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1)  morainic clay
冰碛粘土
2)  moraine soil
冰碛土
1.
The results indicate that high failure probability of benches is primarily depended on inherent variability of strength,anti?weathering ability and hydro?physical properties of moraine soil.
分析结果表明,台阶边坡破坏概率较高,主要是由冰碛土强度的固有不确定性、抗风化能力以及水理性质决定的,而边坡结构因素对其影响不显著。
2.
Taking the Kangdi airport as an example,the moraine soil characteristics and reinforcement methods are discussed in this paper.
冰体融化后,包裹在冰川体内的碎屑物质直接堆积沉积称冰碛土,其特点是无层序,无分选,块石、砾石、砂及粘性土杂乱堆积,常具架空结构,力学性质差异大。
3.
Aiming at the moraine soil slope in west wall of Taihe Iron Mine,a method based on the results of in-situ test and laboratory test for moraine soil which couples automata(CA) with FLAC3D to conduct triaxial simulation test is presented and shear strength model for moraine soil is established.
针对太和铁矿西端帮冰碛土边坡这一具体工程,提出以冰碛土原位试验和室内试验成果为基础,耦合元胞自动机(CA)和FLAC3D进行冰碛土三轴数值模拟试验并建立其抗剪强度模型的方法;提出基于数值模拟,有效整合数值分析、极限平衡分析和可靠度分析方法的边坡稳定性综合分析方法。
3)  Geologic model of drift clay
冰碛土地质模型
4)  moraine [英][mə'reɪn]  [美][mə'ren]
冰碛
1.
There are many moraine slopes which are high and steep along the north bank of Purlung Tsangpo River because of construction of Sichuan-Tibet Highway.
在帕隆藏布北岸的川藏公路上,有许多冰碛高陡切坡。
2.
The research area is located at the head area of Urumqi Rjver,above 3000m and in al-pine periglacial environment.On the moraines of the Last Glaciation and Neo一glaciation al-pine meadow soils develop from 3000 to 3700 m.
末次冰期冰碛和新冰期冰碛上发育高山草甸土,海拔3000-3700m。
3.
This paper is intended to present a preliminary model of transfo(?) mation from moraine to the deposits of glacial debris flow, to describe the distinguishing marks between the two types of deposits, and to compare and study some characteristics of granularity, light and heavy mineral, clay mineral and gravel fabric of them.
继初步建立起冰碛转化为冰川泥石流堆积模式及其沉积判别标志后,又对它们的粒度特征、矿物特征与砾石组构特征等进行了悉心研究。
5)  till [英][tɪl]  [美][tɪl]
冰碛
6)  glacial clay
冰川粘土
补充资料:冰碛石

冰碛石是指冻结在冰川中的石块,随着冰川的融化而沉积在一起的沉积物。他和其他沉积物的最大区别就是他的分选性差,大小混合,还有,磨圆度也很差,棱角分明。

冰碛石主要分布在曾经出现过大量冰川的地区,比如北欧,加拿大都是第四纪冰川的中心,这些地方不仅冰碛石很多,还有大量的冰渍湖。

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