1) mobility of debris
泥石的流动性
2) creep debris flow
蠕动性泥石流
1.
This paper expounds in detail micro-features on creep debris flow taken from Huarna beside 212-road in electron microscope.
本文以位于国道２１２线甘肃化马泥石流为例，基于多年来的现场观察及室内电镜分析，比较深入地研究了蠕动性泥石流的显微结构及显微构造特征。
3) debris flow movement
泥石流活动
1.
According to a large amount of field measurements and indoor annual measuring data and research on the distribution characteristics of debris flow movement deposits in different stages since the late Cenozoic Era,we believe that the large scale debris flow movement in the east border of the Tibetan Plateau and its surrounding regions since the late Cenozoic Era started from the late Pliocene.
本文根据大量野外考察资料和室内测年数据 ,通过对晚新生代以来不同时段泥石流沉积物的分布特征研究 ,总结了青藏高原东部及华北地区第四纪泥石流活动的规律。
5) viscous debris flow
黏性泥石流
1.
According to observational data of viscous debris flows with hyper-concentration , distinct causes of formation for different graded bedding in debris flow deposits have been analyzed by use of its rheology and the ratio of flow plug .
根据高浓度黏性泥石流的观测资料 ,应用不同类型黏性泥石流的流变特性和流体结构的分类指标—流核比 ,对高浓度黏性泥石流堆积中的混杂层、筛积层和粗化层理结构进行了成因差异分析。
2.
Method for determining the critical grain size of viscous debris flow based on energy dissipation principle;
通过在云南蒋家沟实施6组现场泥石流模拟试验,结果表明试验沟道的泥石流分界粒径处在5~6mm之间,与前人成果基本相符,同时分析了分界粒径与最小能量耗损和容重之间的变化规律,即分界粒径随着最小能坡损失和容重的增加而呈缓慢的增大趋势等,为建立了非均质黏性泥石流动力学模型奠定了基础。
6) viscous debris flow
粘性泥石流
1.
2-D numerical simulation of viscous debris flows;
二维非恒定粘性泥石流运动堆积的数值模拟
2.
Impact force calculation of viscous debris flow based momentum conservation;
基于动量守恒的粘性泥石流冲击力计算
3.
Stress-strain properties of viscous debris flow and determination of volocity parameter;
粘性泥石流体的应力应变特性和流速参数的确定
补充资料：肠蠕动和肠蠕动波
肠蠕动和肠蠕动波
peristalsis and peristaltic wave
患者仰卧，显露出全腹，检查者观察其腹部外形，可发现特殊的局限性腹壁膨隆或肿物。其为位置不定的鼓胀现象，大小不一，长短不等。有的为局部鼓包，有的具肠管外形。触之表面光滑、质软、囊感。叩诊多呈鼓音，此即肠形。肠形上有时可见不规则的波动，有的间或出现，有的此起彼伏，即肠蠕动波。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条