相互作用”《粘土科学》7. 227-242 (1989)。
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- 影响因子:0
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J.K.Torrauce,M.Ohtsubo: "Ariake Bay quick clays:A comparison with the general model" Soils and Foundations.
J.K.Torrauce,M.Ohtsubo:“有明湾快速粘土:与一般模型的比较”土壤和基础。
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- 发表时间:
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- 影响因子:0
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Masami OHTSUBO;Motomu IBARAKI: "Particleーsize characterization of flocs and sedimentation volume in electrolyte claysuspeusious" Applied Clay 5 cience.
Masami OHTSUBO;Motomu IBARAKI:“电解质粘土中絮凝体的粒径表征和沉降体积”Applied Clay 5 Science。
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OHTSUBO Masami其他文献
OHTSUBO Masami的其他文献
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